diff --git a/Tables/CMIP6_3hr.json b/Tables/CMIP6_3hr.json index d08a0734..3e8d8f6a 100644 --- a/Tables/CMIP6_3hr.json +++ b/Tables/CMIP6_3hr.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table 3hr", "realm": "atmos", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -40,7 +40,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Surface Upward Latent Heat Flux", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Upward' indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "hfls", "type": "real", @@ -58,7 +58,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Surface Upward Sensible Heat Flux", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Upward' indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called 'turbulent' heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. Unless indicated in the cell_methods attribute, a quantity is assumed to apply to the whole area of each horizontal grid box. Previously, the qualifier where_type was used to specify that the quantity applies only to the part of the grid box of the named type. Names containing the where_type qualifier are deprecated and newly created data should use the cell_methods attribute to indicate the horizontal area to which the quantity applies.", "dimensions": "longitude latitude time", "out_name": "hfss", "type": "real", @@ -74,7 +74,7 @@ "standard_name": "specific_humidity", "units": "1", "cell_methods": "area: mean time: point", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Near-Surface Specific Humidity", "comment": "Near-surface (usually, 2 meter) specific humidity.", "dimensions": "longitude latitude time1 height2m", @@ -110,7 +110,7 @@ "standard_name": "moisture_content_of_soil_layer", "units": "kg m-2", "cell_methods": "area: mean where land time: point", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Moisture in Upper Portion of Soil Column", "comment": "The mass of water in all phases in the upper 10cm of the soil layer.", "dimensions": "longitude latitude time1 sdepth1", @@ -202,7 +202,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Surface Downwelling Longwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'longwave' means longwave radiation. Downwelling radiation is radiation from above. It does not mean 'net downward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "rlds", "type": "real", @@ -238,7 +238,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Surface Upwelling Longwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'longwave' means longwave radiation. Upwelling radiation is radiation from below. It does not mean 'net upward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "rlus", "type": "real", @@ -310,7 +310,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Surface Upwelling Shortwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'shortwave' means shortwave radiation. Upwelling radiation is radiation from below. It does not mean 'net upward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "rsus", "type": "real", @@ -344,7 +344,7 @@ "standard_name": "air_temperature", "units": "K", "cell_methods": "area: mean time: point", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Near-Surface Air Temperature", "comment": "near-surface (usually, 2 meter) air temperature", "dimensions": "longitude latitude time1 height2m", @@ -362,7 +362,7 @@ "standard_name": "sea_surface_temperature", "units": "degC", "cell_methods": "area: mean where sea time: point", - "cell_measures": "area: areacella", + "cell_measures": "area: areacello", "long_name": "Sea Surface Temperature", "comment": "Temperature of upper boundary of the liquid ocean, including temperatures below sea-ice and floating ice shelves.", "dimensions": "longitude latitude time1", @@ -398,7 +398,7 @@ "standard_name": "eastward_wind", "units": "m s-1", "cell_methods": "area: mean time: point", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Eastward Near-Surface Wind Speed", "comment": "Eastward component of the near-surface (usually, 10 meters) wind", "dimensions": "longitude latitude time1 height10m", @@ -416,7 +416,7 @@ "standard_name": "northward_wind", "units": "m s-1", "cell_methods": "area: mean time: point", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Northward Near-Surface Wind Speed", "comment": "Northward component of the near surface wind", "dimensions": "longitude latitude time1 height10m", diff --git a/Tables/CMIP6_6hrLev.json b/Tables/CMIP6_6hrLev.json index 56df651f..f380552f 100644 --- a/Tables/CMIP6_6hrLev.json +++ b/Tables/CMIP6_6hrLev.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table 6hrLev", "realm": "atmos", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -15,15 +15,15 @@ }, "variable_entry": { "bs550aer": { - "frequency": "6hrPt", + "frequency": "6hr", "modeling_realm": "aerosol", "standard_name": "volume_lidar_backwards_scattering_coefficient_in_air_due_to_ambient_aerosol_particles", "units": "m-1 sr-1", - "cell_methods": "area: mean time: point", + "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Aerosol backscatter coefficient", "comment": "Aerosol Backscatter at 550nm and 180 degrees, computed from extinction and lidar ratio", - "dimensions": "longitude latitude alevel time1", + "dimensions": "longitude latitude time lambda550nm", "out_name": "bs550aer", "type": "real", "positive": "", @@ -41,7 +41,7 @@ "cell_measures": "area: areacella", "long_name": "Aerosol extinction coefficient", "comment": "Aerosol Extinction at 550nm", - "dimensions": "longitude latitude alevel time1", + "dimensions": "longitude latitude alevel time1 lambda550nm", "out_name": "ec550aer", "type": "real", "positive": "", @@ -58,7 +58,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Specific Humidity", - "comment": "", + "comment": "'specific' means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.", "dimensions": "longitude latitude alevel time1", "out_name": "hus", "type": "real", @@ -69,15 +69,15 @@ "ok_max_mean_abs": "" }, "pfull": { - "frequency": "6hr", + "frequency": "6hrPt", "modeling_realm": "atmos", "standard_name": "air_pressure", "units": "Pa", - "cell_methods": "area: time: mean", + "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Air Pressure", "comment": "Air pressure on model levels", - "dimensions": "longitude latitude alevel time", + "dimensions": "longitude latitude alevel time1", "out_name": "pfull", "type": "real", "positive": "", @@ -130,7 +130,7 @@ "cell_methods": "time: point", "cell_measures": "--OPT", "long_name": "Eastward Wind", - "comment": "", + "comment": "'Eastward' indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude alevel time1", "out_name": "ua", "type": "real", @@ -148,7 +148,7 @@ "cell_methods": "time: point", "cell_measures": "--OPT", "long_name": "Northward Wind", - "comment": "", + "comment": "'Northward' indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude alevel time1", "out_name": "va", "type": "real", diff --git a/Tables/CMIP6_6hrPlev.json b/Tables/CMIP6_6hrPlev.json index 1e7d3e67..3c2cd105 100644 --- a/Tables/CMIP6_6hrPlev.json +++ b/Tables/CMIP6_6hrPlev.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table 6hrPlev", "realm": "atmos", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -38,7 +38,7 @@ "standard_name": "relative_humidity", "units": "%", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Near-Surface Relative Humidity", "comment": "The relative humidity with respect to liquid water for T> 0 C, and with respect to ice for T<0 C.", "dimensions": "longitude latitude time height2m", @@ -58,7 +58,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Specific Humidity", - "comment": "", + "comment": "'specific' means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.", "dimensions": "longitude latitude plev4 time", "out_name": "hus", "type": "real", @@ -94,7 +94,7 @@ "cell_methods": "area: mean time: mean within hours time: maximum over hours", "cell_measures": "area: areacella", "long_name": "Maximum Hourly Precipitation Rate", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "prhmax", "type": "real", @@ -128,9 +128,9 @@ "standard_name": "atmosphere_relative_vorticity", "units": "s-1", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Relative Vorticity at 850 hPa", - "comment": "", + "comment": "Relative vorticity is the upward component of the vorticity vector i.e. the component which arises from horizontal velocity.", "dimensions": "longitude latitude time p850", "out_name": "rv850", "type": "real", @@ -146,7 +146,7 @@ "standard_name": "wind_speed", "units": "m s-1", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Near-Surface Wind Speed", "comment": "near-surface (usually, 10 meters) wind speed.", "dimensions": "longitude latitude time height10m", @@ -164,7 +164,7 @@ "standard_name": "air_temperature", "units": "K", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Surface Air Temperature", "comment": "near-surface (usually, 2 meter) air temperature", "dimensions": "longitude latitude time height2m", @@ -182,7 +182,7 @@ "standard_name": "eastward_wind", "units": "m s-1", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Eastward Wind at 100m", "comment": "Zonal wind at 100m height", "dimensions": "longitude latitude time height100m", @@ -200,7 +200,7 @@ "standard_name": "eastward_wind", "units": "m s-1", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Eastward Near-Surface Wind", "comment": "Eastward component of the near-surface (usually, 10 meters) wind", "dimensions": "longitude latitude time height10m", @@ -218,7 +218,7 @@ "standard_name": "northward_wind", "units": "m s-1", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Northward Wind at 100m", "comment": "Meridional wind at 100m above the surface.", "dimensions": "longitude latitude time height100m", @@ -236,7 +236,7 @@ "standard_name": "northward_wind", "units": "m s-1", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Northward Near-Surface Wind", "comment": "Northward component of the near surface wind", "dimensions": "longitude latitude time height10m", @@ -272,7 +272,7 @@ "standard_name": "wind_speed_of_gust", "units": "m s-1", "cell_methods": "area: mean time: maximum", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Maximum Wind Speed of Gust at 100m", "comment": "Wind speed gust maximum at 100m above surface", "dimensions": "longitude latitude time height100m", @@ -290,7 +290,7 @@ "standard_name": "wind_speed_of_gust", "units": "m s-1", "cell_methods": "area: mean time: maximum", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Maximum Wind Speed of Gust at 10m", "comment": "Wind speed gust maximum at 10m above surface", "dimensions": "longitude latitude time height10m", @@ -308,7 +308,7 @@ "standard_name": "geopotential_height", "units": "m", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Geopotential Height at 1000 hPa", "comment": "Geopotential height on the 1000 hPa surface", "dimensions": "longitude latitude time p1000", diff --git a/Tables/CMIP6_6hrPlevPt.json b/Tables/CMIP6_6hrPlevPt.json index 16846a82..19bf8c92 100644 --- a/Tables/CMIP6_6hrPlevPt.json +++ b/Tables/CMIP6_6hrPlevPt.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table 6hrPlevPt", "realm": "atmos", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -112,7 +112,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Specific Humidity", - "comment": "", + "comment": "'specific' means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.", "dimensions": "longitude latitude plev27 time1", "out_name": "hus", "type": "real", @@ -130,7 +130,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Specific Humidity", - "comment": "", + "comment": "'specific' means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.", "dimensions": "longitude latitude plev7h time1", "out_name": "hus", "type": "real", @@ -146,7 +146,7 @@ "standard_name": "specific_humidity", "units": "1", "cell_methods": "area: mean time: point", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Near-Surface Specific Humidity", "comment": "Near-surface (usually, 2 meter) specific humidity.", "dimensions": "longitude latitude time1 height2m", @@ -200,7 +200,7 @@ "standard_name": "moisture_content_of_soil_layer", "units": "kg m-2", "cell_methods": "area: mean where land time: point", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Water Content of Soil Layer", "comment": "in each soil layer, the mass of water in all phases, including ice. Reported as 'missing' for grid cells occupied entirely by 'sea'", "dimensions": "longitude latitude time1 sdepth1", @@ -218,7 +218,7 @@ "standard_name": "moisture_content_of_soil_layer", "units": "kg m-2", "cell_methods": "area: mean where land time: point", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Moisture in Upper Portion of Soil Column", "comment": "The mass of water in all phases in the upper 10cm of the soil layer.", "dimensions": "longitude latitude time1 sdepth1", @@ -272,9 +272,9 @@ "standard_name": "atmosphere_relative_vorticity", "units": "s-1", "cell_methods": "area: mean time: point", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Relative Vorticity at 850 hPa", - "comment": "", + "comment": "Relative vorticity is the upward component of the vorticity vector i.e. the component which arises from horizontal velocity.", "dimensions": "longitude latitude time1 p850", "out_name": "rv850", "type": "real", @@ -290,7 +290,7 @@ "standard_name": "wind_speed", "units": "m s-1", "cell_methods": "area: mean time: point", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Near-Surface Wind Speed", "comment": "near-surface (usually, 10 meters) wind speed.", "dimensions": "longitude latitude time1 height10m", @@ -434,7 +434,7 @@ "standard_name": "air_temperature", "units": "K", "cell_methods": "area: mean time: point", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Surface Air Temperature", "comment": "near-surface (usually, 2 meter) air temperature", "dimensions": "longitude latitude time1 height2m", @@ -470,7 +470,7 @@ "standard_name": "soil_temperature", "units": "K", "cell_methods": "area: mean where land time: point", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Temperature of Near-Surface Soil Layer", "comment": "Temperature of soil. Reported as missing for grid cells with no land.", "dimensions": "longitude latitude time1 sdepth1", @@ -490,7 +490,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Eastward Wind", - "comment": "", + "comment": "'Eastward' indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude plev3 time1", "out_name": "ua", "type": "real", @@ -508,7 +508,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Eastward Wind", - "comment": "", + "comment": "'Eastward' indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude plev7h time1", "out_name": "ua", "type": "real", @@ -524,7 +524,7 @@ "standard_name": "eastward_wind", "units": "m s-1", "cell_methods": "area: mean time: point", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Eastward Near-Surface Wind", "comment": "Eastward component of the near-surface (usually, 10 meters) wind", "dimensions": "longitude latitude time1 height10m", @@ -544,7 +544,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Northward Wind", - "comment": "", + "comment": "'Northward' indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude plev3 time1", "out_name": "va", "type": "real", @@ -562,7 +562,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Northward Wind", - "comment": "", + "comment": "'Northward' indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude plev7h time1", "out_name": "va", "type": "real", @@ -578,7 +578,7 @@ "standard_name": "northward_wind", "units": "m s-1", "cell_methods": "area: mean time: point", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Northward Near-Surface Wind", "comment": "Northward component of the near surface wind", "dimensions": "longitude latitude time1 height10m", @@ -596,7 +596,7 @@ "standard_name": "atmosphere_relative_vorticity", "units": "s-1", "cell_methods": "area: mean time: point", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "atmosphere_relative_vorticity", "comment": "Mean vorticity over 850,700,600 hPa", "dimensions": "longitude latitude time1 pl700", @@ -634,7 +634,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Geopotential Height", - "comment": "", + "comment": "Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface.", "dimensions": "longitude latitude plev27 time1", "out_name": "zg", "type": "real", @@ -650,7 +650,7 @@ "standard_name": "geopotential_height", "units": "m", "cell_methods": "area: mean time: point", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Geopotential Height at 500 hPa", "comment": "geopotential height on the 500 hPa surface", "dimensions": "longitude latitude time1 p500", @@ -670,7 +670,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Geopotential Height", - "comment": "", + "comment": "Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface.", "dimensions": "longitude latitude plev7h time1", "out_name": "zg", "type": "real", diff --git a/Tables/CMIP6_AERday.json b/Tables/CMIP6_AERday.json index 441d43b7..74ac40b0 100644 --- a/Tables/CMIP6_AERday.json +++ b/Tables/CMIP6_AERday.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table AERday", "realm": "aerosol", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -22,7 +22,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "cloud optical depth", - "comment": "", + "comment": "The optical thickness is the integral along the path of radiation of a volume scattering/absorption/attenuation coefficient. The radiative flux is reduced by a factor exp(-optical_thickness) on traversing the path. A coordinate variable of radiation_wavelength or radiation_frequency can be specified to indicate that the optical thickness applies at specific wavelengths or frequencies. The atmosphere optical thickness applies to radiation passing through the entire atmosphere. 'Cloud' means the component of extinction owing to the presence of liquid or ice water particles. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase.", "dimensions": "longitude latitude time", "out_name": "cod", "type": "real", @@ -77,7 +77,7 @@ "cell_measures": "area: areacella", "long_name": "ambient aerosol optical thickness at 550 nm", "comment": "AOD from the ambient aerosols (i.e., includes aerosol water). Does not include AOD from stratospheric aerosols if these are prescribed but includes other possible background aerosol types. Needs a comment attribute 'wavelength: 550 nm'", - "dimensions": "longitude latitude time", + "dimensions": "longitude latitude time lambda550nm", "out_name": "od550aer", "type": "real", "positive": "", @@ -94,7 +94,7 @@ "cell_methods": "area: mean time: maximum", "cell_measures": "area: areacella", "long_name": "daily maximum O3 volume mixing ratio in lowest model layer", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude time", "out_name": "sfo3max", "type": "real", @@ -128,7 +128,7 @@ "standard_name": "eastward_wind", "units": "m s-1", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Eastward Wind at 10 hPa", "comment": "Zonal wind on the 10 hPa surface", "dimensions": "longitude latitude time p10", @@ -146,7 +146,7 @@ "standard_name": "geopotential_height", "units": "m", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Geopotential Height at 10 hPa", "comment": "Geopotential height on the 10 hPa surface", "dimensions": "longitude latitude time p10", @@ -164,7 +164,7 @@ "standard_name": "geopotential_height", "units": "m", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Geopotential Height at 100 hPa", "comment": "Geopotential height on the 100 hPa surface", "dimensions": "longitude latitude time p100", @@ -182,7 +182,7 @@ "standard_name": "geopotential_height", "units": "m", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Geopotential Height at 1000 hPa", "comment": "Geopotential height on the 1000 hPa surface", "dimensions": "longitude latitude time p1000", @@ -200,7 +200,7 @@ "standard_name": "geopotential_height", "units": "m", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Geopotential Height at 500 hPa", "comment": "geopotential height on the 500 hPa surface", "dimensions": "longitude latitude time p500", diff --git a/Tables/CMIP6_AERhr.json b/Tables/CMIP6_AERhr.json index eee84907..55920a65 100644 --- a/Tables/CMIP6_AERhr.json +++ b/Tables/CMIP6_AERhr.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table AERhr", "realm": "aerosol", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -40,7 +40,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "NO2 volume mixing ratio in lowest model layer", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude time", "out_name": "sfno2", "type": "real", @@ -58,7 +58,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "O3 volume mixing ratio in lowest model layer", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude time", "out_name": "sfo3", "type": "real", @@ -76,7 +76,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "PM2.5 mass mixing ratio in lowest model layer", - "comment": "", + "comment": "Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of X to the mass of Y (including X). A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. 'Aerosol' means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. 'Ambient_aerosol' means that the aerosol is measured or modelled at the ambient state of pressure, temperature and relative humidity that exists in its immediate environment. 'Ambient aerosol particles' are aerosol particles that have taken up ambient water through hygroscopic growth. The extent of hygroscopic growth depends on the relative humidity and the composition of the particles. 'Pm2p5 aerosol' means atmospheric particulate compounds with an aerodynamic diameter of less than or equal to 2.5 micrometers.", "dimensions": "longitude latitude time", "out_name": "sfpm25", "type": "real", @@ -92,7 +92,7 @@ "standard_name": "air_temperature", "units": "K", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Surface Temperature", "comment": "near-surface (usually, 2 meter) air temperature", "dimensions": "longitude latitude time height2m", diff --git a/Tables/CMIP6_AERmon.json b/Tables/CMIP6_AERmon.json index 72b148e7..32dba05a 100644 --- a/Tables/CMIP6_AERmon.json +++ b/Tables/CMIP6_AERmon.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table AERmon", "realm": "aerosol", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -22,8 +22,8 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "ambient aerosol absorption optical thickness at 550 nm", - "comment": "", - "dimensions": "longitude latitude time", + "comment": "alias::atmosphere_absorption_optical_thickness_due_to_ambient_aerosol", + "dimensions": "longitude latitude time lambda550nm", "out_name": "abs550aer", "type": "real", "positive": "", @@ -40,7 +40,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Vertically integrated mass content of air in layer", - "comment": "", + "comment": "'Mass_of_air' means the mass due solely to the gaseous constituents of the atmosphere. The standard name for the mass including precipitation and aerosol particles is atmosphere_mass_per_unit_area.", "dimensions": "longitude latitude alevel time", "out_name": "airmass", "type": "real", @@ -94,7 +94,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "C2H2 volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude alevel time", "out_name": "c2h2", "type": "real", @@ -112,7 +112,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "C2H6 volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude alevel time", "out_name": "c2h6", "type": "real", @@ -130,7 +130,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "C3H6 volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude alevel time", "out_name": "c3h6", "type": "real", @@ -148,7 +148,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "C3H8 volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude alevel time", "out_name": "c3h8", "type": "real", @@ -202,7 +202,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "CH3COCH3 volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction 'mole_fraction_of_X_in_Y', where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. Acetone is an organic molecule with the chemical formula CH3CH3CO. The IUPAC name for acetone is propan-2-one. Acetone is a member of the group of organic compounds known as ketones. There are standard names for the ketone group as well as for some of the individual species.", "dimensions": "longitude latitude alevel time", "out_name": "ch3coch3", "type": "real", @@ -220,7 +220,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "CH4 volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude alevel time", "out_name": "ch4", "type": "real", @@ -328,7 +328,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "CO volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude alevel time", "out_name": "co", "type": "real", @@ -346,7 +346,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "CO2 volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude alevel time", "out_name": "co2", "type": "real", @@ -364,7 +364,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "cloud optical depth", - "comment": "", + "comment": "The optical thickness is the integral along the path of radiation of a volume scattering/absorption/attenuation coefficient. The radiative flux is reduced by a factor exp(-optical_thickness) on traversing the path. A coordinate variable of radiation_wavelength or radiation_frequency can be specified to indicate that the optical thickness applies at specific wavelengths or frequencies. The atmosphere optical thickness applies to radiation passing through the entire atmosphere. 'Cloud' means the component of extinction owing to the presence of liquid or ice water particles. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase.", "dimensions": "longitude latitude time", "out_name": "cod", "type": "real", @@ -382,7 +382,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "DMS volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude alevel time", "out_name": "dms", "type": "real", @@ -904,7 +904,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Formaldehyde volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude alevel time", "out_name": "hcho", "type": "real", @@ -922,7 +922,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "HCl volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. The chemical formula of hydrogen chloride is HCl.", "dimensions": "longitude latitude alevel time", "out_name": "hcl", "type": "real", @@ -940,7 +940,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "HNO3 volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude alevel time", "out_name": "hno3", "type": "real", @@ -958,7 +958,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Isoprene volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude alevel time", "out_name": "isop", "type": "real", @@ -976,7 +976,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "photolysis rate of NO2", - "comment": "", + "comment": "'Photolysis' is a chemical reaction in which a chemical compound is broken down by photons. The 'reaction rate' is the rate at which the reactants of a chemical reaction form the products. The chemical formula for nitrogen dioxide is NO2.", "dimensions": "longitude latitude alevel time", "out_name": "jno2", "type": "real", @@ -1048,7 +1048,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "liquid water path", - "comment": "", + "comment": "'Content' indicates a quantity per unit area. The 'atmosphere content' of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used.", "dimensions": "longitude latitude time", "out_name": "lwp", "type": "real", @@ -1066,7 +1066,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Aerosol water mass mixing ratio", - "comment": "", + "comment": "Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of X to the mass of Y (including X). 'Aerosol' means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. 'Ambient_aerosol' means that the aerosol is measured or modelled at the ambient state of pressure, temperature and relative humidity that exists in its immediate environment. 'Ambient aerosol particles' are aerosol particles that have taken up ambient water through hygroscopic growth. The extent of hygroscopic growth depends on the relative humidity and the composition of the particles.", "dimensions": "longitude latitude alevel time", "out_name": "mmraerh2o", "type": "real", @@ -1084,7 +1084,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Elemental carbon mass mixing ratio", - "comment": "", + "comment": "Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of X to the mass of Y (including X). 'Aerosol' means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. 'Dry aerosol particles' means aerosol particles without any water uptake. Chemically, 'elemental carbon' is the carbonaceous fraction of particulate matter that is thermally stable in an inert atmosphere to high temperatures near 4000K and can only be gasified by oxidation starting at temperatures above 340 C. It is assumed to be inert and non-volatile under atmospheric conditions and insoluble in any solvent (Ogren and Charlson, 1983).", "dimensions": "longitude latitude alevel time", "out_name": "mmrbc", "type": "real", @@ -1102,7 +1102,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Dust aerosol mass mixing ratio", - "comment": "", + "comment": "Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of X to the mass of Y (including X). 'Aerosol' means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. 'Dry aerosol particles' means aerosol particles without any water uptake.", "dimensions": "longitude latitude alevel time", "out_name": "mmrdust", "type": "real", @@ -1120,7 +1120,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "NH4 mass mixing ratio", - "comment": "", + "comment": "Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of X to the mass of Y (including X). 'Mass_fraction_of_ammonium' means that the mass is expressed as mass of NH4. 'Aerosol' means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. 'Dry aerosol particles' means aerosol particles without any water uptake.", "dimensions": "longitude latitude alevel time", "out_name": "mmrnh4", "type": "real", @@ -1138,7 +1138,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "NO3 aerosol mass mixing ratio", - "comment": "", + "comment": "Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of X to the mass of Y (including X). 'Mass_fraction_of_nitrate' means that the mass is expressed as mass of NO3. 'Aerosol' means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. 'Dry aerosol particles' means aerosol particles without any water uptake.", "dimensions": "longitude latitude alevel time", "out_name": "mmrno3", "type": "real", @@ -1228,7 +1228,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Aerosol sulfate mass mixing ratio", - "comment": "", + "comment": "Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of X to the mass of Y (including X). 'Mass_fraction_of_sulfate' means that the mass is expressed as mass of SO4. 'Aerosol' means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. 'Dry aerosol particles' means aerosol particles without any water uptake.", "dimensions": "longitude latitude alevel time", "out_name": "mmrso4", "type": "real", @@ -1246,7 +1246,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Secondary organic aerosol mass mixing ratio", - "comment": "", + "comment": "Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of X to the mass of Y (including X). 'Aerosol' means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. 'Dry aerosol particles' means aerosol particles without any water uptake. 'Secondary particulate organic matter' means particulate organic matter formed within the atmosphere from gaseous precursors. The sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol is particulate_organic_matter_dry_aerosol.", "dimensions": "longitude latitude alevel time", "out_name": "mmrsoa", "type": "real", @@ -1264,7 +1264,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Sea Salt mass mixing ratio", - "comment": "", + "comment": "alias::mass_fraction_of_seasalt_dry_aerosol_particles_in_air", "dimensions": "longitude latitude alevel time", "out_name": "mmrss", "type": "real", @@ -1282,7 +1282,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "N2O volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. The chemical formula of nitrous oxide is N2O.", "dimensions": "longitude latitude alevel time", "out_name": "n2o", "type": "real", @@ -1300,7 +1300,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Artificial tracer with 50 day lifetime", - "comment": "", + "comment": "Mole fraction is used in the construction 'mole_fraction_of_X_in_Y', where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. 'Artificial tracer' means a passive atmospheric tracer that is used to study atmospheric transport and deposition. To specify the length of the tracer lifetime in the atmosphere, a scalar coordinate variable with the standard name of tracer_lifetime should be used.", "dimensions": "longitude latitude alevel time", "out_name": "nh50", "type": "real", @@ -1318,7 +1318,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "NO volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude alevel time", "out_name": "no", "type": "real", @@ -1336,7 +1336,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "NO2 volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude alevel time", "out_name": "no2", "type": "real", @@ -1354,7 +1354,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Ozone volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude alevel time", "out_name": "o3", "type": "real", @@ -1445,7 +1445,7 @@ "cell_measures": "area: areacella", "long_name": "ambient aerosol optical thickness at 550 nm", "comment": "AOD from the ambient aerosols (i.e., includes aerosol water). Does not include AOD from stratospheric aerosols if these are prescribed but includes other possible background aerosol types. Needs a comment attribute 'wavelength: 550 nm'", - "dimensions": "longitude latitude time", + "dimensions": "longitude latitude time lambda550nm", "out_name": "od550aer", "type": "real", "positive": "", @@ -1463,7 +1463,7 @@ "cell_measures": "area: areacella", "long_name": "aerosol water aod@550nm", "comment": "proposed name: atmosphere_optical_thickness_due_to_water_ambient_aerosol", - "dimensions": "longitude latitude time", + "dimensions": "longitude latitude time lambda550nm", "out_name": "od550aerh2o", "type": "real", "positive": "", @@ -1481,7 +1481,7 @@ "cell_measures": "area: areacella", "long_name": "bb aod@550nm", "comment": "total organic aerosol AOD due to biomass burning (excluding so4, nitrate BB components)", - "dimensions": "longitude latitude time", + "dimensions": "longitude latitude time lambda550nm", "out_name": "od550bb", "type": "real", "positive": "", @@ -1498,8 +1498,8 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "black carbon aod@550nm", - "comment": "", - "dimensions": "longitude latitude time", + "comment": "The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. The optical thickness is the integral along the path of radiation of a volume scattering/absorption/attenuation coefficient. The radiative flux is reduced by a factor exp(-optical_thickness) on traversing the path. The atmosphere optical thickness applies to radiation passing through the entire atmosphere. 