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- W2012591723 abstract "Abstract Results are presented of calculations on the generation of residual vorticity by tidal currents over the bottom topography of the Southern Bight of the North Sea. A typical order of magnitude is 10−6 to 10−7 s −1. This is compared with current measurements on calm days, when similar magnitudes are found. At windspeeds less than about 5 m/s tidal generation of residual vorticity is important; at higher windspeeds wind effects begin to dominate. Our results are relevant in understanding the spatial variability of residual currents, because a non-zero vorticity implies the existence of horizontal gradients in the residual current field." @default.
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- W2012591723 date "1981-08-01" @default.
- W2012591723 modified "2023-09-24" @default.
- W2012591723 title "Residual vorticity induced by the action of tidal currents in combination with bottom topography in the Southern Bight of the North Sea" @default.
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- W2012591723 doi "https://doi.org/10.1080/03091928108208775" @default.
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