HIGHLIGHTS
SUMMARY
The deuterium content of a measurement is traditionally given in parts per thousand relative to the deuterium content of ocean water (i.e., δD; "Methods"). The degree to which isotopic variations follow one or the other of these precipitation or evaporation relationships is readily quantified by normalizing the δD to a reference water vapor concentration. The authors use monthly gridded AIRS deuterium measurements during 2003-2015 ("Methods") and corresponding δD_004 estimates ("Methods") to analyze seasonal, interannual, and spatial variability in ET-P for the Amazon and surrounding regions. The authors estimate the accuracy of . . .
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