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Erosional dam breach modelling for multi-glacial lake outburst process and downstream flood exposure assessment in the Eastern Himalayas

Arindam Chowdhury, Sazeda Begam, Tomáš Kroczek, Vít Vilímek, Milap Chand Sharma, Sunil Kumar De

2024Journal of Hydrology7 citationsDOIOpen Access PDF

Abstract

• First integrated and robust physical moraine-dam breaching and outburst process chain scenarios for the Gurudongmar Lake Complex. • First and detailed downstream GLOF exposure mapping assessment for all 19 settlement sites within the valley. • Gurudongmar Lake Complex hosts a total ∼ 148 × 10 6 m 3 volume of water, reflecting quite a high GLOF peak in the downstream Tista River valley. • In any largest-case GLOF scenarios (1C, 4C, 5C—80% outburst volume), a GLOF from the Gurudongmar Lake Complex could exceed the magnitude of the October 2023 South Lhonak Lake flood event. • Thangu Valley and Chungthang Town have the highest potential losses and a high risk of inundation due to their size. Accelerating global warming has led to the retreat of glaciers and the concurrent expansion of glacial lakes in the Himalayas, increasing the risk of glacial lake outburst floods (GLOFs) with potential to destroy infrastructure and lives in the downstream river valley. In the Sikkim Himalayas, the potentially hazardous Gurudongmar lake complex (GLC) consists of four lakes containing approximately 148 × 10 6 m 3 of water with an enlargement rate of 74 ± 3 %. Therefore, evaluating possible GLOF hazards from GLC under the current scenario is very important. We have presented in this paper an integrated and robust GLOF model that combines the physical moraine-dam breach using TELEMAC 2D and SISYPHE with 1-D inundation modelling using HEC-RAS for the multi-lake complex to estimate the peak flood (m 3 /s), flood depth (m), and flow velocity (m/sec) and finally assess the downstream inundation exposure. The present study also incorporates different breaching scenarios calculated based on remote sensing and field survey data of surrounding moraine-dam parameters of the GLC. In the largest-cases of GLOFs, with an 80 % overtopping dam breach, the flood peak would reach 5833.7, 7684.0, and 8882.0 m 3 /s for scenarios 1C, 4C, and 5C, respectively. These floods would release a total volume of 39.9, 48.5, and 59.4 × 10 6 m 3 of water for the three scenarios, respectively. The downstream flood exposure assessment is based on different land use types and flood heights observed across nine scenarios (labelled 1A–5C) for each settlement using a 15 × 15 m fishnet method. The results for all 19 settlement sites along the main Tista River channel show a logical trend of increasing potential exposures. However, when the water volumes from GL-2 and GL-1 or GL-3 and GL-1 are combined, the risk of a potential flood rises. An increase in the potential flood depth directly results in higher exposure to infrastructure. The GLOF exposure levels for each scenario at 19 settlement sites differed. However, the Thangu Valley and Chungthang town have the highest inundation exposure due to their size and potential losses. This research article contributes to developing moraine-dam erosional breach modelling for multi-glacial lake outburst scenarios and downstream flood exposure assessment in the Hindu Kush-Karakoram-Himalayan region.

Topics & Concepts

Flood mythHydrology (agriculture)Glacial periodGeologyGlacial lakePhysical geographyGeomorphologyEnvironmental scienceGeotechnical engineeringGeographyArchaeologyCryospheric studies and observationsLandslides and related hazardsWinter Sports Injuries and Performance
Erosional dam breach modelling for multi-glacial lake outburst process and downstream flood exposure assessment in the Eastern Himalayas | Litcius