Modeling insights into deuterium excess as an indicator of water vapor source conditions
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Lewis (previously Bretherton), Sophie
LeGrande, Allegra N.
Kelley, Maxwell
Schmidt, Gavin A.
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Wiley-Blackwell Publishing Ltd
Abstract
Deuterium excess (d) is interpreted in conventional paleoclimate reconstructions as a tracer of oceanic source region conditions, such as temperature, where precipitation originates. Previous studies have adopted coisotopic approaches (using both d18O and
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Journal of Geophysical Research: Atmospheres
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Restricted until
2037-12-31