Geometry of the Meridional Overturning Circulation at the Last Glacial Maximum
Understanding the contribution of ocean circulation to glacial–interglacial climate change is a major focus of paleoceanography. Specifically, many have tried to determine whether the volumes and depths of Antarctic- and North Atlantic–sourced waters in the deep ocean changed at the Last Glacial...
Main Authors: | , , |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
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American Meteorological Society
2022
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Online Access: | https://doi.org/10.1175/jcli-d-21-0671.1 |