Energy conservative and - stable schemes for the two - layer shallow water equations
نویسنده
چکیده
The two-layer shallow water equations model the flow of two fluids of different densities, superimposed on each other, under the influence of gravity. The main assumption in the derivation is that the horizontal length scales are much bigger than the vertical scales, and that one can therefore neglect variations in depth of density and velocity.Furthermore, it is assumed that no mixing occurs between the fluids. In one spatial dimension the equations have the form
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تاریخ انتشار 2010