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Evanescent Pressure Gradient Response in the Upper Ocean to Subinertial Wind Stress Forcing of Finite Wavelength
Pressure Gradient Upper Ocean Subinertial Wind Stress Finite Wavelength
2009/1/7
The idea that Ekman transport driven by the mean synoptic wind stress on the f0-plane is a robust result is true only for infinite scale lengths of the wind stress forcing. For finite scale wavelength...