Numerical Study of Barotropic and Barocl
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Stefan Diebels
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Article
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1995
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Elsevier Science
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English
โ 348 KB
The fluid motion in a strongly stratified lake can be described by a set of nonlinear dispersive partial differential equations derived from the equations of motion. These model equations are solved numerically by an implicit finite difference scheme. Variable topography and the influence of the fre