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• W2087648054 endingPage "713" @default.
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• W2087648054 abstract "A two-dimensional numerical model is applied to a coastal ocean wherein alongshore elevation and density gradients, normally calculated by a three-dimensional model, are instead supplied by climatologically averaged data for the California Current System between 25 and 40°N. Surface wind stress is also obtained from climatological data. Both surface and bottom boundary layers are resolved in the model calculations; a second moment turbulence closure submodel supplies vertical diffusivities. Near steady state solutions are possible when surface buoyancy flux is imposed at the surface. Model results are as follows: Southward wind stress produces a broad equatorward current with an embedded coastal jet in accordance with previous studies. Positive wind stress curl reduces the jet current and produces a poleward undercurrent which then surfaces as the curl is increased. The jet currents are reduced and poleward flow increases as bottom steepness increases; to a lesser extent, inclusion of the beta effect has a similar effect. The existence of near bottom, poleward or equatorward flow is explained rather simply in terms of the bottom stress resulting from the alongshore balance of surface wind stress and vertically integrated pressure gradient, the latter involving the alongshore surface elevation and density gradient. A further finding is that the upwelling circulation associated with wind stress is confined to the top 200 to 300 m of the ocean along the California coast." @default.
• W2087648054 created "2016-06-24" @default.
• W2087648054 creator A5083284681 @default.
• W2087648054 date "1986-01-01" @default.
• W2087648054 modified "2023-10-14" @default.
• W2087648054 title "Numerical simulation and analysis of the mean coastal circulation off California" @default.
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• W2087648054 doi "https://doi.org/10.1016/0278-4343(86)90033-6" @default.
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