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Self-Advection of Density Perturbations on a Sloping Continental Shelf
Density Perturbations Self-Advection Sloping Continental Shelf
2009/2/5
Bottom water movement on the continental shelf is modeled by the nonlinear interaction between long-shore bottom geostrophic flow and the density field. Bottom geostrophic velocity, subject to linear ...
Circulation Induced by River Inflow in Well Mixed Water over a Sloping Continental Shelf
River Inflow Sloping Continental Shelf Well Mixed Water
2009/1/21
The pressure field over a sloping continental shelf subject to freshwater runoff at the coast can be resolved into a nearly two-dimensional dynamic height field and a residual field, the latter arisin...
Obliquely Incident Poincaré Waves on a Sloping Continental Shelf
Sloping Continental Shelf Obliquely Incident Poincaré Waves
2008/11/24
An analytical theory of barotropic tides propagating onto a sloping continental shelf from the deep ocean is developed. The plane Poincaré waves incident from the deep ocean are obliquely angled, and ...