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- W3836851 abstract "The Strait of Gibraltar is a channel with a permanent two-layer flow strongly modulated by energetic tidal currents. Compared with the open ocean thermocline, turbulent dissipation rates, ε, are high throughout the strait. Two flow regimes, however, have particularly intense dissipation: the lee west of Camarinal Sill during strong outflow of Mediterranean water, and the internal bore or solitary wave propagating eastward from the sill after reversal of the tide. Overturns exceeding 50 m and ε greater than 10-3 W kg-1 were observed in the lee of the sill. Dissipation rates of 10-5 to 10-4 W kg-1 were found behind the leading edge of the bore as it moved eastward through Tarifa Narrows, dropping the interface more than 100 m in less than 15 minutes." @default.
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- W3836851 date "1988-01-01" @default.
- W3836851 modified "2023-09-26" @default.
- W3836851 title "Turbulent Dissipation in the Strait of Gibraltar and Associated Mixing" @default.
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- W3836851 doi "https://doi.org/10.1016/s0422-9894(08)70547-6" @default.
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