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dc.contributor.authorSangrà, Pablo-
dc.contributor.authorPascual, Ananda-
dc.contributor.authorRodríguez-Santana, Ángel-
dc.contributor.authorMachín, Francisco-
dc.contributor.authorMason, Evan-
dc.contributor.authorMcWilliams, James C.-
dc.contributor.authorPelegrí, Josep Lluís-
dc.contributor.authorDong, Changming-
dc.contributor.authorRubio, Ana M.-
dc.contributor.authorArístegui, Javier-
dc.contributor.authorMarrero-Díaz, Ángeles-
dc.contributor.authorHernández Guerra, Alonso-
dc.contributor.authorMartínez-Marrero, Antonio-
dc.contributor.authorAuladell, Maricel-
dc.date.accessioned2009-11-11T08:18:39Z-
dc.date.available2009-11-11T08:18:39Z-
dc.date.issued2009-12-
dc.identifier.citationDeep-Sea Research Part I: Oceanographic Research Papers 56(12): 2100-2114 (2009)en_US
dc.identifier.issn0967-0637-
dc.identifier.urihttp://hdl.handle.net/10261/18475-
dc.description16 pages, 11 figures, 3 tableen_US
dc.description.abstractWe report, from remote sensing and in situ observations, a new type of permanent structure in the eastern subtropical Atlantic Ocean, that we call the ‘‘Canary Eddy Corridor’’. The phenomenon, is a zonal long-lived (43 months) mesoscale eddy corridor, whose source is the flow perturbation of the Canary Current and the Trade Winds at the Canary Islands. The latitudinal range of the corridor spans 221N–291N and extends from the Canaries to at least 32ºW, near the mid-Atlantic. This is the main region of longlived westward-propagating eddies in the subtropical northeast Atlantic. From a agedistribution study we observe that at least 10% of mesoscale eddies in this region are long-lived, with a dominance of anticyclones over cyclones. Another four westwardpropagating eddy corridors were also detected: two small corridors north and south of the Azores Front; a small zonal corridor located near 31ºN, south of the island of Madeira; and a small corridor located near the Cape Blanc giant filament. The existence of these corridors may change, at least for the northeastern subtropical Atlantic, the general idea that mesoscale eddies are disorganized, ubiquitous structures in the ocean. The Canary Eddy Corridor constitutes a direct zonal pathway that conveys water massand biogeochemical properties offshore from the Canary Island/Northwest Africa upwelling system, and may be seen as a recurrent offshore pump of organic matter and carbon to the oligotrophic ocean interior. Estimates of volume and mass transport indicate that Canary Eddy Corridor westward transport is more than one-fourth of the southward transport of the Canary Current. The westward transport of kinetic energy by the eddies of the Canary Corridor is as important as the southward transport by the Canary Current. The total primary production related to the Corridor may be as high as the total primary production of the northwest Africa upwelling system for the same latitude rangeen_US
dc.description.sponsorshipThis work was supported by the Spanish government through projects RODA (CTM2004-06842) and CANOA (CTM2005-00444/MAR), and by the US National Science Foundation project ‘‘Vorticity generation and eddy evolution in island wakes’’ (OCE 06-23011) and by NASA project ‘‘NNX08AI84G’’en_US
dc.format.extent8985 bytes-
dc.format.mimetypeapplication/pdf-
dc.language.isoengen_US
dc.publisherElsevieren_US
dc.rightsclosedAccessen_US
dc.subjectEddy corridoren_US
dc.subjectLong-lived eddiesen_US
dc.subjectEddies demographyen_US
dc.subjectEddy trackingen_US
dc.subjectNortheastern subtropical Atlanticen_US
dc.titleThe Canary Eddy Corridor: A major pathway for long-lived eddies in the subtropical North Atlanticen_US
dc.typeartículoen_US
dc.identifier.doi10.1016/j.dsr.2009.08.008-
dc.description.peerreviewedPeer revieweden_US
dc.relation.publisherversionhttps://doi.org/10.1016/j.dsr.2009.08.008en_US
dc.type.coarhttp://purl.org/coar/resource_type/c_6501es_ES
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextNo Fulltext-
item.cerifentitytypePublications-
item.openairetypeartículo-
item.languageiso639-1en-
item.grantfulltextnone-
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