Identificador persistente para citar o vincular este elemento: http://hdl.handle.net/10553/49053
Campo DC Valoridioma
dc.contributor.authorKnoll, M.en_US
dc.contributor.authorHernandez-Guerra, Aen_US
dc.contributor.authorLenz, B.en_US
dc.contributor.authorLópez Laatzen, F.en_US
dc.contributor.authorMachin, Fen_US
dc.contributor.authorMüller, T. J.en_US
dc.contributor.authorSiedler, G.en_US
dc.contributor.otherMachin, Francisco-
dc.contributor.otherHernandez-Guerra, Alonso-
dc.date.accessioned2018-11-24T03:33:17Z-
dc.date.available2018-11-24T03:33:17Z-
dc.date.issued2002en_US
dc.identifier.issn0967-0645en_US
dc.identifier.urihttp://hdl.handle.net/10553/49053-
dc.description.abstractTo study the Eastern Boundary Current system off Northwest Africa in detail several CTD/ADCP-sections and long-term mooring work were carried out in the channel between Lanzarote and Africa. The observations are compared with a fine-resolution model, which was developed in the framework of the CANIGO project. The water masses, which are observed in this area, are characterised and classified in density ranges. The current field shows a high spatial and temporal variability with maximum velocities of about 35 cm/s. Seasonal means as well as currents averaged across the channel are only a few cm/s. In the surface water a steady southward flow in the middle of the channel indicates the Canary Current in this area. During fall a strong northward current is observed close to the African shelf. Though the Canary Current strengthens during summer and fall due to an increase of the trade winds, the transport in the channel decreases or turns northward during that time due to the enhanced poleward current at the eastern side. A northward undercurrent with a mean velocity of +2.3 cm/s is observed at the African slope in 950 m depth. The poleward transport of AAIW increases during fall and a strong influence of relatively fresh AAIW is observed during that time. Most of the observations fit well to the results of the CANIGO model, but the occurrence of MW at the bottom of the channel and the corresponding southward flow cannot be resolved by the model.en_US
dc.languageengen_US
dc.publisher0967-0645-
dc.relation.ispartofDeep-Sea Research Part II: Topical Studies in Oceanographyen_US
dc.sourceDeep-Sea Research Part Ii-Topical Studies In Oceanography [ISSN 0967-0645], v. 49 (17), p. 3427-3440en_US
dc.subject251007 Oceanografía físicaen_US
dc.subject.otherCanary Islandsen_US
dc.subject.otherAfrican coasten_US
dc.titleThe Eastern Boundary Current system between the Canary Islands and the African Coasten_US
dc.typeinfo:eu-repo/semantics/Articlees
dc.typeArticlees
dc.identifier.doi10.1016/S0967-0645(02)00105-4
dc.identifier.scopus0036392932-
dc.identifier.isi000178183000003-
dcterms.isPartOfDeep-Sea Research Part Ii-Topical Studies In Oceanography-
dcterms.sourceDeep-Sea Research Part Ii-Topical Studies In Oceanography[ISSN 0967-0645],v. 49 (17), p. 3427-3440-
dc.contributor.authorscopusid15749504500-
dc.contributor.authorscopusid6701736545-
dc.contributor.authorscopusid7004037280-
dc.contributor.authorscopusid6506580233-
dc.contributor.authorscopusid6602804374-
dc.contributor.authorscopusid56408776800-
dc.contributor.authorscopusid36505067700-
dc.description.lastpage3440-
dc.description.firstpage3427-
dc.relation.volume49-
dc.investigacionCienciasen_US
dc.type2Artículoen_US
dc.contributor.daisngid3685105-
dc.contributor.daisngid660191-
dc.contributor.daisngid6319834-
dc.contributor.daisngid7384830-
dc.contributor.daisngid1451397-
dc.contributor.daisngid2931366-
dc.contributor.daisngid773534-
dc.identifier.investigatorRIDA-9287-2009-
dc.identifier.investigatorRIDA-4747-2008-
dc.utils.revisionen_US
dc.contributor.wosstandardWOS:Knoll, M
dc.contributor.wosstandardWOS:Hernandez-Guerra, A
dc.contributor.wosstandardWOS:Lenz, B
dc.contributor.wosstandardWOS:Laatzen, FL
dc.contributor.wosstandardWOS:Machin, F
dc.contributor.wosstandardWOS:Muller, TJ
dc.contributor.wosstandardWOS:Siedler, G
dc.date.coverdateOctubre 2002
dc.identifier.ulpgces
dc.description.scieSCIE
item.grantfulltextnone-
item.fulltextSin texto completo-
crisitem.author.deptGIR IOCAG: Oceanografía Física-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.deptDepartamento de Física-
crisitem.author.deptGIR ECOAQUA: Oceanografía Física y Geofísica Aplicada-
crisitem.author.deptIU de Investigación en Acuicultura Sostenible y Ec-
crisitem.author.deptDepartamento de Física-
crisitem.author.orcid0000-0002-4883-8123-
crisitem.author.orcid0000-0002-4281-6804-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.parentorgIU de Investigación en Acuicultura Sostenible y Ec-
crisitem.author.fullNameHernández Guerra, Alonso-
crisitem.author.fullNameMachín Jiménez, Francisco José-
Colección:Artículos
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