A MULTI-LEVEL NUMERICAL MODEL OF COASTAL
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A. D. Rao; S. Chamarthi
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Article
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1997
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John Wiley and Sons
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English
β 754 KB
A two-dimensional baroclinic model is described for coastal upwelling in a vertical plane perpendicular to the coast. The model consists of equations of motion, continuity and turbulence energy along with equations for salinity and thermal energy and an equation of state. The role of density gradien