Sinking of Dense North Atlantic Waters in a Global Ocean Model: Location and Controls

We investigate the characteristics of the sinking of dense waters in the North Atlantic Ocean that constitute the downwelling limb of the Atlantic Meridional Overturning Circulation (AMOC) as simulated by two global ocean models: an eddy-permitting model at 1/4° resolution and its coarser 1° counterpart. In line with simple geostrophic...