'Aerosol' means the suspended liquid or solid particles in air (except cloud droplets). 'Ambient aerosol' is aerosol that has taken up ambient water through hygroscopic growth. The extent of hygroscopic growth depends on the relative humidity and the composition of the aerosol. Black carbon aerosol is composed of elemental carbon. It is strongly light absorbing.", + "dimensions": "longitude latitude time lambda550nm", "out_name": "od550bc", "type": "real", "positive": "", @@ -1517,7 +1517,7 @@ "cell_measures": "area: areacella", "long_name": "ambient aerosol optical thickness at 550 nm", "comment": "AOD from the ambient aerosols in clear skies if od550aer is for all-sky (i.e., includes aerosol water). Does not include AOD from stratospheric aerosols if these are prescribed but includes other possible background aerosol types. Needs a comment attribute 'wavelength: 550 nm'", - "dimensions": "longitude latitude time", + "dimensions": "longitude latitude time lambda550nm", "out_name": "od550csaer", "type": "real", "positive": "", @@ -1534,8 +1534,8 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "dust aod@550nm", - "comment": "", - "dimensions": "longitude latitude time", + "comment": "alias::atmosphere_optical_thickness_due_to_dust_ambient_aerosol", + "dimensions": "longitude latitude time lambda550nm", "out_name": "od550dust", "type": "real", "positive": "", @@ -1553,7 +1553,7 @@ "cell_measures": "area: areacella", "long_name": "ambient fine mode aerosol optical thickness at 550 nm", "comment": "od550 due to particles with wet diameter less than 1 um (ambient here means wetted). When models do not include explicit size information, it can be assumed that all anthropogenic aerosols and natural secondary aerosols have diameter less than 1 um.", - "dimensions": "longitude latitude time", + "dimensions": "longitude latitude time lambda550nm", "out_name": "od550lt1aer", "type": "real", "positive": "", @@ -1565,13 +1565,13 @@ "od550no3": { "frequency": "mon", "modeling_realm": "aerosol", - "standard_name": "atmosphere_optical_thickness_due_to_nitrate_ambient_aerosol", + "standard_name": "atmosphere_optical_thickness_due_to_nitrate_ambient_aerosol_particles", "units": "1", "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "nitrate aod@550nm", "comment": "proposed name: atmosphere_optical_thickness_due_to_nitrate_ambient_aerosol", - "dimensions": "longitude latitude time", + "dimensions": "longitude latitude time lambda550nm", "out_name": "od550no3", "type": "real", "positive": "", @@ -1588,8 +1588,8 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "total organic aerosol aod@550nm", - "comment": "", - "dimensions": "longitude latitude time", + "comment": "alias::atmosphere_optical_thickness_due_to_particulate_organic_matter_ambient_aerosol", + "dimensions": "longitude latitude time lambda550nm", "out_name": "od550oa", "type": "real", "positive": "", @@ -1601,13 +1601,13 @@ "od550so4": { "frequency": "mon", "modeling_realm": "aerosol", - "standard_name": "atmosphere_optical_thickness_due_to_sulfate_ambient_aerosol", + "standard_name": "atmosphere_optical_thickness_due_to_sulfate_ambient_aerosol_particles", "units": "1", "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "sulfate aod@550nm", "comment": "proposed name: atmosphere_optical_thickness_due_to_sulfate_ambient_aerosol", - "dimensions": "longitude latitude time", + "dimensions": "longitude latitude time lambda550nm", "out_name": "od550so4", "type": "real", "positive": "", @@ -1625,7 +1625,7 @@ "cell_measures": "area: areacella", "long_name": "soa aod@550nm", "comment": "total organic aerosol AOD due to secondary aerosol formation", - "dimensions": "longitude latitude time", + "dimensions": "longitude latitude time lambda550nm", "out_name": "od550soa", "type": "real", "positive": "", @@ -1642,8 +1642,8 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "sea salt aod@550nm", - "comment": "", - "dimensions": "longitude latitude time", + "comment": "alias::atmosphere_optical_thickness_due_to_seasalt_ambient_aerosol", + "dimensions": "longitude latitude time lambda550nm", "out_name": "od550ss", "type": "real", "positive": "", @@ -1678,7 +1678,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "OH volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude alevel time", "out_name": "oh", "type": "real", @@ -1696,7 +1696,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "PAN volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude alevel time", "out_name": "pan", "type": "real", @@ -1912,7 +1912,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "SO2 volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude alevel time", "out_name": "so2", "type": "real", @@ -2020,7 +2020,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "air temperature at cloud top", - "comment": "", + "comment": "cloud_top refers to the top of the highest cloud. Air temperature is the bulk temperature of the air, not the surface (skin) temperature.", "dimensions": "longitude latitude time", "out_name": "ttop", "type": "real", @@ -2038,7 +2038,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Eastward Wind", - "comment": "", + "comment": "'Eastward' indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude alevel time", "out_name": "ua", "type": "real", @@ -2056,7 +2056,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Northward Wind", - "comment": "", + "comment": "'Northward' indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude alevel time", "out_name": "va", "type": "real", @@ -2074,7 +2074,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Upward Air Velocity", - "comment": "", + "comment": "A velocity is a vector quantity. 'Upward' indicates a vector component which is positive when directed upward (negative downward). Upward air velocity is the vertical component of the 3D air velocity vector. The standard name downward_air_velocity may be used for a vector component with the opposite sign convention.", "dimensions": "longitude latitude alevel time", "out_name": "wa", "type": "real", @@ -2092,7 +2092,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "wet deposition rate of black carbon aerosol mass", - "comment": "", + "comment": "'tendency_of_X' means derivative of X with respect to time. 'Content' indicates a quantity per unit area. The 'atmosphere content' of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including 'content_of_atmosphere_layer' are used. The mass is the total mass of the particles. 'Aerosol' means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. 'Dry aerosol particles' means aerosol particles without any water uptake. The specification of a physical process by the phrase 'due_to_' process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. 'Wet deposition' means deposition by precipitation.", "dimensions": "longitude latitude time", "out_name": "wetbc", "type": "real", @@ -2110,7 +2110,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "wet deposition rate of dust", - "comment": "", + "comment": "'Content' indicates a quantity per unit area. The 'atmosphere content' of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including 'content_of_atmosphere_layer' are used. The mass is the total mass of the particles. 'Aerosol' means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. 'Dry aerosol particles' means aerosol particles without any water uptake. 'Wet deposition' means deposition by precipitation. 'tendency_of_X' means derivative of X with respect to time.", "dimensions": "longitude latitude time", "out_name": "wetdust", "type": "real", @@ -2128,7 +2128,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "wet deposition rate of nh3", - "comment": "", + "comment": "'tendency_of_X' means derivative of X with respect to time. 'Content' indicates a quantity per unit area. 'Wet deposition' means deposition by precipitation.", "dimensions": "longitude latitude time", "out_name": "wetnh3", "type": "real", @@ -2146,7 +2146,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "wet deposition rate of nh4", - "comment": "", + "comment": "'Content' indicates a quantity per unit area. The 'atmosphere content' of a quantity refers to the vertical integral from the surface to the top of the atmosphere. For the content between specified levels in the atmosphere, standard names including content_of_atmosphere_layer are used. The mass is the total mass of the particles. 'Aerosol' means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. 'Dry aerosol particles' means aerosol particles without any water uptake. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. 'Wet deposition' means deposition by precipitation. 'tendency_of_X' means derivative of X with respect to time.", "dimensions": "longitude latitude time", "out_name": "wetnh4", "type": "real", @@ -2200,7 +2200,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "wet deposition rate of so2", - "comment": "", + "comment": "'tendency_of_X' means derivative of X with respect to time. 'Content' indicates a quantity per unit area. 'Wet deposition' means deposition by precipitation.", "dimensions": "longitude latitude time", "out_name": "wetso2", "type": "real", @@ -2236,7 +2236,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "wet deposition rate of seasalt", - "comment": "", + "comment": "alias::tendency_of_atmosphere_mass_content_of_seasalt_dry_aerosol_particles_due_to_wet_deposition", "dimensions": "longitude latitude time", "out_name": "wetss", "type": "real", @@ -2254,7 +2254,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Geopotential Height", - "comment": "", + "comment": "Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface.", "dimensions": "longitude latitude alevel time", "out_name": "zg", "type": "real", diff --git a/Tables/CMIP6_AERmonZ.json b/Tables/CMIP6_AERmonZ.json index 05aae2cf..3a8966c4 100644 --- a/Tables/CMIP6_AERmonZ.json +++ b/Tables/CMIP6_AERmonZ.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table AERmonZ", "realm": "aerosol", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -40,7 +40,7 @@ "cell_methods": "longitude: mean time: mean", "cell_measures": "", "long_name": "CH4 volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "latitude plev39 time", "out_name": "ch4", "type": "real", @@ -94,7 +94,7 @@ "cell_methods": "longitude: mean time: mean", "cell_measures": "", "long_name": "HCl volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. The chemical formula of hydrogen chloride is HCl.", "dimensions": "latitude plev39 time", "out_name": "hcl", "type": "real", @@ -112,7 +112,7 @@ "cell_methods": "longitude: mean time: mean", "cell_measures": "", "long_name": "HNO3 volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "latitude plev39 time", "out_name": "hno3", "type": "real", @@ -130,7 +130,7 @@ "cell_methods": "longitude: mean time: mean", "cell_measures": "", "long_name": "HO2 volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. The chemical formula of hydroperoxyl radical is HO2.", "dimensions": "latitude plev39 time", "out_name": "ho2", "type": "real", @@ -166,7 +166,7 @@ "cell_methods": "longitude: mean time: mean", "cell_measures": "", "long_name": "N2O volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. The chemical formula of nitrous oxide is N2O.", "dimensions": "latitude plev39 time", "out_name": "n2o", "type": "real", @@ -202,7 +202,7 @@ "cell_methods": "longitude: mean time: mean", "cell_measures": "", "long_name": "Ozone volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "latitude plev39 time", "out_name": "o3", "type": "real", @@ -220,7 +220,7 @@ "cell_methods": "longitude: mean time: mean", "cell_measures": "", "long_name": "OH volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "latitude plev39 time", "out_name": "oh", "type": "real", @@ -256,7 +256,7 @@ "cell_methods": "longitude: mean time: mean", "cell_measures": "", "long_name": "Eastward Wind", - "comment": "", + "comment": "'Eastward' indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "latitude plev39 time", "out_name": "ua", "type": "real", @@ -274,7 +274,7 @@ "cell_methods": "longitude: mean time: mean", "cell_measures": "", "long_name": "Northward Wind", - "comment": "", + "comment": "'Northward' indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "latitude plev39 time", "out_name": "va", "type": "real", @@ -310,7 +310,7 @@ "cell_methods": "longitude: mean time: mean", "cell_measures": "", "long_name": "Geopotential Height", - "comment": "", + "comment": "Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface.", "dimensions": "latitude plev39 time", "out_name": "zg", "type": "real", diff --git a/Tables/CMIP6_Amon.json b/Tables/CMIP6_Amon.json index f6d39b4f..aa5117d3 100644 --- a/Tables/CMIP6_Amon.json +++ b/Tables/CMIP6_Amon.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table Amon", "realm": "atmos atmosChem", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -112,7 +112,7 @@ "cell_methods": "time: mean", "cell_measures": "area: areacella", "long_name": "Mole Fraction of CH4", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude plev19 time", "out_name": "ch4", "type": "real", @@ -130,7 +130,7 @@ "cell_methods": "area: mean time: mean within years time: mean over years", "cell_measures": "area: areacella", "long_name": "Mole Fraction of CH4", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude plev19 time2", "out_name": "ch4", "type": "real", @@ -310,7 +310,7 @@ "cell_methods": "time: mean", "cell_measures": "area: areacella", "long_name": "Mole Fraction of CO2", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude plev19 time", "out_name": "co2", "type": "real", @@ -328,7 +328,7 @@ "cell_methods": "area: mean time: mean within years time: mean over years", "cell_measures": "area: areacella", "long_name": "Mole Fraction of CO2", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude plev19 time2", "out_name": "co2", "type": "real", @@ -472,7 +472,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Surface Upward Latent Heat Flux", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Upward' indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "hfls", "type": "real", @@ -490,7 +490,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Surface Upward Sensible Heat Flux", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Upward' indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called 'turbulent' heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. Unless indicated in the cell_methods attribute, a quantity is assumed to apply to the whole area of each horizontal grid box. Previously, the qualifier where_type was used to specify that the quantity applies only to the part of the grid box of the named type. Names containing the where_type qualifier are deprecated and newly created data should use the cell_methods attribute to indicate the horizontal area to which the quantity applies.", "dimensions": "longitude latitude time", "out_name": "hfss", "type": "real", @@ -524,7 +524,7 @@ "standard_name": "relative_humidity", "units": "%", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Near-Surface Relative Humidity", "comment": "The relative humidity with respect to liquid water for T> 0 C, and with respect to ice for T<0 C.", "dimensions": "longitude latitude time height2m", @@ -544,7 +544,7 @@ "cell_methods": "time: mean", "cell_measures": "area: areacella", "long_name": "Specific Humidity", - "comment": "", + "comment": "'specific' means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.", "dimensions": "longitude latitude plev19 time", "out_name": "hus", "type": "real", @@ -560,7 +560,7 @@ "standard_name": "specific_humidity", "units": "1", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Near-Surface Specific Humidity", "comment": "Near-surface (usually, 2 meter) specific humidity.", "dimensions": "longitude latitude time height2m", @@ -598,7 +598,7 @@ "cell_methods": "time: mean", "cell_measures": "area: areacella", "long_name": "Mole Fraction of N2O", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. The chemical formula of nitrous oxide is N2O.", "dimensions": "longitude latitude plev19 time", "out_name": "n2o", "type": "real", @@ -616,7 +616,7 @@ "cell_methods": "area: mean time: mean within years time: mean over years", "cell_measures": "area: areacella", "long_name": "Mole Fraction of N2O", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. The chemical formula of nitrous oxide is N2O.", "dimensions": "longitude latitude plev19 time2", "out_name": "n2o", "type": "real", @@ -670,7 +670,7 @@ "cell_methods": "time: mean", "cell_measures": "area: areacella", "long_name": "Mole Fraction of O3", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude plev19 time", "out_name": "o3", "type": "real", @@ -688,7 +688,7 @@ "cell_methods": "area: mean time: mean within years time: mean over years", "cell_measures": "area: areacella", "long_name": "Mole Fraction of O3", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude plev19 time2", "out_name": "o3", "type": "real", @@ -850,7 +850,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Surface Downwelling Longwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'longwave' means longwave radiation. Downwelling radiation is radiation from above. It does not mean 'net downward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "rlds", "type": "real", @@ -886,7 +886,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Surface Upwelling Longwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'longwave' means longwave radiation. Upwelling radiation is radiation from below. It does not mean 'net upward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "rlus", "type": "real", @@ -994,7 +994,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Surface Upwelling Shortwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'shortwave' means shortwave radiation. Upwelling radiation is radiation from below. It does not mean 'net upward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "rsus", "type": "real", @@ -1118,7 +1118,7 @@ "standard_name": "wind_speed", "units": "m s-1", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Near-Surface Wind Speed", "comment": "near-surface (usually, 10 meters) wind speed.", "dimensions": "longitude latitude time height10m", @@ -1154,7 +1154,7 @@ "standard_name": "air_temperature", "units": "K", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Near-Surface Air Temperature", "comment": "near-surface (usually, 2 meter) air temperature", "dimensions": "longitude latitude time height2m", @@ -1264,7 +1264,7 @@ "cell_methods": "time: mean", "cell_measures": "area: areacella", "long_name": "Eastward Wind", - "comment": "", + "comment": "'Eastward' indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude plev19 time", "out_name": "ua", "type": "real", @@ -1280,7 +1280,7 @@ "standard_name": "eastward_wind", "units": "m s-1", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Eastward Near-Surface Wind", "comment": "Eastward component of the near-surface (usually, 10 meters) wind", "dimensions": "longitude latitude time height10m", @@ -1300,7 +1300,7 @@ "cell_methods": "time: mean", "cell_measures": "area: areacella", "long_name": "Northward Wind", - "comment": "", + "comment": "'Northward' indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude plev19 time", "out_name": "va", "type": "real", @@ -1316,7 +1316,7 @@ "standard_name": "northward_wind", "units": "m s-1", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Northward Near-Surface Wind", "comment": "Northward component of the near surface wind", "dimensions": "longitude latitude time height10m", @@ -1354,7 +1354,7 @@ "cell_methods": "time: mean", "cell_measures": "area: areacella", "long_name": "Geopotential Height", - "comment": "", + "comment": "Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface.", "dimensions": "longitude latitude plev19 time", "out_name": "zg", "type": "real", diff --git a/Tables/CMIP6_CF3hr.json b/Tables/CMIP6_CF3hr.json index 15e09ff6..b56b2a2c 100644 --- a/Tables/CMIP6_CF3hr.json +++ b/Tables/CMIP6_CF3hr.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table CF3hr", "realm": "atmos", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -346,7 +346,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Surface Upward Latent Heat Flux", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Upward' indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time1", "out_name": "hfls", "type": "real", @@ -364,7 +364,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Surface Upward Sensible Heat Flux", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Upward' indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called 'turbulent' heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. Unless indicated in the cell_methods attribute, a quantity is assumed to apply to the whole area of each horizontal grid box. Previously, the qualifier where_type was used to specify that the quantity applies only to the part of the grid box of the named type. Names containing the where_type qualifier are deprecated and newly created data should use the cell_methods attribute to indicate the horizontal area to which the quantity applies.", "dimensions": "longitude latitude time1", "out_name": "hfss", "type": "real", @@ -380,7 +380,7 @@ "standard_name": "relative_humidity", "units": "%", "cell_methods": "area: mean time: point", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Near-Surface Relative Humidity", "comment": "The relative humidity with respect to liquid water for T> 0 C, and with respect to ice for T<0 C.", "dimensions": "longitude latitude time1 height2m", @@ -778,7 +778,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Surface Downwelling Longwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'longwave' means longwave radiation. Downwelling radiation is radiation from above. It does not mean 'net downward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time1", "out_name": "rlds", "type": "real", @@ -814,7 +814,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Surface Upwelling Longwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'longwave' means longwave radiation. Upwelling radiation is radiation from below. It does not mean 'net upward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time1", "out_name": "rlus", "type": "real", @@ -922,7 +922,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Surface Upwelling Shortwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'shortwave' means shortwave radiation. Upwelling radiation is radiation from below. It does not mean 'net upward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time1", "out_name": "rsus", "type": "real", @@ -1046,7 +1046,7 @@ "standard_name": "wind_speed", "units": "m s-1", "cell_methods": "area: mean time: point", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Near-Surface Wind Speed", "comment": "near-surface (usually, 10 meters) wind speed.", "dimensions": "longitude latitude time1 height10m", @@ -1138,7 +1138,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Altitude of Model Full-Levels", - "comment": "", + "comment": "'Height_above_X' means the vertical distance above the named surface X. A reference ellipsoid is a mathematical figure that approximates the geoid. The geoid is a surface of constant geopotential with which mean sea level would coincide if the ocean were at rest. The ellipsoid is an approximation because the geoid is an irregular shape. A number of reference ellipsoids are defined for use in the field of geodesy. To specify which reference ellipsoid is being used, a grid_mapping variable should be attached to the data variable as described in Chapter 5.6 of the CF Convention.", "dimensions": "longitude latitude alevel time1", "out_name": "zfull", "type": "real", @@ -1156,7 +1156,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Altitude of Model Half-Levels", - "comment": "", + "comment": "'Height_above_X' means the vertical distance above the named surface X. A reference ellipsoid is a mathematical figure that approximates the geoid. The geoid is a surface of constant geopotential with which mean sea level would coincide if the ocean were at rest. The ellipsoid is an approximation because the geoid is an irregular shape. A number of reference ellipsoids are defined for use in the field of geodesy. To specify which reference ellipsoid is being used, a grid_mapping variable should be attached to the data variable as described in Chapter 5.6 of the CF Convention.", "dimensions": "longitude latitude alevhalf time1", "out_name": "zhalf", "type": "real", diff --git a/Tables/CMIP6_CFday.json b/Tables/CMIP6_CFday.json index 3badf94f..b3ddf48c 100644 --- a/Tables/CMIP6_CFday.json +++ b/Tables/CMIP6_CFday.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table CFday", "realm": "atmos", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -110,7 +110,7 @@ "standard_name": "cloud_area_fraction_in_atmosphere_layer", "units": "%", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "CALIPSO High Level Cloud Fraction", "comment": "Percentage cloud cover in layer centred on 220hPa", "dimensions": "longitude latitude time p220", @@ -182,7 +182,7 @@ "standard_name": "cloud_area_fraction_in_atmosphere_layer", "units": "%", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "CALIPSO Low Level Cloud Fraction", "comment": "Percentage cloud cover in layer centred on 840hPa", "dimensions": "longitude latitude time p840", @@ -200,7 +200,7 @@ "standard_name": "cloud_area_fraction_in_atmosphere_layer", "units": "%", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "CALIPSO Mid Level Cloud Fraction", "comment": "Percentage cloud cover in layer centred on 560hPa", "dimensions": "longitude latitude time p560", @@ -310,7 +310,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Specific Humidity", - "comment": "", + "comment": "'specific' means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.", "dimensions": "longitude latitude alevel time", "out_name": "hus", "type": "real", @@ -560,7 +560,7 @@ "standard_name": "air_temperature", "units": "K", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Air Temperature", "comment": "Air temperature at 700hPa", "dimensions": "longitude latitude time p700", @@ -580,7 +580,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Eastward Wind", - "comment": "", + "comment": "'Eastward' indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude alevel time", "out_name": "ua", "type": "real", @@ -598,7 +598,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Northward Wind", - "comment": "", + "comment": "'Northward' indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude alevel time", "out_name": "va", "type": "real", @@ -632,7 +632,7 @@ "standard_name": "lagrangian_tendency_of_air_pressure", "units": "Pa s-1", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "omega (=dp/dt)", "comment": "Omega (vertical velocity in pressure coordinates, positive downwards) at 500 hPa level;", "dimensions": "longitude latitude time p500", @@ -652,7 +652,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Geopotential Height", - "comment": "", + "comment": "Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface.", "dimensions": "longitude latitude alevel time", "out_name": "zg", "type": "real", diff --git a/Tables/CMIP6_CFmon.json b/Tables/CMIP6_CFmon.json index da74c752..9489ac21 100644 --- a/Tables/CMIP6_CFmon.json +++ b/Tables/CMIP6_CFmon.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table CFmon", "realm": "atmos", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -74,7 +74,7 @@ "standard_name": "cloud_area_fraction_in_atmosphere_layer", "units": "%", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "CALIPSO Percentage High Level Cloud", "comment": "Percentage cloud cover in layer centred on 220hPa", "dimensions": "longitude latitude time p220", @@ -146,7 +146,7 @@ "standard_name": "cloud_area_fraction_in_atmosphere_layer", "units": "%", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "CALIPSO Percentage Low Level Cloud", "comment": "Percentage cloud cover in layer centred on 840hPa", "dimensions": "longitude latitude time p840", @@ -164,7 +164,7 @@ "standard_name": "cloud_area_fraction_in_atmosphere_layer", "units": "%", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "CALIPSO Percentage Mid Level Cloud", "comment": "Percentage cloud cover in layer centred on 560hPa", "dimensions": "longitude latitude time p560", @@ -346,7 +346,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Specific Humidity", - "comment": "", + "comment": "'specific' means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.", "dimensions": "longitude latitude alevel time", "out_name": "hus", "type": "real", diff --git a/Tables/CMIP6_CFsubhr.json b/Tables/CMIP6_CFsubhr.json index e9a48086..9ce608c8 100644 --- a/Tables/CMIP6_CFsubhr.json +++ b/Tables/CMIP6_CFsubhr.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table CFsubhr", "realm": "atmos", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -292,7 +292,7 @@ "cell_methods": "area: point time: point", "cell_measures": "", "long_name": "Surface Upward Latent Heat Flux", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Upward' indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "site time1", "out_name": "hfls", "type": "real", @@ -310,7 +310,7 @@ "cell_methods": "area: point time: point", "cell_measures": "", "long_name": "Surface Upward Sensible Heat Flux", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Upward' indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called 'turbulent' heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. Unless indicated in the cell_methods attribute, a quantity is assumed to apply to the whole area of each horizontal grid box. Previously, the qualifier where_type was used to specify that the quantity applies only to the part of the grid box of the named type. Names containing the where_type qualifier are deprecated and newly created data should use the cell_methods attribute to indicate the horizontal area to which the quantity applies.", "dimensions": "site time1", "out_name": "hfss", "type": "real", @@ -364,7 +364,7 @@ "cell_methods": "area: point time: point", "cell_measures": "", "long_name": "Specific Humidity", - "comment": "", + "comment": "'specific' means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.", "dimensions": "alevel site time1", "out_name": "hus", "type": "real", @@ -400,7 +400,7 @@ "cell_methods": "area: point", "cell_measures": "", "long_name": "Latitude", - "comment": "", + "comment": "Latitude is positive northward; its units of degree_north (or equivalent) indicate this explicitly. In a latitude-longitude system defined with respect to a rotated North Pole, the standard name of grid_latitude should be used instead of latitude. Grid latitude is positive in the grid-northward direction, but its units should be plain degree.", "dimensions": "site", "out_name": "lat", "type": "real", @@ -418,7 +418,7 @@ "cell_methods": "area: point", "cell_measures": "", "long_name": "Longitude", - "comment": "", + "comment": "Longitude is positive eastward; its units of degree_east (or equivalent) indicate this explicitly. In a latitude-longitude system defined with respect to a rotated North Pole, the standard name of grid_longitude should be used instead of longitude. Grid longitude is positive in the grid-eastward direction, but its units should be plain degree.", "dimensions": "site", "out_name": "lon", "type": "real", @@ -634,7 +634,7 @@ "cell_methods": "area: point time: point", "cell_measures": "", "long_name": "Surface Downwelling Longwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'longwave' means longwave radiation. Downwelling radiation is radiation from above. It does not mean 'net downward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "site time1", "out_name": "rlds", "type": "real", @@ -706,7 +706,7 @@ "cell_methods": "area: point time: point", "cell_measures": "", "long_name": "Surface Upwelling Longwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'longwave' means longwave radiation. Upwelling radiation is radiation from below. It does not mean 'net upward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "site time1", "out_name": "rlus", "type": "real", @@ -886,7 +886,7 @@ "cell_methods": "area: point time: point", "cell_measures": "", "long_name": "Surface Upwelling Shortwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'shortwave' means shortwave radiation. Upwelling radiation is radiation from below. It does not mean 'net upward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "site time1", "out_name": "rsus", "type": "real", @@ -1336,7 +1336,7 @@ "cell_methods": "area: point time: point", "cell_measures": "", "long_name": "Eastward Wind", - "comment": "", + "comment": "'Eastward' indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "alevel site time1", "out_name": "ua", "type": "real", @@ -1372,7 +1372,7 @@ "cell_methods": "area: point time: point", "cell_measures": "", "long_name": "Northward Wind", - "comment": "", + "comment": "'Northward' indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "alevel site time1", "out_name": "va", "type": "real", @@ -1426,7 +1426,7 @@ "cell_methods": "area: point time: point", "cell_measures": "", "long_name": "Geopotential Height", - "comment": "", + "comment": "Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface.", "dimensions": "alevel site time1", "out_name": "zg", "type": "real", diff --git a/Tables/CMIP6_E1hr.json b/Tables/CMIP6_E1hr.json index e88c53b9..4d4f8dc4 100644 --- a/Tables/CMIP6_E1hr.json +++ b/Tables/CMIP6_E1hr.