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Upper-troposphere and lower-stratosphere water vapor retrievals from the 1400 and 1900 nm water vapor bands

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Figure

Figure 1. The vertical profile of water vapor mixing ratio used in theMODTRAN5 tropical atmosphere
Figure 2. (left) Water vapor transmittance (modeled at SSFR sam-pling and resolution) in a tropical atmosphere is shown from thesurface (black), 14 km (blue) and 18 km (red) to the top of the at-mosphere
Figure 5. Water vapor number density profiles from the NOAA water instrument. The red points correspond to the in situ water vapornumber densities during the descent and ascent for the two profiles
Figure 7. Same as Fig. 6 for profiles during the third and fourthATTREX science flights.
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