The North Atlantic Ocean plays a key role in modulating global climate (e.g., Marshall et al., 2001). Surface currents of the North Atlantic, including the Gulf Stream and its northern extension, the North Atlantic Current, bring relatively warm, salty waters northward as the surface components of the Atlantic Meridional Overturning Circulation (AMOC). At higher latitudes, these waters exchange heat with the atmosphere and cool to form dense, sinking water masses (deep-water formation) that return southward at depth, contributing to global ocean circulation (e.g., Broecker, 1991;Lynch-Stieglitz et al., 2007). The strength and structure of these currents, the rate of deep-water formation, and ocean-atmosphere interactions across the