Glacial AMOC shoaling despite vigorous tidal dissipation: vertical stratification matters
<p>During the Last Glacial Maximum (LGM), tidal dissipation was about 3-fold higher than today, which could have led to a considerable increase in vertical mixing. This increase might have enhanced the glacial Atlantic Meridional Overturning Circulation (AMOC), contradicting the shoaled AMOC i...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2024-09-01
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| Series: | Climate of the Past |
| Online Access: | https://cp.copernicus.org/articles/20/2001/2024/cp-20-2001-2024.pdf |