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- W2057381888 abstract "Abstract The tidal stress formulation is used to investigate the dynamics generating and governing tidally induced meso-scale recirculations in wide coastal sea straits for an idealized barotropic tidal wave. Particular attention is paid to the Lagrangian aspects of the residual dynamics and we present a first-order estimate of the Lagrangian tidal stress field in terms of a quasi-Eulerian field. The strength of the Lagrangian tidal stress may be related in a simple expression to the gradient of the bottom friction strength and the area swept out by the principal tidal current ellipse. We apply the analysis to the rectification processes active over a strongly sloping escarpment within an idealized representation of a wide coastal sea strait. It is demonstrated that the residual circulation for each of the Eulerian, Stokes’and Lagrangian cases is essentially governed by forced quasigeostrophic dynamics with source term being the curl of the relevant tidal stress. When the spatial dimension of the source term approaches the dimension of the basin, coastal boundary conditions become important. Finally, it is shown that the generation of an observed cyclonic basin-wide eddy in eastern Dixon Entrance, British Columbia, Canada is consistent with a tidal rectification process active over the strongly sloping escarpment connecting Dixon Entrance and Hecate Strait. It is concluded that a sufficiently strong rectification process active over a limited sector of the eddy circumference may substantially influence the circulation within adjacent bodies of water where no significant tidal nonlinearities are present." @default.
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- W2057381888 date "1991-11-01" @default.
- W2057381888 modified "2023-09-26" @default.
- W2057381888 title "Lagrangian tidal stress and basin-wide residual eddy dynamics in wide coastal sea straits" @default.
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- W2057381888 doi "https://doi.org/10.1080/03091929108227776" @default.
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