Please use this identifier to cite or link to this item: http://hdl.handle.net/10773/25177
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dc.contributor.authorAlvarez, I.pt_PT
dc.contributor.authorGomez-Gesteira, M.pt_PT
dc.contributor.authorDeCastro, M.pt_PT
dc.contributor.authorLorenzo, M. N.pt_PT
dc.contributor.authorCrespo, A. J. C.pt_PT
dc.contributor.authorDias, J. M.pt_PT
dc.date.accessioned2019-01-21T16:39:01Z-
dc.date.available2019-01-21T16:39:01Z-
dc.date.issued2011-
dc.identifier.issn0278-4343pt_PT
dc.identifier.urihttp://hdl.handle.net/10773/25177-
dc.description.abstractUpwelling conditions have been simultaneously analyzed along the western and northern coast of the Iberian Peninsula in terms of wind forcing and water temperature response. The wind forcing analysis showed that the season under more upwelling favorable conditions corresponds to spring–summer (April–September) along the western coast and only to summer (June–August) along the northern one. Taking into account the upwelling period common to both coasts (June–August), it was observed that the occurrence of upwelling events simultaneously along both coasts is the most probable situation (∼46%) followed by upwelling unfavorable conditions also along both coasts (∼26%). The analysis of sea surface temperature data also showed the existence of an upwelling season in spring–summer along both coasts, although upwelling events are more frequent and intense along the western coast than along the northern one. Chlorophyll concentrations showed a high seasonal variability at the western coast with the highest concentrations values in spring–summer months while at the northern coast the maximum values were observed in spring and autumn.pt_PT
dc.description.sponsorshipThis work is supported by the Ministerio de Ciencia e Innovacion under projects CTM2007-62546-C03-03/MAR and CGL2009-09143 and by Xunta de Galicia under projects PGIDIT06PXIB383285PR and PGIDIT06PXIB383288PR. Authors thank the valuable comments of Dr. M. Varela and Dr. J.L. Gomez-Gesteira which helped to improve the quality of the manuscript. One of us (I.A.) has been supported by the Fundação para a Ciência e a Tecnologia through a post-doctoral grant (SFRH/BPD/38292/2007).pt_PT
dc.language.isoengpt_PT
dc.publisherElsevierpt_PT
dc.relationinfo:eu-repo/grantAgreement/FCT/SFRH/SFRH%2FBPD%2F38292%2F2007/PTpt_PT
dc.rightsrestrictedAccesspt_PT
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/pt_PT
dc.subjectUpwellingpt_PT
dc.subjectIberian Peninsulapt_PT
dc.subjectEkman transportpt_PT
dc.subjectSSTpt_PT
dc.subjectChlorophyllpt_PT
dc.titleComparative analysis of upwelling influence between the western and northern coast of the Iberian Peninsulapt_PT
dc.typearticlept_PT
dc.description.versionpublishedpt_PT
dc.peerreviewedyespt_PT
degois.publication.firstPage388pt_PT
degois.publication.issue5pt_PT
degois.publication.lastPage399pt_PT
degois.publication.titleContinental Shelf Researchpt_PT
degois.publication.volume31pt_PT
dc.identifier.doi10.1016/j.csr.2010.07.009pt_PT
dc.identifier.essn1873-6955pt_PT
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