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FORCING OF GULF STREAM POSITION AND STRENGTH BY WIND AND OCEAN CIRCULATION
The Gulf Stream (GS) is the western boundary current of the North Atlantic Subtropical Gyre, which in turn is part of the Atlantic Meridional Overturning Circulation (AMOC). As a wind driven gyre, the Gulf Stream is sensitive to changes in the dominant wind patterns represented by the North Atlantic Oscillation (NAO). Under ...