000148840 001__ 148840
000148840 005__ 20250123145736.0
000148840 0247_ $$2doi$$a10.1016/j.geomorph.2004.11.012
000148840 0248_ $$2sideral$$a55928
000148840 037__ $$aART-2005-55928
000148840 041__ $$aeng
000148840 100__ $$0(orcid)0000-0002-0826-3492$$aChueca Cia, J.$$uUniversidad de Zaragoza
000148840 245__ $$aResponses to Climatic Changes Since the Little Ice Age on Maladeta Glacier (Central Pyrenees)
000148840 260__ $$c2005
000148840 5060_ $$aAccess copy available to the general public$$fUnrestricted
000148840 5203_ $$aThe evolution of Maladeta Glacier (Maladeta massif, central Spanish Pyrenees) since the Little Ice Age maximum is analyzed in this work. The extent of the glacier was mapped into 10 stages using morainic deposits and graphic documents. Climatic data (temperature and precipitation) were reconstructed by using dendroclimatic techniques complemented by recent instrumental records. The results thus obtained confirm the control of the above mentioned climatic factors, particularly annual temperature and winter precipitation, in the evolution of Maladeta Glacier, which has receded from an extent of 152.3 ha in 1820–1830 to 54.5 ha in 2000, a 35.7% reduction in size. The rate of ice wastage has varied during that period, defining several phases of glacial stabilization (1820–1830 to 1857; 1914–1920 to 1934–1935; 1957 to 1981), moderated glacial depletion (1901–1904 to 1914–1920; 1934–1935 to 1957) and marked glacial depletion (1857 to 1901–1904; 1981 to 2000). The evolution of Maladeta Glacier is also in keeping with trends observed from other alpine Mediterranean glaciers, which have experienced a consistent rise in their equilibrium line altitudes during the 19th and 20th centuries as well as associated and prolonged periods of negative mass balance.
000148840 540__ $$9info:eu-repo/semantics/openAccess$$aby-nc-nd$$uhttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
000148840 590__ $$a1.508$$b2005
000148840 591__ $$aGEOLOGY$$b8 / 36 = 0.222$$c2005$$dQ1$$eT1
000148840 591__ $$aGEOGRAPHY, PHYSICAL$$b12 / 30 = 0.4$$c2005$$dQ2$$eT2
000148840 591__ $$aGEOSCIENCES, MULTIDISCIPLINARY$$b33 / 128 = 0.258$$c2005$$dQ2$$eT1
000148840 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/acceptedVersion
000148840 700__ $$0(orcid)0000-0003-2627-7166$$aJulián Andres, A.$$uUniversidad de Zaragoza
000148840 700__ $$0(orcid)0000-0001-8979-0253$$aSaz Sanchez, M.A.$$uUniversidad de Zaragoza
000148840 700__ $$aCreus Novau, J.
000148840 700__ $$aLópez Moreno, J.I.
000148840 7102_ $$13006$$2430$$aUniversidad de Zaragoza$$bDpto. Geograf. Ordenac.Territ.$$cÁrea Geografía Física
000148840 773__ $$g68, 3-4 (2005), 167-182$$pGeomorphology$$tGEOMORPHOLOGY$$x0169-555X
000148840 8564_ $$s1117678$$uhttps://zaguan.unizar.es/record/148840/files/texto_completo.pdf$$yPostprint
000148840 8564_ $$s1406150$$uhttps://zaguan.unizar.es/record/148840/files/texto_completo.jpg?subformat=icon$$xicon$$yPostprint
000148840 909CO $$ooai:zaguan.unizar.es:148840$$particulos$$pdriver
000148840 951__ $$a2025-01-23-14:55:18
000148840 980__ $$aARTICLE