HIGHLIGHTS
SUMMARY
The cospectrum of wind stress and surface currents quantifies the surface kinetic energy fluxes (Fig 2a). At smaller scales (10-200 km) and low frequencies ( and amp;lt; 1 day-1), namely the meso- and | Vol:(1234567890) 13:5915 | submesocale ranges, the wind act as an energy sink for the ocean, removing energy at a rate of - 0.05 mW m-2. At smaller scales (10-200 km) and higher frequencies (>1 day-1), the wind also act as an energy sink (- 0.2 mW m-2). The "IW killing", which corresponds to a . . .
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