A positive climatic feedback mechanism for Himalayan glaciation-Reference-Cited by-同舟云学术

A positive climatic feedback mechanism for Himalayan glaciation

Published:2000-04 Issue: Volume:65-66 Page:3-13
ISSN:1040-6182
Container-title:Quaternary International
language:en
Short-container-title:Quaternary International

Author:

Bush Andrew B.G

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference24 articles.

1. The role of the Indian summer monsoon and the mid-latitude westerlies in Himalayan glaciation;Benn;Journal of Geological Society,1998

2. The influence of continental ice, atmospheric CO2, and land albedo on the climate of the last glacial maximum;Broccoli;Climate Dynamics,1987

3. Bush, A.B.G., 2000. Orbital forcing versus sea surface temperature forcing and the implications for early Holocene climate. Quaternary Research, submitted for publication.

4. The climate of the Last Glacial Maximum: results from a coupled atmosphere-ocean general circulation model;Bush;Journal of Geophysical Research,1999

5. Atmospheric circulation patterns during glacial inception;Crowley;Quaternary Research,1984

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