By Jaques C.J. Nihoul (Eds.)
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Additional resources for Bottom Turbulence, Proceedings of The 8th International Liege Colloquium on Ocean Hydrodynamics
I ::::::::: ..... ,\ 1 : : : : : : : : : : : : : ,.. ,,, ......... , , , , , I _ _ . q[ ... \, , , ......... oo TIM . 6. : Current vectors at various levels from surface to bottom, s = O ( 0 . 2 5 ) 1 . 2 cm/sec. The vertical cross section illustrates the very large surface current produced b the wind with some return flow near the edges of the basin Two small vertical gyres at the northern and southern end of the basin have also developed. The next two plots show the diminution of the surface current, at its energy passes through the viscosity effect deeper into the basin.
M. DAVIES Institute of Oceanographic Sciences, Bidston Observatory, Birkenhead, Nerseyside L43 7RA, England. ABSTRACT This paper extends previous work by Davies (1976a), solving the three-dimensional hydrodynamic equations for tides and storm surges using a n expansion of B-splines, by allowing depth variation of vertical eddy viscosity and studying the influence of such variation on vertical current structure. The effect of changes in the surface and the bottom eddy viscosities upon current profile, for wind-driven motion in a rectangular basin, is examined in detail.
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