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A Theory of Upwelling Over the Shelf Break     Upwelling  Shelf Break       font style='font-size:12px;'> 2009/3/24
The three-dimensional circulation produced in a homogeneous ocean by a steady wind stress is investigated when the bottom topography contains a discontinuity in gradient, such as occurs at the edge ...
On the Possibilities of Coastal, Mid-Shelf, and Shelf Break Upwelling     Coastal  Mid-Shelf  Shelf Break Upwelling       font style='font-size:12px;'> 2009/3/24
The steady-state circulation on a continental shelf under the combined influence of a wind stress, a surface density distribution, and a longshore current over the shelf break is investigated in a lin...
We present current observations from depths of 20, 50, 100 and 175 m obtained over a 3-year period near the northeast Gulf of Alaska shelf break, and emphasize a 2-year continuous segment from 50 m de...
Time series of a 40-day (13 March-23 April 1979) wind and current observational experiment are analyzed. The wind data originated from the Fortaleza Airport Weather Station (Ceará, Brazil), and the cu...
The properties of the semidiurnal internal tide, in the region of the shelf-break, at a location on the Australian North West Shelf are discussed. Information is derived from an analysis of thermistor...
A small scale but energetic and highly nonlinear anticyclonic eddy was observed near the New England Shelf Break in July 1983. Satellite images show a tongue of shelf water 15 km wide flowing offshore...
Hydraulic Jump and Undular Bore Formation on a Shelf Break     Hydraulic Jump  Undular Bore Formation  Shelf Break       font style='font-size:12px;'> 2009/1/6
The evolution of the semidiurnal internal tide as it propagates across the Australian North West Shelf is discussed analytically. As the tide is of long wavelength and small amplitude, this evolution ...
Internal Tides over a Shelf Break:Analytical Model and Observations     Internal Tides  Shelf Break       font style='font-size:12px;'> 2008/12/27
Data collected on Cruise ONDINE 85 organized by the Service Hydrophique et Ocèanographique de la Marine, at two points (P1 and P6) near the continental shelf break of the Bay of Biscay, show very larg...
A mechanism is described for the formation or a front at the edge of a continental shelf in an initially linearly stratified fluid lacking horizontal density gradients. A primitive equation numerical ...
A depth-independent model for the tidal rectification process is developed in order to explain the residual Eulerian velocity observed at the top of a shelf edge. An approximation of the nonlinear equ...
Analyses of data from three shipborne surveys describe the quasi-synoptic density and velocity fields near Barrow Canyon, Alaska. The canyon parallels the northwestern coast of Alaska and contains thr...

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