Atlantic Ocean circulation changes preceded millennial tropical South America rainfall events during the last glacial
During the last glacial period, Greenland's climate shifted between cold (stadial) and warm (interstadial) phases that were accompanied by ocean circulation changes characterized by reduced Atlantic Meridional Overturning Circulation (AMOC) during stadials. Here we present new data from the wes...
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| Main Authors: | , , , , , , , |
|---|---|
| Format: | Article (Journal) |
| Language: | English |
| Published: |
16 Jan. 2015
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| In: |
Geophysical research letters
Year: 2015, Volume: 42, Issue: 2, Pages: 411-418 |
| ISSN: | 1944-8007 |
| DOI: | 10.1002/2014GL062512 |
| Online Access: | Verlag, lizenzpflichtig, Volltext: https://doi.org/10.1002/2014GL062512 Verlag, lizenzpflichtig, Volltext: https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1002/2014GL062512 |
| Author Notes: | Pierre Burckel, Claire Waelbroeck, Jeanne Marie Gherardi, Sylvain Pichat, Helge Arz, Joerg Lippold, Trond Dokken, and François Thil |