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dc.contributor.authorSánchez-López, Guiomares_ES
dc.contributor.authorHernández, Armandes_ES
dc.contributor.authorPla-Rabes, S.es_ES
dc.contributor.authorTrigo, Ricardo M.es_ES
dc.contributor.authorToro, M.es_ES
dc.contributor.authorGranados, I.es_ES
dc.contributor.authorSáez, Albertoes_ES
dc.contributor.authorMasqué, Perees_ES
dc.contributor.authorPueyo Mur, Juan Josées_ES
dc.contributor.authorRubio de Ingles, Maria Jesuses_ES
dc.contributor.authorGiralt, Santiagoes_ES
dc.date.accessioned2016-09-14T09:15:28Z-
dc.date.available2016-09-14T09:15:28Z-
dc.date.issued2016-08-
dc.identifier.citationQuaternary Science Reviews, 149: 135-150 (2016)es_ES
dc.identifier.issn0277-3791-
dc.identifier.urihttp://hdl.handle.net/10261/136717-
dc.description.abstractA multi-proxy characterization of the uppermost sedimentary infill of an Iberian alpine lake (Cimera, 2140 m a.s.l.) was performed to establish the climatic and environmental conditions for the Iberian Central Range (ICR) over the last two millennia. This multi-proxy characterization was used to reconstruct the intense runoff events, lake productivity and soil erosion in the lake catchment and interpret these factors in terms of temperature and precipitation variability. The Roman Period (RP; 200 BCE – 500 CE) beginning was characterized by an alternation between cold and warm periods as indicated by short-lived oscillations of intense runoff conditions and soil erosion, although warm conditions dominated the end of the period and the Early Middle Age (EMA; 500–900 CE) onset in the ICR. A noticeable decrease in intense runoff events and a progressive decrease in soil erosion during the late EMA indicated a shift to colder temperatures. In terms of precipitation, both the RP and EMA climate periods displayed a transition from dry to wet conditions that led to a decrease in lake productivity. The Medieval Climate Anomaly (MCA; 900–1300 CE) was characterized by warm and dry conditions with frequent intense runoff episodes and increases in lake productivity and soil erosion, whereas the Little Ice Age (LIA; 1300–1850 CE) showed the opposite characteristics. The Industrial Era (1850–2012 CE) presented an increase in lake productivity that likely demonstrates the influence of global warming. The spatio-temporal integration of the Cimera record with other Iberian reconstructions has been used to identify the main climate drivers over this region. During the RP and EMA, N–S and E–W humidity gradients were dominant, whereas during the MCA and LIA, these gradients were not evident. These differences could be ascribed to interactions between the North Atlantic Oscillation (NAO) and East Atlantic (EA) phases. During the RP, the general warm conditions and the E–W humidity gradient indicate a dominant interplay between a negative NAO phase and a positive EA phase (NAO−–EA+), whereas the opposite conditions during the EMA indicate a NAO+–EA− interaction. The dominant warm and arid conditions during the MCA and the cold and wet conditions during the LIA indicate the interplay of the NAO+–EA+ and NAO−–EA−, respectively. Furthermore, the higher solar irradiance during the RP and MCA may support the predominance of the EA+ phase, whereas the opposite scenario during the EMA and LIA may support the predominance of the EA− phase, which would favour the occurrence of frequent and persistent blocking events in the Atlantic region during these periods. © 2016 Elsevier Ltdes_ES
dc.description.sponsorshipThis workwas financed by the Spanish Ministry of Economy and Competitiveness through the PALEONAO project (CGL2010-15767/BTE), the RapidNAO project (CGL2013-40608-R) and a PhD JAE grant (JAEPRE2011-01171, BOE 03/02/2011) to Guiomar Sánchez from the Spanish National Research Council (CSIC). Pere Masqué was partly supported by the Generalitat de Catalunya to the research group MERS (2014 SGR-1356). Armand Hernández was supported by the Portuguese Science Foundation (FCT) through a post-doctoral grant (SFRH/BPD/79923/2011).es_ES
dc.language.isoenges_ES
dc.publisherElsevieres_ES
dc.rightsclosedAccesses_ES
dc.subjectAlpine lakees_ES
dc.subjectEAes_ES
dc.subjectIberian climatees_ES
dc.subjectLacustrine sedimentses_ES
dc.subjectNAOes_ES
dc.subjectSoil erosiones_ES
dc.titleClimate reconstruction for the last two millennia in central Iberia: The role of East Atlantic (EA), North Atlantic Oscillation (NAO) and their interplay over the Iberian Peninsulaes_ES
dc.typeartículoes_ES
dc.identifier.doi10.1016/j.quascirev.2016.07.021-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttp://dx.doi.org/10.1016/j.quascirev.2016.07.021es_ES
dc.identifier.e-issn1873-457X-
dc.contributor.funderMinisterio de Economía y Competitividad (España)es_ES
dc.contributor.funderGeneralitat de Catalunyaes_ES
dc.contributor.funderFundação para a Ciência e a Tecnologia (Portugal)es_ES
dc.relation.csices_ES
oprm.item.hasRevisionno ko 0 false*
dc.identifier.funderhttp://dx.doi.org/10.13039/501100003329es_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/501100002809es_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/501100001871es_ES
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