Weakening of the AMOC and strengthening of Labrador Sea deep convection in response to external freshwater forcing.

ABSTRACT: The Atlantic Meridional Overturning Circulation (AMOC) is a key player in climate. Here, we employ an ensemble of water hosing experiments to examine mechanisms of AMOC weakening and its subsequent impact on the Labrador Sea open-ocean deep convection. The subpolar AMOC decline in response to the external freshwater flux released over the southern Nordic Sea is dominated by that across the eastern subpolar North Atlantic, and the largest subpolar AMOC decline is at the relatively dense level around σ 0 = 27.84 kg m - 3 . The AMOC decline is associated with subsurface cooling in the subpolar North Atlantic and the decline in the deep ocean west-east density contrast across the subpolar basin. Contrary to previous studies showing that the AMOC decline is caused by subsurface warming th

SUBMITTER: Wei X 

PROVIDER: S-EPMC11605065 | biostudies-literature | 2024 Nov

REPOSITORIES: biostudies-literature