Evidence for an eastward flow along the Central and South American Caribbean Coast

11 pages, 8 figures, 2 tables.-- Full-text version available Open Access at: http://www.iim.csic.es/~barton/html/pdfs.html Hydrographic transects suggest an eastward flow with a subsurface core along the entire southern boundary of the Caribbean Sea. The transport of the coastal limb of the Panama-C...

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Published in:Journal of Geophysical Research
Main Authors: Andrade, Carlos Alberto, Barton, Eric D., Mooers, Christopher N. K.
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2003
Subjects:
Online Access:http://hdl.handle.net/10261/2627
https://doi.org/10.1029/2002JC001549
id ftcsic:oai:digital.csic.es:10261/2627
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spelling ftcsic:oai:digital.csic.es:10261/2627 2024-02-11T10:06:35+01:00 Evidence for an eastward flow along the Central and South American Caribbean Coast Andrade, Carlos Alberto Barton, Eric D. Mooers, Christopher N. K. 2003-06-12 653310 bytes application/pdf http://hdl.handle.net/10261/2627 https://doi.org/10.1029/2002JC001549 en eng American Geophysical Union http://dx.doi.org/10.1029/2002JC001549 Journal of Geophysical Research - Part C - Oceans 108(C6): 3185 (2003) 0148-0227 http://hdl.handle.net/10261/2627 doi:10.1029/2002JC001549 open Undercurrents Ocean circulation Caribbean Sea artículo http://purl.org/coar/resource_type/c_6501 2003 ftcsic https://doi.org/10.1029/2002JC001549 2024-01-16T09:18:46Z 11 pages, 8 figures, 2 tables.-- Full-text version available Open Access at: http://www.iim.csic.es/~barton/html/pdfs.html Hydrographic transects suggest an eastward flow with a subsurface core along the entire southern boundary of the Caribbean Sea. The transport of the coastal limb of the Panama-Colombia Gyre (PCG), known as the Panama-Colombia Countercurrent, decreases toward the east (from ∼6 Sv off Panama), as water is lost into the recirculation of the PCG. Off Panama, the flow is strongest at the surface, but, off Colombia, it is strongest at around 100 m. A portion of the counterflow (∼1 Sv) continues eastward along the Colombian coast as far as the Guajira region (12°N, 72°W), where it submerges to become an undercurrent beneath the coastal upwelling center there. The eastward flow also occurs in the Venezuela Basin, beneath the coastal upwelling region off Cariaco Basin and exits the Caribbean through the Grenada Channel at around 200 m depth. Numerical simulations suggest that this flow, counter to the Caribbean Current, is a semi-continuous feature along the entire southern boundary of the Caribbean, and that it is associated with offshore cyclonic eddies. It probably constitutes part of the Sverdrup circulation of the Tropical North Atlantic cyclonic cell. This work had financial support of the Colombian Institute for the Development of Science and Technology COLCIENCIAS, project 96-044 and the Colombian Navy. Also, the Office of Naval Research provided funding for C. N. K. Mooers and E. D. Barton during manuscript preparation. Peer reviewed Article in Journal/Newspaper North Atlantic Digital.CSIC (Spanish National Research Council) Barton ENVELOPE(-58.733,-58.733,-62.233,-62.233) Journal of Geophysical Research 108 C6
institution Open Polar
collection Digital.CSIC (Spanish National Research Council)
op_collection_id ftcsic
language English
topic Undercurrents
Ocean circulation
Caribbean Sea
spellingShingle Undercurrents
Ocean circulation
Caribbean Sea
Andrade, Carlos Alberto
Barton, Eric D.
Mooers, Christopher N. K.
Evidence for an eastward flow along the Central and South American Caribbean Coast
topic_facet Undercurrents
Ocean circulation
Caribbean Sea
description 11 pages, 8 figures, 2 tables.-- Full-text version available Open Access at: http://www.iim.csic.es/~barton/html/pdfs.html Hydrographic transects suggest an eastward flow with a subsurface core along the entire southern boundary of the Caribbean Sea. The transport of the coastal limb of the Panama-Colombia Gyre (PCG), known as the Panama-Colombia Countercurrent, decreases toward the east (from ∼6 Sv off Panama), as water is lost into the recirculation of the PCG. Off Panama, the flow is strongest at the surface, but, off Colombia, it is strongest at around 100 m. A portion of the counterflow (∼1 Sv) continues eastward along the Colombian coast as far as the Guajira region (12°N, 72°W), where it submerges to become an undercurrent beneath the coastal upwelling center there. The eastward flow also occurs in the Venezuela Basin, beneath the coastal upwelling region off Cariaco Basin and exits the Caribbean through the Grenada Channel at around 200 m depth. Numerical simulations suggest that this flow, counter to the Caribbean Current, is a semi-continuous feature along the entire southern boundary of the Caribbean, and that it is associated with offshore cyclonic eddies. It probably constitutes part of the Sverdrup circulation of the Tropical North Atlantic cyclonic cell. This work had financial support of the Colombian Institute for the Development of Science and Technology COLCIENCIAS, project 96-044 and the Colombian Navy. Also, the Office of Naval Research provided funding for C. N. K. Mooers and E. D. Barton during manuscript preparation. Peer reviewed
format Article in Journal/Newspaper
author Andrade, Carlos Alberto
Barton, Eric D.
Mooers, Christopher N. K.
author_facet Andrade, Carlos Alberto
Barton, Eric D.
Mooers, Christopher N. K.
author_sort Andrade, Carlos Alberto
title Evidence for an eastward flow along the Central and South American Caribbean Coast
title_short Evidence for an eastward flow along the Central and South American Caribbean Coast
title_full Evidence for an eastward flow along the Central and South American Caribbean Coast
title_fullStr Evidence for an eastward flow along the Central and South American Caribbean Coast
title_full_unstemmed Evidence for an eastward flow along the Central and South American Caribbean Coast
title_sort evidence for an eastward flow along the central and south american caribbean coast
publisher American Geophysical Union
publishDate 2003
url http://hdl.handle.net/10261/2627
https://doi.org/10.1029/2002JC001549
long_lat ENVELOPE(-58.733,-58.733,-62.233,-62.233)
geographic Barton
geographic_facet Barton
genre North Atlantic
genre_facet North Atlantic
op_relation http://dx.doi.org/10.1029/2002JC001549
Journal of Geophysical Research - Part C - Oceans 108(C6): 3185 (2003)
0148-0227
http://hdl.handle.net/10261/2627
doi:10.1029/2002JC001549
op_rights open
op_doi https://doi.org/10.1029/2002JC001549
container_title Journal of Geophysical Research
container_volume 108
container_issue C6
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