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Vertical Reynolds Stress Divergence in the Upper Ocean Associated with Linear Wind-Driven, Near-Inertial Waves of Finite Wavelength
Vertical Reynolds Stress Divergence Upper Ocean Linear Wind-Driven Near-Inertial Waves Finite Wavelength
2009/1/12
Study of a schematic linear, wind-driven, inertio–gravity wave model in the upper ocean finds resonant, near-inertial waves of finite horizontal wavelength to have both horizontal and vertical motions...
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...
Finite-Wavelength Instabilities of a Coupled Density Front
Finite-Wavelength Instabilities CoupledDensity Front
2008/12/27
Finite-wavelength instabilities of a coupled density front with zero potential vorticity are found for the single-layer and the two-layer problems. These instabilities result from the resonance betwee...