Future Shoaling of the AMOC and Its Impact on Oceanic Heat Transport to the Subpolar North Atlantic
Abstract The Atlantic Meridional Overturning Circulation (AMOC) carries oceanic heat northward to the subpolar North Atlantic (SPNA), where the surface water cools and sinks to the deep ocean. According to a large‐ensemble simulation under a medium‐to‐high emission scenario, the surface cooling and oceanic heat convergence in the SPNA may decrease to ...
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