Modeling insights into deuterium excess as an indicator of water vapor source conditions
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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|Source:||Journal of Geophysical Research: Atmospheres|
|01_Lewis (previously Bretherton)_Modeling_insights_into_2013.pdf||4.85 MB||Adobe PDF||Request a copy|
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