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dc.contributor.authorSánchez-López, Guiomar-
dc.contributor.authorHernández, Armand-
dc.contributor.authorPla-Rabes, S.-
dc.contributor.authorToro, M.-
dc.contributor.authorGranados, I.-
dc.contributor.authorSigrò, Javier-
dc.contributor.authorTrigo, Ricardo M.-
dc.contributor.authorRubio de Inglés, Maria Jesús-
dc.contributor.authorCamarero, Lluís-
dc.contributor.authorValero-Garcés, Blas L.-
dc.contributor.authorGiralt, Santiago-
dc.date.accessioned2015-03-18T08:22:02Z-
dc.date.available2015-03-18T08:22:02Z-
dc.date.issued2015-
dc.identifier.citationClimate Change : DOI 10.1007/s10584-015-1353-y (2015)es_ES
dc.identifier.issn0165-0009-
dc.identifier.urihttp://hdl.handle.net/10261/112560-
dc.description13 páginas, 3 figuras, 1 tabla.es_ES
dc.description.abstractThree Spanish alpine lakes located in the Central Range (Peñalara Lake and Cimera Lake) and the Pyrenees (Redon Lake) are selected to understand the effects of the North Atlantic Oscillation (NAO) on ice phenology. A conceptual lake model is formulated based on Pearson’s correlation coefficients obtained between season-scale time series of the NAO index, climatic data (i.e., precipitation, air temperature and snow data) and limnological variables (ice phenology records). The results suggest that the effects of the NAO are only reflected in the thawing process via the air temperature and the insulating effect of snow accumulation on the ice cover. An altitude component is evident in our survey because the effects of the NAO on Peñalara Lake (the lowest altitude studied lake) are restricted to winter, whereas for Redon Lake (the highest altitude studied lake), the effects extend into spring. A latitudinal component is also clear when comparing our data with northern European lakes. Snow accumulation primarily depends on the air temperature at high latitudes, and both precipitation and the air temperature control snow accumulation at lower latitudes. Consequently, in northern Europe, the NAO signal is primarily reflected in lake ice phenology via the air temperature, whereas our results confirm that in southern Europe, the strong dependence of precipitation on the NAO determines the importance of the NAO for lake ice cover.es_ES
dc.description.sponsorshipThis research was funded by the Spanish Ministry of Economy and Competitiveness through the PALEONAO project (CGL2010-15767/BTE), RapidNAO project (CGL2013-40608-R) and an undergraduate JAE grant (BOE 03/02/2011) for Guiomar Sánchez from the Spanish Research Council (CSIC).es_ES
dc.language.isoenges_ES
dc.publisherSpringeres_ES
dc.rightsopenAccesses_ES
dc.titleThe effects of the NAO on the ice phenology of Spanish alpine lakeses_ES
dc.typeartículoes_ES
dc.identifier.doi10.1007/s10584-015-1353-y-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttp://dx.doi.org/10.1007/s10584-015-1353-yes_ES
dc.identifier.e-issn1573-1480-
dc.relation.csices_ES
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