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table E1hr", "realm": "atmos", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -148,7 +148,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Eastward Wind", - "comment": "", + "comment": "'Eastward' indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude plev3 time1", "out_name": "ua", "type": "real", @@ -166,7 +166,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Eastward Wind", - "comment": "", + "comment": "'Eastward' indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude plev27 time1", "out_name": "ua", "type": "real", @@ -202,7 +202,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Northward Wind", - "comment": "", + "comment": "'Northward' indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude plev3 time1", "out_name": "va", "type": "real", @@ -220,7 +220,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Northward Wind", - "comment": "", + "comment": "'Northward' indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude plev27 time1", "out_name": "va", "type": "real", @@ -292,7 +292,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Geopotential Height", - "comment": "", + "comment": "Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface.", "dimensions": "longitude latitude plev27 time1", "out_name": "zg", "type": "real", diff --git a/Tables/CMIP6_E1hrClimMon.json b/Tables/CMIP6_E1hrClimMon.json index 9500d33b..561e9f68 100644 --- a/Tables/CMIP6_E1hrClimMon.json +++ b/Tables/CMIP6_E1hrClimMon.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table E1hrClimMon", "realm": "atmos", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", diff --git a/Tables/CMIP6_E3hr.json b/Tables/CMIP6_E3hr.json index 4e8c7ced..8ae3e2b7 100644 --- a/Tables/CMIP6_E3hr.json +++ b/Tables/CMIP6_E3hr.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table E3hr", "realm": "land", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -94,7 +94,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Rainfall Flux", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "prra", "type": "real", @@ -112,7 +112,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Convective Rainfall rate", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "prrc", "type": "real", @@ -308,7 +308,7 @@ "standard_name": "wind_speed", "units": "m s-1", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Near-Surface Wind Speed", "comment": "near-surface (usually, 10 meters) wind speed.", "dimensions": "longitude latitude time height10m", @@ -326,7 +326,7 @@ "standard_name": "eastward_wind", "units": "m s-1", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Eastward Near-Surface Wind", "comment": "Eastward component of the near-surface (usually, 10 meters) wind", "dimensions": "longitude latitude time height10m", @@ -344,7 +344,7 @@ "standard_name": "northward_wind", "units": "m s-1", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Northward Near-Surface Wind", "comment": "Northward component of the near surface wind", "dimensions": "longitude latitude time height10m", diff --git a/Tables/CMIP6_E3hrPt.json b/Tables/CMIP6_E3hrPt.json index 4b4b6974..721585e4 100644 --- a/Tables/CMIP6_E3hrPt.json +++ b/Tables/CMIP6_E3hrPt.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table E3hrPt", "realm": "atmos", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -40,7 +40,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Aerosol level extinction optical depth for each band", - "comment": "", + "comment": "The optical thickness is the integral along the path of radiation of a volume scattering/absorption/attenuation coefficient. The radiative flux is reduced by a factor exp(-optical_thickness) on traversing the path. A coordinate variable of radiation_wavelength or radiation_frequency can be specified to indicate that the optical thickness applies at specific wavelengths or frequencies. 'Absorption optical thickness' means that part of the atmosphere optical thickness that is caused by the absorption of incident radiation. 'Aerosol' means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. 'Ambient_aerosol' means that the aerosol is measured or modelled at the ambient state of pressure, temperature and relative humidity that exists in its immediate environment. 'Ambient aerosol particles' are aerosol particles that have taken up ambient water through hygroscopic growth.", "dimensions": "longitude latitude alevel spectband time1", "out_name": "aeroptbnd", "type": "real", @@ -58,7 +58,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Aerosol level single-scattering albedo for each band", - "comment": "", + "comment": "'Single scattering albedo' is the fraction of radiation in an incident light beam scattered by the particles of an aerosol reference volume for a given wavelength. It is the ratio of the scattering and the extinction coefficients of the aerosol particles in the reference volume. A coordinate variable with a standard name of radiation_wavelength or radiation_frequency should be included to specify either the wavelength or frequency. 'Aerosol' means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. 'Ambient_aerosol' means that the aerosol is measured or modelled at the ambient state of pressure, temperature and relative humidity that exists in its immediate environment. 'Ambient aerosol particles' are aerosol particles that have taken up ambient water through hygroscopic growth. The extent of hygroscopic growth depends on the relative humidity and the composition of the particles.", "dimensions": "longitude latitude alevel spectband time1", "out_name": "aerssabnd", "type": "real", @@ -148,7 +148,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "CH4 volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude alevel time1", "out_name": "ch4", "type": "real", @@ -200,7 +200,7 @@ "standard_name": "cloud_area_fraction_in_atmosphere_layer", "units": "%", "cell_methods": "area: mean time: point", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "CALIPSO High Level Cloud Fraction", "comment": "Percentage cloud cover in layer centred on 220hPa", "dimensions": "longitude latitude time1 p220", @@ -236,7 +236,7 @@ "standard_name": "cloud_area_fraction_in_atmosphere_layer", "units": "%", "cell_methods": "area: mean time: point", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "CALIPSO Percentage Low Level Cloud", "comment": "Percentage cloud cover in layer centred on 840hPa", "dimensions": "longitude latitude time1 p840", @@ -254,7 +254,7 @@ "standard_name": "cloud_area_fraction_in_atmosphere_layer", "units": "%", "cell_methods": "area: mean time: point", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "CALIPSO Mid Level Cloud Fraction", "comment": "Percentage cloud cover in layer centred on 560hPa", "dimensions": "longitude latitude time1 p560", @@ -310,7 +310,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "CO2 volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude alevel time1", "out_name": "co2", "type": "real", @@ -328,7 +328,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Specific Humidity", - "comment": "", + "comment": "'specific' means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.", "dimensions": "longitude latitude alevel time1", "out_name": "hus", "type": "real", @@ -346,7 +346,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Specific Humidity", - "comment": "", + "comment": "'specific' means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.", "dimensions": "longitude latitude plev7h time1", "out_name": "hus", "type": "real", @@ -364,8 +364,8 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "MODIS Optical Thickness-Particle Size joint distribution, ice", - "comment": "", - "dimensions": "longitude latitude plev7c effectRadIc tau time1", + "comment": "'Layer' means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. 'X_area_fraction' means the fraction of horizontal area occupied by X. 'X_area' means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called 'cloud amount' and 'cloud cover'.", + "dimensions": "longitude latitude effectRadIc tau time1", "out_name": "jpdftaureicemodis", "type": "real", "positive": "", @@ -382,8 +382,8 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "MODIS Optical Thickness-Particle Size joint distribution, liquid", - "comment": "", - "dimensions": "longitude latitude plev7c effectRadLi tau time1", + "comment": "'Layer' means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. 'X_area_fraction' means the fraction of horizontal area occupied by X. 'X_area' means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called 'cloud amount' and 'cloud cover'.", + "dimensions": "longitude latitude effectRadLi tau time1", "out_name": "jpdftaureliqmodis", "type": "real", "positive": "", @@ -400,7 +400,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "N2O volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. The chemical formula of nitrous oxide is N2O.", "dimensions": "longitude latitude alevel time1", "out_name": "n2o", "type": "real", @@ -418,7 +418,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Ozone volume mixing ratio", - "comment": "", + "comment": "Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude alevel time1", "out_name": "o3", "type": "real", @@ -773,7 +773,7 @@ "solbnd": { "frequency": "3hrPt", "modeling_realm": "atmos", - "standard_name": "solar_irradiance", + "standard_name": "toa_incoming_shortwave_flux", "units": "W m-2", "cell_methods": "time: point", "cell_measures": "area: areacella", @@ -832,7 +832,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Eastward Wind", - "comment": "", + "comment": "'Eastward' indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude plev7h time1", "out_name": "ua", "type": "real", @@ -850,7 +850,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Northward Wind", - "comment": "", + "comment": "'Northward' indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude plev7h time1", "out_name": "va", "type": "real", diff --git a/Tables/CMIP6_E6hrZ.json b/Tables/CMIP6_E6hrZ.json index 2caab197..ab8060b2 100644 --- a/Tables/CMIP6_E6hrZ.json +++ b/Tables/CMIP6_E6hrZ.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table E6hrZ", "realm": "atmos", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", diff --git a/Tables/CMIP6_Eday.json b/Tables/CMIP6_Eday.json index 08784065..ef3690f3 100644 --- a/Tables/CMIP6_Eday.json +++ b/Tables/CMIP6_Eday.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table Eday", "realm": "land", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -77,7 +77,7 @@ "cell_measures": "area: areacella", "long_name": "Aerosol optical depth at 550 nm due to stratospheric volcanic aerosols", "comment": "aerosol optical depth at 550 nm due to stratospheric volcanic aerosols", - "dimensions": "longitude latitude time", + "dimensions": "longitude latitude time lambda550nm", "out_name": "aod550volso4", "type": "real", "positive": "", @@ -94,7 +94,7 @@ "cell_methods": "area: mean where land time: mean", "cell_measures": "area: areacella", "long_name": "Aerodynamic resistance", - "comment": "", + "comment": "The 'aerodynamic_resistance' is the resistance to mixing through the boundary layer toward the surface by means of the dominant process, turbulent transport. Reference: Wesely, M. L., 1989, doi:10.1016/0004-6981(89)90153-4.", "dimensions": "longitude latitude time", "out_name": "ares", "type": "real", @@ -220,7 +220,7 @@ "cell_methods": "area: mean where land time: mean", "cell_measures": "area: areacella", "long_name": "Canopy covered area percentage", - "comment": "", + "comment": "'X_area_fraction' means the fraction of horizontal area occupied by X. 'X_area' means the horizontal area occupied by X within the grid cell. 'Vegetation' means any plants e.g. trees, shrubs, grass.", "dimensions": "longitude latitude time", "out_name": "cnc", "type": "real", @@ -238,7 +238,7 @@ "cell_methods": "area: mean where land time: mean", "cell_measures": "area: areacella", "long_name": "Total Canopy Water Storage", - "comment": "", + "comment": "'Amount' means mass per unit area. 'Water' means water in all phases, including frozen i.e. ice and snow. 'Canopy' means the plant or vegetation canopy. The canopy water is the water on the canopy.", "dimensions": "longitude latitude time", "out_name": "cw", "type": "real", @@ -544,7 +544,7 @@ "cell_methods": "area: mean where land time: mean", "cell_measures": "area: areacella", "long_name": "Downward Heat Flux at Land Surface", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Downward' indicates a vector component which is positive when directed downward (negative upward). The vertical heat flux in air is the sum of all heat fluxes i.e. radiative, latent and sensible. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "hfdsl", "type": "real", @@ -598,7 +598,7 @@ "cell_methods": "area: mean where land time: mean", "cell_measures": "area: areacella", "long_name": "Surface Upward Latent Heat Flux", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Upward' indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "hfls", "type": "real", @@ -670,7 +670,7 @@ "cell_methods": "area: mean where land time: mean", "cell_measures": "area: areacella", "long_name": "Surface Upward Sensible Heat Flux", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Upward' indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called 'turbulent' heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. Unless indicated in the cell_methods attribute, a quantity is assumed to apply to the whole area of each horizontal grid box. Previously, the qualifier where_type was used to specify that the quantity applies only to the part of the grid box of the named type. Names containing the where_type qualifier are deprecated and newly created data should use the cell_methods attribute to indicate the horizontal area to which the quantity applies.", "dimensions": "longitude latitude time", "out_name": "hfss", "type": "real", @@ -706,7 +706,7 @@ "cell_methods": "time: mean", "cell_measures": "area: areacella", "long_name": "Specific Humidity", - "comment": "", + "comment": "'specific' means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.", "dimensions": "longitude latitude plev19 time", "out_name": "hus", "type": "real", @@ -722,7 +722,7 @@ "standard_name": "specific_humidity", "units": "1", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Specific Humidity", "comment": "", "dimensions": "longitude latitude time p850", @@ -742,8 +742,8 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "MODIS Optical Thickness-Particle Size joint distribution, ice", - "comment": "", - "dimensions": "longitude latitude plev7c effectRadIc tau time", + "comment": "'Layer' means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. 'X_area_fraction' means the fraction of horizontal area occupied by X. 'X_area' means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called 'cloud amount' and 'cloud cover'.", + "dimensions": "longitude latitude effectRadIc tau time", "out_name": "jpdftaureicemodis", "type": "real", "positive": "", @@ -760,8 +760,8 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "MODIS Optical Thickness-Particle Size joint distribution, liquid", - "comment": "", - "dimensions": "longitude latitude plev7c effectRadLi tau time", + "comment": "'Layer' means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. 'X_area_fraction' means the fraction of horizontal area occupied by X. 'X_area' means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called 'cloud amount' and 'cloud cover'.", + "dimensions": "longitude latitude effectRadLi tau time", "out_name": "jpdftaureliqmodis", "type": "real", "positive": "", @@ -778,7 +778,7 @@ "cell_methods": "area: mean where land time: mean", "cell_measures": "area: areacella", "long_name": "Leaf Area Index", - "comment": "", + "comment": "'X_area' means the horizontal area occupied by X within the grid cell.", "dimensions": "longitude latitude time", "out_name": "lai", "type": "real", @@ -973,8 +973,8 @@ "modeling_realm": "ocean", "standard_name": "ocean_mixed_layer_thickness_defined_by_sigma_t", "units": "m", - "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_methods": "area: mean where sea time: mean", + "cell_measures": "area: areacello", "long_name": "Ocean Mixed Layer Thickness Defined by Sigma T", "comment": "Sigma T is potential density referenced to ocean surface.", "dimensions": "longitude latitude time", @@ -1030,7 +1030,7 @@ "cell_methods": "area: mean where land time: mean", "cell_measures": "area: areacella", "long_name": "Subsurface runoff", - "comment": "", + "comment": "Runoff is the liquid water which drains from land. If not specified, 'runoff' refers to the sum of surface runoff and subsurface drainage. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "mrrob", "type": "real", @@ -1061,7 +1061,7 @@ "mrsfl": { "frequency": "day", "modeling_realm": "land", - "standard_name": "frozen_moisture_content_of_soil_layer", + "standard_name": "frozen_water_content_of_soil_layer", "units": "kg m-2", "cell_methods": "area: mean where land time: mean", "cell_measures": "area: areacella", @@ -1079,7 +1079,7 @@ "mrsll": { "frequency": "day", "modeling_realm": "land", - "standard_name": "liquid_moisture_content_of_soil_layer", + "standard_name": "liquid_water_content_of_soil_layer", "units": "kg m-2", "cell_methods": "area: mean where land time: mean", "cell_measures": "area: areacella", @@ -1246,7 +1246,7 @@ "cell_methods": "area: mean time: mean within hours time: maximum over hours", "cell_measures": "area: areacella", "long_name": "Maximum Hourly Precipitation Rate", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "prhmax", "type": "real", @@ -1264,7 +1264,7 @@ "cell_methods": "area: mean where land time: mean", "cell_measures": "area: areacella", "long_name": "Rainfall Flux over Land", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "prra", "type": "real", @@ -1282,7 +1282,7 @@ "cell_methods": "area: mean where land time: mean", "cell_measures": "area: areacella", "long_name": "Convective Rainfall rate", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "prrc", "type": "real", @@ -1484,7 +1484,7 @@ "dimensions": "longitude latitude time", "out_name": "rls", "type": "real", - "positive": "up", + "positive": "down", "valid_min": "", "valid_max": "", "ok_min_mean_abs": "", @@ -1678,7 +1678,7 @@ "cell_methods": "area: mean where land time: mean", "cell_measures": "area: areacella", "long_name": "Re-freezing of water in the snow", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. The surface called 'surface' means the lower boundary of the atmosphere. 'Surface snow and ice refreezing flux' means the mass flux of surface meltwater which refreezes within the snow or firn.", "dimensions": "longitude latitude time", "out_name": "snrefr", "type": "real", @@ -1747,8 +1747,8 @@ "modeling_realm": "ocean", "standard_name": "depth_of_isosurface_of_sea_water_potential_temperature", "units": "m", - "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_methods": "area: mean where sea time: mean", + "cell_measures": "area: areacello", "long_name": "20C isotherm depth", "comment": "", "dimensions": "longitude latitude time", @@ -1784,7 +1784,7 @@ "standard_name": "air_temperature", "units": "K", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Air Temperature", "comment": "Temperature on the 500 hPa surface", "dimensions": "longitude latitude time p500", @@ -1802,7 +1802,7 @@ "standard_name": "air_temperature", "units": "K", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Air Temperature", "comment": "Air temperature at 850hPa", "dimensions": "longitude latitude time p850", @@ -2102,17 +2102,17 @@ "ok_min_mean_abs": "", "ok_max_mean_abs": "" }, - "tsnl": { + "tsn": { "frequency": "day", - "modeling_realm": "land", - "standard_name": "snow_temperature", + "modeling_realm": "landIce land", + "standard_name": "temperature_in_surface_snow", "units": "K", - "cell_methods": "area: mean where land time: mean", + "cell_methods": "area: mean where land time: mean (with samples weighted by snow mass)", "cell_measures": "area: areacella", - "long_name": "Temperature profile in the snow", - "comment": "Temperature in the snow pack present in the grid-cell. 3D variable for multi-layer snow schemes.", - "dimensions": "longitude latitude snowdepth time", - "out_name": "tsnl", + "long_name": "Snow Internal Temperature", + "comment": "This temperature is averaged over all the snow in the grid cell that rests on land or land ice. When computing the time-mean here, the time samples, weighted by the mass of snow on the land portion of the grid cell, are accumulated and then divided by the sum of the weights. Reported as missing in regions free of snow on land.", + "dimensions": "longitude latitude time", + "out_name": "tsn", "type": "real", "positive": "", "valid_min": "", @@ -2146,7 +2146,7 @@ "cell_methods": "time: mean", "cell_measures": "area: areacella", "long_name": "Eastward Wind", - "comment": "", + "comment": "'Eastward' indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude plev19 time", "out_name": "ua", "type": "real", @@ -2164,7 +2164,7 @@ "cell_methods": "time: mean", "cell_measures": "area: areacella", "long_name": "Northward Wind", - "comment": "", + "comment": "'Northward' indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude plev19 time", "out_name": "va", "type": "real", @@ -2218,7 +2218,7 @@ "cell_methods": "time: mean", "cell_measures": "area: areacella", "long_name": "Geopotential Height", - "comment": "", + "comment": "Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface.", "dimensions": "longitude latitude plev19 time", "out_name": "zg", "type": "real", @@ -2236,7 +2236,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Height of Boundary Layer", - "comment": "", + "comment": "The atmosphere boundary layer thickness is the 'depth' or 'height' of the (atmosphere) planetary boundary layer.", "dimensions": "longitude latitude time", "out_name": "zmla", "type": "real", diff --git a/Tables/CMIP6_EdayZ.json b/Tables/CMIP6_EdayZ.json index 8e63a737..ea7076cc 100644 --- a/Tables/CMIP6_EdayZ.json +++ b/Tables/CMIP6_EdayZ.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table EdayZ", "realm": "atmos", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -58,7 +58,7 @@ "cell_methods": "longitude: mean time: mean", "cell_measures": "", "long_name": "Specific Humidity", - "comment": "", + "comment": "'specific' means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.", "dimensions": "latitude plev19 time", "out_name": "hus", "type": "real", @@ -112,7 +112,7 @@ "cell_methods": "longitude: mean time: mean", "cell_measures": "", "long_name": "Eastward Wind", - "comment": "", + "comment": "'Eastward' indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "latitude plev39 time", "out_name": "ua", "type": "real", @@ -220,7 +220,7 @@ "cell_methods": "longitude: mean time: mean", "cell_measures": "", "long_name": "Northward Wind", - "comment": "", + "comment": "'Northward' indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "latitude plev19 time", "out_name": "va", "type": "real", @@ -274,7 +274,7 @@ "cell_methods": "longitude: mean time: mean", "cell_measures": "", "long_name": "Geopotential Height", - "comment": "", + "comment": "Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface.", "dimensions": "latitude plev19 time", "out_name": "zg", "type": "real", diff --git a/Tables/CMIP6_Efx.json b/Tables/CMIP6_Efx.json index fe979c6b..1bb75555 100644 --- a/Tables/CMIP6_Efx.json +++ b/Tables/CMIP6_Efx.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table Efx", "realm": "land", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -22,7 +22,7 @@ "cell_methods": "area: mean where land", "cell_measures": "area: areacella", "long_name": "Clay Fraction", - "comment": "", + "comment": "'Volume fraction' is used in the construction volume_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude sdepth", "out_name": "clayfrac", "type": "real", @@ -233,12 +233,12 @@ "siltfrac": { "frequency": "fx", "modeling_realm": "atmos", - "standard_name": "missing", + "standard_name": "volume_fraction_of_silt_in_soil", "units": "1", "cell_methods": "area: mean where land", "cell_measures": "area: areacella", "long_name": "Silt Fraction", - "comment": "", + "comment": "'Volume fraction' is used in the construction volume_fraction_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude sdepth", "out_name": "siltfrac", "type": "real", @@ -274,7 +274,7 @@ "cell_methods": "area: mean where land", "cell_measures": "area: areacella", "long_name": "canopy height", - "comment": "", + "comment": "Height is the vertical distance above the surface. 'Canopy' means the plant or vegetation canopy.", "dimensions": "longitude latitude", "out_name": "vegHeight", "type": "real", diff --git a/Tables/CMIP6_Emon.json b/Tables/CMIP6_Emon.json index 0d58deb3..674b3ee2 100644 --- a/Tables/CMIP6_Emon.json +++ b/Tables/CMIP6_Emon.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table Emon", "realm": "atmos", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -382,7 +382,7 @@ "cell_methods": "area: time: mean where natural_grasses (comment: mask=grassFrac)", "cell_measures": "area: areacella", "long_name": "Carbon mass in litter on grass tiles", - "comment": "", + "comment": "'Content' indicates a quantity per unit area. 'Litter carbon' is dead inorganic material in or above the soil quantified as the mass of carbon which it contains.", "dimensions": "longitude latitude time", "out_name": "cLitterGrass", "type": "real", @@ -400,7 +400,7 @@ "cell_methods": "area: time: mean where shrubs (comment: mask=shrubFrac)", "cell_measures": "area: areacella", "long_name": "Carbon mass in litter on shrub tiles", - "comment": "", + "comment": "'Content' indicates a quantity per unit area. 'Litter carbon' is dead inorganic material in or above the soil quantified as the mass of carbon which it contains.", "dimensions": "longitude latitude time", "out_name": "cLitterShrub", "type": "real", @@ -454,7 +454,7 @@ "cell_methods": "area: time: mean where trees (comment: mask=treeFrac)", "cell_measures": "area: areacella", "long_name": "Carbon mass in litter on tree tiles", - "comment": "", + "comment": "'Content' indicates a quantity per unit area. 'Litter carbon' is dead inorganic material in or above the soil quantified as the mass of carbon which it contains.", "dimensions": "longitude latitude time", "out_name": "cLitterTree", "type": "real", @@ -525,9 +525,9 @@ "units": "kg m-2", "cell_methods": "area: mean where land time: mean", "cell_measures": "area: areacella", - "long_name": "Carbon mass in soil pool above 1m depth", + "long_name": "Carbon Mass in Soil Pool above 1m Depth", "comment": "Report missing data over ocean grid cells. For fractional land report value averaged over the land fraction.", - "dimensions": "longitude latitude time", + "dimensions": "longitude latitude time sdepth10", "out_name": "cSoilAbove1m", "type": "real", "positive": "", @@ -536,24 +536,6 @@ "ok_min_mean_abs": "", "ok_max_mean_abs": "" }, - "cSoilBelow1m": { - "frequency": "mon", - "modeling_realm": "land", - "standard_name": "soil_carbon_content", - "units": "kg m-2", - "cell_methods": "area: mean where land time: mean", - "cell_measures": "area: areacella", - "long_name": "Carbon Mass in Soil Pool below 1m Depth", - "comment": "", - "dimensions": "longitude latitude time", - "out_name": "cSoilBelow1m", - "type": "real", - "positive": "", - "valid_min": "", - "valid_max": "", - "ok_min_mean_abs": "", - "ok_max_mean_abs": "" - }, "cSoilGrass": { "frequency": "mon", "modeling_realm": "land", @@ -562,7 +544,7 @@ "cell_methods": "area: time: mean where natural_grasses (comment: mask=grassFrac)", "cell_measures": "area: areacella", "long_name": "Carbon mass in soil on grass tiles", - "comment": "", + "comment": "'Content' indicates a quantity per unit area. The 'soil content' of a quantity refers to the vertical integral from the surface down to the bottom of the soil model. For the content between specified levels in the soil, standard names including content_of_soil_layer are used.", "dimensions": "longitude latitude time", "out_name": "cSoilGrass", "type": "real", @@ -591,15 +573,15 @@ "ok_max_mean_abs": "" }, "cSoilPools": { - "frequency": "monPt", + "frequency": "mon", "modeling_realm": "land", "standard_name": "soil_carbon_content_by_pool", "units": "kg m-2", - "cell_methods": "area: mean where land time: point", + "cell_methods": "area: mean where land time: mean", "cell_measures": "area: areacella", "long_name": "Carbon mass in each model soil pool (summed over vertical levels)", "comment": "for models with multiple soil carbon pools, report each pool here. If models also have vertical discretaisation these should be aggregated", - "dimensions": "longitude latitude soilpools time1", + "dimensions": "longitude latitude soilpools time", "out_name": "cSoilPools", "type": "real", "positive": "", @@ -616,7 +598,7 @@ "cell_methods": "area: time: mean where shrubs (comment: mask=shrubFrac)", "cell_measures": "area: areacella", "long_name": "Carbon mass in soil on shrub tiles", - "comment": "", + "comment": "'Content' indicates a quantity per unit area. The 'soil content' of a quantity refers to the vertical integral from the surface down to the bottom of the soil model. For the content between specified levels in the soil, standard names including content_of_soil_layer are used.", "dimensions": "longitude latitude time", "out_name": "cSoilShrub", "type": "real", @@ -634,7 +616,7 @@ "cell_methods": "area: time: mean where trees (comment: mask=treeFrac)", "cell_measures": "area: areacella", "long_name": "Carbon mass in soil on tree tiles", - "comment": "", + "comment": "'Content' indicates a quantity per unit area. The 'soil content' of a quantity refers to the vertical integral from the surface down to the bottom of the soil model. For the content between specified levels in the soil, standard names including content_of_soil_layer are used.", "dimensions": "longitude latitude time", "out_name": "cSoilTree", "type": "real", @@ -688,7 +670,7 @@ "cell_methods": "area: time: mean where natural_grasses (comment: mask=grassFrac)", "cell_measures": "area: areacella", "long_name": "Carbon mass in vegetation on grass tiles", - "comment": "", + "comment": "'Content' indicates a quantity per unit area. 'Vegetation' means any plants e.g. trees, shrubs, grass.", "dimensions": "longitude latitude time", "out_name": "cVegGrass", "type": "real", @@ -706,7 +688,7 @@ "cell_methods": "area: time: mean where shrubs (comment: mask=shrubFrac)", "cell_measures": "area: areacella", "long_name": "Carbon mass in vegetation on shrub tiles", - "comment": "", + "comment": "'Content' indicates a quantity per unit area. 'Vegetation' means any plants e.g. trees, shrubs, grass.", "dimensions": "longitude latitude time", "out_name": "cVegShrub", "type": "real", @@ -724,7 +706,7 @@ "cell_methods": "area: time: mean where trees (comment: mask=treeFrac)", "cell_measures": "area: areacella", "long_name": "Carbon mass in vegetation on tree tiles", - "comment": "", + "comment": "'Content' indicates a quantity per unit area. 'Vegetation' means any plants e.g. trees, shrubs, grass.", "dimensions": "longitude latitude time", "out_name": "cVegTree", "type": "real", @@ -796,7 +778,7 @@ "cell_methods": "time: mean", "cell_measures": "area: areacella", "long_name": "CALIPSO ice cloud Fraction", - "comment": "", + "comment": "'Layer' means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be 'model_level_number', but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. 'X_area_fraction' means the fraction of horizontal area occupied by X. Cloud area fraction is also called 'cloud amount' and 'cloud cover'.", "dimensions": "longitude latitude alt40 time", "out_name": "clcalipsoice", "type": "real", @@ -922,7 +904,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "MODIS Ice Cloud Area Percentage", - "comment": "", + "comment": "'X_area_fraction' means the fraction of horizontal area occupied by X. Cloud area fraction is also called 'cloud amount' and 'cloud cover'. The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer.", "dimensions": "longitude latitude time", "out_name": "climodis", "type": "real", @@ -958,7 +940,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "MODIS Total Cloud Cover Percentage", - "comment": "", + "comment": "'X_area_fraction' means the fraction of horizontal area occupied by X. 'X_area' means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called 'cloud amount' and 'cloud cover'. The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer.", "dimensions": "longitude latitude time", "out_name": "cltmodis", "type": "real", @@ -976,7 +958,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "MODIS Liquid Cloud Fraction", - "comment": "", + "comment": "'X_area_fraction' means the fraction of horizontal area occupied by X. Cloud area fraction is also called 'cloud amount' and 'cloud cover'. The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. The chemical formula for water is H2O.", "dimensions": "longitude latitude time", "out_name": "clwmodis", "type": "real", @@ -1205,12 +1187,12 @@ "dissi14c": { "frequency": "mon", "modeling_realm": "ocnBgChem", - "standard_name": "mole_concentration_of_dissolved_inorganic_c14_in_sea_water", + "standard_name": "mole_concentration_of_dissolved_inorganic_carbon14_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Concentration of DI14C", - "comment": "", + "comment": "Mole concentration means number of moles per unit volume, also called 'molarity', and is used in the construction 'mole_concentration_of_X_in_Y', where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. 'Dissolved inorganic carbon' describes a family of chemical species in solution, including carbon dioxide, carbonic acid and the carbonate and bicarbonate anions. 'Dissolved inorganic carbon' is the term used in standard names for all species belonging to the family that are represented within a given model. The list of individual species that are included in a quantity having a group chemical standard name can vary between models. Where possible, the data variable should be accompanied by a complete description of the species represented, for example, by using a comment attribute.", "dimensions": "longitude latitude olevel time", "out_name": "dissi14c", "type": "real", @@ -1229,7 +1211,7 @@ "cell_measures": "area: areacella", "long_name": "Aerosol extinction coefficient", "comment": "Aerosol Extinction at 550nm", - "dimensions": "longitude latitude alevel time", + "dimensions": "longitude latitude alevel time1 lambda550nm", "out_name": "ec550aer", "type": "real", "positive": "", @@ -1300,7 +1282,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Sinking Particulate Iron Flux", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. 