Please use this identifier to cite or link to this item: http://dspace.mediu.edu.my:8181/xmlui/handle/10261/5381
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dc.creatorPelegrí, Josep Lluís-
dc.creatorMarrero-Díaz, Ángeles-
dc.creatorPérez Rodríguez, Pilar-
dc.date2008-06-26T11:34:54Z-
dc.date2008-06-26T11:34:54Z-
dc.date2001-
dc.date.accessioned2017-01-31T01:59:16Z-
dc.date.available2017-01-31T01:59:16Z-
dc.identifierScientia Marina 65(Suppl.1): 241-250 (2001)-
dc.identifier0214-8358 (print edition)-
dc.identifier1886-8134 (online edition)-
dc.identifierhttp://hdl.handle.net/10261/5381-
dc.identifier10.3989/scimar.2001.65s1241-
dc.identifier.urihttp://dspace.mediu.edu.my:8181/xmlui/handle/10261/5381-
dc.descriptionPublicación online disponible en: http://www.icm.csic.es/scimar/index.php-
dc.descriptionWe analysed historical data (Fraga and Manríquez, 1974; Manríquez and Fraga, 1978) to investigate the relation between the position of the Cape Verde frontal region and the geostrophic velocity field in summer and winter. The position of the front is well determined in the plotting of the salinity and nutrient distributions in isopycnic coordinates. The geostrophic velocity shows sharp gradients as a function of density and distance on sections normal to the coast. These gradients are reasonable well correlated with the frontal position and indicate the existence of strong meridional interleaving. The flow field relative to 400 m illustrates this interleaving as fluctuations on a westward mean flow. The surface temperature distribution undergoes very large latitudinal displacements but may help to locate the presence of north and south surface water.-
dc.descriptionThis work was supported by the Spanish government through CICYT´s project MAR96-1893. The principal author, PPR, wishes to thank the Ministerio de Educación y Ciencia of the Spanish government for funding during this work.-
dc.descriptionPeer reviewed-
dc.format1256319 bytes-
dc.formatapplication/pdf-
dc.languageeng-
dc.publisherCSIC - Instituto de Ciencias del Mar (ICM)-
dc.relationhttp://dx.doi.org/10.3989/scimar.2001.65s1241-
dc.rightsopenAccess-
dc.subjectCape Verde-
dc.subjectFrontal zone-
dc.subjectWater masses-
dc.subjectGeostrophic transport-
dc.subjectIsopycnic coordinates-
dc.titleDynamical characteristics of the Cape Verde frontal zone-
dc.typeArtículo-
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