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Evaluating the strength of the land–atmosphere moisture feedback in Earth system models using satellite observations

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Figure

Figure 1. Conceptual description of coupling metrics:TWSA values (in units of water height) during the maximum andminimum months, respectively, and ATMmospheric component, demonstrating the forcing limb of the feed-back loop, in which TWSAditions, as well
Table 1. Remote sensing products used for analysis.
Table 2. CMIP5 models used for analysis.
Figure 4. Interannual variability (standard deviation) of VPDequivalent quantities from the LENS ensemble meandi from AIRS (a), PPTdi from GPCP (b), SW↓di from CERES (c) and the (d–f).
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