'Sinking' is the gravitational settling of particulate matter suspended in a liquid. A sinking flux is positive downwards and is calculated relative to the movement of the surrounding fluid.", "dimensions": "longitude latitude olevel time", "out_name": "expfe", "type": "real", @@ -1318,7 +1300,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Sinking Particulate Organic Nitrogen Flux", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. 'Sinking' is the gravitational settling of particulate matter suspended in a liquid. A sinking flux is positive downwards and is calculated relative to the movement of the surrounding fluid.", "dimensions": "longitude latitude olevel time", "out_name": "expn", "type": "real", @@ -1336,7 +1318,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Sinking Particulate Organic Phosphorus Flux", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. 'Sinking' is the gravitational settling of particulate matter suspended in a liquid. A sinking flux is positive downwards and is calculated relative to the movement of the surrounding fluid.", "dimensions": "longitude latitude olevel time", "out_name": "expp", "type": "real", @@ -1354,7 +1336,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Sinking Particulate Silica Flux", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. 'Sinking' is the gravitational settling of particulate matter suspended in a liquid. A sinking flux is positive downwards and is calculated relative to the movement of the surrounding fluid.", "dimensions": "longitude latitude olevel time", "out_name": "expsi", "type": "real", @@ -1371,7 +1353,7 @@ "units": "kg m-2 s-1", "cell_methods": "area: mean where land time: mean", "cell_measures": "area: areacella", - "long_name": "carbon mass flux into atmosphere due to any human activity", + "long_name": "Carbon Mass Flux from Vegetation, Litter or Soil Pools into the Atmosphere due to Any Human Activity", "comment": "will require some careful definition to make sure we capture everything - any human activity that releases carbon to the atmosphere instead of into product pool goes here. E.g. Deforestation fire, harvest assumed to decompose straight away, grazing...", "dimensions": "longitude latitude time", "out_name": "fAnthDisturb", @@ -2056,7 +2038,7 @@ "cell_methods": "area: time: mean where landuse", "cell_measures": "area: areacella", "long_name": "Anthropogenic heat flux generated from non-renewable human primary energy consumption, including energy use by vehicles, commercial and residential buildings, industry, and power plants. Primary energy refers to energy in natural resources, fossil and nonfossil, before conversion into other forms, such as electricity.", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Upward' indicates a vector component which is positive when directed upward (negative downward). The vertical heat flux in air is the sum of all heat fluxes i.e. radiative, latent and sensible. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. The specification of a physical process by the phrase 'due_to_' process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. 'Anthropogenic' means influenced, caused, or created by human activity. The heat flux due to anthropogenic energy consumption results from non-renewable human primary energy consumption, including energy use by vehicles, commercial and residential buildings, industry, and power plants. Primary energy refers to energy in natural resources, fossil and non-fossil, before conversion into other forms, such as electricity.", "dimensions": "longitude latitude landUse time", "out_name": "fahLut", "type": "real", @@ -2066,24 +2048,6 @@ "ok_min_mean_abs": "", "ok_max_mean_abs": "" }, - "fbddtalk": { - "frequency": "mon", - "modeling_realm": "ocnBgChem", - "standard_name": "integral_wrt_depth_of_tendency_of_sea_water_alkalinity_expressed_as_mole_equivalent_due_to_biological_processes", - "units": "mol m-2 s-1", - "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", - "long_name": "Rate of Change of Biological Alkalinity due to Biological Activity", - "comment": "vertical integral of net biological terms in time rate of change of alkalinity", - "dimensions": "longitude latitude olevel time", - "out_name": "fbddtalk", - "type": "real", - "positive": "", - "valid_min": "", - "valid_max": "", - "ok_min_mean_abs": "", - "ok_max_mean_abs": "" - }, "fbddtdic": { "frequency": "mon", "modeling_realm": "ocnBgChem", @@ -2102,24 +2066,6 @@ "ok_min_mean_abs": "", "ok_max_mean_abs": "" }, - "fbddtdife": { - "frequency": "mon", - "modeling_realm": "ocnBgChem", - "standard_name": "tendency_of_ocean_mole_content_of_dissolved_inorganic_iron_due_to_biological_processes", - "units": "mol m-2 s-1", - "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", - "long_name": "Rate of Change of Dissolved Inorganic Iron due to Biological Activity", - "comment": "vertical integral of net biological terms in time rate of change of dissolved inorganic iron", - "dimensions": "longitude latitude olevel time", - "out_name": "fbddtdife", - "type": "real", - "positive": "", - "valid_min": "", - "valid_max": "", - "ok_min_mean_abs": "", - "ok_max_mean_abs": "" - }, "fbddtdin": { "frequency": "mon", "modeling_realm": "ocnBgChem", @@ -2200,7 +2146,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Rate of Change of Net Dissolved Inorganic Carbon", - "comment": "", + "comment": "'Content' indicates a quantity per unit area. 'tendency_of_X' means derivative of X with respect to time. 'Dissolved inorganic carbon' describes a family of chemical species in solution, including carbon dioxide, carbonic acid and the carbonate and bicarbonate anions. 'Dissolved inorganic carbon' isthe term used in standard names for all species belonging to the family that are represented within a given model. The list of individual species that are included in a quantity having a group chemical standard name can vary between models. Where possible, the data variable should be accompanied by a complete description of the species represented, for example, by using a comment attribute.", "dimensions": "longitude latitude olevel time", "out_name": "fddtdic", "type": "real", @@ -2290,7 +2236,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Total air-sea flux of 14CO2", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Downward' indicates a vector component which is positive when directed downward (negative upward). In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. In ocean biogeochemistry models, an 'abiotic analogue' is used to simulate the effect on a modelled variable when biological effects on ocean carbon concentration and alkalinity are ignored. The phrase 'expressed_as' is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. Carbon14 is a radioactive isotope of carbon having six protons and eight neutrons, used in radiocarbon dating.", "dimensions": "longitude latitude time", "out_name": "fg14co2", "type": "real", @@ -2434,7 +2380,7 @@ "cell_methods": "area: time: mean where landuse", "cell_measures": "area: areacella", "long_name": "gross primary productivity on land use tile", - "comment": "", + "comment": "'Production of carbon' means the production of biomass expressed as the mass of carbon which it contains. Gross primary production is the rate of synthesis of biomass from inorganic precursors by autotrophs ('producers'), for example, photosynthesis in plants or phytoplankton. The producers also respire some of this biomass and the difference is 'net_primary_production'. 'Productivity' means production per unit area. The phrase 'expressed_as' is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A.", "dimensions": "longitude latitude landUse time", "out_name": "gppLut", "type": "real", @@ -2596,7 +2542,7 @@ "cell_methods": "area: time: mean where landuse", "cell_measures": "area: areacella", "long_name": "latent heat flux on land use tile", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Upward' indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude landUse time", "out_name": "hflsLut", "type": "real", @@ -2614,7 +2560,7 @@ "cell_methods": "area: time: mean where landuse", "cell_measures": "area: areacella", "long_name": "sensible heat flux on land use tile", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Upward' indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called 'turbulent' heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. Unless indicated in the cell_methods attribute, a quantity is assumed to apply to the whole area of each horizontal grid box. Previously, the qualifier where_type was used to specify that the quantity applies only to the part of the grid box of the named type. Names containing the where_type qualifier are deprecated and newly created data should use the cell_methods attribute to indicate the horizontal area to which the quantity applies.", "dimensions": "longitude latitude landUse time", "out_name": "hfssLut", "type": "real", @@ -2650,7 +2596,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Specific Humidity", - "comment": "", + "comment": "'specific' means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.", "dimensions": "longitude latitude plev7h time", "out_name": "hus", "type": "real", @@ -2668,7 +2614,7 @@ "cell_methods": "time: mean", "cell_measures": "area: areacella", "long_name": "Specific Humidity", - "comment": "", + "comment": "'specific' means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.", "dimensions": "longitude latitude plev27 time", "out_name": "hus", "type": "real", @@ -2794,8 +2740,8 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "MODIS Optical Thickness-Particle Size joint distribution, ice", - "comment": "", - "dimensions": "longitude latitude plev7c effectRadIc tau time", + "comment": "'Layer' means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. 'X_area_fraction' means the fraction of horizontal area occupied by X. 'X_area' means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called 'cloud amount' and 'cloud cover'.", + "dimensions": "longitude latitude effectRadIc tau time", "out_name": "jpdftaureicemodis", "type": "real", "positive": "", @@ -2812,8 +2758,8 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "MODIS Optical Thickness-Particle Size joint distribution, liquid", - "comment": "", - "dimensions": "longitude latitude plev7c effectRadLi tau time", + "comment": "'Layer' means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. 'X_area_fraction' means the fraction of horizontal area occupied by X. 'X_area' means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called 'cloud amount' and 'cloud cover'.", + "dimensions": "longitude latitude effectRadLi tau time", "out_name": "jpdftaureliqmodis", "type": "real", "positive": "", @@ -3010,7 +2956,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "NO3 aerosol mass mixing ratio", - "comment": "", + "comment": "Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of X to the mass of Y (including X). 'Mass_fraction_of_nitrate' means that the mass is expressed as mass of NO3. 'Aerosol' means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol particles take up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the particles. 'Dry aerosol particles' means aerosol particles without any water uptake.", "dimensions": "longitude latitude time", "out_name": "mmrno3", "type": "real", @@ -3059,7 +3005,7 @@ "mrsfl": { "frequency": "mon", "modeling_realm": "land", - "standard_name": "frozen_moisture_content_of_soil_layer", + "standard_name": "frozen_water_content_of_soil_layer", "units": "kg m-2", "cell_methods": "area: mean where land time: mean", "cell_measures": "area: areacella", @@ -3077,7 +3023,7 @@ "mrsll": { "frequency": "mon", "modeling_realm": "land", - "standard_name": "liquid_moisture_content_of_soil_layer", + "standard_name": "liquid_water_content_of_soil_layer", "units": "kg m-2", "cell_methods": "area: mean where land time: mean", "cell_measures": "area: areacella", @@ -3100,7 +3046,7 @@ "cell_methods": "area: time: mean where landuse", "cell_measures": "area: areacella", "long_name": "Total soil moisture", - "comment": "", + "comment": "alias::soil_moisture_content", "dimensions": "longitude latitude landUse time", "out_name": "mrsoLut", "type": "real", @@ -3550,7 +3496,7 @@ "cell_methods": "area: time: mean where landuse", "cell_measures": "area: areacella", "long_name": "net primary productivity on land use tile", - "comment": "", + "comment": "'Production of carbon' means the production of biomass expressed as the mass of carbon which it contains. Net primary production is the excess of gross primary production (rate of synthesis of biomass from inorganic precursors) by autotrophs ('producers'), for example, photosynthesis in plants or phytoplankton, over the rate at which the autotrophs themselves respire some of this biomass. 'Productivity' means production per unit area. The phrase 'expressed_as' is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A.", "dimensions": "longitude latitude landUse time", "out_name": "nppLut", "type": "real", @@ -3748,7 +3694,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "tendency of sea water conservative temperature expressed as heat content due to residual mean (sum of Eulerian + parameterized) advection", - "comment": "", + "comment": "'tendency_of_X' means derivative of X with respect to time. 'Content' indicates a quantity per unit area. The phrase 'expressed_as_heat_content' means that this quantity is calculated as the specific heat capacity times density of sea water multiplied by the conservative temperature of the sea water in the grid cell. Conservative Temperature is defined as part of the Thermodynamic Equation of Seawater 2010 (TEOS-10) which was adopted in 2010 by the International Oceanographic Commission (IOC). Conservative Temperature is specific potential enthalpy (which has the standard name sea_water_specific_potential_enthalpy) divided by a fixed value of the specific heat capacity of sea water, namely cp_0 = 3991.86795711963 J kg-1 K-1. Conservative Temperature is a more accurate measure of the 'heat content' of sea water, by a factor of one hundred, than is potential temperature. Because of this, it can be regarded as being proportional to the heat content of sea water per unit mass. Reference: www.teos-10.", "dimensions": "longitude latitude olevel time", "out_name": "ocontemprmadvect", "type": "real", @@ -3803,7 +3749,7 @@ "cell_measures": "area: areacella", "long_name": "Stratospheric Optical depth at 550 nm (all aerosols) 2D-field (here we limit the computation of OD to the stratosphere only)", "comment": "From tropopause to stratopause as defined by the model", - "dimensions": "longitude latitude time", + "dimensions": "longitude latitude time lambda550nm", "out_name": "od550aerso", "type": "real", "positive": "", @@ -3821,7 +3767,7 @@ "cell_measures": "area: areacella", "long_name": "Stratospheric Optical depth at 550 nm (sulphate only) 2D-field (here we limit the computation of OD to the stratosphere only)", "comment": "Balkanski - LSCE", - "dimensions": "longitude latitude time", + "dimensions": "longitude latitude time lambda550nm", "out_name": "od550so4so", "type": "real", "positive": "", @@ -3874,7 +3820,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "integral wrt depth of product of sea water density and potential temperature", - "comment": "", + "comment": "The phrase 'integral_wrt_X_of_Y' means int Y dX. The data variable should have an axis for X specifying the limits of the integral as bounds. The phrase 'wrt' means 'with respect to'. The phrase 'product_of_X_and_Y' means X*Y. Depth is the vertical distance below the surface. Sea water density is the in-situ density (not the potential density). For Boussinesq models, density is the constant Boussinesq reference density, a quantity which has the standard name reference_sea_water_density_for_boussinesq_approximation. Potential temperature is the temperature a parcel of air or sea water would have if moved adiabatically to sea level pressure.", "dimensions": "longitude latitude time", "out_name": "opottempmint", "type": "real", @@ -3946,7 +3892,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "tendency of sea water potential temperature expressed as heat content due to residual mean advection", - "comment": "", + "comment": "The phrase 'tendency_of_X' means derivative of X with respect to time. 'Content' indicates a quantity per unit area. The phrase 'expressed_as_heat_content' means that this quantity is calculated as the specific heat capacity times density of sea water multiplied by the potential temperature of the sea water in the grid cell. Potential temperature is the temperature a parcel of air or sea water would have if moved adiabatically to sea level pressure. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. The phrase 'residual_mean_advection' refers to the sum of the model's resolved advective transport plus any parameterized advective transport. Parameterized advective transport includes processes such as parameterized mesoscale and submesoscale transport, as well as any other advectively parameterized transport.", "dimensions": "longitude latitude olevel time", "out_name": "opottemprmadvect", "type": "real", @@ -4072,7 +4018,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "tendency of sea water salinity expressed as salt content due to residual mean advection", - "comment": "", + "comment": "The phrase 'tendency_of_X' means derivative of X with respect to time. 'Content' indicates a quantity per unit area. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. The phrase 'residual_mean_advection' refers to the sum of the model's resolved advective transport plus any parameterized advective transport. Parameterized advective transport includes processes such as parameterized mesoscale and submesoscale transport, as well as any other advectively parameterized transport. When the parameterized advective transport is represented in the model as a skew-diffusion rather than an advection, then the parameterized skew diffusion should be included in this diagnostic, since the convergence of skew-fluxes are identical (in the continuous formulation) to the convergence of advective fluxes.", "dimensions": "longitude latitude olevel time", "out_name": "osaltrmadvect", "type": "real", @@ -4324,7 +4270,7 @@ "cell_methods": "area: mean time: mean within hours time: maximum over hours", "cell_measures": "area: areacella", "long_name": "Maximum Hourly Precipitation Rate", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "prhmax", "type": "real", @@ -4414,7 +4360,7 @@ "cell_methods": "area: time: mean where landuse", "cell_measures": "area: areacella", "long_name": "plant respiration on land use tile", - "comment": "", + "comment": "'Respiration carbon' refers to the rate at which biomass is respired expressed as the mass of carbon which it contains. Plant respiration is the sum of respiration by parts of plants both above and below the soil. Plants which photosynthesise are autotrophs i.e. 'producers' of the biomass which they respire from inorganic precursors using sunlight for energy. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude landUse time", "out_name": "raLut", "type": "real", @@ -4684,7 +4630,7 @@ "cell_methods": "area: time: mean where landuse", "cell_measures": "area: areacella", "long_name": "soil heterotrophic respiration on land use tile", - "comment": "", + "comment": "'Respiration carbon' refers to the rate at which biomass is respired expressed as the mass of carbon which it contains. Heterotrophic respiration is respiration by heterotrophs ('consumers'), which are organisms (including animals and decomposers) that consume other organisms or dead organic material, rather than synthesising organic material from inorganic precursors using energy from the environment (especially sunlight) as autotrophs ('producers') do. Heterotrophic respiration goes on both above and within the soil. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude landUse time", "out_name": "rhLut", "type": "real", @@ -4796,7 +4742,7 @@ "dimensions": "longitude latitude time", "out_name": "rls", "type": "real", - "positive": "up", + "positive": "down", "valid_min": "", "valid_max": "", "ok_min_mean_abs": "", @@ -4810,7 +4756,7 @@ "cell_methods": "area: time: mean where landuse", "cell_measures": "area: areacella", "long_name": "Surface Upwelling Longwave on Land Use Tile", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'longwave' means longwave radiation. Upwelling radiation is radiation from below. It does not mean 'net upward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude landUse time", "out_name": "rlusLut", "type": "real", @@ -4828,7 +4774,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "net rate of absorption of shortwave energy in ocean layer", - "comment": "", + "comment": "'shortwave' means shortwave radiation. 'Layer' means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. Net absorbed radiation is the difference between absorbed and emitted radiation.", "dimensions": "longitude latitude olevel time", "out_name": "rsdoabsorb", "type": "real", @@ -4900,7 +4846,7 @@ "cell_methods": "area: time: mean where landuse", "cell_measures": "area: areacella", "long_name": "Surface Upwelling Shortwave on Land Use Tile", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'shortwave' means shortwave radiation. Upwelling radiation is radiation from below. It does not mean 'net upward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude landUse time", "out_name": "rsusLut", "type": "real", @@ -4988,7 +4934,7 @@ "standard_name": "wind_speed", "units": "m s-1", "cell_methods": "area: mean time: maximum within days time: mean over days", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Mean Daily Maximum Near-Surface Wind Speed", "comment": "Daily maximum near-surface (usually, 10 meters) wind speed.", "dimensions": "longitude latitude time height10m", @@ -5163,15 +5109,15 @@ "ok_max_mean_abs": "" }, "tSoilPools": { - "frequency": "monPt", + "frequency": "mon", "modeling_realm": "land", "standard_name": "soil_carbon_turnover_rate_by_pool", "units": "s-1", - "cell_methods": "area: mean where land time: point", + "cell_methods": "area: mean where land time: mean", "cell_measures": "area: areacella", "long_name": "turnover rate of each model soil carbon pool", "comment": "defined as 1/(turnover time) for each soil pool. Use the same pools reported under cSoilPools", - "dimensions": "longitude latitude soilpools time1", + "dimensions": "longitude latitude soilpools time", "out_name": "tSoilPools", "type": "real", "positive": "", @@ -5206,7 +5152,7 @@ "cell_methods": "area: time: mean where landuse", "cell_measures": "area: areacella", "long_name": "near-surface air temperature (2m above displacement height, i.e. t_ref) on land use tile", - "comment": "", + "comment": "Air temperature is the bulk temperature of the air, not the surface (skin) temperature.", "dimensions": "longitude latitude landUse time height2m", "out_name": "tasLut", "type": "real", @@ -5294,7 +5240,7 @@ "standard_name": "sea_water_potential_temperature", "units": "degC", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "area: areacello", "long_name": "Depth average potential temperature of upper 2000m", "comment": "Upper 2000m, 2D field", "dimensions": "longitude latitude time depth2000m", @@ -5312,7 +5258,7 @@ "standard_name": "sea_water_potential_temperature", "units": "degC", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "area: areacello", "long_name": "Depth average potential temperature of upper 300m", "comment": "Upper 300m, 2D field", "dimensions": "longitude latitude time depth300m", @@ -5330,7 +5276,7 @@ "standard_name": "sea_water_potential_temperature", "units": "degC", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "area: areacello", "long_name": "Depth average potential temperature of upper 700m", "comment": "Upper 700m, 2D field", "dimensions": "longitude latitude time depth700m", @@ -5522,24 +5468,6 @@ "ok_min_mean_abs": "", "ok_max_mean_abs": "" }, - "tomint": { - "frequency": "mon", - "modeling_realm": "ocean", - "standard_name": "integral_wrt_depth_of_product_of_sea_water_density_and_prognostic_temperature", - "units": "1e-3 kg m-2", - "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello", - "long_name": "integral wrt depth of product of sea water density and prognostic temperature", - "comment": "Full column sum of density*cell thickness*prognostic temperature. If the model is Boussinesq, then use Boussinesq reference density for the density factor.", - "dimensions": "longitude latitude time", - "out_name": "tomint", - "type": "real", - "positive": "", - "valid_min": "", - "valid_max": "", - "ok_min_mean_abs": "", - "ok_max_mean_abs": "" - }, "treeFracBdlDcd": { "frequency": "mon", "modeling_realm": "land", @@ -5674,7 +5602,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Eastward Wind", - "comment": "", + "comment": "'Eastward' indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude plev7h time", "out_name": "ua", "type": "real", @@ -5692,7 +5620,7 @@ "cell_methods": "time: mean", "cell_measures": "area: areacella", "long_name": "Eastward Wind", - "comment": "", + "comment": "'Eastward' indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude plev27 time", "out_name": "ua", "type": "real", @@ -5836,7 +5764,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Northward Wind", - "comment": "", + "comment": "'Northward' indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude plev7h time", "out_name": "va", "type": "real", @@ -5854,7 +5782,7 @@ "cell_methods": "time: mean", "cell_measures": "area: areacella", "long_name": "Northward Wind", - "comment": "", + "comment": "'Northward' indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude plev27 time", "out_name": "va", "type": "real", @@ -5890,7 +5818,7 @@ "cell_methods": "area: mean where land time: mean", "cell_measures": "area: areacella", "long_name": "canopy height", - "comment": "", + "comment": "Height is the vertical distance above the surface. 'Canopy' means the plant or vegetation canopy.", "dimensions": "longitude latitude time", "out_name": "vegHeight", "type": "real", @@ -5908,7 +5836,7 @@ "cell_methods": "area: time: mean where crops (comment: mask=cropFrac)", "cell_measures": "area: areacella", "long_name": "Vegetation height averaged over the crop fraction of a grid cell.", - "comment": "", + "comment": "Height is the vertical distance above the surface. 'Canopy' means the plant or vegetation canopy.", "dimensions": "longitude latitude time", "out_name": "vegHeightCrop", "type": "real", @@ -5926,7 +5854,7 @@ "cell_methods": "area: time: mean where natural_grasses (comment: mask=grassFrac)", "cell_measures": "area: areacella", "long_name": "Vegetation height averaged over the grass fraction of a grid cell.", - "comment": "", + "comment": "Height is the vertical distance above the surface. 'Canopy' means the plant or vegetation canopy.", "dimensions": "longitude latitude time", "out_name": "vegHeightGrass", "type": "real", @@ -5944,7 +5872,7 @@ "cell_methods": "area: mean where land time: mean", "cell_measures": "area: areacella", "long_name": "Vegetation height averaged over the pasture fraction of a grid cell.", - "comment": "", + "comment": "Height is the vertical distance above the surface. 'Canopy' means the plant or vegetation canopy.", "dimensions": "longitude latitude time", "out_name": "vegHeightPasture", "type": "real", @@ -5962,7 +5890,7 @@ "cell_methods": "area: time: mean where shrubs (comment: mask=shrubFrac)", "cell_measures": "area: areacella", "long_name": "Vegetation height averaged over the shrub fraction of a grid cell.", - "comment": "", + "comment": "Height is the vertical distance above the surface. 'Canopy' means the plant or vegetation canopy.", "dimensions": "longitude latitude time", "out_name": "vegHeightShrub", "type": "real", @@ -5980,7 +5908,7 @@ "cell_methods": "area: time: mean where trees (comment: mask=treeFrac)", "cell_measures": "area: areacella", "long_name": "Vegetation height averaged over the tree fraction of a grid cell.", - "comment": "", + "comment": "Height is the vertical distance above the surface. 'Canopy' means the plant or vegetation canopy.", "dimensions": "longitude latitude time", "out_name": "vegHeightTree", "type": "real", @@ -6250,7 +6178,7 @@ "cell_methods": "time: mean", "cell_measures": "area: areacella", "long_name": "Geopotential Height", - "comment": "", + "comment": "Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface.", "dimensions": "longitude latitude plev27 time", "out_name": "zg", "type": "real", diff --git a/Tables/CMIP6_EmonZ.json b/Tables/CMIP6_EmonZ.json index bb2d8aad..7327ebe6 100644 --- a/Tables/CMIP6_EmonZ.json +++ b/Tables/CMIP6_EmonZ.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table EmonZ", "realm": "atmos", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", diff --git a/Tables/CMIP6_Esubhr.json b/Tables/CMIP6_Esubhr.json index b2c720e8..9618bf00 100644 --- a/Tables/CMIP6_Esubhr.json +++ b/Tables/CMIP6_Esubhr.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table Esubhr", "realm": "atmos", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -40,7 +40,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Surface Upward Latent Heat Flux", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Upward' indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time1", "out_name": "hfls", "type": "real", @@ -58,7 +58,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Surface Upward Sensible Heat Flux", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Upward' indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called 'turbulent' heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. Unless indicated in the cell_methods attribute, a quantity is assumed to apply to the whole area of each horizontal grid box. Previously, the qualifier where_type was used to specify that the quantity applies only to the part of the grid box of the named type. Names containing the where_type qualifier are deprecated and newly created data should use the cell_methods attribute to indicate the horizontal area to which the quantity applies.", "dimensions": "longitude latitude time1", "out_name": "hfss", "type": "real", @@ -76,7 +76,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Specific Humidity", - "comment": "", + "comment": "'specific' means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.", "dimensions": "longitude latitude alevel time1", "out_name": "hus", "type": "real", @@ -92,7 +92,7 @@ "standard_name": "specific_humidity", "units": "1", "cell_methods": "area: mean time: point", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Near-Surface Specific Humidity", "comment": "Near-surface (usually, 2 meter) specific humidity.", "dimensions": "longitude latitude time1 height2m", @@ -344,7 +344,7 @@ "standard_name": "air_temperature", "units": "K", "cell_methods": "area: mean time: point", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Surface Air Temperature", "comment": "near-surface (usually, 2 meter) air temperature", "dimensions": "longitude latitude time1 height2m", @@ -562,7 +562,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Eastward Wind", - "comment": "", + "comment": "'Eastward' indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude alevel time1", "out_name": "ua", "type": "real", @@ -580,7 +580,7 @@ "cell_methods": "area: mean time: point", "cell_measures": "area: areacella", "long_name": "Northward Wind", - "comment": "", + "comment": "'Northward' indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude alevel time1", "out_name": "va", "type": "real", diff --git a/Tables/CMIP6_Eyr.json b/Tables/CMIP6_Eyr.json index b6ea9bbb..d4cc859d 100644 --- a/Tables/CMIP6_Eyr.json +++ b/Tables/CMIP6_Eyr.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table Eyr", "realm": "land", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", diff --git a/Tables/CMIP6_IfxAnt.json b/Tables/CMIP6_IfxAnt.json index afdf5617..404bed74 100644 --- a/Tables/CMIP6_IfxAnt.json +++ b/Tables/CMIP6_IfxAnt.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table IfxAnt", "realm": "landIce", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", diff --git a/Tables/CMIP6_IfxGre.json b/Tables/CMIP6_IfxGre.json index 9f6a4358..4df80d64 100644 --- a/Tables/CMIP6_IfxGre.json +++ b/Tables/CMIP6_IfxGre.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table IfxGre", "realm": "landIce", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", diff --git a/Tables/CMIP6_ImonAnt.json b/Tables/CMIP6_ImonAnt.json index 9f726f19..9f99e4ed 100644 --- a/Tables/CMIP6_ImonAnt.json +++ b/Tables/CMIP6_ImonAnt.