The shallow water equations in spherical geometry provide a first prototype for developing and testing numerical algorithms for atmospheric circulation models. Since the seventies these models have often been solved with spectral methods. Increasing demands on grid resolution combined with massive p
Time Integration of the Shallow Water Equations in Spherical Geometry
✍ Scribed by D. Lanser; J.G. Blom; J.G. Verwer
- Publisher
- Elsevier Science
- Year
- 2001
- Tongue
- English
- Weight
- 206 KB
- Volume
- 171
- Category
- Article
- ISSN
- 0021-9991
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✦ Synopsis
The shallow water equations in spherical geometry provide a prototype for developing and testing numerical algorithms for atmospheric circulation models. In a previous paper we have studied a spatial discretization of these equations based on an Osher-type finite-volume method on stereographic and latitude-longitude grids. The current paper is a companion devoted to time integration. Our main aim is to discuss and demonstrate a third-order, A-stable, Runge-Kutta-Rosenbrock method. To reduce the costs related to the linear algebra operations, this linearly implicit method is combined with approximate matrix factorization. Its efficiency is demonstrated by comparison with a classical, third-order explicit, Runge-Kutta method. For that purpose we use a known test set from literature. The comparison shows that the Rosenbrock method is by far superior.
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