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Journal: Ocean Science ×Author: Simon Stuart ×Clear All Filters
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Ocean Science · 2021 · Vol. 17 · Issue 5 · Copernicus Publications / European Geosciences Union
Wintertime convection in the North Atlantic Ocean is a key component of the global climate as it produces dense waters at high latitudes that flow equatorward as part of the Atlantic Meridional Overturning Circulation (AMOC). Recent work has highlighted the dominant role of the Irminger and Iceland basins in the production of North Atlantic Deep Water. Dense water formation in these basins is mainly explained by buoyancy forci...