A multigrid semi-implicit ยฎnite difference method is presented to solve the two-dimensional shallow water equations which describe the behaviour of basin water under the inยฏuence of the Coriolis force, atmospheric pressure gradients and tides. The semi-implicit ยฎnite difference method discretizes im
A particle-in-cell method for the solution of two-layer shallow-water equations
โ Scribed by Benoit Cushman-Roisin; Oleg E. Esenkov; Benedict J. Mathias
- Publisher
- John Wiley and Sons
- Year
- 2000
- Tongue
- English
- Weight
- 831 KB
- Volume
- 32
- Category
- Article
- ISSN
- 0271-2091
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โฆ Synopsis
A particle-in-cell (PIC) numerical method developed for the study of shallow-water dynamics, when the moving fluid layer is laterally confined by the intersection of its top and bottom surfaces, is described. The effect of ambient rotation is included for application to geophysical fluids, particularly open-ocean buoyant vortices in which the underlying density interface outcrops to the surface around the rim of the vortex. Extensions to include the dynamical effect of a second moving layer (baroclinicity) and the presence of a lateral rigid boundary (sidewall) are also described. Although the method was developed for oceanographic investigations, applications to other fluid mechanics problems would be straightforward.
๐ SIMILAR VOLUMES
A novel scheme has been developed for data reconstruction within a Godunovtype method for solving the shallow-water equations with source terms. In contrast to conventional data reconstruction methods based on conservative variables, the water surface level is chosen as the basis for data reconstruc