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dc.contributor.authorEmmer, Adam
dc.contributor.authorVilímek, Vit
dc.contributor.authorKlimes, Jan
dc.contributor.authorCochachin Rapre, Alejo
dc.coverage.spatialCuenca Santa
dc.date.accessioned2019-01-03T21:47:40Z
dc.date.available2019-01-03T21:47:40Z
dc.date.issued2014
dc.identifier.citationEmmer A., Vilímek V., Klimes J., Cochachin A. (2014) Glacier Retreat, Lakes Development and Associated Natural Hazards in Cordilera Blanca, Peru. Shan W., Guo Y., Wang F., Marui H., Strom A. (eds) Landslides in Cold Regions in the Context of Climate Change. Environmental Science and Engineering. Springer, Chames_ES
dc.identifier.issnISSN: 1863-5520, ESSN: 1863-5539es_ES
dc.identifier.urihttps://hdl.handle.net/20.500.12543/3200
dc.descriptionFiliación institucional de autor: Alejo Cochachín Rapre /Autoridad Nacional del Agua - Unidad de Glaciología y Recursos Hídricos (ANA-UGRH), Huaraz, Perues_ES
dc.descriptionOriginal abstract: Cordillera Blanca is the heaviest glacierized tropical range in the world. Due to the global climate change, most of glaciers are retreating and thinning. Glacier retreat leads to the formation and development of all types of potentially hazardous glacial lakes (bedrock-dammed, moraine-dammed, and ice-dammed). Potential hazardousness of glacial lakes is strongly interconnected with dynamic slope movements: (1) sudden release of water from glacial lakes (also known as glacial lake outburst floods—GLOF) is mainly caused by dynamic slope movement into the lake (about 80 % in the Cordillera Blanca); (2) released water may easily transform into debris-flow or mud-flow, thanks to its high erosion and transport potential. Based on field study and remotely sensed images, this contribution documents glacier retreat in the Cordillera Blanca with regards to formation and development of new potentially hazardous glacial lakes, which evolve mainly in elevations of about 4,600–5,000 m a.s.l. We introduce and describe three hazardous events associated with glacier retreat in the last decade.es_ES
dc.descriptionLibro en período de embargoes_ES
dc.description.abstractSeñala que la Cordillera Blanca es la cordillera tropical más glaciar del mundo y es afectada por el cambio climático, teniendo como consecuencia la retirada de los glaciares que conduce a la formación y desarrollo de todos los tipos de lagos glaciares potencialmente peligrosos (roca de la base, presa de morrena y presa de hielo) cuya peligrosidad potencial está fuertemente interconectada con los movimientos de pendiente dinámicos.es_ES
dc.formatapplication/pdfes_ES
dc.language.isoenges_ES
dc.publisherSpringer, Chames_ES
dc.relation.ispartofseriesLandslides in Cold Regions in the Context of Climate Change, 2014es_ES
dc.rightsinfo:eu-repo/semantics/closedAccesses_ES
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 International*
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.sourceAutoridad Nacional del Aguaes_ES
dc.sourceRepositorio institucional - ANAes_ES
dc.subjectCambio climáticoes_ES
dc.subjectGestión de riesgos de desastres en recursos hídricoses_ES
dc.subjectMonitoreo de lagunas y glaciareses_ES
dc.titleGlacier Retreat, Lakes Development and Associated Natural Hazards in Cordillera Blanca, Perues_ES
dc.typeinfo:eu-repo/semantics/bookPartes_ES
dc.identifier.journalLandslides in Cold Regions in the Context of Climate Changees_ES
dc.identifier.doihttps://doi.org/10.1007/978-3-319-00867-7_17es_ES


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