A Forward-in-Time Advection Scheme and A
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David E. Stevens; S. Bretherton
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Article
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1996
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Elsevier Science
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English
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the Boussinesq approximation is constant, while in the anelastic approximation is a known function of height z. This paper presents a new forward-in-time advection method for nearly incompressible flow, MU, and its application to an adaptive For many flows, a ''multilevel'' scheme that incorporates