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dc.contributor.authorGilcoto, Migueles_ES
dc.contributor.authorLargier, J.es_ES
dc.contributor.authorBarton, Eric D.es_ES
dc.contributor.authorPiedracoba, Silviaes_ES
dc.contributor.authorTorres, R.es_ES
dc.contributor.authorGraña, R.es_ES
dc.contributor.authorAlonso Pérez, Fernandoes_ES
dc.contributor.authorVillacieros-Robineau, Nicoláses_ES
dc.contributor.authorGranda Grandoso, Francisco de laes_ES
dc.date.accessioned2017-06-06T11:23:59Z-
dc.date.available2017-06-06T11:23:59Z-
dc.date.issued2017-
dc.identifier.citationGeophysical Research Letters 44(5): 2388-2397 (2017)es_ES
dc.identifier.issn0094-8276-
dc.identifier.urihttp://hdl.handle.net/10261/150965-
dc.description10 páginas, 4 figurases_ES
dc.description.abstractBays/estuaries forced by local wind show bidirectional exchange flow. When forced by remote wind, they exhibit unidirectional flow adjustment to coastal sea level. Acoustic Doppler Current Profiler observations over 1 year show that the Ria de Vigo (Iberian Upwelling) responds to coastal wind events with bidirectional exchange flow. The duration of the upwelling and downwelling events, estimated from the current variability, was ~3.3 days and ~2.6 days, respectively. Vectorial correlations reveal a rapid response to upwelling/downwelling, in which currents lag local wind by <6 h and remote wind by <14 h, less than the Ekman spinup (17.8 h). This rapidity arises from the ria's narrowness (nonrotational local response), equatorward orientation (additive remote and local wind responses), depth greater than the Ekman depth (penetration of shelf circulation into the interior), and vertical stratification (shear reinforcing shelf circulation). Similar rapid responses are expected in other narrow bays where local and remote winds act together and stratification enhances bidirectional flowes_ES
dc.description.sponsorshipThe field work and data analysis were supported by the Spanish Ministry of Economy and Competitivity under STRAMIX research project (CTM2012-35155). Writing up was completed with the aid of support from Xunta de Galicia (Contrato Programa Xunta-CSIC). J.L.L. thanks California Sea grant (2014-R/HCME-04) for supportes_ES
dc.language.isoenges_ES
dc.publisherAmerican Geophysical Uniones_ES
dc.relation.isversionofPublisher's versiones_ES
dc.rightsopenAccessen_EN
dc.titleRapid response to coastal upwelling in a semienclosed bayes_ES
dc.typeartículoes_ES
dc.identifier.doi10.1002/2016GL072416-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttp://dx.doi.org/10.1002/2016GL072416es_ES
dc.identifier.e-issn1944-8007-
dc.embargo.terms2017-08-16es_ES
dc.relation.csices_ES
oprm.item.hasRevisionno ko 0 false*
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