Water vapour source impacts on oxygen isotope variability in tropical precipitation during Heinrich events
Water isotope records such as speleothems provide extensive evidence of past tropical hydrological changes. During Heinrich events, isotopic changes in monsoon regions have been interpreted as implying a widespread drying through the Northern Hemisphere tropics and an anti-phased precipitation response in the south. Here, we examine the sources of this variability using a water isotope-enabled general circulation model, Goddard Institute for Space Studies ModelE. We incorporate a new suite of...[Show more]
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|Source:||Climate of the Past Discussions|
|01_Lewis (previously Bretherton)_Water_vapour_source_impacts_on_2010.pdf||4.41 MB||Adobe PDF||Request a copy|
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