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Evidence for deflection of the Gulf Stream at the Charleston rise

Journal Article · · Gulfstream; (United States)
OSTI ID:5881532
It has long been known that the Gulf Stream meanders laterally along the whole of the South Atlantic Bight (the continental margin between Capes Canaveral and Hatteras), but a quasi-permanent deflection of the Gulf Stream has recently been postulated offshore of Charleston, South Carolina. This supposition is supported by hydrographic data, nutrient data, and remotely sensed imagery of the sea surface topography.
DOE Contract Number:
EY-76-S-09-0902
OSTI ID:
5881532
Journal Information:
Gulfstream; (United States), Journal Name: Gulfstream; (United States) Vol. 4:9
Country of Publication:
United States
Language:
English