{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,6,30]],"date-time":"2026-06-30T00:41:58Z","timestamp":1782780118993,"version":"3.54.5"},"reference-count":55,"publisher":"Wiley","issue":"10","license":[{"start":{"date-parts":[[2012,5,9]],"date-time":"2012-05-09T00:00:00Z","timestamp":1336521600000},"content-version":"vor","delay-in-days":0,"URL":"http:\/\/onlinelibrary.wiley.com\/termsAndConditions#vor"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Earth Surf Processes Landf"],"published-print":{"date-parts":[[2012,8]]},"abstract":"<jats:title>ABSTRACT<\/jats:title><jats:p>This paper focuses on the historical range of variability of landslide activity and its relation to climate in the Aconcagua Park, Argentina. Landslide frequency data are obtained through historic compilation, including the review of more than 85 data sources and personal interviews with members of the local community. Based on these records, the study analyzes major landslide triggering mechanisms and evaluates the role of climate. Slope instability in Aconcagua Park appears to be mainly forced by the melting of snow accumulated during the winter season, which in turn promotes soil saturation and landslide occurrence the following spring\u2013summer (December\u2013February). This finding is supported by a strong correlation between landslides and stream flows of Andean rivers. These peaks occur during warmer seasons, fed by snow and ice\u2010glacier melting. In contrast, the correlation between landslide frequency and precipitation (diary\/accumulative\/monthly\/annual) is less certain; and the relationship of landslide to temperature records (mean annual temperature\/mean temperature during November\u2013February period) is weak. Copyright \u00a9 2012 John Wiley &amp; Sons, Ltd.<\/jats:p>","DOI":"10.1002\/esp.3239","type":"journal-article","created":{"date-parts":[[2012,3,16]],"date-time":"2012-03-16T07:39:34Z","timestamp":1331883574000},"page":"1106-1119","source":"Crossref","is-referenced-by-count":31,"title":["The role of snow melting upon landslides in the central Argentinean Andes"],"prefix":"10.1002","volume":"37","author":[{"given":"Stella","family":"Moreiras","sequence":"first","affiliation":[{"name":"CONICET \u2013 IANIGLA, CCT  Mendoza Argentina"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Maria Sol","family":"Lisboa","sequence":"additional","affiliation":[{"name":"Facultad de Ciencias Agrarias Universidad Nacional de Cuyo  Mendoza Argentina"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Leandro","family":"Mastrantonio","sequence":"additional","affiliation":[{"name":"Facultad de Ciencias Agrarias Universidad Nacional de Cuyo  Mendoza Argentina"}],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"311","published-online":{"date-parts":[[2012,5,9]]},"reference":[{"issue":"1","key":"e_1_2_11_2_1","first-page":"63","article-title":"Cambios en el r\u00e9gimen interanual de la precipitaci\u00f3n estival en la regi\u00f3n Centro\u2010Argentina","volume":"24","author":"Agosta EA","year":"1999","journal-title":"Meteorology"},{"key":"e_1_2_11_3_1","volume-title":"Geolog\u00eda de la regi\u00f3n de Aconcagua, provincias de San Juan y Mendoza","author":"Aguirre\u2010Urreta B","year":"1996"},{"key":"e_1_2_11_4_1","first-page":"887","volume-title":"Landslides","author":"Bandhari RK","year":"1991"},{"key":"e_1_2_11_5_1","doi-asserted-by":"publisher","DOI":"10.1029\/2004GL020229"},{"key":"e_1_2_11_6_1","volume-title":"Journal of a Voyage a Passage Across the Cordillera de los Andes in the Winter of 1827","author":"Brandt CH","year":"1900"},{"key":"e_1_2_11_7_1","first-page":"149","article-title":"Chapters for a climatic history of South America","volume":"32","author":"Caviedes CN","year":"1991","journal-title":"Beitr\u00e4ge zur Regionalen und Angewandten Klimatologie, Freiburger Geographische Hefte"},{"key":"e_1_2_11_8_1","first-page":"189","volume-title":"Cerro Aconcagua. 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