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Spectrum of Wind-Driven Baroclinic Fluctuations of the Ocean in the Midlatitudes
Spectrum Wind-Driven Baroclinic Fluctuations Ocean Midlatitudes
2008/6/13
In the midlatitudes, the thermocline depth variations are largely due to Rossby waves of first baroclinic mode forced by stochastic wind stress. The frequency spectrum of this oceanic response is inve...