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- W1994849908 abstract "The previously reported occurrence of tidal fronts on the Patagonian Shelf (Carreto et al., 1986, Journal of Plankton Research,8, 15–28; Glorioso, 1987, Continental Shelf Research, 7, 27–34), motivated the application of a numerical model to solve the shallow-water equations with external forcing by the principal-lunar semidiurnal tide (M2) prescribed along the open boundary. The mean width of the Patagonian Shelf is comparable with a quarter wavelength of the semidiurnal tide, giving the conditions for standing wave resonance at that frequency (Webb, 1975, Deep-Sea Research,23, 1–15). The region is well recognized by its large tidal elevations and by the speed of the tidal wave changing phase very rapidly. Some of the results obtained from the modelling exercise include the mapping of the M2 tidal constants, the Simpson-Hunter stratification parameter, the mean sea surface elevation, and the distribution of tidal energy dissipation by bottom friction. These results agree qualitatively with the ship data available and with satellite infrared imagery." @default.
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- W1994849908 date "1994-02-01" @default.
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- W1994849908 title "Numerical modelling of the M2 tide on the northern Patagonian Shelf" @default.
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- W1994849908 doi "https://doi.org/10.1016/0278-4343(94)90016-7" @default.
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