NH015-0006
Modelling the impact of a GLOF scenario at laguna parón, cordillera blanca, Perú, using a novel multi-phase topographical and geological procedure

Wednesday, 9 December 2020
Poster
Juan Carlos Torres Lázaro1, Hilbert Villafane Gomez1, Adriana Caballero Bedriñana1, Harrinson Jara Infantes2, Enver Melgarejo Romero2, Julia Araujo Reyes1, Christian Yarleque1, Stephan Harrison3, Ryan Wilson4, Joanne Laura Wood3 and Neil F Glasser5, (1)National Research Institute for Glaciers and Mountain's Ecosystems (INAIGEM), Huaraz, Peru, (2)National Research Institute for Glaciers and Mountain's Ecosystems (INAIGEM), Lima, Peru, (3)University of Exeter, College of Life and Environmental Sciences, Exeter, United Kingdom, (4)University of Huddersfield, Biological and Geographical Sciences., Huddersfield, United Kingdom, (5)Aberystwyth University, Department of Geography and Earth Sciences, Aberystwyth, United Kingdom
Abstract:
The Cordillera Blanca is undergoing rapid deglaciation due to climatic warming, especially since the late 20th century. This process has resulted in the formation of new glacial lakes and an increase in the volume of existing lakes, some of which pose a risk in the form of Glacier Lake Outburst Floods (GLOF); such as Laguna Parón in the Cordillera Blanca, which represents a significant hazard to the city of Caraz and smaller populations located in the Llullán-Parón sub-basin. Here, we model a potential dam breach and GLOF generation scenario at Laguna Parón using a novel numerical modelling procedure that, amongst other factors, considers the geological structure of the natural dam. Overall, this procedure includes four distinct phases: (1) estimation of the potential for ice avalanche impact on Laguna Parón sourced from surrounding glacial cirques; (2) modelling of subsequent impulsive wave generation and propagation; (3) analysis of the hydraulic parameters of a possible breach of the natural dam, considering the non-erodible material within empirical estimations of the hydrograph where the composition of the dam is interpreted based on surface geological mapping and drill sampling carried out in the area; and (4) simulation of a potential GLOF using the FLO-2D model with input data from the previous phases. Modelling results indicate that Laguna Parón is most at risk from ice avalanches that originate from the adjacent Hatunraju glacier and that such events have the potential to generate impulse waves that could initiate erosion and a subsequent breach of the natural dam. Considering a worst-case ice avalanche scenario, our results indicate the potential generation of a GLOF with average peaks flow of 25,264.22 m3/s. This GLOF event would reach the urban area of the city of Caraz in around 36-42 minutes with flow rates and flood heights fluctuating between 11.2 m/s to 22.4 m/s and 9.9 m to 19.7 m, respectively.