North Atlantic Deep Water (NADW) is a key component of the global ocean circulation system, particularly within the Atlantic Meridional Overturning Circulation (AMOC). It refers to a body of cold, dense water that forms in the North Atlantic Ocean, primarily in areas such as the Labrador Sea, the Greenland Sea, and the Norwegian Sea. NADW is characterized by its relatively high salinity and low temperature, which contributes to its density.
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