Barotropic-Baroclinic Time Splitting for
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Robert L. Higdon; Roland A. de Szoeke
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Article
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1997
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Elsevier Science
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English
⚖ 752 KB
external waves were not present. The restriction on the time step can be removed by using an implicit method [11]; Numerical models of ocean circulation admit motions varying on a wide range of time scales. These motions include fast external this approach requires that a large system of algebraic