This paper describes a numerical method with two time levels for solving partial differential equations that represent layered models of ocean circulation. The method is designed to be used with a barotropic-baroclinic splitting that separates the fast and slow motions into subsystems that are solve
โฆ LIBER โฆ
A finite-element model of two-layer ocean circulation
โ Scribed by R. Bermejo
- Publisher
- John Wiley and Sons
- Year
- 1990
- Tongue
- English
- Weight
- 602 KB
- Volume
- 29
- Category
- Article
- ISSN
- 0029-5981
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