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Article

Evolution of a Potentially Dangerous Glacial Lake on the Kanchenjunga Glacier, Nepal, Predictive Flood Models, and Prospective Community Response

1
Institute of Arctic and Alpine Research, University of Colorado at Boulder, Boulder, CO 80309, USA
2
School of Geography, Politics and Sociology, Newcastle University, Newcastle NE1 7RU, UK
3
Appalachian Ecology, Elkins, WV 26241, USA
4
International Centre for Integrated Mountain Development, Lalitpur 44700, Nepal
*
Author to whom correspondence should be addressed.
Water 2025, 17(10), 1457; https://doi.org/10.3390/w17101457
Submission received: 7 March 2025 / Revised: 2 May 2025 / Accepted: 8 May 2025 / Published: 12 May 2025
(This article belongs to the Special Issue Study of Hydrological Mechanisms: Floods and Landslides)

Abstract

During a research expedition to the Kanchenjunga Conservation Area (KCA), eastern Nepal, in April–June 2024, local concern was expressed about the rapid development of meltwater ponds upon the terminus of the Kanchenjunga glacier since 2020, especially in terms of the possible formation of a large and potentially dangerous glacial lake. Our resultant study of the issue included informal interviews with local informants, comparison of time series satellite composite images acquired by Sentinel-2 Multispectral Instrument, and modeling of different lake development, outburst flood scenarios, and prospective downstream impacts. Assuming that the future glacial lake will be formed by the merging of present-day supraglacial ponds, filling the low-gradient area beneath the present-day glacier terminal complex, we estimated the potential volume of a Kanchenjunga proglacial lake to be 33 × 106 m3. Potential mass movement-triggered outburst floods would travel downstream distances of almost 120 km even under the small magnitude scenario, and under the worst-case scenario would reach the Indo-Gangetic Plain and cross the border into India, exposing up to 90 buildings and 44 bridges. In response, we suggest that the lower Kanchenjunga glacier region be regularly monitored by both local communities and Kathmandu-based research entities over the next decade. The development of user-friendly early warning systems, hazard mapping and zoning programs, cryospheric hazards awareness building programs, and construction of locally appropriate flood mitigation measures are recommended. Finally, the continued development and refinement of the models presented here could provide governments and remote communities with a set of inexpensive and reliable tools capable of providing the basic information needed for communities to make informed decisions regarding hazard mitigation, adaptive, and/or preventive measures related to changing glaciers.
Keywords: Kanchenjunga; evolving glacial lakes; community concern; predictive models; flood risk Kanchenjunga; evolving glacial lakes; community concern; predictive models; flood risk

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MDPI and ACS Style

Byers, A.C.; Rinzin, S.; Byers, E.; Wangchuk, S. Evolution of a Potentially Dangerous Glacial Lake on the Kanchenjunga Glacier, Nepal, Predictive Flood Models, and Prospective Community Response. Water 2025, 17, 1457. https://doi.org/10.3390/w17101457

AMA Style

Byers AC, Rinzin S, Byers E, Wangchuk S. Evolution of a Potentially Dangerous Glacial Lake on the Kanchenjunga Glacier, Nepal, Predictive Flood Models, and Prospective Community Response. Water. 2025; 17(10):1457. https://doi.org/10.3390/w17101457

Chicago/Turabian Style

Byers, Alton C., Sonam Rinzin, Elizabeth Byers, and Sonam Wangchuk. 2025. "Evolution of a Potentially Dangerous Glacial Lake on the Kanchenjunga Glacier, Nepal, Predictive Flood Models, and Prospective Community Response" Water 17, no. 10: 1457. https://doi.org/10.3390/w17101457

APA Style

Byers, A. C., Rinzin, S., Byers, E., & Wangchuk, S. (2025). Evolution of a Potentially Dangerous Glacial Lake on the Kanchenjunga Glacier, Nepal, Predictive Flood Models, and Prospective Community Response. Water, 17(10), 1457. https://doi.org/10.3390/w17101457

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