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The Dynamics of Oceanic Fronts. Part II：Shelf Water Structure Due to Freshwater Discharge
Shelf Water Structure Freshwater Discharge Oceanic Fronts
2009/2/10
In Part I of this series, a framework was introduced for the study of oceanic frontal dynamics. The dynamics was studied by posing an initial value problem, starting with a near-surface discharge of b...
Frictional Response of Continental Shelf Water to Local Wind Forcing
coastal sea level Continental Shelf Water Local Wind Forcing
2009/1/16
Because of relatively strong tidal currants and little notification, the response of continental shelf water to wired off South Carolina is predominantly frictional and barotropic. Currents measured a...
The Influence of Sloping Mean Density Surfaces on Low-Frequency Shelf Water Flow
Sloping Mean Density Surfaces Low-Frequency Shelf Water Flow
2009/1/7
A model is derived to explore the influence of sloping mean density surfaces on low-frequency wind-driven, frictional shelf water flow. The model coastline, isobaths and mean density field do not vary...
Numerical Study of Shelf Water Motion Driven by the Kuroshio：Barotropic Model
Barotropic Model Shelf Water Motion Driven coastal regions
2008/12/23
The barotropic response of the shelf and coastal regions south of Japan to short-term variations in the Kuroshio was studied numerically with an inflow–outflow model. The onshore–offshore movements of...
Entrainment of Shelf Water by a Bifurcating Continental Boundary Current
Bifurcating Continental Boundary Current Shelf Water cyclonic vorticity
2008/12/12
At the northeast corner of Taiwan the direction of the continental slope isobaths changes rapidly relative to the oncoming Kuroshio, so that the inertia of a small inshore fraction of this current cau...