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dc.contributor.authorLorenzo-Lacruz, Jorge-
dc.contributor.authorVicente Serrano, Sergio M.-
dc.contributor.authorLópez-Moreno, Juan I.-
dc.contributor.authorGonzález-Hidalgo, José C.-
dc.contributor.authorMorán-Tejeda, Enrique-
dc.date.accessioned2012-06-28T09:03:40Z-
dc.date.available2012-06-28T09:03:40Z-
dc.date.issued2011-08-24-
dc.identifier.citationHydrology and Earth System Sciences 15 (8): 2581–2597 (2011)es_ES
dc.identifier.issn1027-5606-
dc.identifier.urihttp://hdl.handle.net/10261/52417-
dc.description17 páginas, 7 figurases_ES
dc.description.abstract[EN] In this study we analyzed the influence of the North Atlantic Oscillation (NAO) on the streamflow in 187 sub-basins of the Iberian Peninsula. Monthly and one-month lagged correlations were conducted to assess the spatio-temporal extent of the NAO influence on Iberian river discharges. Analysis of the persistence of the winter NAO throughout the year was also undertaken, together with analysis of streamflow anomalies during positive and negative NAO phases. Moving-window correlation analyses were conducted to assess potential changes in the temporal evolution of the NAO influence on Iberian streamflows. The results show that the NAO has a large impact on surface water resources throughout the Iberian Peninsula during winter, and in the Atlantic watershed during autumn. We showed that water resources management and snowmelt are causing the persistent dependence of streamflows on the previous winter NAO. We found that strongly positive streamflow anomalies occurred during winter, especially in the Atlantic watershed, and provide evidence of non-stationarity and spatial variability in the NAO influence on Iberian water resources.es_ES
dc.description.sponsorshipWe would like to thank the Centro de Estudios Hidrográficos (CEDEX), Sistema Nacional de Información de Recursos Hídricos (SNIRH), Agencia Catalana de l’Aigua, Agencia Andaluza del Agua and Augas de Galicia for providing the hydrological data used in this study. We also want to thank to the Climate Research Unit for the North Atlantic Oscillation data. This work has been supported by a pre-doctoral fellowship by the Aragón Government (Spain), and by the research projects CGL2006-11619/HID and CGL2008-01189/BTE, financed by the Spanish Commission of Science and Technology and FEDER, EUROGEOSS (FP7-ENV-2008-1-226487), ACQWA (FP7-ENV- 2007-1-212250) financed by the VII Framework Programme of the European Commission, and “La nieve en el Pirineo Aragonés y su respuesta a la variabilidad climática” financed by “Obra Social La Caixa” and the Aragón Government.es_ES
dc.language.isoenges_ES
dc.publisherEuropean Geosciences Uniones_ES
dc.relationinfo:eu-repo/grantAgreement/EC/FP7/226487es_ES
dc.rightsopenAccesses_ES
dc.titleThe response of Iberian rivers to the North Atlantic Oscillationes_ES
dc.typeartículoes_ES
dc.identifier.doi10.5194/hess-15-2581-2011-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttp://dx.doi.org/10.5194/hess-15-2581-2011es_ES
dc.identifier.e-issn1607-7938-
dc.type.coarhttp://purl.org/coar/resource_type/c_6501es_ES
item.languageiso639-1en-
item.fulltextWith Fulltext-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.cerifentitytypePublications-
item.grantfulltextopen-
item.openairetypeartículo-
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