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Articles 151 - 157 of 157
Full-Text Articles in Oceanography and Atmospheric Sciences and Meteorology
Observation Of Shelfwater Overrunning The Southern Slope Sea, Ajoy Kumar
Observation Of Shelfwater Overrunning The Southern Slope Sea, Ajoy Kumar
OES Theses and Dissertations
Analyses of two years (1992 and 1993) of high resolution (1.47 km2) sea surface temperature satellite images of the southern Mid-Atlantic Bight (MAB), showed that unusually extensive overhang of shelf water occurs episodically, and coherently over along shelf distances of several hundred kilometers. These episodes are dubbed overrunning of the Slope Sea by shelf water. The overrunning volume has a "face" and a "back" (southern and northern limit). It transports substantial quantities of shelf water southward, and does not retreat onto the shelf, but eventually joins the western edge of the Gulf Stream in the vicinity of Chesapeake …
Circulation, Winter 1996, Center For Coastal Physical Oceanography, Old Dominion University
Circulation, Winter 1996, Center For Coastal Physical Oceanography, Old Dominion University
CCPO Circulation
Winter 1996 issue of CCPO Circulation featuring article "The Ocean Mesoscale"
Toga Notes - October 1994 - Number 17, Nova Southeastern University
Toga Notes - October 1994 - Number 17, Nova Southeastern University
TOGA Notes
No abstract provided.
Toga Notes - October 1993 - Number 13, Nova Southeastern University
Toga Notes - October 1993 - Number 13, Nova Southeastern University
TOGA Notes
No abstract provided.
Flow Kinematics And Dynamics Of The Gulf Stream From Composite Imagery, Caitlin Patrice Mullen
Flow Kinematics And Dynamics Of The Gulf Stream From Composite Imagery, Caitlin Patrice Mullen
OES Theses and Dissertations
A unique set of contemporaneous satellite-tracked drifters and five-day composite satellite images of the North Atlantic is studied in order to infer the near-surface flow kinematics and dynamics of the Gulf Stream. Using fractal and spectral analyses, two kinematic models, and a potential vorticity model, detailed comparisons are made between these data sets.
Fractal and spectral analyses show that the data set is not fractal, there is no geographic variability, and there is not a strong fractal scaling link between the drifter trajectories and composite temperature fronts as had been postulated by several investigators. These results indicate considerably more work …
Toga Notes - July 1993 - Number 12, Nova Southeastern University
Toga Notes - July 1993 - Number 12, Nova Southeastern University
TOGA Notes
No abstract provided.
Toga Notes - January 1995 - Number 18, Nova Southeastern University
Toga Notes - January 1995 - Number 18, Nova Southeastern University
TOGA Notes
No abstract provided.