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• W2622632252 endingPage "420" @default.
• W2622632252 startingPage "397" @default.
• W2622632252 abstract "The oceanic bottom boundary layer extracts energy and momentum from the overlying flow, mediates the fate of near-bottom substances, and generates bedforms that retard the flow and affect benthic processes. The bottom boundary layer is forced by winds, waves, tides, and buoyancy and is influenced by surface waves, internal waves, and stratification by heat, salt, and suspended sediments. This review focuses on the coastal ocean. The main points are that (a) classical turbulence concepts and modern turbulence parameterizations provide accurate representations of the structure and turbulent fluxes under conditions in which the underlying assumptions hold, (b) modern sensors and analyses enable high-quality direct or near-direct measurements of the turbulent fluxes and dissipation rates, and (c) the remaining challenges include the interaction of waves and currents with the erodible seabed, the impact of layer-scale two- and three-dimensional instabilities, and the role of the bottom boundary layer in shelf-slope exchange." @default.
• W2622632252 created "2017-06-15" @default.
• W2622632252 creator A5052141695 @default.
• W2622632252 creator A5072194730 @default.
• W2622632252 date "2018-01-03" @default.
• W2622632252 modified "2023-10-01" @default.
• W2622632252 title "The Bottom Boundary Layer" @default.
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