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dc.contributor.authorMergili, Martin
dc.contributor.authorEmmer, Adam
dc.contributor.authorJuricová, Anna
dc.contributor.authorCochachin Rapre, Alejo
dc.contributor.authorFischer, Jan-Thomas
dc.contributor.authorHuggel, Christian
dc.contributor.authorPudasaini, Shiva P.
dc.date.accessioned2018-12-20T15:28:33Z
dc.date.available2018-12-20T15:28:33Z
dc.date.issued2018-01
dc.identifier.citationMergili, M., Emmer, A., Juricová, A. et al. (2018) How well can we simulate complex hydrogeomorphic process chains? The 2012 multi-lake outburst flood in the Santa Cruz Valley (Cordillera Blanca, Perú). Earth Surface Processes and Landforms, 43 (7), 1373–1389. doi: https://doi.org/10.1002/esp.4318es_PE
dc.identifier.issnISSN: 0197-9337, ESSN: 1096-9837es_PE
dc.identifier.urihttps://hdl.handle.net/20.500.12543/3160
dc.descriptionFiliación institucional de autor: Alejo Cochachín Rapre / Autoridad Nacional del Agua - Unidad de Glaciología y Recursos Hídricos (ANA-UGRH), Huaraz, Perues_PE
dc.descriptionOriginal abstract: Changing high-mountain environments are characterized by destabilizing ice, rock or debris slopes connected to evolving glacial lakes. Such configurations may lead to potentially devastating sequences of mass movements (process chains or cascades). Computer simulations are supposed to assist in anticipating the possible consequences of such phenomena in order to reduce the losses. The present study explores the potential of the novel computational tool r.avaflow for simulating complex process chains. r.avaflow employs an enhanced version of the Pudasaini (2012) general two-phase mass flow model, allowing consideration of the interactions between solid and fluid components of the flow. We back-calculate an event that occurred in 2012 when a landslide from a moraine slope triggered a multi-lake outburst flood in the Artizón and Santa Cruz valleys, Cordillera Blanca, Peru, involving four lakes and a substantial amount of entrained debris along the path. The documented and reconstructed flow patterns are reproduced in a largely satisfactory way in the sense of empirical adequacy. However, small variations in the uncertain parameters can fundamentally influence the behaviour of the process chain through threshold effects and positive feedbacks. Forward simulations of possible future cascading events will rely on more comprehensive case and parameter studies, but particularly on the development of appropriate strategies for decision-making based on uncertain simulation results.es_PE
dc.descriptionArtículo en acceso abiertoes_PE
dc.description.abstractExplora el potencial de la nueva herramienta computacional r.avaflow en relación a la simulación de complejas cadenas de procesos relacionados a la desestabilización de laderas de hielo, rocas o escombros conectadas a lagos glaciares en evolución. Asimismo, realiza el cálculo de un evento ocurrido en 2012 cuando un deslizamiento de tierra provocó una inundación de varios lagos en los valles de Artizón y Santa Cruz (Cordillera Blanca, Perú) con cuatro lagos y una cantidad sustancial de escombros arrastrados a lo largo del camino.es_PE
dc.formatapplication/pdfes_PE
dc.language.isoenges_PE
dc.publisherWileyes_PE
dc.relation.ispartofseriesEarth Surface Processes and Landforms, 2018, Volume 43, Issue 7, pp 1373–1389es_PE
dc.relation.urihttps://onlinelibrary.wiley.com/doi/full/10.1002/esp.4318
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.titleHow well can we simulate complex hydrogeomorphic process chains? The 2012 multi-lake outburst flood in the Santa Cruz Valley (Cordillera Blanca, Perú)es_PE
dc.typeinfo:eu-repo/semantics/articlees_PE
dc.identifier.doihttps://doi.org/10.1002/esp.4318es_PE
dc.coverage.basinCuenca Santa


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