Enhanced Atlantic Meridional Overturning Circulation supports the Last Glacial Inception
The Atlantic Meridional Overturning Circulation (AMOC) is a key feature of the climate system. However, its role during climate change is still poorly constrained particularly during an Interglacial to Glacial climate transition and the associated global cooling. We present here the first reconstruc...
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Published in | Quaternary science reviews Vol. 30; no. 13; pp. 1576 - 1582 |
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Main Authors | , , , , , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier Ltd
01.06.2011
Elsevier |
Subjects | |
Online Access | Get full text |
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