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The Flow of a Two-Layer Fluid over Topography in a Polar Ocean
Two-Layer Fluid Topography Polar Ocean
2009/3/24
A two-layer model is constructed for wind-driven flow over topography in a closed polar basin where the variation of Coriolis force with latitude is negligible. The model equations are reduced using s...
The problem of water waves propagating over a mud bottom, characterized as a laminar viscous fluid, is treated in several ways. First, two complete models are present, each valid for different lower (...