000130825 001__ 130825
000130825 005__ 20240131210811.0
000130825 0247_ $$2doi$$a10.5194/cp-8-683-2012
000130825 0248_ $$2sideral$$a99975
000130825 037__ $$aART-2012-99975
000130825 041__ $$aeng
000130825 100__ $$aMorellón, M.
000130825 245__ $$aA multi-proxy perspective on millennium-long climate variability in the Southern Pyrenees
000130825 260__ $$c2012
000130825 5060_ $$aAccess copy available to the general public$$fUnrestricted
000130825 5203_ $$aThis paper reviews multi-proxy paleoclimatic reconstructions with robust age-control derived from lacustrine, dendrochronological and geomorphological records and characterizes the main environmental changes that occurred in the Southern Pyrenees during the last millennium. Warmer and relatively arid conditions prevailed during the Medieval Climate Anomaly (MCA, ca. 900-1300 AD), with a significant development of xerophytes and Mediterranean vegetation and limited deciduous tree formations (mesophytes). The Little Ice Age (LIA, 1300-1800 AD) was generally colder and moister, with an expansion of deciduous taxa and cold-adapted montane conifers. Two major phases occurred within this period: (i) a transition MCA-LIA, characterized by fluctuating, moist conditions and relatively cold temperatures (ca. 1300 and 1600 AD); and (ii) a second period, characterized by the coldest and most humid conditions, coinciding with maximum (recent) glacier advances (ca. 1600-1800 AD). Glaciers retreated after the LIA when warmer and more arid conditions dominated, interrupted by a short-living cooling episode during the late 19th to early 20th centuries. Some records suggest a response to solar activity with colder and slightly moister conditions during solar minima. Centennial-scale hydrological fluctuations are in phase with reconstructions of NAO variability, which appears to be one of the main climate mechanisms influencing rainfall variations in the region during the last millennium. © 2012 Author(s).
000130825 536__ $$9info:eu-repo/grantAgreement/ES/CICYT/CALIBRE-CGL2006-13327-C4-01$$9info:eu-repo/grantAgreement/ES/CICYT/DINAMO-CGL2009-07992D$$9info:eu-repo/grantAgreement/ES/CICYT/GRACCIE-CSD2007-00067$$9info:eu-repo/grantAgreement/ES/MINECO/REN2003-09130-C02-02
000130825 540__ $$9info:eu-repo/semantics/openAccess$$aby$$uhttp://creativecommons.org/licenses/by/3.0/es/
000130825 590__ $$a3.556$$b2012
000130825 591__ $$aMETEOROLOGY & ATMOSPHERIC SCIENCES$$b10 / 74 = 0.135$$c2012$$dQ1$$eT1
000130825 591__ $$aGEOSCIENCES, MULTIDISCIPLINARY$$b16 / 172 = 0.093$$c2012$$dQ1$$eT1
000130825 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/publishedVersion
000130825 700__ $$aPérez-Sanz, A.
000130825 700__ $$aCorella, J. P.
000130825 700__ $$aBüntgen, U.
000130825 700__ $$aCatalán, J.
000130825 700__ $$aGonzález-Sampériz, P.
000130825 700__ $$aGonzález-Trueba, J. J.
000130825 700__ $$aLópez-Sáez, J. A.
000130825 700__ $$aMoreno, A.
000130825 700__ $$aPla-Rabes, S.
000130825 700__ $$0(orcid)0000-0001-8979-0253$$aSaz-Sánchez, M. A.$$uUniversidad de Zaragoza
000130825 700__ $$aScussolini, P.
000130825 700__ $$aSerrano, E.
000130825 700__ $$aSteinhilber, F.
000130825 700__ $$aStefanova, V.
000130825 700__ $$aVegas-Vilarrúbia, T.
000130825 700__ $$aValero-Garcés, B.
000130825 7102_ $$13006$$2010$$aUniversidad de Zaragoza$$bDpto. Geograf. Ordenac.Territ.$$cÁrea Análisis Geográfico Regi.
000130825 773__ $$g8, 2 (2012), 683-700$$pClim. past.$$tClimate of the Past$$x1814-9324
000130825 8564_ $$s680157$$uhttps://zaguan.unizar.es/record/130825/files/texto_completo.pdf$$yVersión publicada
000130825 8564_ $$s2698656$$uhttps://zaguan.unizar.es/record/130825/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
000130825 909CO $$ooai:zaguan.unizar.es:130825$$particulos$$pdriver
000130825 951__ $$a2024-01-31-19:24:16
000130825 980__ $$aARTICLE