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table ImonAnt", "realm": "atmos", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -40,7 +40,7 @@ "cell_methods": "area: time: mean where ice_sheet", "cell_measures": "area: areacellg", "long_name": "Surface Upward Latent Heat Flux", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Upward' indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "xant yant time", "out_name": "hfls", "type": "real", @@ -58,7 +58,7 @@ "cell_methods": "area: time: mean where ice_sheet", "cell_measures": "area: areacellg", "long_name": "Surface Upward Sensible Heat Flux", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Upward' indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called 'turbulent' heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. Unless indicated in the cell_methods attribute, a quantity is assumed to apply to the whole area of each horizontal grid box. Previously, the qualifier where_type was used to specify that the quantity applies only to the part of the grid box of the named type. Names containing the where_type qualifier are deprecated and newly created data should use the cell_methods attribute to indicate the horizontal area to which the quantity applies.", "dimensions": "xant yant time", "out_name": "hfss", "type": "real", @@ -256,7 +256,7 @@ "cell_methods": "area: time: mean where ice_sheet", "cell_measures": "area: areacellg", "long_name": "Rainfall Flux over Land Ice", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "xant yant time", "out_name": "prra", "type": "real", @@ -292,7 +292,7 @@ "cell_methods": "area: time: mean where ice_sheet", "cell_measures": "area: areacellg", "long_name": "Surface Downwelling Longwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'longwave' means longwave radiation. Downwelling radiation is radiation from above. It does not mean 'net downward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "xant yant time", "out_name": "rlds", "type": "real", @@ -310,7 +310,7 @@ "cell_methods": "area: time: mean where ice_sheet", "cell_measures": "area: areacellg", "long_name": "Surface Upwelling Longwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'longwave' means longwave radiation. Upwelling radiation is radiation from below. It does not mean 'net upward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "xant yant time", "out_name": "rlus", "type": "real", @@ -346,7 +346,7 @@ "cell_methods": "area: time: mean where ice_sheet", "cell_measures": "area: areacellg", "long_name": "Surface Upwelling Shortwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'shortwave' means shortwave radiation. Upwelling radiation is radiation from below. It does not mean 'net upward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "xant yant time", "out_name": "rsus", "type": "real", diff --git a/Tables/CMIP6_ImonGre.json b/Tables/CMIP6_ImonGre.json index f1066fbb..856c4aa4 100644 --- a/Tables/CMIP6_ImonGre.json +++ b/Tables/CMIP6_ImonGre.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table ImonGre", "realm": "atmos", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -40,7 +40,7 @@ "cell_methods": "area: time: mean where ice_sheet", "cell_measures": "area: areacellg", "long_name": "Surface Upward Latent Heat Flux", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Upward' indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "xgre ygre time", "out_name": "hfls", "type": "real", @@ -58,7 +58,7 @@ "cell_methods": "area: time: mean where ice_sheet", "cell_measures": "area: areacellg", "long_name": "Surface Upward Sensible Heat Flux", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Upward' indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called 'turbulent' heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. Unless indicated in the cell_methods attribute, a quantity is assumed to apply to the whole area of each horizontal grid box. Previously, the qualifier where_type was used to specify that the quantity applies only to the part of the grid box of the named type. Names containing the where_type qualifier are deprecated and newly created data should use the cell_methods attribute to indicate the horizontal area to which the quantity applies.", "dimensions": "xgre ygre time", "out_name": "hfss", "type": "real", @@ -256,7 +256,7 @@ "cell_methods": "area: time: mean where ice_sheet", "cell_measures": "area: areacellg", "long_name": "Rainfall Flux over Land Ice", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "xgre ygre time", "out_name": "prra", "type": "real", @@ -292,7 +292,7 @@ "cell_methods": "area: time: mean where ice_sheet", "cell_measures": "area: areacellg", "long_name": "Surface Downwelling Longwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'longwave' means longwave radiation. Downwelling radiation is radiation from above. It does not mean 'net downward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "xgre ygre time", "out_name": "rlds", "type": "real", @@ -310,7 +310,7 @@ "cell_methods": "area: time: mean where ice_sheet", "cell_measures": "area: areacellg", "long_name": "Surface Upwelling Longwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'longwave' means longwave radiation. Upwelling radiation is radiation from below. It does not mean 'net upward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "xgre ygre time", "out_name": "rlus", "type": "real", @@ -346,7 +346,7 @@ "cell_methods": "area: time: mean where ice_sheet", "cell_measures": "area: areacellg", "long_name": "Surface Upwelling Shortwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'shortwave' means shortwave radiation. Upwelling radiation is radiation from below. It does not mean 'net upward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "xgre ygre time", "out_name": "rsus", "type": "real", diff --git a/Tables/CMIP6_IyrAnt.json b/Tables/CMIP6_IyrAnt.json index 0718cb22..82178509 100644 --- a/Tables/CMIP6_IyrAnt.json +++ b/Tables/CMIP6_IyrAnt.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table IyrAnt", "realm": "atmos", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", diff --git a/Tables/CMIP6_IyrGre.json b/Tables/CMIP6_IyrGre.json index 24b49084..01ca78c5 100644 --- a/Tables/CMIP6_IyrGre.json +++ b/Tables/CMIP6_IyrGre.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table IyrGre", "realm": "atmos", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", diff --git a/Tables/CMIP6_LImon.json b/Tables/CMIP6_LImon.json index ebfac434..0833d502 100644 --- a/Tables/CMIP6_LImon.json +++ b/Tables/CMIP6_LImon.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table LImon", "realm": "landIce land", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -256,7 +256,7 @@ "cell_methods": "area: time: mean where ice_sheet", "cell_measures": "area: areacella", "long_name": "Ice Sheet Surface Downwelling Longwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'longwave' means longwave radiation. Downwelling radiation is radiation from above. It does not mean 'net downward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "rldsIs", "type": "real", @@ -274,7 +274,7 @@ "cell_methods": "area: time: mean where ice_sheet", "cell_measures": "area: areacella", "long_name": "Ice Sheet Surface Upwelling Longwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'longwave' means longwave radiation. Upwelling radiation is radiation from below. It does not mean 'net upward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "rlusIs", "type": "real", @@ -310,7 +310,7 @@ "cell_methods": "area: time: mean where ice_sheet", "cell_measures": "area: areacella", "long_name": "Ice Sheet Surface Upwelling Shortwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'shortwave' means shortwave radiation. Upwelling radiation is radiation from below. It does not mean 'net upward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "rsusIs", "type": "real", diff --git a/Tables/CMIP6_Lmon.json b/Tables/CMIP6_Lmon.json index 6c6692de..8c13d784 100644 --- a/Tables/CMIP6_Lmon.json +++ b/Tables/CMIP6_Lmon.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table Lmon", "realm": "land", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -490,7 +490,7 @@ "cell_methods": "area: mean where land time: mean", "cell_measures": "area: areacella", "long_name": "Leaf Area Index", - "comment": "", + "comment": "'X_area' means the horizontal area occupied by X within the grid cell.", "dimensions": "longitude latitude time", "out_name": "lai", "type": "real", @@ -596,7 +596,7 @@ "standard_name": "moisture_content_of_soil_layer", "units": "kg m-2", "cell_methods": "area: mean where land time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Moisture in Upper Portion of Soil Column", "comment": "The mass of water in all phases in the upper 10cm of the soil layer.", "dimensions": "longitude latitude time sdepth1", diff --git a/Tables/CMIP6_Oclim.json b/Tables/CMIP6_Oclim.json index 64bc74fc..d846970f 100644 --- a/Tables/CMIP6_Oclim.json +++ b/Tables/CMIP6_Oclim.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table Oclim", "realm": "ocean", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", diff --git a/Tables/CMIP6_Oday.json b/Tables/CMIP6_Oday.json index c8f992a2..c951ead2 100644 --- a/Tables/CMIP6_Oday.json +++ b/Tables/CMIP6_Oday.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table Oday", "realm": "ocnBgChem", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -76,7 +76,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Sea Surface Salinity", - "comment": "", + "comment": "Sea surface salinity is the salt content of sea water close to the sea surface, often on the Practical Salinity Scale of 1978. However, the unqualified term 'salinity' is generic and does not necessarily imply any particular method of calculation. The units of salinity are dimensionless and the units attribute should normally be given as 1e-3 or 0.001 i.e. parts per thousand. Sea surface salinity is often abbreviated as 'SSS'. For the salinity of sea water at a particular depth or layer, a data variable of 'sea_water_salinity' or one of the more precisely defined salinities should be used with a vertical coordinate axis.", "dimensions": "longitude latitude time", "out_name": "sos", "type": "real", diff --git a/Tables/CMIP6_Odec.json b/Tables/CMIP6_Odec.json index 02858f58..25ac1ede 100644 --- a/Tables/CMIP6_Odec.json +++ b/Tables/CMIP6_Odec.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table Odec", "realm": "ocean", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -32,6 +32,24 @@ "ok_min_mean_abs": "", "ok_max_mean_abs": "" }, + "bigthetao": { + "frequency": "dec", + "modeling_realm": "ocean", + "standard_name": "sea_water_conservative_temperature", + "units": "degC", + "cell_methods": "area: mean where sea time: mean", + "cell_measures": "area: areacello volume: volcello", + "long_name": "Sea Water Convervative Temperature", + "comment": "Sea water conservative temperature (this should be contributed only for models using conservative temperature as prognostic field)", + "dimensions": "longitude latitude olevel time", + "out_name": "bigthetao", + "type": "real", + "positive": "", + "valid_min": "", + "valid_max": "", + "ok_min_mean_abs": "", + "ok_max_mean_abs": "" + }, "bigthetaoga": { "frequency": "dec", "modeling_realm": "ocean", @@ -86,6 +104,24 @@ "ok_min_mean_abs": "", "ok_max_mean_abs": "" }, + "masscello": { + "frequency": "dec", + "modeling_realm": "ocean", + "standard_name": "sea_water_mass_per_unit_area", + "units": "kg m-2", + "cell_methods": "area: mean where sea time: mean", + "cell_measures": "area: areacello volume: volcello", + "long_name": "Sea Water Mass Per Unit Area", + "comment": "Tracer grid-cell mass per unit area used for computing tracer budgets. For Boussinesq models with static ocean grid cell thickness, masscello = rhozero*thickcello, where thickcello is static cell thickness and rhozero is constant Boussinesq reference density. More generally, masscello is time dependent and reported as part of Omon.", + "dimensions": "longitude latitude olevel time", + "out_name": "masscello", + "type": "real", + "positive": "", + "valid_min": "", + "valid_max": "", + "ok_min_mean_abs": "", + "ok_max_mean_abs": "" + }, "masso": { "frequency": "dec", "modeling_realm": "ocean", @@ -104,6 +140,24 @@ "ok_min_mean_abs": "", "ok_max_mean_abs": "" }, + "msftmrho": { + "frequency": "dec", + "modeling_realm": "ocean", + "standard_name": "ocean_meridional_overturning_mass_streamfunction", + "units": "kg s-1", + "cell_methods": "longitude: mean (comment: basin mean[ along zig-zag grid path]) time: mean", + "cell_measures": "", + "long_name": "Ocean Meridional Overturning Mass Streamfunction", + "comment": "Overturning mass streamfunction arising from all advective mass transport processes, resolved and parameterized.", + "dimensions": "latitude rho basin time", + "out_name": "msftmrho", + "type": "real", + "positive": "", + "valid_min": "", + "valid_max": "", + "ok_min_mean_abs": "", + "ok_max_mean_abs": "" + }, "msftmz": { "frequency": "dec", "modeling_realm": "ocean", @@ -122,6 +176,42 @@ "ok_min_mean_abs": "", "ok_max_mean_abs": "" }, + "msftyrho": { + "frequency": "dec", + "modeling_realm": "ocean", + "standard_name": "ocean_y_overturning_mass_streamfunction", + "units": "kg s-1", + "cell_methods": "time: mean grid_longitude: mean", + "cell_measures": "", + "long_name": "Ocean Y Overturning Mass Streamfunction", + "comment": "Overturning mass streamfunction arising from all advective mass transport processes, resolved and parameterized.", + "dimensions": "latitude rho basin time", + "out_name": "msftyrho", + "type": "real", + "positive": "", + "valid_min": "", + "valid_max": "", + "ok_min_mean_abs": "", + "ok_max_mean_abs": "" + }, + "msftyz": { + "frequency": "dec", + "modeling_realm": "ocean", + "standard_name": "ocean_y_overturning_mass_streamfunction", + "units": "kg s-1", + "cell_methods": "time: mean grid_longitude: mean", + "cell_measures": "", + "long_name": "Ocean Y Overturning Mass Streamfunction", + "comment": "Overturning mass streamfunction arising from all advective mass transport processes, resolved and parameterized.", + "dimensions": "latitude olevel basin time", + "out_name": "msftyz", + "type": "real", + "positive": "", + "valid_min": "", + "valid_max": "", + "ok_min_mean_abs": "", + "ok_max_mean_abs": "" + }, "sfdsi": { "frequency": "dec", "modeling_realm": "ocean seaIce", @@ -166,7 +256,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Sea Water Salinity", - "comment": "", + "comment": "Sea water salinity is the salt content of sea water, often on the Practical Salinity Scale of 1978. However, the unqualified term 'salinity' is generic and does not necessarily imply any particular method of calculation. The units of salinity are dimensionless and the units attribute should normally be given as 1e-3 or 0.001 i.e. parts per thousand. There are standard names for the more precisely defined salinity quantities: sea_water_knudsen_salinity, S_K (used for salinity observations between 1901 and 1966), sea_water_cox_salinity, S_C (used for salinity observations between 1967 and 1977), sea_water_practical_salinity, S_P (used for salinity observations from 1978 to the present day), sea_water_absolute_salinity, S_A, sea_water_preformed_salinity, S_*, and sea_water_reference_salinity. Practical Salinity is reported on the Practical Salinity Scale of 1978 (PSS-78), and is usually based on the electrical conductivity of sea water in observations since the 1960s.", "dimensions": "longitude latitude olevel time", "out_name": "so", "type": "real", @@ -184,7 +274,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "", "long_name": "Global Mean Sea Water Salinity", - "comment": "", + "comment": "Sea water salinity is the salt content of sea water, often on the Practical Salinity Scale of 1978. However, the unqualified term 'salinity' is generic and does not necessarily imply any particular method of calculation. The units of salinity are dimensionless and the units attribute should normally be given as 1e-3 or 0.001 i.e. parts per thousand. There are standard names for the more precisely defined salinity quantities: sea_water_knudsen_salinity, S_K (used for salinity observations between 1901 and 1966), sea_water_cox_salinity, S_C (used for salinity observations between 1967 and 1977), sea_water_practical_salinity, S_P (used for salinity observations from 1978 to the present day), sea_water_absolute_salinity, S_A, sea_water_preformed_salinity, S_*, and sea_water_reference_salinity. Practical Salinity is reported on the Practical Salinity Scale of 1978 (PSS-78), and is usually based on the electrical conductivity of sea water in observations since the 1960s.", "dimensions": "time", "out_name": "soga", "type": "real", @@ -202,7 +292,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Sea Surface Salinity", - "comment": "", + "comment": "Sea surface salinity is the salt content of sea water close to the sea surface, often on the Practical Salinity Scale of 1978. However, the unqualified term 'salinity' is generic and does not necessarily imply any particular method of calculation. The units of salinity are dimensionless and the units attribute should normally be given as 1e-3 or 0.001 i.e. parts per thousand. Sea surface salinity is often abbreviated as 'SSS'. For the salinity of sea water at a particular depth or layer, a data variable of 'sea_water_salinity' or one of the more precisely defined salinities should be used with a vertical coordinate axis.", "dimensions": "longitude latitude time", "out_name": "sos", "type": "real", @@ -220,7 +310,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "", "long_name": "Global Average Sea Surface Salinity", - "comment": "", + "comment": "Sea surface salinity is the salt content of sea water close to the sea surface, often on the Practical Salinity Scale of 1978. However, the unqualified term 'salinity' is generic and does not necessarily imply any particular method of calculation. The units of salinity are dimensionless and the units attribute should normally be given as 1e-3 or 0.001 i.e. parts per thousand. Sea surface salinity is often abbreviated as 'SSS'. For the salinity of sea water at a particular depth or layer, a data variable of 'sea_water_salinity' or one of the more precisely defined salinities should be used with a vertical coordinate axis.", "dimensions": "time", "out_name": "sosga", "type": "real", @@ -310,7 +400,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Ocean Model Cell Thickness", - "comment": "", + "comment": "'Thickness' means the vertical extent of a layer. 'Cell' refers to a model grid-cell.", "dimensions": "longitude latitude olevel time", "out_name": "thkcello", "type": "real", @@ -392,6 +482,24 @@ "ok_min_mean_abs": "", "ok_max_mean_abs": "" }, + "volcello": { + "frequency": "dec", + "modeling_realm": "ocean", + "standard_name": "ocean_volume", + "units": "m3", + "cell_methods": "area: mean where sea time: mean", + "cell_measures": "area: areacello volume: volcello", + "long_name": "Ocean Grid-Cell Volume", + "comment": "grid-cell volume ca. 2000.", + "dimensions": "longitude latitude olevel time", + "out_name": "volcello", + "type": "real", + "positive": "", + "valid_min": "", + "valid_max": "", + "ok_min_mean_abs": "", + "ok_max_mean_abs": "" + }, "volo": { "frequency": "dec", "modeling_realm": "ocean", @@ -436,7 +544,7 @@ "cell_methods": "time: mean", "cell_measures": "--OPT", "long_name": "Sea Water Z Velocity", - "comment": "", + "comment": "A velocity is a vector quantity. 'Upward' indicates a vector component which is positive when directed upward (negative downward).", "dimensions": "longitude latitude olevel time", "out_name": "wo", "type": "real", diff --git a/Tables/CMIP6_Ofx.json b/Tables/CMIP6_Ofx.json index 0777eaf4..a3ffc1d6 100644 --- a/Tables/CMIP6_Ofx.json +++ b/Tables/CMIP6_Ofx.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table Ofx", "realm": "ocean", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -40,7 +40,7 @@ "cell_methods": "area: mean", "cell_measures": "area: areacello", "long_name": "Region Selection Index", - "comment": "", + "comment": "A variable with the standard name of region contains strings which indicate geographical regions. These strings must be chosen from the standard region list.", "dimensions": "longitude latitude", "out_name": "basin", "type": "integer", @@ -78,7 +78,7 @@ "cell_methods": "area: mean", "cell_measures": "area: areacello", "long_name": "Upward Geothermal Heat Flux at Sea Floor", - "comment": "", + "comment": "'Upward' indicates a vector component which is positive when directed upward (negative downward). In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude", "out_name": "hfgeou", "type": "real", @@ -132,7 +132,7 @@ "cell_methods": "area: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Ocean Model Cell Thickness", - "comment": "", + "comment": "'Thickness' means the vertical extent of a layer. 'Cell' refers to a model grid-cell.", "dimensions": "longitude latitude olevel", "out_name": "thkcello", "type": "real", diff --git a/Tables/CMIP6_Omon.json b/Tables/CMIP6_Omon.json index 664d5e43..1d7b0398 100644 --- a/Tables/CMIP6_Omon.json +++ b/Tables/CMIP6_Omon.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table Omon", "realm": "ocnBgChem", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -38,10 +38,10 @@ "standard_name": "mole_concentration_of_aragonite_expressed_as_carbon_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Aragonite Concentration", "comment": "Sum of particulate aragonite components (e.g. Phytoplankton, Detrital, etc.)", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "arag", "type": "real", "positive": "", @@ -56,10 +56,10 @@ "standard_name": "mole_concentration_of_bacteria_expressed_as_carbon_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Bacterial Carbon Concentration", "comment": "Sum of bacterial carbon component concentrations", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "bacc", "type": "real", "positive": "", @@ -74,10 +74,10 @@ "standard_name": "mole_concentration_of_particulate_organic_matter_expressed_as_iron_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Mole Concentration of Particulate Organic Matter expressed as Iron in sea water", "comment": "Sum of particulate organic iron component concentrations", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "bfe", "type": "real", "positive": "", @@ -95,7 +95,7 @@ "cell_measures": "area: areacello", "long_name": "Surface Mole Concentration of Particulate Organic Matter expressed as Iron in sea water", "comment": "sum of particulate organic iron component concentrations", - "dimensions": "longitude latitude time depth0m", + "dimensions": "longitude latitude time", "out_name": "bfeos", "type": "real", "positive": "", @@ -146,10 +146,10 @@ "standard_name": "mole_concentration_of_particulate_matter_expressed_as_silicon_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Mole Concentration of Particulate Organic Matter expressed as silicon in sea water", "comment": "Sum of particulate silica component concentrations", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "bsi", "type": "real", "positive": "", @@ -167,7 +167,7 @@ "cell_measures": "area: areacello", "long_name": "Surface Mole Concentration of Particulate Organic Matter expressed as Silicon in sea water", "comment": "sum of particulate silica component concentrations", - "dimensions": "longitude latitude time depth0m", + "dimensions": "longitude latitude time", "out_name": "bsios", "type": "real", "positive": "", @@ -182,10 +182,10 @@ "standard_name": "mole_concentration_of_calcite_expressed_as_carbon_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Calcite Concentration", "comment": "Sum of particulate calcite component concentrations (e.g. Phytoplankton, Detrital, etc.)", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "calc", "type": "real", "positive": "", @@ -202,7 +202,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Moles Per Unit Mass of CFC-11 in sea water", - "comment": "", + "comment": "Mole concentration means number of moles per unit volume, also called 'molarity', and is used in the construction 'mole_concentration_of_X_in_Y', where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula of CFC11 is CFCl3. The IUPAC name fof CFC11 is trichloro-fluoro-methane.", "dimensions": "longitude latitude olevel time", "out_name": "cfc11", "type": "real", @@ -220,7 +220,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Moles Per Unit Mass of CFC-12 in sea water", - "comment": "", + "comment": "Mole concentration means number of moles per unit volume, also called 'molarity', and is used in the construction 'mole_concentration_of_X_in_Y', where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for CFC12 is CF2Cl2. The IUPAC name for CFC12 is dichloro-difluoro-methane.", "dimensions": "longitude latitude olevel time", "out_name": "cfc12", "type": "real", @@ -236,10 +236,10 @@ "standard_name": "mass_concentration_of_phytoplankton_expressed_as_chlorophyll_in_sea_water", "units": "kg m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Mass Concentration of Total Chlorophyll in sea water", "comment": "Sum of chlorophyll from all phytoplankton group concentrations. In most models this is equal to chldiat+chlmisc, that is the sum of Diatom Chlorophyll Mass Concentration and Other Phytoplankton Chlorophyll Mass Concentration", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "chl", "type": "real", "positive": "", @@ -254,10 +254,10 @@ "standard_name": "mass_concentration_of_calcareous_phytoplankton_expressed_as_chlorophyll_in_sea_water", "units": "kg m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Mass Concentration of Calcareous Phytoplankton expressed as Chlorophyll in sea water", "comment": "chlorophyll concentration from the calcite-producing phytoplankton component alone", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "chlcalc", "type": "real", "positive": "", @@ -275,7 +275,7 @@ "cell_measures": "area: areacello", "long_name": "Surface Mass Concentration of Calcareous Phytoplankton expressed as Chlorophyll in sea water", "comment": "chlorophyll concentration from the calcite-producing phytoplankton component alone", - "dimensions": "longitude latitude time depth0m", + "dimensions": "longitude latitude time", "out_name": "chlcalcos", "type": "real", "positive": "", @@ -290,10 +290,10 @@ "standard_name": "mass_concentration_of_diatoms_expressed_as_chlorophyll_in_sea_water", "units": "kg m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Mass Concentration of Diatom expressed as Chlorophyll in sea water", "comment": "Chlorophyll from diatom phytoplankton component concentration alone", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "chldiat", "type": "real", "positive": "", @@ -311,7 +311,7 @@ "cell_measures": "area: areacello", "long_name": "Surface Mass Concentration of Diatoms expressed as Chlorophyll in sea water", "comment": "chlorophyll from diatom phytoplankton component concentration alone", - "dimensions": "longitude latitude time depth0m", + "dimensions": "longitude latitude time", "out_name": "chldiatos", "type": "real", "positive": "", @@ -326,10 +326,10 @@ "standard_name": "mass_concentration_of_diazotrophs_expressed_as_chlorophyll_in_sea_water", "units": "kg m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Mass Concentration of Diazotrophs expressed as Chlorophyll in sea water", "comment": "Chlorophyll concentration from the diazotrophic phytoplankton component alone", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "chldiaz", "type": "real", "positive": "", @@ -347,7 +347,7 @@ "cell_measures": "area: areacello", "long_name": "Surface Mass Concentration of Diazotrophs expressed as Chlorophyll in sea water", "comment": "chlorophyll concentration from the diazotrophic phytoplankton component alone", - "dimensions": "longitude latitude time depth0m", + "dimensions": "longitude latitude time", "out_name": "chldiazos", "type": "real", "positive": "", @@ -362,10 +362,10 @@ "standard_name": "mass_concentration_of_miscellaneous_phytoplankton_expressed_as_chlorophyll_in_sea_water", "units": "kg m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Mass Concentration of Other Phytoplankton expressed as Chlorophyll in sea water", "comment": "Chlorophyll from additional phytoplankton component concentrations alone", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "chlmisc", "type": "real", "positive": "", @@ -383,7 +383,7 @@ "cell_measures": "area: areacello", "long_name": "Surface Mass Concentration of Other Phytoplankton expressed as Chlorophyll in sea water", "comment": "chlorophyll from additional phytoplankton component concentrations alone", - "dimensions": "longitude latitude time depth0m", + "dimensions": "longitude latitude time", "out_name": "chlmiscos", "type": "real", "positive": "", @@ -401,7 +401,7 @@ "cell_measures": "area: areacello", "long_name": "Surface Mass Concentration of Total Phytoplankton expressed as Chlorophyll in sea water", "comment": "Sum of chlorophyll from all phytoplankton group concentrations at the sea surface. In most models this is equal to chldiat+chlmisc, that is the sum of 'Diatom Chlorophyll Mass Concentration' plus 'Other Phytoplankton Chlorophyll Mass Concentration'", - "dimensions": "longitude latitude time depth0m", + "dimensions": "longitude latitude time", "out_name": "chlos", "type": "real", "positive": "", @@ -416,10 +416,10 @@ "standard_name": "mass_concentration_of_picophytoplankton_expressed_as_chlorophyll_in_sea_water", "units": "kg m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Mass Concentration of Picophytoplankton expressed as Chlorophyll in sea water", "comment": "chlorophyll concentration from the picophytoplankton (<2 um) component alone", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "chlpico", "type": "real", "positive": "", @@ -437,7 +437,7 @@ "cell_measures": "area: areacello", "long_name": "Surface Mass Concentration of Picophytoplankton expressed as Chlorophyll in sea water", "comment": "chlorophyll concentration from the picophytoplankton (<2 um) component alone", - "dimensions": "longitude latitude time depth0m", + "dimensions": "longitude latitude time", "out_name": "chlpicoos", "type": "real", "positive": "", @@ -452,10 +452,10 @@ "standard_name": "mole_concentration_of_carbonate_expressed_as_carbon_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Carbonate ion Concentration", - "comment": "", - "dimensions": "longitude latitude olevel time", + "comment": "'Mole concentration' means number of moles per unit volume, also called'molarity', and is used in the construction mole_concentration_of_X_in_Y, whereX is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The phrase 'expressed_as' is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. The chemical formula of the carbonate anion is CO3 with a charge of minus two.", + "dimensions": "longitude latitude time depth0m", "out_name": "co3", "type": "real", "positive": "", @@ -470,10 +470,10 @@ "standard_name": "mole_concentration_of_carbonate_abiotic_analogue_expressed_as_carbon_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Abiotic Carbonate ion Concentration", - "comment": "", - "dimensions": "longitude latitude olevel time", + "comment": "Mole concentration means number of moles per unit volume, also called 'molarity', and is used in the construction 'mole_concentration_of_X_in_Y', where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. In ocean biogeochemistry models, an 'abiotic analogue' is used to simulate the effect on a modelled variable when biological effects on ocean carbon concentration and alkalinity are ignored. The phrase 'expressed_as' is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. The chemical formula of the carbonate anion is CO3 with an electrical charge of minus two.", + "dimensions": "longitude latitude time depth0m", "out_name": "co3abio", "type": "real", "positive": "", @@ -488,10 +488,10 @@ "standard_name": "mole_concentration_of_carbonate_natural_analogue_expressed_as_carbon_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Natural Carbonate ion Concentration", - "comment": "", - "dimensions": "longitude latitude olevel time", + "comment": "Mole concentration means number of moles per unit volume, also called 'molarity', and is used in the construction 'mole_concentration_of_X_in_Y', where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. In ocean biogeochemistry models, a 'natural analogue' is used to simulate the effect on a modelled variable of imposing preindustrial atmospheric carbon dioxide concentrations, even when the model as a whole may be subjected to varying forcings. The phrase 'expressed_as' is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. The chemical formula of the carbonate anion is CO3 with an electrical charge of minus two.", + "dimensions": "longitude latitude time depth0m", "out_name": "co3nat", "type": "real", "positive": "", @@ -506,10 +506,10 @@ "standard_name": "mole_concentration_of_carbonate_expressed_as_carbon_at_equilibrium_with_pure_aragonite_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Carbonate ion Concentration for sea water in equilibrium with pure Aragonite", - "comment": "", - "dimensions": "longitude latitude olevel time", + "comment": "Mole concentration means number of moles per unit volume, also called 'molarity', and is used in the construction 'mole_concentration_of_X_in_Y', where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The phrase 'expressed_as' is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. The chemical formula of the carbonate anion is CO3 with an electrical charge of minus two. Aragonite is a mineral that is a polymorph of calcium carbonate. The chemical formula of aragonite is CaCO3. At a given salinity, the thermodynamic equilibrium is that between dissolved carbonate ion and solid aragonite. Standard names also exist for calcite, another polymorph of calcium carbonate.", + "dimensions": "longitude latitude time depth0m", "out_name": "co3satarag", "type": "real", "positive": "", @@ -524,10 +524,10 @@ "standard_name": "mole_concentration_of_carbonate_expressed_as_carbon_at_equilibrium_with_pure_calcite_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Carbonate ion Concentration for sea water in equilibrium with pure Calcite", - "comment": "", - "dimensions": "longitude latitude olevel time", + "comment": "Mole concentration means number of moles per unit volume, also called 'molarity', and is used in the construction 'mole_concentration_of_X_in_Y', where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The phrase 'expressed_as' is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. The chemical formula of the carbonate anion is CO3 with an electrical charge of minus two. Calcite is a mineral that is a polymorph of calcium carbonate. The chemical formula of calcite is CaCO3. At a given salinity, the thermodynamic equilibrium is that between dissolved carbonate ion and solid calcite. Standard names also exist for aragonite, another polymorph of calcium carbonate.", + "dimensions": "longitude latitude time depth0m", "out_name": "co3satcalc", "type": "real", "positive": "", @@ -542,10 +542,10 @@ "standard_name": "mole_concentration_of_organic_detritus_expressed_as_carbon_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Detrital Organic Carbon Concentration", "comment": "Sum of detrital organic carbon component concentrations", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "detoc", "type": "real", "positive": "", @@ -560,10 +560,10 @@ "standard_name": "mole_concentration_of_dissolved_iron_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Mole Concentration of Dissolved Iron in sea water", "comment": "Dissolved iron in sea water, including both