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...

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Bibliographic Details
Main Authors: Pavia, Frank J., Jones, C. Spencer, Hines, Sophia K.
Format: Article in Journal/Newspaper
Language:unknown
Published: American Meteorological Society 2022
Subjects:
Online Access:https://doi.org/10.1175/jcli-d-21-0671.1