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A Numerical Model of the Depth-Dependent, Wind-Driven Upwelling Circulation on a Continental shelf
Depth-Dependent Continental shelf Wind-Driven Upwelling Circulation
2009/2/23
A numerical model of the upwelling circulation on a continental shelf is presented which employs f-plane dynamics. is continuously stratified, and assumes that all quantities are uniform alongshore wi...
A Simple Analytical Model of Low-Frequency Wind-Driven Upwelling on a Continental Slope
Low-Frequency Wind-Driven Upwelling Continental Slope
2009/1/13
A simple closed-form analytical solution of a classical coastal upwelling is found in terms of two-dimensional baroclinic waves trapped in a two-layer ocean on a steep continental slope and forced by ...
Steady Wind-driven Upwelling in the Presence of a Baroclinic Coastally Trapped Jet
Wind-driven Upwelling Baroclinic Coastally Trapped Jet
2009/1/12
The usual two-layer model for steady wind-driven upwelling along a uniform coastline is extended to incorporate the effects of an upper-layer jet trapped against the coast. The characteristic width of...
Enhancement of Wind-Driven Upwelling and Downwelling by Alongshore Bathymetric Variability
Wind-Driven Alongshore Bathymetric
2008/6/20
Steady wind-driven flow along a shelf of changing width is described with a frictional barotropic model valid in the limit of small Rossby and Burger number. In these limits, an alongshore wind drives...
The Inner Shelf Response to Wind-Driven Upwelling and Downwelling
Inner Shelf Response Wind-Driven Upwelling Downwelling
2008/6/11
A two-dimensional numerical model is used to study the response to upwelling- and downwelling-favorable winds on a shelf with a strong pycnocline. During upwelling or downwelling, the pycnocline inter...