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dc.contributor.authorMohamed-Santamaría, Saraes_ES
dc.contributor.authorGilcoto, Migueles_ES
dc.contributor.authorPadín, X. A.es_ES
dc.contributor.authorÁlvarez-Fernández, María Jesúses_ES
dc.contributor.authorPérez, Fiz F.es_ES
dc.date.accessioned2018-06-19T11:59:15Z-
dc.date.available2018-06-19T11:59:15Z-
dc.date.issued2018-
dc.identifier.citationEncuentro de Oceanografía Física (2018)es_ES
dc.identifier.urihttp://hdl.handle.net/10261/166624-
dc.description1 poster.-- V Encuentro de Oceanografía Física, Vigo, 20, 21 y 22 de junio de 2018es_ES
dc.description.abstractThe Ría de Vigo belongs to a set of four embayments known as the "Rias Baixas", located on the Eastern boundary of the North Atlantic Ocean, which present a residual circulation pattern in two layers driven by the coastal upwelling/downwelling events occurring at these latitudes. Vigo is the southernmost of the Rías Baixas and its physical and chemical properties use to follow seasonal cycleses_ES
dc.description.sponsorshipFunding for this study was provided by the Spanish Ministry of Economy and Competitiveness under the A.RIOS (CTM2016- 76146-C3) research projectes_ES
dc.language.isoenges_ES
dc.rightsopenAccessen_EN
dc.titleRía de Vigo and adjacent shelf hydrography: seasonal descriptiones_ES
dc.typepóster de congresoes_ES
dc.description.peerreviewedPeer reviewedes_ES
dc.embargo.terms2018-06-24es_ES
dc.relation.csices_ES
oprm.item.hasRevisionno ko 0 false*
Appears in Collections:(IIM) Comunicaciones congresos
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