Derivation of a two-layer non-hydrostatic shallow water model
A theoretical non-hydrostatic model is developed to describe the dynamics of a two-layer shallow water system in the presence of viscous and Coriolis effects. The Navier-Stokes equations are integrated over the water depth in each layer to obtain the layer-mean equations. To close the resulting equa...
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| Format: | Others |
| Language: | en-US |
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Water Resources Research Center, University of Hawaii at Manoa
2012
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| Online Access: | http://hdl.handle.net/10125/21919 |