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The presence of broad, flowing water masses in the deep ocean requires dynamical explanation. Vertical density diffusion andβ-effect are invoked in classical theories; here we show how topographic pot...
Simple Models of Stratification     Simple Models  boundary conditions  buoyancy flux       font style='font-size:12px;'> 2008/12/24
Simple analytical and numerical models of gratified circulation are discussed. The models are driven by buoyancy and mechanical forcing, and buoyancy diffusion is parameterized in term of diapycnal ma...
Simple inverted reduced-gravity models of flow over deep ocean sills are considered, with emphasis placed on the case for which sills are wide with respect to the abyssal Rossby radius. When the lengt...

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