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A model is presented depicting that, for a fully developed sea driven by the wind with speeds above 5 m sec−1, the air in the transition zone immediately above the air-sea interface is mixed wit...
The North Atlantic low frequency variability along 48°N is described from 76 year-long velocity-temperature records obtained as part of the Topogulf project whose main objective was to document the ef...
Mixing in a stratified ocean is controlled by different physics, depending on the large-scale Richardson number. At high Richardson numbers, mixing is controlled by interactions between internal wave ...

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