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How to calculate the amount of radiation that reaches the observation position after the radiation of a molecule or all molecules in the atmosphere is transmitted by atmospheric radiative transmission (linear integration) under different observation methods
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StarsTravel opened this issue
May 8, 2024
· 5 comments
hello,How to calculate the amount of radiation that reaches the observation position after the radiation of a molecule or all molecules in the atmosphere is transmitted by atmospheric radiative transmission (linear integration) under different observation methods?
The different observation methods are shown in the figure below:
For example, how do I change H1, H2, and angle in a tape5 file?
For example, how to calculate the amount of atmospheric radiation after radiation transmission over a certain distance by only one atmospheric molecule, several atmospheric molecules, and all atmospheric molecules, and how to set it in tape5?
How to consider the effects of atmospheric radiation ?
The text was updated successfully, but these errors were encountered:
Please take a look the following example in the example tar package: run_example_user_defined_upwelling. Compare the TAPE5 with the instructions, which will show you which parameters are defined on which lines. Ruuning LBL will provide both the surface (if looking down) and the atmospheric contributions to the TOA radiation. If you want the contribtion of just one molecule you have several options:
Please take a look the following example in the example tar package: run_example_user_defined_upwelling. Compare the TAPE5 with the instructions, which will show you which parameters are defined on which lines. Ruuning LBL will provide both the surface (if looking down) and the atmospheric contributions to the TOA radiation. If you want the contribtion of just one molecule you have several options:
Thank you!! please tell me where is ' run_example_user_defined_upwelling'
hello,How to calculate the amount of radiation that reaches the observation position after the radiation of a molecule or all molecules in the atmosphere is transmitted by atmospheric radiative transmission (linear integration) under different observation methods?
The different observation methods are shown in the figure below:
For example, how do I change H1, H2, and angle in a tape5 file?
For example, how to calculate the amount of atmospheric radiation after radiation transmission over a certain distance by only one atmospheric molecule, several atmospheric molecules, and all atmospheric molecules, and how to set it in tape5?
How to consider the effects of atmospheric radiation ?
The text was updated successfully, but these errors were encountered: