Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/12767
DC FieldValueLanguage
dc.contributor.authorFraile Nuez, Eugenioen_US
dc.contributor.authorHernández-Guerra, Alonsoen_US
dc.contributor.otherFraile-Nuez, Eugenio-
dc.contributor.otherHernandez-Guerra, Alonso-
dc.date.accessioned2015-02-10T03:30:20Z-
dc.date.accessioned2018-06-15T09:20:00Z-
dc.date.available2015-02-10T03:30:20Z-
dc.date.available2018-06-15T09:20:00Z-
dc.date.issued2006en_US
dc.identifier.issn0094-8276en_US
dc.identifier.urihttp://hdl.handle.net/10553/12767-
dc.description.abstractA trans-oceanic section at 24.5°N in the North Atlantic has been sampled at a decadal frequency. This work demonstrates that the wind-driven component of the Meridional Overturning Circulation (MOC) may be monitored using autonomous profiling floats deployed in the eastern North Atlantic Subtropical Gyre. More than 500 CTD vertical profiles from the surface to 2000 m depth, spanning one year (from April 2002 to March 2003), are used to compute the geostrophic transport stream function at 24.5°N. The baroclinic transport obtained from the autonomous profiling floats is not statistically different than that from three hydrographic cruises carried out in 1957, 1981 and 1992. A good agreement is found between the geostrophic transport stream function and the transport derived from the wind field through the Sverdrup relation.en_US
dc.formatapplication/pdfes
dc.languageengen_US
dc.relation.ispartofGeophysical Research Lettersen_US
dc.rightsby-nc-ndes
dc.sourceGeophysical Research Letters [ISSN 0094-8276], v. 33 (3), (L03601)en_US
dc.subject251007 Oceanografía físicaen_US
dc.subject.otherMeridional Overturning Circulationen_US
dc.subject.otherOcean Circulationen_US
dc.subject.otherHydrographic Dataen_US
dc.subject.otherHeat-Transporten_US
dc.subject.otherWater Massesen_US
dc.subject.otherThermoclineen_US
dc.subject.otherMechanismsen_US
dc.subject.otherDesignen_US
dc.titleWind-driven circulation for the eastern North Atlantic Subtropical Gyre from Argo dataen_US
dc.typeinfo:eu-repo/semantics/articleen_US
dc.typeArticleen_US
dc.identifier.doi10.1029/2005GL025122en_US
dc.identifier.scopus33645820635-
dc.identifier.isi000235156500005-
dcterms.isPartOfGeophysical Research Letters-
dcterms.sourceGeophysical Research Letters[ISSN 0094-8276],v. 33 (3)-
dc.contributor.authorscopusid12139561900-
dc.contributor.authorscopusid6701736545-
dc.identifier.absysnet336627-
dc.relation.volume33en_US
dc.investigacionCienciasen_US
dc.rights.accessrightsinfo:eu-repo/semantics/openAccesses
dc.type2Artículoen_US
dc.identifier.wosWOS:000235156500005-
dc.contributor.daisngid1139939-
dc.contributor.daisngid660191-
dc.identifier.investigatorRIDD-1521-2010-
dc.identifier.investigatorRIDA-4747-2008-
dc.utils.revisionen_US
dc.contributor.wosstandardWOS:Fraile-Nuez, E-
dc.contributor.wosstandardWOS:Hernandez-Guerra, A-
dc.date.coverdateFebrero 2006en_US
dc.identifier.ulpgcen_US
dc.contributor.buulpgcBU-BASen_US
dc.description.jcr2,602
dc.description.jcrqQ1
dc.description.scieSCIE
item.grantfulltextopen-
item.fulltextCon texto completo-
crisitem.author.deptGIR IOCAG: Oceanografía Física-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.deptDepartamento de Física-
crisitem.author.orcid0000-0002-4883-8123-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.fullNameFraile Nuez,Eugenio-
crisitem.author.fullNameHernández Guerra, Alonso-
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