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Profiles of CH<sub>4</sub>, HDO, H<sub>2</sub>O, and N<sub>2</sub>O with improved lower tropospheric vertical resolution from Aura TES radiances

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Fig. 1a. Sources, sinks, and processes controlling tropospheric water vapor (courtesy Derek Brown, dissertation).
Figure 1b: sources, sinks, and processes controlling tropospheric 
Fig. 2a. Top: example of radiance measured by TES over a tropical ocean scene. Middle:
Fig. 2b. Same as in Fig. 2a but for H 2 O and HDO.
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