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Ocean Gyre Circulation Changes Associated with the North Atlantic Oscillation
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Ocean Gyre Circulation Changes Associated with the North Atlantic Oscillation
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Journal Article
Ocean Gyre Circulation Changes Associated with the North Atlantic Oscillation
2001
Overview
Observational evidence is presented for interannual to interdecadal variability in the intensity of the North Atlantic gyre circulation related to the atmospheric North Atlantic Oscillation (NAO) patterns. A two-point baroclinic pressure difference between the subtropical and subpolar gyre centers--an oceanic analogue to the much-uses sea level pressure (SLP)-based atmospheric NAO indices--is constructed from time series of potential energy anomaly (PEA) derived from hydrographic measurements in the Labrador Basin and at Station S near Bermuda.
Publisher
American Meteorological Society
