000130750 001__ 130750 000130750 005__ 20240131210810.0 000130750 0247_ $$2doi$$a10.1016/j.earscirev.2017.11.010 000130750 0248_ $$2sideral$$a103262 000130750 037__ $$aART-2018-103262 000130750 041__ $$aeng 000130750 100__ $$aOliva, M. 000130750 245__ $$aThe Little Ice Age in Iberian mountains 000130750 260__ $$c2018 000130750 5203_ $$aThe Little Ice Age (LIA) is known as one of the coldest stages of the Holocene. Most records from the Northern Hemisphere show evidence of significantly colder conditions during the LIA, which in some cases had substantial socio-economic consequences. In this study we investigated the magnitude and timing of climate variability during the LIA in the mountains of the Iberian Peninsula, based on a wide range of natural records (including from glacial, periglacial, and lacustrine/peatland areas; fluvial/alluvial deposits; speleothems; and tree rings), historical documents, and early instrument data. The onset of the LIA commenced in approximately CE 1300, and cold conditions with alternating moisture regimes persisted until approximately CE 1850; the environmental responses ranged from rapid (e.g. tree rings) to delayed (e.g. glaciers). The colder climate of the LIA was accompanied by severe droughts, floods, and cold/heat waves that showed significant spatio-temporal variation across the Iberian mountains. Several phases within the LIA have been detected, including (a) 1300–1480: increasing cooling with moderate climate oscillations; (b) 1480–1570: relatively warmer conditions; (c) 1570–1620: gradual cooling; (d) 1620–1715: coldest climate period of the LIA, particularly during the Maunder Minimum, with temperatures approximately 2 °C below those at present; (e) 1715–1760: warmer temperatures and a low frequency of extreme events; (f) 1760–1800: climate deterioration and more climate extremes (i.e. cold and heat waves, floods and droughts); (g) 1800–1850: highly variable climate conditions alternating with stability (1800–1815), extreme events (1815–1835), and a slight trend of warming associated with intense hydrometeorological events (1835–1850); (h) since 1850: a gradual staggered increase in temperature of approximately 1 °C. Post-LIA warming has led to substantial changes in geo-ecological dynamics, mainly through shrinking of the spatial domain affected by cold climate processes. 000130750 536__ $$9info:eu-repo/grantAgreement/ES/MINECO/CGL2014-58127-C3-1-R$$9info:eu-repo/grantAgreement/ES/MINECO/CGL2015-65569-R$$9info:eu-repo/grantAgreement/ES/MINECO/CGL2015-68144-R$$9info:eu-repo/grantAgreement/ES/MINECO/CGL2015-69985-R$$9info:eu-repo/grantAgreement/ES/MINECO/HAR2013-43701-P 000130750 540__ $$9info:eu-repo/semantics/openAccess$$aAll rights reserved$$uhttp://www.europeana.eu/rights/rr-f/ 000130750 590__ $$a9.53$$b2018 000130750 591__ $$aGEOSCIENCES, MULTIDISCIPLINARY$$b3 / 193 = 0.016$$c2018$$dQ1$$eT1 000130750 592__ $$a3.657$$b2018 000130750 593__ $$aEarth and Planetary Sciences (miscellaneous)$$c2018$$dQ1 000130750 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/publishedVersion 000130750 700__ $$aRuiz-Fernández, J. 000130750 700__ $$aBarriendos, M. 000130750 700__ $$aBenito, G. 000130750 700__ $$0(orcid)0000-0002-7097-8659$$aCuadrat, J.M.$$uUniversidad de Zaragoza 000130750 700__ $$aDomínguez-Castro, F. 000130750 700__ $$aGarcía-Ruiz, J.M. 000130750 700__ $$aGiralt, S. 000130750 700__ $$aGómez-Ortiz, A., Hernández, A. 000130750 700__ $$aLópez-Costas, O. 000130750 700__ $$aLópez-Moreno, J.I. 000130750 700__ $$aLópez-Sáez, J.A. 000130750 700__ $$aMartínez-Cortizas, A. 000130750 700__ $$aMoreno, A. 000130750 700__ $$aProhom, M. 000130750 700__ $$0(orcid)0000-0001-8979-0253$$aSaz, M.A.$$uUniversidad de Zaragoza 000130750 700__ $$aSerrano, E. 000130750 700__ $$0(orcid)0000-0001-6825-3870$$aTejedor, E.$$uUniversidad de Zaragoza 000130750 700__ $$aTrigo, R. 000130750 700__ $$aValero-Garcés, B. 000130750 700__ $$aVicente-Serrano, S.M 000130750 7102_ $$13006$$2010$$aUniversidad de Zaragoza$$bDpto. Geograf. Ordenac.Territ.$$cÁrea Análisis Geográfico Regi. 000130750 773__ $$g117 (2018), 175-208$$pEarth-sci. rev.$$tEarth-Science Reviews$$x0012-8252 000130750 8564_ $$s3418250$$uhttps://zaguan.unizar.es/record/130750/files/texto_completo.pdf$$yVersión publicada 000130750 8564_ $$s2220791$$uhttps://zaguan.unizar.es/record/130750/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada 000130750 909CO $$ooai:zaguan.unizar.es:130750$$particulos$$pdriver 000130750 951__ $$a2024-01-31-19:17:58 000130750 980__ $$aARTICLE