North Atlantic subsurface temperature response controlled by effective freshwater input in “Heinrich” events
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DOI: 10.1016/j.epsl.2020.116247
Abstract: Abstract The northern North Atlantic (NNA) subsurface temperature in response to the slowdown of the Atlantic meridional overturning circulation (AMOC) is crucial for ice sheet calving and recovery of the AMOC in Heinrich events. Paleoclimate… read more here.
Keywords: subsurface; response; subsurface temperature; temperature response ... See more keywords