Fe2+ and Fe3+ ions (but not particulate detrital iron)", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "dfe", "type": "real", "positive": "", @@ -581,7 +581,7 @@ "cell_measures": "area: areacello", "long_name": "Surface Dissolved Iron Concentration", "comment": "dissolved iron in sea water is meant to include both Fe2+ and Fe3+ ions (but not, e.g., particulate detrital iron)", - "dimensions": "longitude latitude time depth0m", + "dimensions": "longitude latitude time", "out_name": "dfeos", "type": "real", "positive": "", @@ -596,10 +596,10 @@ "standard_name": "mole_concentration_of_dissolved_inorganic_carbon13_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Dissolved Inorganic 13Carbon Concentration", "comment": "Dissolved inorganic 14carbon (CO3+HCO3+H2CO3) concentration", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "dissi13c", "type": "real", "positive": "", @@ -617,7 +617,7 @@ "cell_measures": "area: areacello", "long_name": "Surface Dissolved Inorganic 13Carbon Concentration", "comment": "Dissolved inorganic 14carbon (CO3+HCO3+H2CO3) concentration", - "dimensions": "longitude latitude time depth0m", + "dimensions": "longitude latitude time", "out_name": "dissi13cos", "type": "real", "positive": "", @@ -632,10 +632,10 @@ "standard_name": "mole_concentration_of_dissolved_inorganic_carbon14_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Abiotic Dissolved Inorganic 14Carbon Concentration", "comment": "Abiotic Dissolved inorganic 14carbon (CO3+HCO3+H2CO3) concentration", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "dissi14cabio", "type": "real", "positive": "", @@ -653,7 +653,7 @@ "cell_measures": "area: areacello", "long_name": "Surface Abiotic Dissolved Inorganic 14Carbon Concentration", "comment": "Abiotic Dissolved inorganic 14carbon (CO3+HCO3+H2CO3) concentration", - "dimensions": "longitude latitude time depth0m", + "dimensions": "longitude latitude time", "out_name": "dissi14cabioos", "type": "real", "positive": "", @@ -668,10 +668,10 @@ "standard_name": "mole_concentration_of_dissolved_inorganic_carbon_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Dissolved Inorganic Carbon Concentration", "comment": "Dissolved inorganic carbon (CO3+HCO3+H2CO3) concentration", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "dissic", "type": "real", "positive": "", @@ -686,10 +686,10 @@ "standard_name": "mole_concentration_of_dissolved_inorganic_carbon_abiotic_analogue_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Abiotic Dissolved Inorganic Carbon Concentration", "comment": "Abiotic Dissolved inorganic carbon (CO3+HCO3+H2CO3) concentration", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "dissicabio", "type": "real", "positive": "", @@ -707,7 +707,7 @@ "cell_measures": "area: areacello", "long_name": "Surface Abiotic Dissolved Inorganic Carbon Concentration", "comment": "Abiotic Dissolved inorganic carbon (CO3+HCO3+H2CO3) concentration", - "dimensions": "longitude latitude time depth0m", + "dimensions": "longitude latitude time", "out_name": "dissicabioos", "type": "real", "positive": "", @@ -722,10 +722,10 @@ "standard_name": "mole_concentration_of_dissolved_inorganic_carbon_natural_analogue_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Natural Dissolved Inorganic Carbon Concentration", "comment": "Dissolved inorganic carbon (CO3+HCO3+H2CO3) concentration at preindustrial atmospheric xCO2", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "dissicnat", "type": "real", "positive": "", @@ -743,7 +743,7 @@ "cell_measures": "area: areacello", "long_name": "Surface Natural Dissolved Inorganic Carbon Concentration", "comment": "Dissolved inorganic carbon (CO3+HCO3+H2CO3) concentration at preindustrial atmospheric xCO2", - "dimensions": "longitude latitude time depth0m", + "dimensions": "longitude latitude time", "out_name": "dissicnatos", "type": "real", "positive": "", @@ -758,10 +758,10 @@ "standard_name": "mole_concentration_of_dissolved_organic_carbon_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Dissolved Organic Carbon Concentration", "comment": "Sum of dissolved carbon component concentrations explicitly represented (i.e. not ~40 uM refractory unless explicit)", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "dissoc", "type": "real", "positive": "", @@ -796,8 +796,8 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Surface Mole Concentration of Dimethyl Sulphide in sea water", - "comment": "", - "dimensions": "longitude latitude time depth0m", + "comment": "'Mole concentration' means number of moles per unit volume, also called'molarity', and is used in the construction mole_concentration_of_X_in_Y, whereX is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for dimethyl sulfide is (CH3)2S. Dimethyl sulfide is sometimes referred to as DMS.", + "dimensions": "longitude latitude time", "out_name": "dmsos", "type": "real", "positive": "", @@ -814,7 +814,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Delta PCO2", - "comment": "", + "comment": "The partial pressure of a dissolved gas in sea water is the partial pressure in air with which it would be in equilibrium. The partial pressure of a gaseous constituent of air is the pressure which it alone would exert with unchanged temperature and number of moles per unit volume. The surface called 'surface' means the lower boundary of the atmosphere. The chemical formula for carbon dioxide is CO2.", "dimensions": "longitude latitude time depth0m", "out_name": "dpco2", "type": "real", @@ -832,7 +832,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Abiotic Delta PCO2", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. The chemical formula for carbon dioxide is CO2. In ocean biogeochemistry models, an 'abiotic analogue' is used to simulate the effect on a modelled variable when biological effects on ocean carbon concentration and alkalinity are ignored. The partial pressure of a gaseous constituent of air is the pressure which it alone would exert with unchanged temperature and number of moles per unit volume. The partial pressure of a dissolved gas in sea water is the partial pressure in air with which it would be in equilibrium. The partial pressure difference between sea water and air is positive when the partial pressure of the dissolved gas in sea water is greater than the partial pressure in air.", "dimensions": "longitude latitude time depth0m", "out_name": "dpco2abio", "type": "real", @@ -850,7 +850,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Natural Delta PCO2", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. The chemical formula for carbon dioxide is CO2. In ocean biogeochemistry models, a 'natural analogue' is used to simulate the effect on a modelled variable of imposing preindustrial atmospheric carbon dioxide concentrations, even when the model as a whole may be subjected to varying forcings. The partial pressure of a gaseous constituent of air is the pressure which it alone would exert with unchanged temperature and number of moles per unit volume. The partial pressure of a dissolved gas in sea water is the partial pressure in air with which it would be in equilibrium. The partial pressure difference between sea water and air is positive when the partial pressure of the dissolved gas in sea water is greater than the partial pressure in air.", "dimensions": "longitude latitude time depth0m", "out_name": "dpco2nat", "type": "real", @@ -868,7 +868,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Delta PO2", - "comment": "", + "comment": "The partial pressure of a dissolved gas in sea water is the partial pressure in air with which it would be in equilibrium. The partial pressure of a gaseous constituent of air is the pressure which it alone would exert with unchanged temperature and number of moles per unit volume. The surface called 'surface' means the lower boundary of the atmosphere.", "dimensions": "longitude latitude time depth0m", "out_name": "dpo2", "type": "real", @@ -886,7 +886,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Downward Flux of Aragonite", - "comment": "", + "comment": "The phrase 'expressed_as' is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. 'Sinking' is the gravitational settling of particulate matter suspended in a liquid. A sinking flux is positive downwards and is calculated relative to the movement of the surrounding fluid. Aragonite is a mineral that is a polymorph of calcium carbonate. The chemical formula of aragonite is CaCO3. Standard names also exist for calcite, another polymorph of calcium carbonate.", "dimensions": "longitude latitude time depth100m", "out_name": "eparag100", "type": "real", @@ -904,7 +904,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Downward Flux of Particle Organic Carbon", - "comment": "", + "comment": "The phrase 'expressed_as' is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. 'Sinking' is the gravitational settling of particulate matter suspended in a liquid. A sinking flux is positive downwards and is calculated relative to the movement of the surrounding fluid.", "dimensions": "longitude latitude time depth100m", "out_name": "epc100", "type": "real", @@ -922,7 +922,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Downward Flux of Calcite", - "comment": "", + "comment": "The phrase 'expressed_as' is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. 'Sinking' is the gravitational settling of particulate matter suspended in a liquid. A sinking flux is positive downwards and is calculated relative to the movement of the surrounding fluid. Calcite is a mineral that is a polymorph of calcium carbonate. The chemical formula of calcite is CaCO3. Standard names also exist for aragonite, another polymorph of calcium carbonate.", "dimensions": "longitude latitude time depth100m", "out_name": "epcalc100", "type": "real", @@ -940,7 +940,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Downward Flux of Particulate Iron", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. 'Sinking' is the gravitational settling of particulate matter suspended in a liquid. A sinking flux is positive downwards and is calculated relative to the movement of the surrounding fluid.", "dimensions": "longitude latitude time depth100m", "out_name": "epfe100", "type": "real", @@ -958,7 +958,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Downward Flux of Particulate Nitrogen", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. 'Sinking' is the gravitational settling of particulate matter suspended in a liquid. A sinking flux is positive downwards and is calculated relative to the movement of the surrounding fluid.", "dimensions": "longitude latitude time depth100m", "out_name": "epn100", "type": "real", @@ -976,7 +976,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Downward Flux of Particulate Phosphorus", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. 'Sinking' is the gravitational settling of particulate matter suspended in a liquid. A sinking flux is positive downwards and is calculated relative to the movement of the surrounding fluid.", "dimensions": "longitude latitude time depth100m", "out_name": "epp100", "type": "real", @@ -994,7 +994,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Downward Flux of Particulate Silica", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. 'Sinking' is the gravitational settling of particulate matter suspended in a liquid. A sinking flux is positive downwards and is calculated relative to the movement of the surrounding fluid.", "dimensions": "longitude latitude time depth100m", "out_name": "epsi100", "type": "real", @@ -1174,7 +1174,7 @@ "cell_methods": "area: mean where sea depth: sum where sea (top 100m only) time: mean", "cell_measures": "area: areacello", "long_name": "Rate of Change of Net Dissolved Inorganic Carbon", - "comment": "", + "comment": "'Content' indicates a quantity per unit area. 'tendency_of_X' means derivative of X with respect to time. 'Dissolved inorganic carbon' describes a family of chemical species in solution, including carbon dioxide, carbonic acid and the carbonate and bicarbonate anions. 'Dissolved inorganic carbon' isthe term used in standard names for all species belonging to the family that are represented within a given model. The list of individual species that are included in a quantity having a group chemical standard name can vary between models. Where possible, the data variable should be accompanied by a complete description of the species represented, for example, by using a comment attribute.", "dimensions": "longitude latitude time olayer100m", "out_name": "fddtdic", "type": "real", @@ -1259,7 +1259,7 @@ "fg13co2": { "frequency": "mon", "modeling_realm": "ocnBgChem", - "standard_name": "surface_downward_mass_flux_of_carbon13_dioxide_abiotic_analogue_expressed_as_carbon13", + "standard_name": "air_sea_flux_of_13CO2", "units": "kg m-2 s-1", "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", @@ -1480,7 +1480,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Iron Loss to Sediments", - "comment": "", + "comment": "'Content' indicates a quantity per unit area. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. 'tendency_of_X' means derivative of X with respect to time.", "dimensions": "longitude latitude time", "out_name": "frfe", "type": "real", @@ -1534,7 +1534,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Nitrogen Loss to Sediments and through Denitrification", - "comment": "", + "comment": "'Content' indicates a quantity per unit area. The specification of a physical process by the phrase due_to_process means that the quantity named is asingle term in a sum of terms which together compose the general quantity named by omitting the phrase. 'Denitrification' is the conversion of nitrate into gasesous compounds such as nitric oxide, nitrous oxide and molecular nitrogen which are then emitted to the atmosphere. 'Sedimentation' is the sinking of particulate matter to the floor of a body of water. 'tendency_of_X' means derivative of X with respect to time.", "dimensions": "longitude latitude time", "out_name": "frn", "type": "real", @@ -1606,7 +1606,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Surface Downward Net Flux of Nitrogen", - "comment": "", + "comment": "'Content' indicates a quantity per unit area. The specification of a physical process by the phrase due_to_process means that the quantity named is asingle term in a sum of terms which together compose the general quantity named by omitting the phrase. Deposition of nitrogen into the ocean is the sum of dry and wet depositionof nitrogen species onto the ocean surface from the atmosphere. 'Nitrogen fixation' means the production of ammonia from nitrogen gas. Organisms that fix nitrogen are termed 'diazotrophs'. Diazotrophic phytoplankton can fix atmospheric nitrogen, thus increasing the content of nitrogen in the ocean. Runoff is the liquid water which drains from land. If not specified, 'runoff' refers to the sum of surface runoff and subsurface drainage.'tendency_of_X' means derivative of X with respect to time.", "dimensions": "longitude latitude time depth0m", "out_name": "fsn", "type": "real", @@ -1624,7 +1624,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Total Grazing of Phytoplankton by Zooplankton", - "comment": "", + "comment": "'tendency_of_X' means derivative of X with respect to time. Mole concentration means number of moles per unit volume, also called 'molarity', and is used in the construction 'mole_concentration_of_X_in_Y', where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The phrase 'expressed_as' is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. The specification of a physical process by the phrase 'due_to_' process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase.", "dimensions": "longitude latitude olevel time", "out_name": "graz", "type": "real", @@ -1732,7 +1732,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Heat Flux Correction", - "comment": "", + "comment": "Flux correction is also called 'flux adjustment'. A positive flux correction is downward i.e. added to the ocean. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "hfcorr", "type": "real", @@ -1786,7 +1786,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Upward Geothermal Heat Flux at Sea Floor", - "comment": "", + "comment": "'Upward' indicates a vector component which is positive when directed upward (negative downward). In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "hfgeou", "type": "real", @@ -1804,7 +1804,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Heat Flux into Sea Water due to Iceberg Thermodynamics", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. ' Iceberg thermodynamics' refers to the addition or subtraction of mass due to surface and basal fluxes, i.e., due to melting, sublimation and fusion.", "dimensions": "longitude latitude olevel time", "out_name": "hfibthermds", "type": "real", @@ -1822,7 +1822,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Heat Flux into Sea Water due to Iceberg Thermodynamics", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. ' Iceberg thermodynamics' refers to the addition or subtraction of mass due to surface and basal fluxes, i.e., due to melting, sublimation and fusion.", "dimensions": "longitude latitude time", "out_name": "hfibthermds", "type": "real", @@ -1876,7 +1876,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Temperature Flux due to Runoff Expressed as Heat Flux into Sea Water", - "comment": "", + "comment": "Runoff is the liquid water which drains from land. If not specified, 'runoff' refers to the sum of surface runoff and subsurface drainage. The quantity with standard name temperature_flux_due_to_runoff_expressed_as_heat_flux_into_sea_water is the heat carried by the transfer of water into the liquid ocean by the process of runoff. This quantity additonally includes melt water from sea ice and icebergs. It is calculated relative to the heat that would be transported by runoff water entering the sea at zero degrees Celsius. It is calculated as the product QrunoffCpTrunoff, where Q runoff is the mass flux of liquid runoff entering the sea water (kg m-2 s-1), Cp is the specific heat capacity of water, and Trunoff is the temperature in degrees Celsius of the runoff water. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude olevel time", "out_name": "hfrunoffds", "type": "real", @@ -1894,7 +1894,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Temperature Flux due to Runoff Expressed as Heat Flux into Sea Water", - "comment": "", + "comment": "Runoff is the liquid water which drains from land. If not specified, 'runoff' refers to the sum of surface runoff and subsurface drainage. The quantity with standard name temperature_flux_due_to_runoff_expressed_as_heat_flux_into_sea_water is the heat carried by the transfer of water into the liquid ocean by the process of runoff. This quantity additonally includes melt water from sea ice and icebergs. It is calculated relative to the heat that would be transported by runoff water entering the sea at zero degrees Celsius. It is calculated as the product QrunoffCpTrunoff, where Q runoff is the mass flux of liquid runoff entering the sea water (kg m-2 s-1), Cp is the specific heat capacity of water, and Trunoff is the temperature in degrees Celsius of the runoff water. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "hfrunoffds", "type": "real", @@ -1912,7 +1912,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Heat Flux into Sea Water due to Frazil Ice Formation", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. 'Frazil' consists of needle like crystals of ice, typically between three and four millimeters in diameter, which form as sea water begins to freeze. Salt is expelled during the freezing process and frazil ice consists of nearly pure fresh water.", "dimensions": "longitude latitude olevel time", "out_name": "hfsifrazil", "type": "real", @@ -1930,7 +1930,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Heat Flux into Sea Water due to Frazil Ice Formation", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. 'Frazil' consists of needle like crystals of ice, typically between three and four millimeters in diameter, which form as sea water begins to freeze. Salt is expelled during the freezing process and frazil ice consists of nearly pure fresh water.", "dimensions": "longitude latitude time", "out_name": "hfsifrazil", "type": "real", @@ -1948,7 +1948,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Heat Flux into Sea Water due to Snow Thermodynamics", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. 'Snow thermodynamics' refers to the addition or subtraction of mass due to surface and basal fluxes, i.e., due to melting, sublimation and fusion.", "dimensions": "longitude latitude olevel time", "out_name": "hfsnthermds", "type": "real", @@ -1966,7 +1966,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Heat Flux into Sea Water due to Snow Thermodynamics", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. 'Snow thermodynamics' refers to the addition or subtraction of mass due to surface and basal fluxes, i.e., due to melting, sublimation and fusion.", "dimensions": "longitude latitude time", "out_name": "hfsnthermds", "type": "real", @@ -2089,7 +2089,7 @@ "modeling_realm": "ocnBgChem", "standard_name": "ocean_mass_content_of_dissolved_inorganic_carbon", "units": "kg m-2", - "cell_methods": "area: mean where sea time: mean", + "cell_methods": "area: mean where sea depth: sum where sea time: mean", "cell_measures": "area: areacello", "long_name": "Dissolved Inorganic Carbon Content", "comment": "Vertically integrated DIC", @@ -2107,7 +2107,7 @@ "modeling_realm": "ocnBgChem", "standard_name": "ocean_mass_content_of_dissolved_organic_carbon", "units": "kg m-2", - "cell_methods": "area: mean where sea time: mean", + "cell_methods": "area: mean where sea depth: sum where sea time: mean", "cell_measures": "area: areacello", "long_name": "Dissolved Organic Carbon Content", "comment": "Vertically integrated DOC (explicit pools only)", @@ -2125,7 +2125,7 @@ "modeling_realm": "ocnBgChem", "standard_name": "tendency_of_ocean_mole_content_of_aragonite_expressed_as_carbon_due_to_biological_production", "units": "mol m-2 s-1", - "cell_methods": "area: mean where sea time: mean", + "cell_methods": "area: mean where sea depth: sum where sea time: mean", "cell_measures": "area: areacello", "long_name": "Aragonite Production", "comment": "Vertically integrated aragonite production", @@ -2143,7 +2143,7 @@ "modeling_realm": "ocnBgChem", "standard_name": "tendency_of_ocean_mole_content_of_iron_due_to_biological_production", "units": "mol m-2 s-1", - "cell_methods": "area: mean where sea time: mean", + "cell_methods": "area: mean where sea depth: sum where sea time: mean", "cell_measures": "area: areacello", "long_name": "Iron Production", "comment": "Vertically integrated biogenic iron production", @@ -2161,7 +2161,7 @@ "modeling_realm": "ocnBgChem", "standard_name": "tendency_of_ocean_mole_content_of_nitrogen_due_to_biological_production", "units": "mol m-2 s-1", - "cell_methods": "area: mean where sea time: mean", + "cell_methods": "area: mean where sea depth: sum where sea time: mean", "cell_measures": "area: areacello", "long_name": "Nitrogen Production", "comment": "Vertically integrated biogenic nitrogen production", @@ -2179,7 +2179,7 @@ "modeling_realm": "ocnBgChem", "standard_name": "tendency_of_ocean_mole_content_of_phosphorus_due_to_biological_production", "units": "mol m-2 s-1", - "cell_methods": "area: mean where sea time: mean", + "cell_methods": "area: mean where sea depth: sum where sea time: mean", "cell_measures": "area: areacello", "long_name": "Phosphorus Production", "comment": "Vertically integrated biogenic phosphorus production", @@ -2197,7 +2197,7 @@ "modeling_realm": "ocnBgChem", "standard_name": "tendency_of_ocean_mole_content_of_silicon_due_to_biological_production", "units": "mol m-2 s-1", - "cell_methods": "area: mean where sea time: mean", + "cell_methods": "area: mean where sea depth: sum where sea time: mean", "cell_measures": "area: areacello", "long_name": "Silica Production", "comment": "Vertically integrated biogenic silica production", @@ -2215,7 +2215,7 @@ "modeling_realm": "ocnBgChem", "standard_name": "tendency_of_ocean_mole_content_of_calcite_expressed_as_carbon_due_to_biological_production", "units": "mol m-2 s-1", - "cell_methods": "area: mean where sea time: mean", + "cell_methods": "area: mean where sea depth: sum where sea time: mean", "cell_measures": "area: areacello", "long_name": "Calcite Production", "comment": "Vertically integrated calcite production", @@ -2233,7 +2233,7 @@ "modeling_realm": "ocnBgChem", "standard_name": "tendency_of_ocean_mole_content_of_elemental_nitrogen_due_to_fixation", "units": "mol m-2 s-1", - "cell_methods": "area: mean where sea time: mean", + "cell_methods": "area: mean where sea depth: sum where sea time: mean", "cell_measures": "area: areacello", "long_name": "Nitrogen Fixation Rate in Ocean", "comment": "Vertically integrated nitrogen fixation", @@ -2251,7 +2251,7 @@ "modeling_realm": "ocnBgChem", "standard_name": "ocean_mass_content_of_particulate_organic_matter_expressed_as_carbon", "units": "kg m-2", - "cell_methods": "area: mean where sea time: mean", + "cell_methods": "area: mean where sea depth: sum where sea time: mean", "cell_measures": "area: areacello", "long_name": "Particulate Organic Carbon Content", "comment": "Vertically integrated POC", @@ -2269,7 +2269,7 @@ "modeling_realm": "ocnBgChem", "standard_name": "net_primary_mole_productivity_of_biomass_expressed_as_carbon_by_phytoplankton", "units": "mol m-2 s-1", - "cell_methods": "area: mean where sea time: mean", + "cell_methods": "area: mean where sea depth: sum where sea time: mean", "cell_measures": "area: areacello", "long_name": "Primary Organic Carbon Production by All Types of Phytoplankton", "comment": "Vertically integrated total primary (organic carbon) production by phytoplankton. This should equal the sum of intpdiat+intpphymisc, but those individual components may be unavailable in some models.", @@ -2287,10 +2287,10 @@ "modeling_realm": "ocnBgChem", "standard_name": "net_primary_mole_productivity_of_biomass_expressed_as_carbon_by_calcareous_phytoplankton", "units": "mol m-2 s-1", - "cell_methods": "area: mean where sea time: mean", + "cell_methods": "area: mean where sea depth: sum where sea time: mean", "cell_measures": "area: areacello", "long_name": "Net Primary Mole Productivity of Carbon by Calcareous Phytoplankton", - "comment": "", + "comment": "'Production of carbon' means the production of biomass expressed as the mass of carbon which it contains. Net primary production is the excess of gross primary production (rate of synthesis of biomass from inorganic precursors) by autotrophs ('producers'), for example, photosynthesis in plants or phytoplankton, over the rate at which the autotrophs themselves respire some of this biomass. 'Productivity' means production per unit area. Phytoplankton are autotrophic prokaryotic or eukaryotic algae that live near the water surface where there is sufficient light to support photosynthesis. 'Calcareous phytoplankton' are phytoplankton that produce calcite. The phrase 'expressed_as' is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. Calcite is a mineral that is a polymorph of calcium carbonate.", "dimensions": "longitude latitude time", "out_name": "intppcalc", "type": "real", @@ -2305,7 +2305,7 @@ "modeling_realm": "ocnBgChem", "standard_name": "net_primary_mole_productivity_of_biomass_expressed_as_carbon_by_diatoms", "units": "mol m-2 s-1", - "cell_methods": "area: mean where sea time: mean", + "cell_methods": "area: mean where sea depth: sum where sea time: mean", "cell_measures": "area: areacello", "long_name": "Net Primary Organic Carbon Production by Diatoms", "comment": "Vertically integrated primary (organic carbon) production by the diatom phytoplankton component alone", @@ -2323,10 +2323,10 @@ "modeling_realm": "ocnBgChem", "standard_name": "net_primary_mole_productivity_of_biomass_expressed_as_carbon_by_diazotrophs", "units": "mol m-2 s-1", - "cell_methods": "area: mean where sea time: mean", + "cell_methods": "area: mean where sea depth: sum where sea time: mean", "cell_measures": "area: areacello", "long_name": "Net Primary Mole Productivity of Carbon by Diazotrophs", - "comment": "", + "comment": "'Production of carbon' means the production of biomass expressed as the mass of carbon which it contains. Net primary production is the excess of gross primary production (rate of synthesis of biomass from inorganic precursors) by autotrophs ('producers'), for example, photosynthesis in plants or phytoplankton, over the rate at which the autotrophs themselves respire some of this biomass. 'Productivity' means production per unit area. In ocean modelling, diazotrophs are phytoplankton of the phylum cyanobacteria distinct from other phytoplankton groups in their ability to fix nitrogen gas in addition to nitrate and ammonium. Phytoplankton are autotrophic prokaryotic or eukaryotic algae that live near the water surface where there is sufficient light to support photosynthesis. The phrase 'expressed_as' is used in the construction A_expressed_as_B, where B is a chemical constituent of A.", "dimensions": "longitude latitude time", "out_name": "intppdiaz", "type": "real", @@ -2341,7 +2341,7 @@ "modeling_realm": "ocnBgChem", "standard_name": "net_primary_mole_productivity_of_biomass_expressed_as_carbon_by_miscellaneous_phytoplankton", "units": "mol m-2 s-1", - "cell_methods": "area: mean where sea time: mean", + "cell_methods": "area: mean where sea depth: sum where sea time: mean", "cell_measures": "area: areacello", "long_name": "Net Primary Organic Carbon Production by Other Phytoplankton", "comment": "Vertically integrated total primary (organic carbon) production by other phytoplankton components alone", @@ -2359,7 +2359,7 @@ "modeling_realm": "ocnBgChem", "standard_name": "net_primary_mole_productivity_of_biomass_expressed_as_carbon_due_to_nitrate_utilization", "units": "mol m-2 s-1", - "cell_methods": "area: mean where sea time: mean", + "cell_methods": "area: mean where sea depth: sum where sea time: mean", "cell_measures": "area: areacello", "long_name": "Primary Organic Carbon Production by Phytoplankton Based on Nitrate Uptake Alone", "comment": "Vertically integrated primary (organic carbon) production by phytoplankton based on nitrate uptake alone", @@ -2377,10 +2377,10 @@ "modeling_realm": "ocnBgChem", "standard_name": "net_primary_mole_productivity_of_biomass_expressed_as_carbon_by_picophytoplankton", "units": "mol m-2 s-1", - "cell_methods": "area: mean where sea time: mean", + "cell_methods": "area: mean where sea depth: sum where sea time: mean", "cell_measures": "area: areacello", "long_name": "Net Primary Mole Productivity of Carbon by Picophytoplankton", - "comment": "", + "comment": "'Production of carbon' means the production of biomass expressed as the mass of carbon which it contains. Net primary production is the excess of gross primary production (rate of synthesis of biomass from inorganic precursors) by autotrophs ('producers'), for example, photosynthesis in plants or phytoplankton, over the rate at which the autotrophs themselves respire some of this biomass. 'Productivity' means production per unit area. Picophytoplankton are phytoplankton of less than 2 micrometers in size. Phytoplankton are autotrophic prokaryotic or eukaryotic algae that live near the water surface where there is sufficient light to support photosynthesis. The phrase 'expressed_as' is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A.", "dimensions": "longitude latitude time", "out_name": "intpppico", "type": "real", @@ -2398,7 +2398,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Iron limitation of Calcareous Phytoplankton", - "comment": "", + "comment": "'Calcareous phytoplankton' are phytoplankton that produce calcite. Calcite is a mineral that is a polymorph of calcium carbonate. The chemical formula of calcite is CaCO3. Phytoplankton are algae that grow where there is sufficient light to support photosynthesis. 'Iron growth limitation' means the ratio of the growth rate of a species population in the environment (where there is a finite availability of iron) to the theoretical growth rate if there were no such limit on iron availability.", "dimensions": "longitude latitude time", "out_name": "limfecalc", "type": "real", @@ -2416,7 +2416,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Iron limitation of Diatoms", - "comment": "", + "comment": "Diatoms are phytoplankton with an external skeleton made of silica. Phytoplankton are algae that grow where there is sufficient light to support photosynthesis. 'Iron growth limitation' means the ratio of the growth rate of a species population in the environment (where there is a finite availability of iron) to the theoretical growth rate if there were no such limit on iron availability.", "dimensions": "longitude latitude time", "out_name": "limfediat", "type": "real", @@ -2434,7 +2434,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Iron limitation of Diazotrophs", - "comment": "", + "comment": "In ocean modelling, diazotrophs are phytoplankton of the phylum cyanobacteria distinct from other phytoplankton groups in their ability to fix nitrogen gas in addition to nitrate and ammonium. Phytoplankton are algae that grow where there is sufficient light to support photosynthesis. 'Iron growth limitation' means the ratio of the growth rate of a species population in the environment (where there is a finite availability of iron) to the theoretical growth rate if there were no such limit on iron availability.", "dimensions": "longitude latitude time", "out_name": "limfediaz", "type": "real", @@ -2452,7 +2452,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Iron Limitation of Other Phytoplankton", - "comment": "", + "comment": "Phytoplankton are algae that grow where there is sufficient light to support photosynthesis. 'Miscellaneous phytoplankton' are all those phytoplankton that are not diatoms, diazotrophs, calcareous phytoplankton, picophytoplankton or other separately named components of the phytoplankton population. 