Weakening Circulation Drives Greenland Anomaly
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Weakened Atlantic Meridional Overturning CirculationScienceDaily
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The Atlantic’s chilling secret: A century of data reveals ocean current collapse
78% Informative
Researchers from the University of California, Riverside show that only one explanation fits both observed ocean temperatures and salinity patterns: the Atlantic Meridional Overturning Circulation , or AMOC , is slowing down.
A slowdown in this system means less warm, salty water reaches the sub-polar region, resulting in the cooling and freshening observed south of Greenland .
Weakened Atlantic Meridional Overturning Circulation causes the historical North Atlantic Warming Hole . Communications Earth & Environment, 2025 ; 6 ( 1 ) DOI: 10.1038 /s43247-025-02403-0 Cite This Page:.
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