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Characterization and evaluation of AIRS-based estimates of the deuterium content of water vapor

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Figure

Figure 1. (a) AIRS radiance at approximately 8 µm for a typicaltropical scene. (b) The total column (log) Jacobian for H2O nor-malized by the AIRS NESR
Figure 2. The rows of the averaging kernel matrix for the HDO re-trieval corresponding to the radiance shown in Fig
Figure 3. (a) The mean tropospheric deuterium content (in “per mil” or units of parts per thousand relative to the deuterium content of theocean or SMOW) for 1 June 2006 as inferred from AIRS radiance measurements
Table 1. Comparison between averaged TES and AIRS HDO/H2Oratio (750–350 hPa). The units are in parts per thousand relative toStandard Mean Ocean Water

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