'Iron growth limitation' means the ratio of the growth rate of a species population in the environment (where there is a finite availability of iron) to the theoretical growth rate if there were no such limit on iron availability.", "dimensions": "longitude latitude time", "out_name": "limfemisc", "type": "real", @@ -2470,7 +2470,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Iron limitation of Picophytoplankton", - "comment": "", + "comment": "Picophytoplankton are phytoplankton of less than 2 micrometers in size. Phytoplankton are algae that grow where there is sufficient light to support photosynthesis. 'Iron growth limitation' means the ratio of the growth rate of a species population in the environment (where there is a finite availability of iron) to the theoretical growth rate if there were no such limit on iron availability.", "dimensions": "longitude latitude time", "out_name": "limfepico", "type": "real", @@ -2488,7 +2488,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Irradiance limitation of Calcareous Phytoplankton", - "comment": "", + "comment": "'Calcareous phytoplankton' are phytoplankton that produce calcite. Calcite is a mineral that is a polymorph of calcium carbonate. The chemical formula of calcite is CaCO3. Phytoplankton are algae that grow where there is sufficient light to support photosynthesis. The specification of a physical process by the phrase 'due_to_' process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. 'Irradiance' means the power per unit area (called radiative flux in other standard names), the area being normal to the direction of flow of the radiant energy. Solar irradiance is essential to the photosynthesis reaction and its presence promotes the growth of phytoplankton populations.", "dimensions": "longitude latitude time", "out_name": "limirrcalc", "type": "real", @@ -2506,7 +2506,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Irradiance limitation of Diatoms", - "comment": "", + "comment": "Diatoms are phytoplankton with an external skeleton made of silica. Phytoplankton are algae that grow where there is sufficient light to support photosynthesis. The specification of a physical process by the phrase 'due_to_' process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. 'Irradiance' means the power per unit area (called radiative flux in other standard names), the area being normal to the direction of flow of the radiant energy. Solar irradiance is essential to the photosynthesis reaction and its presence promotes the growth of phytoplankton populations. 'Growth limitation due to solar irradiance' means the ratio of the growth rate of a species population in the environment (where the amount of sunlight reaching a location may be limited) to the theoretical growth rate if there were no such limit on solar irradiance.", "dimensions": "longitude latitude time", "out_name": "limirrdiat", "type": "real", @@ -2524,7 +2524,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Irradiance limitation of Diazotrophs", - "comment": "", + "comment": "In ocean modelling, diazotrophs are phytoplankton of the phylum cyanobacteria distinct from other phytoplankton groups in their ability to fix nitrogen gas in addition to nitrate and ammonium. Phytoplankton are algae that grow where there is sufficient light to support photosynthesis. The specification of a physical process by the phrase 'due_to_' process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. 'Irradiance' means the power per unit area (called radiative flux in other standard names), the area being normal to the direction of flow of the radiant energy. Solar irradiance is essential to the photosynthesis reaction and its presence promotes the growth of phytoplankton populations.", "dimensions": "longitude latitude time", "out_name": "limirrdiaz", "type": "real", @@ -2542,7 +2542,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Irradiance Limitation of Other Phytoplankton", - "comment": "", + "comment": "Phytoplankton are algae that grow where there is sufficient light to support photosynthesis. 'Miscellaneous phytoplankton' are all those phytoplankton that are not diatoms, diazotrophs, calcareous phytoplankton, picophytoplankton or other separately named components of the phytoplankton population. The specification of a physical process by the phrase 'due_to_' process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. 'Irradiance' means the power per unit area (called radiative flux in other standard names), the area being normal to the direction of flow of the radiant energy. Solar irradiance is essential to the photosynthesis reaction and its presence promotes the growth of phytoplankton populations.", "dimensions": "longitude latitude time", "out_name": "limirrmisc", "type": "real", @@ -2560,7 +2560,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Irradiance limitation of Picophytoplankton", - "comment": "", + "comment": "Picophytoplankton are phytoplankton of less than 2 micrometers in size. Phytoplankton are algae that grow where there is sufficient light to support photosynthesis. The specification of a physical process by the phrase 'due_to_' process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. 'Irradiance' means the power per unit area (called radiative flux in other standard names), the area being normal to the direction of flow of the radiant energy. Solar irradiance is essential to the photosynthesis reaction and its presence promotes the growth of phytoplankton populations. 'Growth limitation due to solar irradiance' means the ratio of the growth rate of a species population in the environment (where the amount of sunlight reaching a location may be limited) to the theoretical growth rate if there were no such limit on solar irradiance.", "dimensions": "longitude latitude time", "out_name": "limirrpico", "type": "real", @@ -2578,7 +2578,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Nitrogen limitation of Calcareous Phytoplankton", - "comment": "", + "comment": "'Calcareous phytoplankton' are phytoplankton that produce calcite. Calcite is a mineral that is a polymorph of calcium carbonate. The chemical formula of calcite is CaCO3. Phytoplankton are algae that grow where there is sufficient light to support photosynthesis. 'Nitrogen growth limitation' means the ratio of the growth rate of a species population in the environment (where there is a finite availability of nitrogen) to the theoretical growth rate if there were no such limit on nitrogen availability.", "dimensions": "longitude latitude time", "out_name": "limncalc", "type": "real", @@ -2596,7 +2596,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Nitrogen limitation of Diatoms", - "comment": "", + "comment": "Diatoms are phytoplankton with an external skeleton made of silica. Phytoplankton are algae that grow where there is sufficient light to support photosynthesis. 'Nitrogen growth limitation' means the ratio of the growth rate of a species population in the environment (where there is a finite availability of nitrogen) to the theoretical growth rate if there were no such limit on nitrogen availability.", "dimensions": "longitude latitude time", "out_name": "limndiat", "type": "real", @@ -2614,7 +2614,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Nitrogen limitation of Diazotrophs", - "comment": "", + "comment": "In ocean modelling, diazotrophs are phytoplankton of the phylum cyanobacteria distinct from other phytoplankton groups in their ability to fix nitrogen gas in addition to nitrate and ammonium. Phytoplankton are algae that grow where there is sufficient light to support photosynthesis. 'Nitrogen growth limitation' means the ratio of the growth rate of a species population in the environment (where there is a finite availability of nitrogen) to the theoretical growth rate if there were no such limit on nitrogen availability.", "dimensions": "longitude latitude time", "out_name": "limndiaz", "type": "real", @@ -2632,7 +2632,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Nitrogen Limitation of Other Phytoplankton", - "comment": "", + "comment": "Phytoplankton are algae that grow where there is sufficient light to support photosynthesis. 'Miscellaneous phytoplankton' are all those phytoplankton that are not diatoms, diazotrophs, calcareous phytoplankton, picophytoplankton or other separately named components of the phytoplankton population. 'Nitrogen growth limitation' means the ratio of the growth rate of a species population in the environment (where there is a finite availability of nitrogen) to the theoretical growth rate if there were no such limit on nitrogen availability.", "dimensions": "longitude latitude time", "out_name": "limnmisc", "type": "real", @@ -2650,7 +2650,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Nitrogen limitation of Picophytoplankton", - "comment": "", + "comment": "Picophytoplankton are phytoplankton of less than 2 micrometers in size. Phytoplankton are algae that grow where there is sufficient light to support photosynthesis. 'Nitrogen growth limitation' means the ratio of the growth rate of a species population in the environment (where there is a finite availability of nitrogen) to the theoretical growth rate if there were no such limit on nitrogen availability.", "dimensions": "longitude latitude time", "out_name": "limnpico", "type": "real", @@ -2704,7 +2704,7 @@ "cell_methods": "time: mean", "cell_measures": "", "long_name": "Sea Water Transport", - "comment": "", + "comment": "Transport across_line means that which crosses a particular line on the Earth's surface; formally this means the integral along the line of the normal component of the transport.", "dimensions": "oline time", "out_name": "mfo", "type": "real", @@ -2776,7 +2776,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Square of Ocean Mixed Layer Thickness Defined by Sigma T", - "comment": "", + "comment": "The ocean mixed layer is the upper part of the ocean, regarded as being well-mixed. The base of the mixed layer defined by temperature, sigma, sigma_theta or sigma_t is the level at which the quantity indicated differs from its surface value by a certain amount. 'Thickness' means the vertical extent of a layer. 'square_of_X' means X*X.", "dimensions": "longitude latitude time", "out_name": "mlotstsq", "type": "real", @@ -2990,10 +2990,10 @@ "standard_name": "mole_concentration_of_ammonium_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Dissolved Ammonium Concentration", - "comment": "", - "dimensions": "longitude latitude olevel time", + "comment": "Mole concentration means moles (amount of substance) per unit volume and is used in the construction mole_concentration_of_X_in_Y, where X is a material constituent of Y.", + "dimensions": "longitude latitude time depth0m", "out_name": "nh4", "type": "real", "positive": "", @@ -3008,10 +3008,10 @@ "standard_name": "mole_concentration_of_nitrate_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Dissolved Nitrate Concentration", - "comment": "", - "dimensions": "longitude latitude olevel time", + "comment": "Mole concentration means moles (amount of substance) per unit volume and is used in the construction mole_concentration_of_X_in_Y, where X is a material constituent of Y.", + "dimensions": "longitude latitude time depth0m", "out_name": "no3", "type": "real", "positive": "", @@ -3028,8 +3028,8 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Surface Dissolved Nitrate Concentration", - "comment": "", - "dimensions": "longitude latitude time depth0m", + "comment": "Mole concentration means moles (amount of substance) per unit volume and is used in the construction mole_concentration_of_X_in_Y, where X is a material constituent of Y.", + "dimensions": "longitude latitude time", "out_name": "no3os", "type": "real", "positive": "", @@ -3044,10 +3044,10 @@ "standard_name": "mole_concentration_of_dissolved_molecular_oxygen_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Dissolved Oxygen Concentration", - "comment": "", - "dimensions": "longitude latitude olevel time", + "comment": "'Mole concentration' means number of moles per unit volume, also called'molarity', and is used in the construction mole_concentration_of_X_in_Y, whereX is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'.", + "dimensions": "longitude latitude time depth0m", "out_name": "o2", "type": "real", "positive": "", @@ -3064,7 +3064,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Oxygen Minimum Concentration", - "comment": "", + "comment": "'Mole concentration' means number of moles per unit volume, also called 'molarity', and is used in the construction mole_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The concentration of any chemical species, whether particulate or dissolved, may vary with depth in the ocean. A depth profile may go through one or more local minima in concentration. The mole_concentration_of_molecular_oxygen_in_sea_water_at_shallowest_local_minimum_in_vertical_profile is the mole concentration of oxygen at the local minimum in the concentration profile that occurs closest to the sea surface.", "dimensions": "longitude latitude time", "out_name": "o2min", "type": "real", @@ -3082,8 +3082,8 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Surface Dissolved Oxygen Concentration", - "comment": "", - "dimensions": "longitude latitude time depth0m", + "comment": "'Mole concentration' means number of moles per unit volume, also called'molarity', and is used in the construction mole_concentration_of_X_in_Y, whereX is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'.", + "dimensions": "longitude latitude time", "out_name": "o2os", "type": "real", "positive": "", @@ -3098,10 +3098,10 @@ "standard_name": "mole_concentration_of_dissolved_molecular_oxygen_in_sea_water_at_saturation", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Dissolved Oxygen Concentration at Saturation", - "comment": "", - "dimensions": "longitude latitude olevel time", + "comment": "'Mole concentration at saturation' means the mole concentration in a saturated solution. Mole concentration means number of moles per unit volume, also called 'molarity', and is used in the construction 'mole_concentration_of_X_in_Y', where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'.", + "dimensions": "longitude latitude time depth0m", "out_name": "o2sat", "type": "real", "positive": "", @@ -3118,8 +3118,8 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Surface Dissolved Oxygen Concentration at Saturation", - "comment": "", - "dimensions": "longitude latitude time depth0m", + "comment": "'Mole concentration at saturation' means the mole concentration in a saturated solution. Mole concentration means number of moles per unit volume, also called 'molarity', and is used in the construction 'mole_concentration_of_X_in_Y', where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'.", + "dimensions": "longitude latitude time", "out_name": "o2satos", "type": "real", "positive": "", @@ -3136,7 +3136,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Square of Brunt Vaisala Frequency in Sea Water", - "comment": "", + "comment": "The phrase 'square_of_X' means X*X. Frequency is the number of oscillations of a wave per unit time. Brunt-Vaisala frequency is also sometimes called 'buoyancy frequency' and is a measure of the vertical stratification of the medium.", "dimensions": "longitude latitude olevel time", "out_name": "obvfsq", "type": "real", @@ -3164,24 +3164,6 @@ "ok_min_mean_abs": "", "ok_max_mean_abs": "" }, - "pbfe": { - "frequency": "mon", - "modeling_realm": "ocnBgChem", - "standard_name": "tendency_of_mole_concentration_of_iron_in_sea_water_due_to_biological_production", - "units": "mol m-3 s-1", - "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello", - "long_name": "Biogenic Iron Production", - "comment": "", - "dimensions": "longitude latitude time depth0m", - "out_name": "pbfe", - "type": "real", - "positive": "", - "valid_min": "", - "valid_max": "", - "ok_min_mean_abs": "", - "ok_max_mean_abs": "" - }, "pbo": { "frequency": "mon", "modeling_realm": "ocean", @@ -3190,7 +3172,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Sea Water Pressure at Sea floor", - "comment": "", + "comment": "'Sea water pressure' is the pressure that exists in the medium of sea water. It includes the pressure due to overlying sea water, sea ice, air and any other medium that may be present.", "dimensions": "longitude latitude time", "out_name": "pbo", "type": "real", @@ -3200,34 +3182,16 @@ "ok_min_mean_abs": "", "ok_max_mean_abs": "" }, - "pbsi": { - "frequency": "mon", - "modeling_realm": "ocnBgChem", - "standard_name": "tendency_of_mole_concentration_of_silicon_in_sea_water_due_to_biological_production", - "units": "mol m-3 s-1", - "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello", - "long_name": "Biogenic Silica Production", - "comment": "", - "dimensions": "longitude latitude time depth0m", - "out_name": "pbsi", - "type": "real", - "positive": "", - "valid_min": "", - "valid_max": "", - "ok_min_mean_abs": "", - "ok_max_mean_abs": "" - }, "ph": { "frequency": "mon", "modeling_realm": "ocnBgChem", "standard_name": "sea_water_ph_reported_on_total_scale", "units": "1", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "pH", "comment": "negative log of hydrogen ion concentration with the concentration expressed as mol H kg-1.", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "ph", "type": "real", "positive": "", @@ -3242,10 +3206,10 @@ "standard_name": "sea_water_ph_abiotic_analogue_reported_on_total_scale", "units": "1", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Abiotic pH", "comment": "negative log10 of hydrogen ion concentration with the concentration expressed as mol H kg-1 (abiotic component)..", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "phabio", "type": "real", "positive": "", @@ -3263,7 +3227,7 @@ "cell_measures": "area: areacello", "long_name": "Surface Abiotic pH", "comment": "negative log10 of hydrogen ion concentration with the concentration expressed as mol H kg-1.", - "dimensions": "longitude latitude time depth0m", + "dimensions": "longitude latitude time", "out_name": "phabioos", "type": "real", "positive": "", @@ -3278,10 +3242,10 @@ "standard_name": "sea_water_ph_natural_analogue_reported_on_total_scale", "units": "1", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Natural pH", "comment": "negative log10 of hydrogen ion concentration with the concentration expressed as mol H kg-1.", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "phnat", "type": "real", "positive": "", @@ -3299,7 +3263,7 @@ "cell_measures": "area: areacello", "long_name": "Surface Natural pH", "comment": "negative log10 of hydrogen ion concentration with the concentration expressed as mol H kg-1.", - "dimensions": "longitude latitude time depth0m", + "dimensions": "longitude latitude time", "out_name": "phnatos", "type": "real", "positive": "", @@ -3314,10 +3278,10 @@ "standard_name": "mole_concentration_of_phytoplankton_expressed_as_carbon_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Phytoplankton Carbon Concentration", "comment": "sum of phytoplankton carbon component concentrations. In most (all?) cases this is the sum of phycdiat and phycmisc (i.e., 'Diatom Carbon Concentration' and 'Non-Diatom Phytoplankton Carbon Concentration'", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "phyc", "type": "real", "positive": "", @@ -3332,10 +3296,10 @@ "standard_name": "mole_concentration_of_calcareous_phytoplankton_expressed_as_carbon_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Mole Concentration of Calcareous Phytoplankton expressed as Carbon in sea water", "comment": "carbon concentration from calcareous (calcite-producing) phytoplankton component alone", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "phycalc", "type": "real", "positive": "", @@ -3353,7 +3317,7 @@ "cell_measures": "area: areacello", "long_name": "Surface Phytoplankton Carbon Concentration", "comment": "sum of phytoplankton organic carbon component concentrations at the sea surface", - "dimensions": "longitude latitude time depth0m", + "dimensions": "longitude latitude time", "out_name": "phycos", "type": "real", "positive": "", @@ -3368,10 +3332,10 @@ "standard_name": "mole_concentration_of_diatoms_expressed_as_carbon_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Mole Concentration of Diatoms expressed as Carbon in sea water", "comment": "carbon from the diatom phytoplankton component concentration alone", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "phydiat", "type": "real", "positive": "", @@ -3386,10 +3350,10 @@ "standard_name": "mole_concentration_of_diazotrophs_expressed_as_carbon_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Mole Concentration of Diazotrophs Expressed as Carbon in sea water", "comment": "carbon concentration from the diazotrophic phytoplankton component alone", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "phydiaz", "type": "real", "positive": "", @@ -3404,10 +3368,10 @@ "standard_name": "mole_concentration_of_phytoplankton_expressed_as_iron_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Mole Concentration of Total Phytoplankton expressed as Iron in sea water", "comment": "sum of phytoplankton iron component concentrations", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "phyfe", "type": "real", "positive": "", @@ -3425,7 +3389,7 @@ "cell_measures": "area: areacello", "long_name": "Surface Mole Concentration of Total Phytoplankton expressed as Iron in Sea Water", "comment": "sum of phytoplankton iron component concentrations", - "dimensions": "longitude latitude time depth0m", + "dimensions": "longitude latitude time", "out_name": "phyfeos", "type": "real", "positive": "", @@ -3440,10 +3404,10 @@ "standard_name": "mole_concentration_of_miscellaneous_phytoplankton_expressed_as_carbon_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Mole Concentration of Miscellaneous Phytoplankton expressed as Carbon in sea water", "comment": "carbon concentration from additional phytoplankton component alone", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "phymisc", "type": "real", "positive": "", @@ -3458,10 +3422,10 @@ "standard_name": "mole_concentration_of_phytoplankton_expressed_as_nitrogen_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Mole Concentration of Total Phytoplankton expressed as Nitrogen in sea water", "comment": "sum of phytoplankton nitrogen component concentrations", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "phyn", "type": "real", "positive": "", @@ -3479,7 +3443,7 @@ "cell_measures": "area: areacello", "long_name": "Surface Mole Concentration of Phytoplankton Nitrogen in sea water", "comment": "sum of phytoplankton nitrogen component concentrations", - "dimensions": "longitude latitude time depth0m", + "dimensions": "longitude latitude time", "out_name": "phynos", "type": "real", "positive": "", @@ -3494,10 +3458,10 @@ "standard_name": "mole_concentration_of_phytoplankton_expressed_as_phosphorus_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Mole Concentration of Total Phytoplankton expressed as Phosphorus in sea water", "comment": "sum of phytoplankton phosphorus components", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "phyp", "type": "real", "positive": "", @@ -3512,10 +3476,10 @@ "standard_name": "mole_concentration_of_picophytoplankton_expressed_as_carbon_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Mole Concentration of Picophytoplankton expressed as Carbon in sea water", "comment": "carbon concentration from the picophytoplankton (<2 um) component alone", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "phypico", "type": "real", "positive": "", @@ -3533,7 +3497,7 @@ "cell_measures": "area: areacello", "long_name": "Surface Mole Concentration of Total Phytoplankton expressed as Phosphorus in sea water", "comment": "sum of phytoplankton phosphorus components", - "dimensions": "longitude latitude time depth0m", + "dimensions": "longitude latitude time", "out_name": "phypos", "type": "real", "positive": "", @@ -3548,10 +3512,10 @@ "standard_name": "mole_concentration_of_phytoplankton_expressed_as_silicon_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Mole Concentration of Total Phytoplankton expressed as Silicon in sea water", "comment": "sum of phytoplankton silica component concentrations", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "physi", "type": "real", "positive": "", @@ -3569,7 +3533,7 @@ "cell_measures": "area: areacello", "long_name": "Surface Mole Concentration of Total Phytoplankton expressed as Silicon in sea water", "comment": "sum of phytoplankton silica component concentrations", - "dimensions": "longitude latitude time depth0m", + "dimensions": "longitude latitude time", "out_name": "physios", "type": "real", "positive": "", @@ -3578,34 +3542,16 @@ "ok_min_mean_abs": "", "ok_max_mean_abs": "" }, - "pnitrate": { - "frequency": "mon", - "modeling_realm": "ocnBgChem", - "standard_name": "tendency_of_mole_concentration_of_particulate_organic_matter_expressed_as_carbon_in_sea_water_due_to_nitrate_utilization", - "units": "mol m-3 s-1", - "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello", - "long_name": "Primary Carbon Production by Phytoplankton due to Nitrate Uptake Alone", - "comment": "Primary (organic carbon) production by phytoplankton due to nitrate uptake alone", - "dimensions": "longitude latitude time depth0m", - "out_name": "pnitrate", - "type": "real", - "positive": "", - "valid_min": "", - "valid_max": "", - "ok_min_mean_abs": "", - "ok_max_mean_abs": "" - }, "po4": { "frequency": "mon", "modeling_realm": "ocnBgChem", "standard_name": "mole_concentration_of_dissolved_inorganic_phosphorus_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Total Dissolved Inorganic Phosphorus Concentration", - "comment": "", - "dimensions": "longitude latitude olevel time", + "comment": "Mole concentration means number of moles per unit volume, also called 'molarity', and is used in the construction 'mole_concentration_of_X_in_Y', where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. 'Dissolved inorganic phosphorus' means the sum of all inorganic phosphorus in solution (including phosphate, hydrogen phosphate, dihydrogen phosphate, and phosphoric acid).", + "dimensions": "longitude latitude time depth0m", "out_name": "po4", "type": "real", "positive": "", @@ -3620,10 +3566,10 @@ "standard_name": "mole_concentration_of_particulate_organic_matter_expressed_as_nitrogen_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Mole Concentration of Particulate Organic Matter expressed as Nitrogen in sea water", "comment": "sum of particulate organic nitrogen component concentrations", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "pon", "type": "real", "positive": "", @@ -3641,7 +3587,7 @@ "cell_measures": "area: areacello", "long_name": "Surface Mole Concentration of Particulate Organic Matter expressed as Nitrogen in sea water", "comment": "sum of particulate organic nitrogen component concentrations", - "dimensions": "longitude latitude time depth0m", + "dimensions": "longitude latitude time", "out_name": "ponos", "type": "real", "positive": "", @@ -3656,10 +3602,10 @@ "standard_name": "mole_concentration_of_particulate_organic_matter_expressed_as_phosphorus_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Mole Concentration of Particulate Organic Matter expressed as Phosphorus in sea water", "comment": "sum of particulate organic phosphorus component concentrations", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "pop", "type": "real", "positive": "", @@ -3677,7 +3623,7 @@ "cell_measures": "area: areacello", "long_name": "Surface Mole Concentration of Particulate Organic Matter expressed as Phosphorus in sea water", "comment": "sum of particulate organic phosphorus component concentrations", - "dimensions": "longitude latitude time depth0m", + "dimensions": "longitude latitude time", "out_name": "popos", "type": "real", "positive": "", @@ -3692,10 +3638,10 @@ "standard_name": "tendency_of_mole_concentration_of_particulate_organic_matter_expressed_as_carbon_in_sea_water_due_to_net_primary_production", "units": "mol m-3 s-1", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Primary Carbon Production by Total Phytoplankton", "comment": "total primary (organic carbon) production by phytoplankton", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "pp", "type": "real", "positive": "", @@ -3712,7 +3658,7 @@ "cell_methods": "area: mean where ice_free_sea over sea time: mean", "cell_measures": "area: areacello", "long_name": "Rainfall Flux where Ice Free Ocean over Sea", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "prra", "type": "real", @@ -3748,7 +3694,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Sea Water Pressure at Sea Water Surface", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Sea water pressure' is the pressure that exists in the medium of sea water. It includes the pressure due to overlying sea water, sea ice, air and any other medium that may be present.", "dimensions": "longitude latitude time", "out_name": "pso", "type": "real", @@ -3784,7 +3730,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Downwelling Shortwave Radiation in Sea Water", - "comment": "", + "comment": "Downwelling radiation is radiation from above. It does not mean 'net downward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. 'shortwave' means shortwave radiation.", "dimensions": "longitude latitude olevel time", "out_name": "rsdo", "type": "real", @@ -3820,7 +3766,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Moles Per Unit Mass of SF6 in sea water", - "comment": "", + "comment": "Mole concentration means number of moles per unit volume, also called 'molarity', and is used in the construction 'mole_concentration_of_X_in_Y', where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula of sulfur hexafluoride is SF6.", "dimensions": "longitude latitude olevel time", "out_name": "sf6", "type": "real", @@ -3872,10 +3818,10 @@ "standard_name": "mole_concentration_of_dissolved_inorganic_silicon_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Total Dissolved Inorganic Silicon Concentration", - "comment": "", - "dimensions": "longitude latitude olevel time", + "comment": "Mole concentration means number of moles per unit volume, also called 'molarity', and is used in the construction 'mole_concentration_of_X_in_Y', where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. 'Dissolved inorganic silicon' means the sum of all inorganic silicon in solution (including silicic acid and its first dissociated anion SiO(OH)3-).", + "dimensions": "longitude latitude time depth0m", "out_name": "si", "type": "real", "positive": "", @@ -3892,8 +3838,8 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Surface Total Dissolved Inorganic Silicon Concentration", - "comment": "", - "dimensions": "longitude latitude time depth0m", + "comment": "Mole concentration means number of moles per unit volume, also called 'molarity', and is used in the construction 'mole_concentration_of_X_in_Y', where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. 