000056291 001__ 56291
000056291 005__ 20240124152520.0
000056291 0247_ $$2doi$$a10.1007/s00484-015-1033-7
000056291 0248_ $$2sideral$$a92338
000056291 037__ $$aART-2016-92338
000056291 041__ $$aeng
000056291 100__ $$0(orcid)0000-0001-6825-3870$$aTejedor, E.$$uUniversidad de Zaragoza
000056291 245__ $$aTree-ring-based drought reconstruction in the Iberian Range (east of Spain) since 1694
000056291 260__ $$c2016
000056291 5060_ $$aAccess copy available to the general public$$fUnrestricted
000056291 5203_ $$aDroughts are a recurrent phenomenon in the Mediterranean basin with negative consequences for society, economic activities, and natural systems. Nevertheless, the study of drought recurrence and severity in Spain has been limited so far due to the relatively short instrumental period. In this work, we present a reconstruction of the standardized precipitation index (SPI) for the Iberian Range. Growth variations and climatic signals within the network are assessed developing a correlation matrix and the data combined to a single chronology integrating 336 samples from 169 trees of five different pine species distributed throughout the province of Teruel. The new chronology, calibrated against regional instrumental climatic data, shows a high and stable correlation with the July SPI integrating moisture conditions over 12 months forming the basis for a 318-year drought reconstruction. The climate signal contained in this reconstruction is highly significant (p < 0.05) and spatially robust over the interior areas of Spain located above 1000 meters above sea level (masl). According to our SPI reconstruction, seven substantially dry and five wet periods are identified since the late seventeenth century considering =±1.76 standard deviations. Besides these, 36 drought and 28 pluvial years were identified. Some of these years, such as 1725, 1741, 1803, and 1879, are also revealed in other drought reconstructions in Romania and Turkey, suggesting that coherent larger-scale synoptic patterns drove these extreme deviations. Since regional drought deviations are also retained in historical documents, the tree-ring-based reconstruction presented here will allow us to cross-validate drought frequency and magnitude in a highly vulnerable region.
000056291 536__ $$9info:eu-repo/grantAgreement/ES/MINECO/CGL2011-28255
000056291 540__ $$9info:eu-repo/semantics/openAccess$$aby$$uhttp://creativecommons.org/licenses/by/3.0/es/
000056291 590__ $$a2.204$$b2016
000056291 591__ $$aENVIRONMENTAL SCIENCES$$b97 / 229 = 0.424$$c2016$$dQ2$$eT2
000056291 591__ $$aMETEOROLOGY & ATMOSPHERIC SCIENCES$$b38 / 83 = 0.458$$c2016$$dQ2$$eT2
000056291 591__ $$aPHYSIOLOGY$$b43 / 83 = 0.518$$c2016$$dQ3$$eT2
000056291 591__ $$aBIOPHYSICS$$b44 / 73 = 0.603$$c2016$$dQ3$$eT2
000056291 592__ $$a0.799$$b2016
000056291 593__ $$aAtmospheric Science$$c2016$$dQ2
000056291 593__ $$aHealth, Toxicology and Mutagenesis$$c2016$$dQ2
000056291 593__ $$aEcology$$c2016$$dQ2
000056291 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/acceptedVersion
000056291 700__ $$0(orcid)0000-0002-7585-3636$$ade Luis, M.$$uUniversidad de Zaragoza
000056291 700__ $$0(orcid)0000-0002-7097-8659$$aCuadrat, J.M.$$uUniversidad de Zaragoza
000056291 700__ $$aEsper, J.
000056291 700__ $$0(orcid)0000-0001-8979-0253$$aSaz, M.Á.$$uUniversidad de Zaragoza
000056291 7102_ $$13006$$2430$$aUniversidad de Zaragoza$$bDpto. Geograf. Ordenac.Territ.$$cÁrea Geografía Física
000056291 7102_ $$13006$$2010$$aUniversidad de Zaragoza$$bDpto. Geograf. Ordenac.Territ.$$cÁrea Análisis Geográfico Regi.
000056291 773__ $$g60 (2016), 361–372$$pInt. j. biometeorol.$$tINTERNATIONAL JOURNAL OF BIOMETEOROLOGY$$x0020-7128
000056291 8564_ $$s7272890$$uhttps://zaguan.unizar.es/record/56291/files/texto_completo.pdf$$yPostprint
000056291 8564_ $$s36046$$uhttps://zaguan.unizar.es/record/56291/files/texto_completo.jpg?subformat=icon$$xicon$$yPostprint
000056291 909CO $$ooai:zaguan.unizar.es:56291$$particulos$$pdriver
000056291 951__ $$a2024-01-24-15:16:42
000056291 980__ $$aARTICLE