Comments (1)
The most accurate method is to create a TAPE3 with only the gas of interest, while keeping the amounts in the TAPE5 the same. You can also zero out the amounts of all the gases you are not interested in.
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Related Issues (20)
- lnfl can't run HOT 11
- using lblrtm to simulate the radiance of cloudy situation HOT 1
- QUESTION ABOUT H2O ISOTOPOLOGUES HOT 4
- question about lblrtm HOT 2
- error on lblrtm Segmentation fault HOT 6
- How to modify the spectral resolution of the output atmospheric transmittance/radiance HOT 3
- 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 HOT 5
- error on lblrtm HOT 2
- How to read TAPE11 and TAPE12 wtih matlab or python? HOT 2
- On the calculation of atmospheric radiation when observing from an orbital altitude downwards. HOT 11
- When LBLRTM calculates different observation heights, the length and resolution of the output radiometric data are inconsistent, and some of the radiometric data are 0 HOT 2
- Does LBLRTM consider the self absorption effect of gas molecules at high altitudes? HOT 4
- Whether or not gas density profile data needs to be entered? HOT 1
- Please advise on some questions about the parameter units entered in Record 3.5 3.6 HOT 1
- How do you calculate the amount of radiative transport of a single molecule after atmospheric absorption in LBLRTM? HOT 1
- Non local thermal equilibrium? HOT 1
- Whether the radiation profile can be used as an input? HOT 1
- Setting cloud simulation with a user-defined atmosphere profile HOT 1
- lblrtm_v12.17_linux install problems HOT 1
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