Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/50053
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dc.contributor.authorPerez Hernandez, Maria Doloresen_US
dc.contributor.authorHernández-Guerra, Alonsoen_US
dc.contributor.authorFraile Nuez,Eugenioen_US
dc.contributor.authorComas-Rodríguez, Isisen_US
dc.contributor.authorBenítez-Barrios, Verõnica M.en_US
dc.contributor.authorDomínguez-Yanes, J. Franciscoen_US
dc.contributor.authorVélez-Belchí, Pedroen_US
dc.contributor.authorDe Armas, Demetrioen_US
dc.contributor.otherPerez-Hernandez, Maria-
dc.contributor.otherVelez-Belchi, Pedro-
dc.contributor.otherHernandez-Guerra, Alonso-
dc.contributor.otherFraile-Nuez, Eugenio-
dc.date.accessioned2018-11-24T12:53:33Z-
dc.date.available2018-11-24T12:53:33Z-
dc.date.issued2013en_US
dc.identifier.issn2169-9275en_US
dc.identifier.urihttp://hdl.handle.net/10553/50053-
dc.description.abstractThe source of the Canary Current has been inferred from an inverse box model appliedto the hydrographic data of a survey carried out in 2009 in the northeast subtropical gyre(29–37N, 9–24W). The Portugal Current is observed between 13.5 and 14.8W at 37N carrying 1:8+-0:4 Sv southward. This current presumably merges with the eastwardtransport of the Azores Current System and partly contributes to the Mediterranean inflowand partly to the northward recirculation of the Azores Current through the Gulf of Cadiz.The Azores Current System is located in the meridional range 33.50–36.25N at 24.50W.This System transports eastward 7:260:5 Sv in the thermocline layers and 1:160:8Svatintermediate layers. The Azores Current intermediate water mass has the highest portion ofSub-Arctic intermediate water (SAIW) in the region, while the Azores Countercurrentintermediate waters mass is mainly Mediterranean water. The Canary Current extends from 22.25 to 18.50Wat29N, the westernmost position ever observed. This current transports southward -6:2+-0:6 Sv in the thermocline layers and-2:0+-0:8 Sv in the intermediatelayers. This intermediate flow shows a relative maximum of oxygen and a relativeminimum in nutrient concentration, indicating the presence of SAIW. The study concludesthat, at least in fall 2009, the Canary Current extends to the intermediate waters(n<-27:9220 approximately 1600 dbar) and that Azores Current feeds the Canary Currentat surface and intermediate layers.en_US
dc.languageengen_US
dc.relationCtm2005-04701-C02-02-01/Mar. Origen de la Corriente de Canarias.en_US
dc.relationExpedición de Circunnavegación Malaspina 2010: Cambio Global y Exploración Del Océano Globalen_US
dc.relation.ispartofJournal of geophysical research. Oceansen_US
dc.sourceJournal of Geophysical Research: Oceans, v. 118, p. 2874-2891en_US
dc.subject2510 Oceanografíaen_US
dc.subject.otherCanary currenten_US
dc.subject.otherAzores currenten_US
dc.subject.otherInverse box modelen_US
dc.subject.otherEastern boundaryen_US
dc.subject.otherCirculationen_US
dc.titleThe source of the Canary current in fall 2009en_US
dc.typeinfo:eu-repo/semantics/Articleen_US
dc.typeArticleen_US
dc.identifier.doi10.1002/jgrc.20227en_US
dc.identifier.scopus84882791834-
dc.identifier.isi000324885500009-
dcterms.isPartOfJournal Of Geophysical Research-Oceans
dcterms.sourceJournal Of Geophysical Research-Oceans[ISSN 2169-9275],v. 118 (6), p. 2874-2891
dc.contributor.authorscopusid50861902200-
dc.contributor.authorscopusid6701736545-
dc.contributor.authorscopusid12139561900-
dc.contributor.authorscopusid36464839700-
dc.contributor.authorscopusid24398599500-
dc.contributor.authorscopusid55312796800-
dc.contributor.authorscopusid7801599223-
dc.contributor.authorscopusid8236928000-
dc.description.lastpage2891en_US
dc.description.firstpage2874en_US
dc.relation.volume118en_US
dc.investigacionCienciasen_US
dc.type2Artículoen_US
dc.contributor.daisngid3057975-
dc.contributor.daisngid660191-
dc.contributor.daisngid1139939-
dc.contributor.daisngid6273786-
dc.contributor.daisngid2251871-
dc.contributor.daisngid6073466-
dc.contributor.daisngid1378362-
dc.contributor.daisngid2250811-
dc.identifier.investigatorRIDJ-5330-2014-
dc.identifier.investigatorRIDI-9150-2017-
dc.identifier.investigatorRIDA-4747-2008-
dc.identifier.investigatorRIDD-1521-2010-
dc.utils.revisionen_US
dc.contributor.wosstandardWOS:Perez-Hernandez, MD-
dc.contributor.wosstandardWOS:Hernandez-Guerra, A-
dc.contributor.wosstandardWOS:Fraile-Nuez, E-
dc.contributor.wosstandardWOS:Comas-Rodriguez, I-
dc.contributor.wosstandardWOS:Benitez-Barrios, VM-
dc.contributor.wosstandardWOS:Dominguez-Yanes, JF-
dc.contributor.wosstandardWOS:Velez-Belchi, P-
dc.contributor.wosstandardWOS:De Armas, D-
dc.date.coverdateEnero 2013en_US
dc.identifier.ulpgces
dc.description.jcr3,44
dc.description.jcrqQ1
item.grantfulltextopen-
item.fulltextCon texto completo-
crisitem.author.deptIOCAG: Oceanografía Física-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.deptFísica-
crisitem.author.deptIOCAG: Oceanografía Física-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.deptFísica-
crisitem.author.orcid10.1175/JPO-D-13-0136.1-
crisitem.author.orcid0000-0002-4883-8123-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.fullNamePérez Hernández, María Dolores-
crisitem.author.fullNameHernández Guerra, Alonso-
crisitem.author.fullNameFraile Nuez,Eugenio-
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