Meridional transports in the Atlantic Ocean at 7.5N and 24.5N in 1992-1993 and 2010-2011
European Geosciences Union General Assembly 2013, 7-12 April, Vienna, Austria An inverse model has been applied to two oceanographic cruises carried out in 2010 and 2011 at 7.5N and 24.5N, respectively. Results have been compared to a reanalysis of these same sections conducted in 1992 and 1993, in...
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ftcsic:oai:digital.csic.es:10261/89061 2024-02-11T09:58:36+01:00 Meridional transports in the Atlantic Ocean at 7.5N and 24.5N in 1992-1993 and 2010-2011 Hernández Guerra, Alonso Pelegrí, Josep Lluís Fraile-Nuez, Eugenio 2013-04-09 http://hdl.handle.net/10261/89061 en eng European Geosciences Union http://meetingorganizer.copernicus.org/EGU2013/posters/11861 e-issn: 1607-7962 Geophysical Research Abstracts 15: EGU2013-9085 (2013) http://hdl.handle.net/10261/89061 open póster de congreso http://purl.org/coar/resource_type/c_6670 2013 ftcsic 2024-01-16T09:55:13Z European Geosciences Union General Assembly 2013, 7-12 April, Vienna, Austria An inverse model has been applied to two oceanographic cruises carried out in 2010 and 2011 at 7.5N and 24.5N, respectively. Results have been compared to a reanalysis of these same sections conducted in 1992 and 1993, in the frame of theWOCE program. The inverse model encompasses 17 equations and 196/226 unknowns for 1992/2011, corresponding to the velocities in the reference layer. Different constraints have been considered: transport of Antarctic BottomWater and DeepWestern Boundary Current at 7N, transport of the Florida Current, and transport of the Antilles Current and Deep Western Boundary Current at 24N. The analysis shows stronger thermocline and Antarctic Bottom Water transports during 1992-1993 than during 2010-2011 Peer Reviewed Still Image Antarc* Antarctic Digital.CSIC (Spanish National Research Council) Antarctic |
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Open Polar |
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Digital.CSIC (Spanish National Research Council) |
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ftcsic |
language |
English |
description |
European Geosciences Union General Assembly 2013, 7-12 April, Vienna, Austria An inverse model has been applied to two oceanographic cruises carried out in 2010 and 2011 at 7.5N and 24.5N, respectively. Results have been compared to a reanalysis of these same sections conducted in 1992 and 1993, in the frame of theWOCE program. The inverse model encompasses 17 equations and 196/226 unknowns for 1992/2011, corresponding to the velocities in the reference layer. Different constraints have been considered: transport of Antarctic BottomWater and DeepWestern Boundary Current at 7N, transport of the Florida Current, and transport of the Antilles Current and Deep Western Boundary Current at 24N. The analysis shows stronger thermocline and Antarctic Bottom Water transports during 1992-1993 than during 2010-2011 Peer Reviewed |
format |
Still Image |
author |
Hernández Guerra, Alonso Pelegrí, Josep Lluís Fraile-Nuez, Eugenio |
spellingShingle |
Hernández Guerra, Alonso Pelegrí, Josep Lluís Fraile-Nuez, Eugenio Meridional transports in the Atlantic Ocean at 7.5N and 24.5N in 1992-1993 and 2010-2011 |
author_facet |
Hernández Guerra, Alonso Pelegrí, Josep Lluís Fraile-Nuez, Eugenio |
author_sort |
Hernández Guerra, Alonso |
title |
Meridional transports in the Atlantic Ocean at 7.5N and 24.5N in 1992-1993 and 2010-2011 |
title_short |
Meridional transports in the Atlantic Ocean at 7.5N and 24.5N in 1992-1993 and 2010-2011 |
title_full |
Meridional transports in the Atlantic Ocean at 7.5N and 24.5N in 1992-1993 and 2010-2011 |
title_fullStr |
Meridional transports in the Atlantic Ocean at 7.5N and 24.5N in 1992-1993 and 2010-2011 |
title_full_unstemmed |
Meridional transports in the Atlantic Ocean at 7.5N and 24.5N in 1992-1993 and 2010-2011 |
title_sort |
meridional transports in the atlantic ocean at 7.5n and 24.5n in 1992-1993 and 2010-2011 |
publisher |
European Geosciences Union |
publishDate |
2013 |
url |
http://hdl.handle.net/10261/89061 |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_relation |
http://meetingorganizer.copernicus.org/EGU2013/posters/11861 e-issn: 1607-7962 Geophysical Research Abstracts 15: EGU2013-9085 (2013) http://hdl.handle.net/10261/89061 |
op_rights |
open |
_version_ |
1790594292953120768 |