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Deep Planetary Circulation and Topography：Simple Models of Midocean Flows
Deep Planetary Circulation Midocean Flows Topography
2009/1/4
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 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 Models of Flow over Deep Ocean Sills: Planetary and Semigeostrophic Solutions
Simple Models Semigeostrophic Solutions Deep Ocean Sills
2008/10/29
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...