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Continental-Slope Sedimentation: The View from Northern California
Northern California Continental-Slope Sedimentation
2015/8/13
The slope portion of the STRATAFORM program sets out to establish a better understanding of the sedimentary processes important in developing the stratigraphic record of continental slopes over the pa...
Barotropic and Baroclinic Tides over the Continental Slope and Shelf off Oregon
Baroclinic Tides Barotropic Continental Slope Shelf off Oregon
2009/2/13
During the Coastal Upwelling Experiment of 1973, several current meter moorings were deployed on the Oregon continental shelf and slope. Data from 16 current meters and temperature sensors which were ...
Gulf Stream Fluctuations and Meanders over the Onslow Bay Upper Continental Slope
sea surface temperature Onslow Bay Upper Continental Slope
2009/2/9
Gulf Stream fluctuations observed over the 200 and 400 m isobaths off Onslow Bay, North Carolina have a prominent weekly time scale. The principal fluctuations observed during the 4-month winter exper...
Current Meter Observations on the Continental Slope at Two Sites in the Eastern Gulf of Mexico
Current Meter Observations Eastern Gulf of Mexico Continental Slope
2009/2/8
Current-meter observations obtained at two sites on the continental slope of the eastern Gulf of Mexico, at nominal positions of 29°N, 88°W (the Mobile site) and 27.5°N, 85.5°W (the Tampa site) are pr...
Turbulent Dissipation Over the Continental Slope Off Vancouver Island
Continental Slope Vancouver Island internal wave energy
2009/2/6
Thirteen profiles of the rate of viscous dissipation of turbulent kinetic energy &epsi¯ were made over the continental slope off Vancouver Island between 12 and 14 May 1980 in conjunction with CT...
“Pycnobathic” Currents over the Upper Continental Slope
“Pycnobathic” Currents Upper Continental Slope
2009/1/15
The dynamic interaction of a sloping seafloor with along-isobath density variation is calculated for cases involving a sharp pycnocline and a surface-to-bottom front. Pycnocline depth is supposed to v...
Mixed Instabilities in the Gulf Stream over the Continental Slope
Gulf Stream Continental Slope
2009/1/14
A numerical model study is presented of the unstable normal modes of oscillation of a boundary current. The model background current approximates the Gulf Stream south of Cape Hatteras, North Carolina...
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 ...
Hydrographic and Current Observations on the Continental Slope and Shelf of the Western Equatorial Atlantic
North Brazil Coastal Current Continental Slope Western Equatorial Atlantic
2009/1/12
Hydrographic and current-profiling data from December 1980 and current-meter data obtained between September 1980 and November 1981 from the continental slope and shelf of the western equatorial Atlan...
Topographic Waves over the Continental Slope
Topographic Waves Continental Slope Gulf Stream
2009/1/5
Current meter data taken during a one-year period over the continental slope and upper rise in three cross-isobath sections have been examined for energy distribution, coherence, and phase propagation...
A Model of Gulf Stream Frontal Instabilities, Meanders and Eddies along the Continental Slope
Gulf Stream Continental Slope
2009/1/5
For a simplified model of the Gulf Stream front along a vertical-walled continental slope of a constant-depth ocean basin, the dynamics governing frontal instabilities, meanders, and eddies depend pri...
Separation of a Density Current from the Bottom of a Continental Slope
Density Current Bottom of a Continental Slope
2008/10/24
Separation from the continental slope of stratified jets like the Gulf Stream involves the sliding of successive isopycnal layers from a nearly horizontal bottom to the adjacent offshore isopycnal in ...
A Nonlinear Model of the Shoaling and Refraction of Interfacial Solitary Waves in the Ocean. Part II: Oblique Refraction across a Continental Slope and Propagation over a Seamount
Nonlinear Model Interfacial Solitary Waves Oblique Refraction Continental Slope Seamount
2008/7/25
The refraction of internal solitary waves can be due to variations in water depth, nonlinearity, stratification, or shear. This paper addresses the effects of the first two of these effects. Part I of...
The Effect of Continental Slope on Buoyancy-Driven Circulation
Effect of Continental Slope Buoyancy-Driven Circulation
2008/7/21
The effect of continental slope on buoyancy-driven circulation has been studied using a two-layer quasigeostrophic model. In the model, buoyancy flux is incorporated as interfacial mass flux, which co...
Hydrographic observations and current measurements with a Shipboard Acoustic Doppler Current Profiler over the continental shelf–slope junction northeast of Taiwan during 10–17 August 1994 allow the c...