'Dissolved inorganic silicon' means the sum of all inorganic silicon in solution (including silicic acid and its first dissociated anion SiO(OH)3-).", + "dimensions": "longitude latitude time", "out_name": "sios", "type": "real", "positive": "", @@ -3946,7 +3892,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Sea Water Salinity", - "comment": "", + "comment": "Sea water salinity is the salt content of sea water, often on the Practical Salinity Scale of 1978. However, the unqualified term 'salinity' is generic and does not necessarily imply any particular method of calculation. The units of salinity are dimensionless and the units attribute should normally be given as 1e-3 or 0.001 i.e. parts per thousand. There are standard names for the more precisely defined salinity quantities: sea_water_knudsen_salinity, S_K (used for salinity observations between 1901 and 1966), sea_water_cox_salinity, S_C (used for salinity observations between 1967 and 1977), sea_water_practical_salinity, S_P (used for salinity observations from 1978 to the present day), sea_water_absolute_salinity, S_A, sea_water_preformed_salinity, S_*, and sea_water_reference_salinity. Practical Salinity is reported on the Practical Salinity Scale of 1978 (PSS-78), and is usually based on the electrical conductivity of sea water in observations since the 1960s.", "dimensions": "longitude latitude olevel time", "out_name": "so", "type": "real", @@ -3982,7 +3928,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "", "long_name": "Global Mean Sea Water Salinity", - "comment": "", + "comment": "Sea water salinity is the salt content of sea water, often on the Practical Salinity Scale of 1978. However, the unqualified term 'salinity' is generic and does not necessarily imply any particular method of calculation. The units of salinity are dimensionless and the units attribute should normally be given as 1e-3 or 0.001 i.e. parts per thousand. There are standard names for the more precisely defined salinity quantities: sea_water_knudsen_salinity, S_K (used for salinity observations between 1901 and 1966), sea_water_cox_salinity, S_C (used for salinity observations between 1967 and 1977), sea_water_practical_salinity, S_P (used for salinity observations from 1978 to the present day), sea_water_absolute_salinity, S_A, sea_water_preformed_salinity, S_*, and sea_water_reference_salinity. Practical Salinity is reported on the Practical Salinity Scale of 1978 (PSS-78), and is usually based on the electrical conductivity of sea water in observations since the 1960s.", "dimensions": "time", "out_name": "soga", "type": "real", @@ -4000,7 +3946,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Sea Surface Salinity", - "comment": "", + "comment": "Sea surface salinity is the salt content of sea water close to the sea surface, often on the Practical Salinity Scale of 1978. However, the unqualified term 'salinity' is generic and does not necessarily imply any particular method of calculation. The units of salinity are dimensionless and the units attribute should normally be given as 1e-3 or 0.001 i.e. parts per thousand. Sea surface salinity is often abbreviated as 'SSS'. For the salinity of sea water at a particular depth or layer, a data variable of 'sea_water_salinity' or one of the more precisely defined salinities should be used with a vertical coordinate axis.", "dimensions": "longitude latitude time", "out_name": "sos", "type": "real", @@ -4018,7 +3964,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "", "long_name": "Global Average Sea Surface Salinity", - "comment": "", + "comment": "Sea surface salinity is the salt content of sea water close to the sea surface, often on the Practical Salinity Scale of 1978. However, the unqualified term 'salinity' is generic and does not necessarily imply any particular method of calculation. The units of salinity are dimensionless and the units attribute should normally be given as 1e-3 or 0.001 i.e. parts per thousand. Sea surface salinity is often abbreviated as 'SSS'. For the salinity of sea water at a particular depth or layer, a data variable of 'sea_water_salinity' or one of the more precisely defined salinities should be used with a vertical coordinate axis.", "dimensions": "time", "out_name": "sosga", "type": "real", @@ -4054,7 +4000,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Surface Aqueous Partial Pressure of CO2", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. The partial pressure of a dissolved gas in sea water is the partial pressure in air with which it would be in equilibrium. The partial pressure of a gaseous constituent of air is the pressure which it alone would exert with unchanged temperature and number of moles per unit volume. The chemical formula for carbon dioxide is CO2.", "dimensions": "longitude latitude time depth0m", "out_name": "spco2", "type": "real", @@ -4067,12 +4013,12 @@ "spco2abio": { "frequency": "mon", "modeling_realm": "ocnBgChem", - "standard_name": "surface_partial_pressure_of_carbon_dioxide_abiotic_analogue_in_sea_water", + "standard_name": "surface_carbon_dioxide_abiotic_analogue_partial_pressure_difference_between_sea_water_and_air", "units": "Pa", "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Abiotic Surface Aqueous Partial Pressure of CO2", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. The chemical formula for carbon dioxide is CO2. In ocean biogeochemistry models, an 'abiotic analogue' is used to simulate the effect on a modelled variable when biological effects on ocean carbon concentration and alkalinity are ignored. The partial pressure of a gaseous constituent of air is the pressure which it alone would exert with unchanged temperature and number of moles per unit volume. The partial pressure of a dissolved gas in sea water is the partial pressure in air with which it would be in equilibrium. The partial pressure difference between sea water and air is positive when the partial pressure of the dissolved gas in sea water is greater than the partial pressure in air.", "dimensions": "longitude latitude time depth0m", "out_name": "spco2abio", "type": "real", @@ -4085,12 +4031,12 @@ "spco2nat": { "frequency": "mon", "modeling_realm": "ocnBgChem", - "standard_name": "surface_partial_pressure_of_carbon_dioxide_natural_analogue_in_sea_water", + "standard_name": "surface_carbon_dioxide_natural_analogue_partial_pressure_difference_between_sea_water_and_air", "units": "Pa", "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "Natural Surface Aqueous Partial Pressure of CO2", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. The chemical formula for carbon dioxide is CO2. In ocean biogeochemistry models, a 'natural analogue' is used to simulate the effect on a modelled variable of imposing preindustrial atmospheric carbon dioxide concentrations, even when the model as a whole may be subjected to varying forcings. The partial pressure of a gaseous constituent of air is the pressure which it alone would exert with unchanged temperature and number of moles per unit volume. The partial pressure of a dissolved gas in sea water is the partial pressure in air with which it would be in equilibrium. The partial pressure difference between sea water and air is positive when the partial pressure of the dissolved gas in sea water is greater than the partial pressure in air.", "dimensions": "longitude latitude time depth0m", "out_name": "spco2nat", "type": "real", @@ -4106,10 +4052,10 @@ "standard_name": "sea_water_alkalinity_expressed_as_mole_equivalent", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Total Alkalinity", "comment": "total alkalinity equivalent concentration (including carbonate, nitrogen, silicate, and borate components)", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "talk", "type": "real", "positive": "", @@ -4124,10 +4070,10 @@ "standard_name": "sea_water_alkalinity_natural_analogue_expressed_as_mole_equivalent", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Natural Total Alkalinity", "comment": "total alkalinity equivalent concentration (including carbonate, borate, phosphorus, silicon, and nitrogen components) at preindustrial atmospheric xCO2", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "talknat", "type": "real", "positive": "", @@ -4145,7 +4091,7 @@ "cell_measures": "area: areacello", "long_name": "Surface Natural Total Alkalinity", "comment": "total alkalinity equivalent concentration (including carbonate, borate, phosphorus, silicon, and nitrogen components) at preindustrial atmospheric xCO2", - "dimensions": "longitude latitude time depth0m", + "dimensions": "longitude latitude time", "out_name": "talknatos", "type": "real", "positive": "", @@ -4270,7 +4216,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Ocean Model Cell Thickness", - "comment": "", + "comment": "'Thickness' means the vertical extent of a layer. 'Cell' refers to a model grid-cell.", "dimensions": "longitude latitude olevel time", "out_name": "thkcello", "type": "real", @@ -4425,7 +4371,7 @@ "ok_max_mean_abs": "" }, "volcello": { - "frequency": "fx", + "frequency": "mon", "modeling_realm": "ocean", "standard_name": "ocean_volume", "units": "m3", @@ -4648,7 +4594,7 @@ "cell_methods": "time: mean", "cell_measures": "--OPT", "long_name": "Sea Water Z Velocity", - "comment": "", + "comment": "A velocity is a vector quantity. 'Upward' indicates a vector component which is positive when directed upward (negative downward).", "dimensions": "longitude latitude olevel time", "out_name": "wo", "type": "real", @@ -4700,10 +4646,10 @@ "standard_name": "mole_concentration_of_mesozooplankton_expressed_as_carbon_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Mole Concentration of Mesozooplankton expressed as Carbon in sea water", "comment": "carbon concentration from mesozooplankton (20-200 um) component alone", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "zmeso", "type": "real", "positive": "", @@ -4718,10 +4664,10 @@ "standard_name": "mole_concentration_of_microzooplankton_expressed_as_carbon_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Mole Concentration of Microzooplankton expressed as Carbon in sea water", "comment": "carbon concentration from the microzooplankton (<20 um) component alone", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "zmicro", "type": "real", "positive": "", @@ -4736,10 +4682,10 @@ "standard_name": "mole_concentration_of_miscellaneous_zooplankton_expressed_as_carbon_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Mole Concetration of Other Zooplankton expressed as Carbon in sea water", "comment": "carbon from additional zooplankton component concentrations alone (e.g. Micro, meso). Since the models all have different numbers of components, this variable has been included to provide a check for intercomparison between models since some phytoplankton groups are supersets.", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "zmisc", "type": "real", "positive": "", @@ -4772,10 +4718,10 @@ "standard_name": "mole_concentration_of_zooplankton_expressed_as_carbon_in_sea_water", "units": "mol m-3", "cell_methods": "area: mean where sea time: mean", - "cell_measures": "area: areacello volume: volcello", + "cell_measures": "area: areacello", "long_name": "Zooplankton Carbon Concentration", "comment": "sum of zooplankton carbon component concentrations", - "dimensions": "longitude latitude olevel time", + "dimensions": "longitude latitude time depth0m", "out_name": "zooc", "type": "real", "positive": "", diff --git a/Tables/CMIP6_Oyr.json b/Tables/CMIP6_Oyr.json index 038ef686..ddf3c4d5 100644 --- a/Tables/CMIP6_Oyr.json +++ b/Tables/CMIP6_Oyr.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table Oyr", "realm": "ocnBgChem", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -166,7 +166,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Mole Concentration of CFC-11 in sea water", - "comment": "", + "comment": "Mole concentration means number of moles per unit volume, also called 'molarity', and is used in the construction 'mole_concentration_of_X_in_Y', where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula of CFC11 is CFCl3. The IUPAC name fof CFC11 is trichloro-fluoro-methane.", "dimensions": "longitude latitude olevel time", "out_name": "cfc11", "type": "real", @@ -184,7 +184,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Mole Concentration of CFC-12 in sea water", - "comment": "", + "comment": "Mole concentration means number of moles per unit volume, also called 'molarity', and is used in the construction 'mole_concentration_of_X_in_Y', where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for CFC12 is CF2Cl2. The IUPAC name for CFC12 is dichloro-difluoro-methane.", "dimensions": "longitude latitude olevel time", "out_name": "cfc12", "type": "real", @@ -634,7 +634,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Sinking Particulate Iron Flux", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. 'Sinking' is the gravitational settling of particulate matter suspended in a liquid. A sinking flux is positive downwards and is calculated relative to the movement of the surrounding fluid.", "dimensions": "longitude latitude olevel time", "out_name": "expfe", "type": "real", @@ -652,7 +652,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Sinking Particulate Organic Nitrogen Flux", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. 'Sinking' is the gravitational settling of particulate matter suspended in a liquid. A sinking flux is positive downwards and is calculated relative to the movement of the surrounding fluid.", "dimensions": "longitude latitude olevel time", "out_name": "expn", "type": "real", @@ -670,7 +670,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Sinking Particulate Organic Phosphorus Flux", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. 'Sinking' is the gravitational settling of particulate matter suspended in a liquid. A sinking flux is positive downwards and is calculated relative to the movement of the surrounding fluid.", "dimensions": "longitude latitude olevel time", "out_name": "expp", "type": "real", @@ -688,7 +688,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Sinking Particulate Silica Flux", - "comment": "", + "comment": "In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. 'Sinking' is the gravitational settling of particulate matter suspended in a liquid. A sinking flux is positive downwards and is calculated relative to the movement of the surrounding fluid.", "dimensions": "longitude latitude olevel time", "out_name": "expsi", "type": "real", @@ -737,7 +737,7 @@ "fg13co2": { "frequency": "yr", "modeling_realm": "ocnBgChem", - "standard_name": "surface_downward_mass_flux_of_carbon13_dioxide_abiotic_analogue_expressed_as_carbon13", + "standard_name": "air_sea_flux_of_13CO2", "units": "kg m-2 s-1", "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", @@ -832,7 +832,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Total Grazing of Phytoplankton by Zooplankton", - "comment": "", + "comment": "'tendency_of_X' means derivative of X with respect to time. Mole concentration means number of moles per unit volume, also called 'molarity', and is used in the construction 'mole_concentration_of_X_in_Y', where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The phrase 'expressed_as' is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. The specification of a physical process by the phrase 'due_to_' process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase.", "dimensions": "longitude latitude olevel time", "out_name": "graz", "type": "real", @@ -850,7 +850,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Dissolved Nitrate Concentration", - "comment": "", + "comment": "Mole concentration means moles (amount of substance) per unit volume and is used in the construction mole_concentration_of_X_in_Y, where X is a material constituent of Y.", "dimensions": "longitude latitude olevel time", "out_name": "no3", "type": "real", @@ -868,7 +868,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Dissolved Oxygen Concentration", - "comment": "", + "comment": "'Mole concentration' means number of moles per unit volume, also called'molarity', and is used in the construction mole_concentration_of_X_in_Y, whereX is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'.", "dimensions": "longitude latitude olevel time", "out_name": "o2", "type": "real", @@ -886,7 +886,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Dissolved Oxygen Concentration at Saturation", - "comment": "", + "comment": "'Mole concentration at saturation' means the mole concentration in a saturated solution. Mole concentration means number of moles per unit volume, also called 'molarity', and is used in the construction 'mole_concentration_of_X_in_Y', where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'.", "dimensions": "longitude latitude olevel time", "out_name": "o2sat", "type": "real", @@ -994,7 +994,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "tendency of sea water conservative temperature expressed as heat content due to residual mean (sum of Eulerian + parameterized) advection", - "comment": "", + "comment": "'tendency_of_X' means derivative of X with respect to time. 'Content' indicates a quantity per unit area. The phrase 'expressed_as_heat_content' means that this quantity is calculated as the specific heat capacity times density of sea water multiplied by the conservative temperature of the sea water in the grid cell. Conservative Temperature is defined as part of the Thermodynamic Equation of Seawater 2010 (TEOS-10) which was adopted in 2010 by the International Oceanographic Commission (IOC). Conservative Temperature is specific potential enthalpy (which has the standard name sea_water_specific_potential_enthalpy) divided by a fixed value of the specific heat capacity of sea water, namely cp_0 = 3991.86795711963 J kg-1 K-1. Conservative Temperature is a more accurate measure of the 'heat content' of sea water, by a factor of one hundred, than is potential temperature. Because of this, it can be regarded as being proportional to the heat content of sea water per unit mass. Reference: www.teos-10.", "dimensions": "longitude latitude olevel time", "out_name": "ocontemprmadvect", "type": "real", @@ -1048,7 +1048,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello", "long_name": "integral wrt depth of product of sea water density and potential temperature", - "comment": "", + "comment": "The phrase 'integral_wrt_X_of_Y' means int Y dX. The data variable should have an axis for X specifying the limits of the integral as bounds. The phrase 'wrt' means 'with respect to'. The phrase 'product_of_X_and_Y' means X*Y. Depth is the vertical distance below the surface. Sea water density is the in-situ density (not the potential density). For Boussinesq models, density is the constant Boussinesq reference density, a quantity which has the standard name reference_sea_water_density_for_boussinesq_approximation. Potential temperature is the temperature a parcel of air or sea water would have if moved adiabatically to sea level pressure.", "dimensions": "longitude latitude time", "out_name": "opottempmint", "type": "real", @@ -1120,7 +1120,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "tendency of sea water potential temperature expressed as heat content due to residual mean advection", - "comment": "", + "comment": "The phrase 'tendency_of_X' means derivative of X with respect to time. 'Content' indicates a quantity per unit area. The phrase 'expressed_as_heat_content' means that this quantity is calculated as the specific heat capacity times density of sea water multiplied by the potential temperature of the sea water in the grid cell. Potential temperature is the temperature a parcel of air or sea water would have if moved adiabatically to sea level pressure. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. The phrase 'residual_mean_advection' refers to the sum of the model's resolved advective transport plus any parameterized advective transport. Parameterized advective transport includes processes such as parameterized mesoscale and submesoscale transport, as well as any other advectively parameterized transport.", "dimensions": "longitude latitude olevel time", "out_name": "opottemprmadvect", "type": "real", @@ -1228,7 +1228,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "tendency of sea water salinity expressed as salt content due to residual mean advection", - "comment": "", + "comment": "The phrase 'tendency_of_X' means derivative of X with respect to time. 'Content' indicates a quantity per unit area. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. The phrase 'residual_mean_advection' refers to the sum of the model's resolved advective transport plus any parameterized advective transport. Parameterized advective transport includes processes such as parameterized mesoscale and submesoscale transport, as well as any other advectively parameterized transport. When the parameterized advective transport is represented in the model as a skew-diffusion rather than an advection, then the parameterized skew diffusion should be included in this diagnostic, since the convergence of skew-fluxes are identical (in the continuous formulation) to the convergence of advective fluxes.", "dimensions": "longitude latitude olevel time", "out_name": "osaltrmadvect", "type": "real", @@ -1264,7 +1264,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Aragonite Production", - "comment": "", + "comment": "'Mole concentration' means number of moles per unit volume, also called'molarity', and is used in the construction mole_concentration_of_X_in_Y, whereX is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The phrase 'expressed_as' is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. 'tendency_of_X' means derivative of X with respect to time. Aragonite is a mineral that is a polymorph of calcium carbonate. The chemical formula of aragonite is CaCO3.", "dimensions": "longitude latitude olevel time", "out_name": "parag", "type": "real", @@ -1282,7 +1282,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Biogenic Iron Production", - "comment": "", + "comment": "'Mole concentration' means number of moles per unit volume, also called'molarity', and is used in the construction mole_concentration_of_X_in_Y, whereX is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. 'tendency_of_X' means derivative of X with respect to time.", "dimensions": "longitude latitude olevel time", "out_name": "pbfe", "type": "real", @@ -1300,7 +1300,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Biogenic Silica Production", - "comment": "", + "comment": "'Mole concentration' means number of moles per unit volume, also called'molarity', and is used in the construction mole_concentration_of_X_in_Y, whereX is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. 'tendency_of_X' means derivative of X with respect to time.", "dimensions": "longitude latitude olevel time", "out_name": "pbsi", "type": "real", @@ -1318,7 +1318,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Calcite Production", - "comment": "", + "comment": "'Mole concentration' means number of moles per unit volume, also called'molarity', and is used in the construction mole_concentration_of_X_in_Y, whereX is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The phrase 'expressed_as' is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. 'tendency_of_X' means derivative of X with respect to time. Calcite is a mineral that is a polymorph of calcium carbonate. Thechemical formula of calcite is CaCO3.", "dimensions": "longitude latitude olevel time", "out_name": "pcalc", "type": "real", @@ -1624,7 +1624,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Remineralization of Organic Carbon", - "comment": "", + "comment": "'tendency_of_X' means derivative of X with respect to time. Mole concentration means number of moles per unit volume, also called 'molarity', and is used in the construction 'mole_concentration_of_X_in_Y', where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The phrase 'expressed_as' is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. The specification of a physical process by the phrase 'due_to_' process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase.", "dimensions": "longitude latitude olevel time", "out_name": "remoc", "type": "real", @@ -1642,7 +1642,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "net rate of absorption of shortwave energy in ocean layer", - "comment": "", + "comment": "'shortwave' means shortwave radiation. 'Layer' means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. Net absorbed radiation is the difference between absorbed and emitted radiation.", "dimensions": "longitude latitude olevel time", "out_name": "rsdoabsorb", "type": "real", @@ -1660,7 +1660,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Mole Concentration of SF6 in sea water", - "comment": "", + "comment": "Mole concentration means number of moles per unit volume, also called 'molarity', and is used in the construction 'mole_concentration_of_X_in_Y', where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula of sulfur hexafluoride is SF6.", "dimensions": "longitude latitude olevel time", "out_name": "sf6", "type": "real", @@ -1678,7 +1678,7 @@ "cell_methods": "area: mean where sea time: mean", "cell_measures": "area: areacello volume: volcello", "long_name": "Total Dissolved Inorganic Silicon Concentration", - "comment": "", + "comment": "Mole concentration means number of moles per unit volume, also called 'molarity', and is used in the construction 'mole_concentration_of_X_in_Y', where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. 'Dissolved inorganic silicon' means the sum of all inorganic silicon in solution (including silicic acid and its first dissociated anion SiO(OH)3-).", "dimensions": "longitude latitude olevel time", "out_name": "si", "type": "real", @@ -1761,7 +1761,7 @@ "ok_max_mean_abs": "" }, "volcello": { - "frequency": "fx", + "frequency": "yr", "modeling_realm": "ocean", "standard_name": "ocean_volume", "units": "m3", diff --git a/Tables/CMIP6_SIday.json b/Tables/CMIP6_SIday.json index 358924ba..c400ef70 100644 --- a/Tables/CMIP6_SIday.json +++ b/Tables/CMIP6_SIday.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table SIday", "realm": "seaIce", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", diff --git a/Tables/CMIP6_SImon.json b/Tables/CMIP6_SImon.json index d224fae1..716a37d6 100644 --- a/Tables/CMIP6_SImon.json +++ b/Tables/CMIP6_SImon.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table SImon", "realm": "seaIce", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", diff --git a/Tables/CMIP6_coordinate.json b/Tables/CMIP6_coordinate.json index 211d6683..689272c7 100644 --- a/Tables/CMIP6_coordinate.json +++ b/Tables/CMIP6_coordinate.json @@ -414,7 +414,7 @@ "stored_direction": "increasing", "tolerance": "", "type": "double", - "valid_max": "2200.0", + "valid_max": "2020.0", "valid_min": "1980.0", "value": "2000", "z_bounds_factors": "", @@ -681,6 +681,28 @@ "z_factors": "", "bounds_values": "" }, + "lambda550nm": { + "standard_name": "radiation_wavelength", + "units": "nm", + "axis": "", + "long_name": "Radiation Wavelength 550 nanometers", + "climatology": "", + "formula": "", + "must_have_bounds": "yes", + "out_name": "wavelength", + "positive": "", + "requested": "", + "requested_bounds": "", + "stored_direction": "", + "tolerance": "", + "type": "double", + "valid_max": "", + "valid_min": "", + "value": "550.0", + "z_bounds_factors": "", + "z_factors": "", + "bounds_values": "" + }, "landUse": { "standard_name": "area_type", "units": "", @@ -1735,10 +1757,10 @@ "type": "double", "valid_max": "", "valid_min": "", - "value": "0.005, 0.605, 2.1, 4, 6, 8.5, 12.5, 17.5, 22.5, 27.5, 35, 45, 55, 70, 50040", + "value": "", "z_bounds_factors": "", "z_factors": "", - "bounds_values": "0.0 0.01 1.2 3.0 5.0 7.0 10.0 15.0 20.0 25.0 30.0 40.0 50.0 60.0 80.0 100000.0" + "bounds_values": "" }, "sdepth": { "standard_name": "depth", @@ -1777,13 +1799,35 @@ "stored_direction": "increasing", "tolerance": "", "type": "double", - "valid_max": "0.2", + "valid_max": "0.1", "valid_min": "0.0", "value": "0.05", "z_bounds_factors": "", "z_factors": "", "bounds_values": "0.0 0.1" }, + "sdepth10": { + "standard_name": "depth", + "units": "m", + "axis": "Z", + "long_name": "depth", + "climatology": "", + "formula": "", + "must_have_bounds": "yes", + "out_name": "depth", + "positive": "down", + "requested": "", + "requested_bounds": "", + "stored_direction": "increasing", + "tolerance": "", + "type": "double", + "valid_max": "1.0", + "valid_min": "0.0", + "value": "0.5", + "z_bounds_factors": "", + "z_factors": "", + "bounds_values": "0.0 1.0" + }, "siline": { "standard_name": "region", "units": "", @@ -2721,7 +2765,7 @@ "bounds_values": "" }, "typewetla": { - "standard_name": "area_type", + "standard_name": "", "units": "", "axis": "", "long_name": "Wetland", @@ -2737,7 +2781,7 @@ "type": "character", "valid_max": "", "valid_min": "", - "value": "", + "value": "wetlands", "z_bounds_factors": "", "z_factors": "", "bounds_values": "" @@ -2746,7 +2790,7 @@ "standard_name": "", "units": "", "axis": "", - "long_name": "plant functional type", + "long_name": "Vegetation or Land Cover Type", "climatology": "", "formula": "", "must_have_bounds": "no", diff --git a/Tables/CMIP6_day.json b/Tables/CMIP6_day.json index 3c62ae87..85915cad 100644 --- a/Tables/CMIP6_day.json +++ b/Tables/CMIP6_day.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table day", "realm": "atmos", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -40,7 +40,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Surface Upward Latent Heat Flux", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Upward' indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "hfls", "type": "real", @@ -58,7 +58,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Surface Upward Sensible Heat Flux", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'Upward' indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called 'turbulent' heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. Unless indicated in the cell_methods attribute, a quantity is assumed to apply to the whole area of each horizontal grid box. Previously, the qualifier where_type was used to specify that the quantity applies only to the part of the grid box of the named type. Names containing the where_type qualifier are deprecated and newly created data should use the cell_methods attribute to indicate the horizontal area to which the quantity applies.", "dimensions": "longitude latitude time", "out_name": "hfss", "type": "real", @@ -92,7 +92,7 @@ "standard_name": "relative_humidity", "units": "%", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Near-Surface Relative Humidity", "comment": "The relative humidity with respect to liquid water for T> 0 C, and with respect to ice for T<0 C.", "dimensions": "longitude latitude time height2m", @@ -148,7 +148,7 @@ "cell_methods": "time: mean", "cell_measures": "area: areacella", "long_name": "Specific Humidity", - "comment": "", + "comment": "'specific' means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.", "dimensions": "longitude latitude plev8 time", "out_name": "hus", "type": "real", @@ -164,7 +164,7 @@ "standard_name": "specific_humidity", "units": "1", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Near-Surface Specific Humidity", "comment": "Near-surface (usually, 2 meter) specific humidity.", "dimensions": "longitude latitude time height2m", @@ -218,7 +218,7 @@ "standard_name": "moisture_content_of_soil_layer", "units": "kg m-2", "cell_methods": "area: mean where land time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Moisture in Upper Portion of Soil Column", "comment": "The mass of water in all phases in the upper 10cm of the soil layer.", "dimensions": "longitude latitude time sdepth1", @@ -310,7 +310,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Surface Downwelling Longwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'longwave' means longwave radiation. Downwelling radiation is radiation from above. It does not mean 'net downward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "rlds", "type": "real", @@ -328,7 +328,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Surface Upwelling Longwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'longwave' means longwave radiation. Upwelling radiation is radiation from below. It does not mean 'net upward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "rlus", "type": "real", @@ -382,7 +382,7 @@ "cell_methods": "area: time: mean", "cell_measures": "area: areacella", "long_name": "Surface Upwelling Shortwave Radiation", - "comment": "", + "comment": "The surface called 'surface' means the lower boundary of the atmosphere. 'shortwave' means shortwave radiation. Upwelling radiation is radiation from below. It does not mean 'net upward'. When thought of as being incident on a surface, a radiative flux is sometimes called 'irradiance'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called 'vector irradiance'. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics.", "dimensions": "longitude latitude time", "out_name": "rsus", "type": "real", @@ -398,7 +398,7 @@ "standard_name": "wind_speed", "units": "m s-1", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Daily-Mean Near-Surface Wind Speed", "comment": "near-surface (usually, 10 meters) wind speed.", "dimensions": "longitude latitude time height10m", @@ -416,7 +416,7 @@ "standard_name": "wind_speed", "units": "m s-1", "cell_methods": "area: mean time: maximum", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Daily Maximum Near-Surface Wind Speed", "comment": "Daily maximum near-surface (usually, 10 meters) wind speed.", "dimensions": "longitude latitude time height10m", @@ -488,7 +488,7 @@ "standard_name": "air_temperature", "units": "K", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Near-Surface Air Temperature", "comment": "near-surface (usually, 2 meter) air temperature", "dimensions": "longitude latitude time height2m", @@ -562,7 +562,7 @@ "cell_methods": "time: mean", "cell_measures": "area: areacella", "long_name": "Eastward Wind", - "comment": "", + "comment": "'Eastward' indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude plev8 time", "out_name": "ua", "type": "real", @@ -578,7 +578,7 @@ "standard_name": "eastward_wind", "units": "m s-1", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Eastward Near-Surface Wind", "comment": "Eastward component of the near-surface (usually, 10 meters) wind", "dimensions": "longitude latitude time height10m", @@ -598,7 +598,7 @@ "cell_methods": "time: mean", "cell_measures": "area: areacella", "long_name": "Northward Wind", - "comment": "", + "comment": "'Northward' indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)", "dimensions": "longitude latitude plev8 time", "out_name": "va", "type": "real", @@ -614,7 +614,7 @@ "standard_name": "northward_wind", "units": "m s-1", "cell_methods": "area: time: mean", - "cell_measures": "area: areacella", + "cell_measures": "", "long_name": "Northward Near-Surface Wind", "comment": "Northward component of the near surface wind", "dimensions": "longitude latitude time height10m", @@ -652,7 +652,7 @@ "cell_methods": "time: mean", "cell_measures": "area: areacella", "long_name": "Geopotential Height", - "comment": "", + "comment": "Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface.", "dimensions": "longitude latitude plev8 time", "out_name": "zg", "type": "real", diff --git a/Tables/CMIP6_formula_terms.json b/Tables/CMIP6_formula_terms.json index 9e502502..e8ebe7cd 100644 --- a/Tables/CMIP6_formula_terms.json +++ b/Tables/CMIP6_formula_terms.json @@ -19,7 +19,7 @@ "units": "Pa", "dimensions": "", "out_name": "p0", - "type": "" + "type": "double" }, "b": { "long_name": "vertical coordinate formula term: b(k)", @@ -61,14 +61,14 @@ "units": "m", "dimensions": "", "out_name": "ztop", - "type": "" + "type": "double" }, "ptop": { "long_name": "pressure at top of model", "units": "Pa", "dimensions": "", "out_name": "ptop", - "type": "" + "type": "double" }, "a_bnds": { "long_name": "vertical coordinate formula term: a(k+1/2)", diff --git a/Tables/CMIP6_fx.json b/Tables/CMIP6_fx.json index 402b249b..e0013f6a 100644 --- a/Tables/CMIP6_fx.json +++ b/Tables/CMIP6_fx.json @@ -1,10 +1,10 @@ { "Header": { - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "table_id": "Table fx", "realm": "land", "cmor_version": "3.2", - "table_date": "14 February 2018", + "table_date": "07 March 2018", "missing_value": "1e20", "int_missing_value": "-999", "product": "model-output", @@ -148,7 +148,7 @@ "cell_methods": "area: mean", "cell_measures": "area: areacella", "long_name": "Altitude of Model Full-Levels", - "comment": "", + "comment": "'Height_above_X' means the vertical distance above the named surface X. A reference ellipsoid is a mathematical figure that approximates the geoid. The geoid is a surface of constant geopotential with which mean sea level would coincide if the ocean were at rest. The ellipsoid is an approximation because the geoid is an irregular shape. A number of reference ellipsoids are defined for use in the field of geodesy. To specify which reference ellipsoid is being used, a grid_mapping variable should be attached to the data variable as described in Chapter 5.6 of the CF Convention.", "dimensions": "longitude latitude alevel", "out_name": "zfull", "type": "real", diff --git a/Tables/CMIP6_grids.json b/Tables/CMIP6_grids.json index 285c9189..861951d8 100644 --- a/Tables/CMIP6_grids.json +++ b/Tables/CMIP6_grids.json @@ -4,9 +4,9 @@ "cmor_version": "3.2", "Conventions": "CF-1.7 CMIP-6.2", "table_id": "Table grids", - "data_specs_version": "01.00.21", + "data_specs_version": "01.00.22", "missing_value": "1e20", - "table_date": "14 February 2018" + "table_date": "07 March 2018" }, "mapping_entry": { "sample_user_mapping": {