Identificador persistente para citar o vincular este elemento: http://hdl.handle.net/10553/46711
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dc.contributor.authorFernández-Castro, B.en_US
dc.contributor.authorMouriño-Carballido, B.en_US
dc.contributor.authorBenítez-Barrios, V. M.en_US
dc.contributor.authorChouciño, P.en_US
dc.contributor.authorFraile Nuez,Eugenioen_US
dc.contributor.authorGraña, R.en_US
dc.contributor.authorPiedeleu, M.en_US
dc.contributor.authorRodríguez-Santana, A.en_US
dc.contributor.otherMourino, Beatriz-
dc.contributor.otherRodriguez-Santana, Angel-
dc.contributor.otherFernandez Castro, Bieito-
dc.contributor.otherFraile Nuez, Eugenio-
dc.date.accessioned2018-11-23T07:18:14Z-
dc.date.available2018-11-23T07:18:14Z-
dc.date.issued2014en_US
dc.identifier.issn0967-0637en_US
dc.identifier.urihttp://hdl.handle.net/10553/46711-
dc.description.abstractMeasurements of microstructure turbulence were carried out, in the upper 300 m, in the tropical and subtropical Atlantic and Pacific oceans during the Malaspina 2010 expedition, by using a microstructure turbulence (MSS) profiler. Diapycnal diffusivity () was estimated from dissipation rates of turbulent kinetic energy (ε) measured by the MSS profiler, and also from hydrographic and meteorological data by using the K-profile parameterization (KPP). In the mixing layer, averaged () and ε () were three and one orders of magnitude higher, respectively, compared to the ocean interior ( and ). In general, the KPP showed a good agreement with diffusivity estimates derived from microstructure observations, both in the mixing layer and in the ocean interior. The KPP also reproduced the main regional patterns observed in the ocean interior. The analysis of turbulence generation mechanisms below the mixing layer showed that shear-induced mixing was more important in those regions influenced by the equatorial undercurrent, where averaged diffusivity was . Favorable conditions for salt fingers formation were more frequently observed in the Atlantic, where, as a consequence of this process, diffusivity could increase up to 20%. This result could have important implications for the transport of heat and dissolved substances in these regions.en_US
dc.languageengen_US
dc.publisher0967-0637-
dc.relationModelo Físico-Químico Para la Región Macaronesica. Evaluación y Potencial Aplicación Aperacionalen_US
dc.relation.ispartofDeep-Sea Research Part I: Oceanographic Research Papersen_US
dc.sourceDeep-Sea Research Part I: Oceanographic Research Papers [ISSN 0967-0637], v. 94, p. 15-30en_US
dc.subject251007 Oceanografía físicaen_US
dc.subject.otherMicrostructure turbulenceen_US
dc.subject.otherTropical and subtropical oceansen_US
dc.subject.otherDiffusivityen_US
dc.subject.otherK-profile parameterizationen_US
dc.subject.otherSalt fingersen_US
dc.titleMicrostructure turbulence and diffusivity parameterization in the tropical and subtropical Atlantic, Pacific and Indian Oceans during the Malaspina 2010 expeditionen_US
dc.typeinfo:eu-repo/semantics/Articleen_US
dc.typeArticleen_US
dc.identifier.doi10.1016/j.dsr.2014.08.006en_US
dc.identifier.scopus84907533681-
dc.identifier.isi000345820100002-
dcterms.isPartOfDeep-Sea Research Part I-Oceanographic Research Papers-
dcterms.sourceDeep-Sea Research Part I-Oceanographic Research Papers[ISSN 0967-0637],v. 94, p. 15-30-
dc.contributor.authorscopusid55328276500-
dc.contributor.authorscopusid23027967000-
dc.contributor.authorscopusid24398599500-
dc.contributor.authorscopusid21233296900-
dc.contributor.authorscopusid12139561900-
dc.contributor.authorscopusid37123775000-
dc.contributor.authorscopusid35072816600-
dc.contributor.authorscopusid55954140200-
dc.description.lastpage30en_US
dc.description.firstpage15en_US
dc.relation.volume94en_US
dc.investigacionCienciasen_US
dc.type2Artículoen_US
dc.identifier.wosWOS:000345820100002-
dc.contributor.daisngid3605654-
dc.contributor.daisngid1617789-
dc.contributor.daisngid2689889-
dc.contributor.daisngid2251871-
dc.contributor.daisngid6135836-
dc.contributor.daisngid1139939-
dc.contributor.daisngid5384158-
dc.contributor.daisngid6555405-
dc.contributor.daisngid1821092-
dc.identifier.investigatorRIDE-8635-2016-
dc.identifier.investigatorRIDH-8596-2015-
dc.identifier.investigatorRIDC-4321-2015-
dc.identifier.investigatorRIDNo ID-
dc.identifier.externalWOS:000345820100002-
dc.contributor.wosstandardWOS:Fernandez-Castro, B-
dc.contributor.wosstandardWOS:Mourino-Carballido, B-
dc.contributor.wosstandardWOS:Benitez-Barrios, VM-
dc.contributor.wosstandardWOS:Choucino, P-
dc.contributor.wosstandardWOS:Fraile-Nuez, E-
dc.contributor.wosstandardWOS:Grana, R-
dc.contributor.wosstandardWOS:Piedeleu, M-
dc.contributor.wosstandardWOS:Rodriguez-Santana, A-
dc.date.coverdateDiciembre 2014en_US
dc.identifier.ulpgces
dc.description.sjr1,557
dc.description.jcr2,566
dc.description.sjrqQ1
dc.description.jcrqQ1
dc.description.scieSCIE
item.fulltextSin texto completo-
item.grantfulltextnone-
crisitem.project.principalinvestigatorGonzález Dávila, Melchor-
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.orcid0000-0003-1960-6777-
crisitem.author.parentorgIU de Investigación en Acuicultura Sostenible y Ec-
crisitem.author.fullNameFraile Nuez,Eugenio-
crisitem.author.fullNameRodríguez Santana, Ángel-
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