Publication: Ensayo de simulaciones numéricas para la prevención de desastres en la laguna 513 (cordillera blanca, Perú)
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2021-09
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En muchas áreas de montaña alrededor del mundo, como consecuencia del impacto del cambio climático actual, el riesgo de Glacier Lake Outburst Floods (GLOFs) se ha incrementado debido a la formación de nuevas lagunas a causa de la retracción de los glaciares. Ese proceso está siendo especialmente relevante en la Cordillera Blanca, la alineación de montañas con glaciares actuales más grande de la zona tropical de la Tierra, donde se localiza el área de estudio de este trabajo. Se ha ensayado una modelización de los eventos en cascada que serían causa y efecto de un GLOF en la laguna 513, al suroeste del Nevado Hualcán. El modelo consta de tres fases, en las que se han simulado: 1) Una avalancha de hielo y rocas que impacta en la laguna (en el módulo RAMMS AVALANCHE). 2) El tránsito hidráulico del caudal que la avalancha genera en la laguna (en HEC-RAS). 3) El flujo de detritos generado por el desbordamiento de la laguna, que arranca desde la salida del vaso y alcanza los centros poblados localizados vertiente abajo de la laguna, terminando en la ciudad de Carhuaz. Las simulaciones han permitido cartografiar las áreas que podrían ser afectadas por el GLOF, diferenciando peligrosidades media y alta. También se ha desarrollado una aplicación en ArcGIS online como instrumento para facilitar la transferencia de resultados, en relación con la prevención de desastres, a la sociedad local: tomadores de decisiones y población en riesgo.
In many mountain areas around the world, as a consequence of the impact of climate change, the risk of Glacier Lake Outburst Floods (GLOFs) has increased due to the formation of new lakes and the retreat of glaciers. This process is especially showcased in the Cordillera Blanca, the largest alignment of mountains with current glaciers in the tropical zone of the Earth, where the study area of this work is located. A modeling of the cascade events that would be cause and effect of a GLOF has been tested in lake 513, southwest of Nevado Hualcán. The model consists of three phases, in which it has been simulated: 1) An avalanche of ice and rocks that impacts the lake (in the RAMMS AVALANCHE module). 2) The hydraulic transit of the flow that the avalanche generates in the lake (in HEC-RAS). 3) The debris flow generated by the overflow of the lake, which starts from the outlet of the basin and reaches the populated centers located downstream of the lake, ending in the city of Carhuaz. The simulations have made it possible to map the areas that could be affected by the GLOF, differentiating medium and high hazards. An application in ArcGIS online has also been developed as an instrument to facilitate the transfer of results, in relation to disaster prevention, to the local population: decision makers and population at risk.
In many mountain areas around the world, as a consequence of the impact of climate change, the risk of Glacier Lake Outburst Floods (GLOFs) has increased due to the formation of new lakes and the retreat of glaciers. This process is especially showcased in the Cordillera Blanca, the largest alignment of mountains with current glaciers in the tropical zone of the Earth, where the study area of this work is located. A modeling of the cascade events that would be cause and effect of a GLOF has been tested in lake 513, southwest of Nevado Hualcán. The model consists of three phases, in which it has been simulated: 1) An avalanche of ice and rocks that impacts the lake (in the RAMMS AVALANCHE module). 2) The hydraulic transit of the flow that the avalanche generates in the lake (in HEC-RAS). 3) The debris flow generated by the overflow of the lake, which starts from the outlet of the basin and reaches the populated centers located downstream of the lake, ending in the city of Carhuaz. The simulations have made it possible to map the areas that could be affected by the GLOF, differentiating medium and high hazards. An application in ArcGIS online has also been developed as an instrument to facilitate the transfer of results, in relation to disaster prevention, to the local population: decision makers and population at risk.
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