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dc.contributor.authorVilímek, Vit
dc.contributor.authorEmmer, Adam
dc.coverage.spatialCordillera Blanca
dc.date.accessioned2019-01-03T21:47:39Z
dc.date.available2019-01-03T21:47:39Z
dc.date.issued2014-09
dc.identifier.citationVilímek, V. and Emmer, A. (2014) New method for assessing the susceptibility of glacial lakes to outburst floods in the Cordillera Blanca, Peru. Hydrology and Earth System Sciences, 18(9), 3461-3479. doi: https://doi.org/10.5194/hess-18-3461-2014es_PE
dc.identifier.issnISSN: 1027-5606, ESSN: 1607-7938es_PE
dc.identifier.urihttps://hdl.handle.net/20.500.12543/3197
dc.descriptionOriginal abstract: This paper presents a new and easily repeatable method for assessing the susceptibility of glacial lakes to outburst floods (GLOFs) within the Peruvian region of the Cordillera Blanca. The presented method was designed to: (a) be repeatable (from the point of view of the demands on input data), (b) be reproducible (to provide an instructive guide for different assessors), (c) provide multiple results for different GLOF scenarios and (d) be regionally focused on the lakes of the Cordillera Blanca. Based on the input data gained from remotely sensed images and digital terrain models/topographical maps, the susceptibility of glacial lakes to outburst floods is assessed using a combination of decision trees for clarity and numerical calculation for repeatability and reproducibility. A total of seventeen assessed characteristics are used, of which seven have not been used in this context before. Also, several ratios and calculations are defined for the first time. We assume that it is not relevant to represent the overall susceptibility of a particular lake to outburst floods by one result (number), thus it is described in the presented method by five separate results (representing five different GLOF scenarios). These are potentials for (a) dam overtopping resulting from a fast slope movement into the lake, (b) dam overtopping following the flood wave originating in a lake situated upstream, (c) dam failure resulting from a fast slope movement into the lake, (d) dam failure following the flood wave originating in a lake situated upstream and (e) dam failure following a strong earthquake. All of these potentials include two or three components and theoretically range from 0 to 1. The presented method was verified on the basis of assessing the pre-flood conditions of seven lakes which have produced ten glacial lake outburst floods in the past and ten lakes which have not. A comparison of these results showed that the presented method successfully identified lakes susceptible to outburst floods (pre-flood conditions of lakes which have already produced GLOFs).es_PE
dc.descriptionArtículo en acceso abiertoes_PE
dc.description.abstractPresenta un método para evaluar la susceptibilidad de los lagos glaciares a las inundaciones (GLOF) en la región peruana de la Cordillera Blanca. Menciona que utiliza un total de diecisiete características evaluadas, además, por primera vez se definen varias razones y cálculos.es_PE
dc.formatapplication/pdfes_PE
dc.language.isoenges_PE
dc.publisherEGUes_PE
dc.relation.ispartofseriesHydrology and Earth System Sciences, September 2014, Volume 18, Issue 9, pp 3461-3479es_PE
dc.relation.urihttps://www.hydrol-earth-syst-sci.net/18/3461/2014/
dc.rightsinfo:eu-repo/semantics/openAccesses_PE
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 International*
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.sourceAutoridad Nacional del Aguaes_PE
dc.sourceRepositorio institucional - ANAes_PE
dc.subjectComportamiento de eventos extremos de origen glaciar y climáticoes_PE
dc.subjectGestión de riesgos de desastres en recursos hídricoses_PE
dc.subjectMonitoreo de lagunas y glaciareses_PE
dc.titleNew method for assessing the susceptibility of glacial lakes to outburst floods in the Cordillera Blanca, Perues_PE
dc.typeinfo:eu-repo/semantics/articlees_PE
dc.identifier.doihttps://doi.org/10.5194/hess-18-3461-2014es_PE


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