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Modeling insights into deuterium excess as an indicator of water vapor source conditions

Lewis (previously Bretherton), Sophie; LeGrande, Allegra N.; Kelley, Maxwell; Schmidt, Gavin A.

Description

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

CollectionsANU Research Publications
Date published: 2013
Type: Journal article
URI: http://hdl.handle.net/1885/74936
Source: Journal of Geophysical Research: Atmospheres
DOI: 10.1029/2012JD017804

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