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• W1556587807 abstract "Sloping boundaries in rotating, stratified fluids influence flow in their vicinity by supporting both trapped and reflected waves. Internal wave breaking caused by reflection at a sloping boundary produces microscale mixing. Spatial gradients of this mixing in turn may drive mean circulation near boundaries, both along and across isobaths, and may account for significant features of circulation. Trapped free wave and forced evanescent modes are possible at both subinertial and superinertial frequencies. These motions can account for much of the variance observed over topographic features in the ocean and for Eulerian mean currents as well. Without mixing, however, steady eddy fluxes cannot drive Lagrangian mean circulation, according to non-acceleration theorems." @default.
• W1556587807 created "2016-06-24" @default.
• W1556587807 creator A5063539271 @default.
• W1556587807 date "2013-03-19" @default.
• W1556587807 modified "2023-09-23" @default.
• W1556587807 title "Waves, Mixing, and Transports Over Sloping Boundaries" @default.
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• W1556587807 doi "https://doi.org/10.1029/ce054p0417" @default.
• W1556587807 hasPublicationYear "2013" @default.
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