The AMOC stayed strong even as a major ocean “lifeline” nearly shut down
Summary
Seafloor sediments indicate that the flow of warm, salty water from the Indian Ocean into the Atlantic nearly stopped during a cold period about 3.4 million years ago. The Atlantic Meridional Overturning Circulation did not weaken as expected and became stronger in some regions.
The evidence shows that the AMOC can draw on compensating circulation changes rather than respond
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The AMOC may be more resilient, and more regionally variable, than models built around a single dominant ocean connection suggest.