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Suggestion from J. Toole: perhaps we should write cost functions to constrain 1) isopycnal depth and 2) the salinity - or temperature - on isopycnals?
"The variance of Theta/S - below the surface waters - is far less than T or S on pressure surfaces, which should translate into an up-weighting in the cost function."
It true, much of our large in-situ variance is associated with isopycnal displacements in the presence of vertical T and S gradients.
The text was updated successfully, but these errors were encountered:
It true, much of our large in-situ variance is associated with isopycnal displacements in the presence of vertical T and S gradients.
is true in general I think
Suggestion from J. Toole: ...
Thanks John!! Much appreciated
We might have talked about this at a climode meeting or something like that in fact. K. Haines & a few others have brought it up a few times too I think.
Suggestion from J. Toole: perhaps we should write cost functions to constrain 1) isopycnal depth and 2) the salinity - or temperature - on isopycnals?
"The variance of Theta/S - below the surface waters - is far less than T or S on pressure surfaces, which should translate into an up-weighting in the cost function."
It true, much of our large in-situ variance is associated with isopycnal displacements in the presence of vertical T and S gradients.
The text was updated successfully, but these errors were encountered: