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- W1974419526 abstract "A method for obtaining geostrophic currents in a stratified ocean is discussed. It combines the use of hydrographic data and numerical modelling. For geostrophic flow in a flatbottom stratified ocean it is shown along the lines of Gill and Clarke (1974, Deep-Sea Research, 21, 325–345) that the surface elevation is determined by the barotropic mode. Experience indicates strongly that this also is the case when the depth varies. Hence the surface elevation, or equivalently the surface velocity, can be obtained from the depth-averaged equations. The variation with depth of the current is determined from hydrographic measurements, assuming that the baroclinic field is in geostrophic balance. When integrating in the vertical, the velocity at the sea surface obtained from the numerical computations is used as an absolute reference velocity. The method has been applied to the flow in the Faroe-Shetland Channel using meteorological data for the atmospheric forcing. The field data are from Foldvik andKvinge (1975), and were collected during ‘Overflow—1973’. The computations were performed for one particular wind event associated with an atmospheric low pressure passage. We find a net flux of 2.9 Sv of Atlantic water into the Norwegian Sea for the considered period of time. At the bottom of the channel there was a flow of 0.7 Sv of Norwegian Sea water into the Atlantic in the same period. On examining our calculated vertical velocity profiles in the channel, we find a level of zero motion which is not far from the position of the 35‰ isohaline. These results are discussed in connection with long-time average fluxes reported elsewhere in the literature." @default.
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- W1974419526 date "1986-01-01" @default.
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- W1974419526 title "Geostrophic currents in shelf areas" @default.
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- W1974419526 doi "https://doi.org/10.1016/0278-4343(86)90029-4" @default.
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