In coastal oceanography there is interest in problems modeled by the shallow water equations, where variations in channel depth are accounted for by the presence of source terms. A numerical treatment for the solution of such problems is presented here, in terms of a hybrid approach, which combines
The Surface Gradient Method for the Treatment of Source Terms in the Shallow-Water Equations
β Scribed by J.G. Zhou; D.M. Causon; C.G. Mingham; D.M. Ingram
- Publisher
- Elsevier Science
- Year
- 2001
- Tongue
- English
- Weight
- 261 KB
- Volume
- 168
- Category
- Article
- ISSN
- 0021-9991
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β¦ Synopsis
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 reconstruction. This provides accurate values of the conservative variables at cell interfaces so that the fluxes can be accurately calculated with a Riemann solver. The main advantages are: (1) a simple centered discretization is used for the source terms; (2) the scheme is no more complicated than the conventional method for the homogeneous terms; (3) small perturbations in the water surface elevation can be accurately predicted; and (4) the method is generally suitable for both steady and unsteady shallow-water problems. The accuracy of the scheme has been verified by recourse to both steady and unsteady flow problems. Excellent agreement has been obtained between the numerical predictions and analytical solutions. The results indicate that the new scheme is accurate, simple, efficient, and robust.
π SIMILAR VOLUMES
This paper deals with the numerical solution of the shallow water equations in channels with irregular geometry but with a locally rectangular cross section. This type of channel leads to the presence of source terms involving the gradient of the depth and the breadth of the channel. Extensions of t
## Abstract The present work addresses the numerical prediction of shallow water flows with the application of the HLLE approximate Riemann solver. This Riemann solver has several desirable properties, such as, ease of implementation, satisfaction of entropy conditions, high shock resolution and po