A factored implicit scheme for numerical
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J. M. Augenbaum; S. E. Cohn; E. Isaacson; D. P. Dee; D. Marchesin
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Article
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1985
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John Wiley and Sons
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English
β 662 KB
The nonlinear partial differential equations of atmospheric dynamics govern motion on two time scales, a fast one and a slow one. Only the slow-scale motions are relevant in predicting the evolution of large weather patterns. Implicit numerical methods are therefore attractive for weather prediction