Atlantic Meridional Overturning Circulation

Transport Variability of the Irminger Sea Deep Western Boundary Current from a Mooring Array

The Deep Western Boundary Current (DWBC) in the subpolar North Atlantic is the lower limb of the Atlantic Meridional Overturning Circulation and a key component of the global climate system. Here, a mooring array deployed at 60° N in the Irminger …

Moored Observations of the Deep Western Boundary Current in the NWAtlantic: 2004-2014