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A Determination of Horizontal Divergence in the Gulf Stream off Cape Lookout
Horizontal Divergence Gulf Stream off Cape Lookout
2009/3/9
A horizontal divergence of 2×10−5 sec−1 was determined by tracking three shallow drogues in the speed axis of the Gulf Stream. Concurrent bathythermograph soundings along a drogue track su...
Meanders of the Gulf Stream Downstream from Cape Hatteras 1975–1978
Gulf Stream Downstream Cape Hatteras
2009/2/5
Weekly Gulf Stream paths within 1000 km downstream of Cape Hatteras were obtained for 1975–78 from the Navy's weekly EOFA charts based on satellite IR imagery. They displayed two dominant meander mode...
The K1 Tide on the Continental Shelf from Nova Scotia to Cape Hatteras
K1 Tide Nova Scotia Continental Shelf Cape Hatteras
2009/1/21
A description is given of the K1 tide over the northeast continental shelf off North America from Nova Scotia to Cape Hatteras. Analyzed pressure data obtained from W. Brown and J. Irish (University o...
Baroclinic Flow and Transient-Tracer Fields in the Canary–Cape Verde Basin
Baroclinic Flow Canary–Cape Verde Basin Transient-Tracer Fields
2009/1/12
Simulated transient-tracer distributions (tritium, 3H3, freons) on the isopycnal horizons σ0=26.5 and 26.8 kg m−3 are presented for the East Atlantic, 10° −40°N. Tracer transport is modele...
Coastal Countercurrent and Mesoscale Eddy Formation by Tidal Rectification near an Oceanic Cape
Coastal Countercurrent Mesoscale Eddy Formation Tidal Rectification Oceanic Cape
2009/1/9
Cape St. James is an extensive triangular-shaped promontory located in a tidally energetic region at the southern tip of the Queen Charlotte Islands approximately 150 km off the mainland coast or Brit...
Mixing and Intrusions in a Rotating Cold-Core Feature off Cape Blanco, Oregon
surface water temperature surface structure turbulence-free
2009/1/5
During August 1986, a large cold anomaly was observed in satellite and in situ measurements near Cape Blanco at 42°N, 126°30′W off the Pacific Coast. Detailed vertical profiles of temperature, conduct...
Potential Vorticity Balances and Horizontal Divergence along Particle Trajectories in Gulf Stream Meanders East of Cape Hatteras
Potential Vorticity Balances Horizontal Divergence Particle Trajectories Gulf Stream
2009/1/5
Trajectories of 37 isopycnal RAFOS floats launched in the Gulf Stream off Cape Hatteras have been analyzed to examine the dynamics of meanders from a Lagrangian viewpoint. Using the float data in conj...
Rossby Wave Radiation in the Cape Verde Frontal Zone
Rossby Wave Radiation Cape Verde Frontal Zone
2008/12/22
Radiating baroclinic Rossby waves excited through instability of the Cape Verde frontal zone are proposed as a mechanism for the generation of mesoscale variability at middepth (1000 m) in the southea...
A Meddy off Cape St. Vincent. Part I：Description
Mediterranean source water Cape St. Vincent
2008/12/16
A meddy, an eddy formed from Mediterranean source water, was surveyed in detail with two types of expendable profilers and a CTD instrument. The muddy comprised two distinct, vertically aligned tenses...
Isopycnal and Diapycnal Mixing at the Cape Verde Frontal Zone
Cape Verde Frontal Zone Atlantic Central Waters eastern North Atlantic
2008/12/12
The Cape Verde Frontal Zone separates the North and the South Atlantic Central Waters in the eastern North Atlantic. It also represents the boundary between the ventilated subtropical gyre and the qua...
The Dynamics of the East Australian Current System: The Tasman Front, the East Auckland Current, and the East Cape Current
East Australian Current System Tasman Front East Auckland Current East Cape Current
2008/7/30
The dynamics of the flow field surrounding New Zealand are investigated using a series of global ocean models. The physical mechanisms governing the direction, magnitude, and location of the East Aust...
The Dynamics of the East Australian Current System: The Tasman Front, the East Auckland Current, and the East Cape Current
East Australian Current Tasman Front East Auckland Current East Cape Current
2008/7/30
The dynamics of the flow field surrounding New Zealand are investigated using a series of global ocean models. The physical mechanisms governing the direction, magnitude, and location of the East Aust...
Eddy Shedding from a Boundary Current around a Cape over a Sloping Bottom
Eddy Shedding Boundary Current Cape Sloping Bottom
2008/7/1
The authors discuss laboratory experiments that elucidate the mechanism of formation and westward drift of anticyclonic baroclinic vortices from a buoyant surface current flowing along a lateral bound...
Observations and Laboratory Modeling of Meddy Generation at Cape St. Vincent（图）
Observations Laboratory Modeling Meddy Generation Cape St. Vincent
2008/5/23
The AMUSE, CANIGO, and AMPOR observations provided a large amount of subsurface float data showing evidence of several distinctly different flow behaviors within the Mediterranean Water layers in the ...
Department of Oceanography at the University of Cape Town
海洋物理学 海洋气候学 physical oceanography ocean climatology
2007/12/24
Department of Oceanography at the University of Cape Townaims to advance knowledge of all facets of the ocean environment, and to use this knowledge for the benefit of people everywhere. The emphasis ...