Sequence of events that led to the South Lhonak lake outburst flood in Sikkim, India

On October 4, 2023, a proglacial lake named the South Lhonak lake was the source of a catastrophic Glacier Lake Outburst Flood (GLOF) in the Teesta river basin area, resulting in 24 fatalities and leaving over 70 persons missing. The GLOF also destroyed 13 bridges and a major hydropower plant in the Chungthang region. Over 60,000 individuals in four districts of Sikkim were impacted by this GLOF event. This study examines the factors that led to the GLOF event. Our study shows that the cause of this GLOF was initiated by a landslide, that dumped a substantial amount (~ 38.31 million m3) of debris into the South Lhonak Lake. Furthermore, the glacier that was connected to the lake, lost a big chunk of ice mass (~ 7 million m3) due to calving. The combination of these two processes led to the collapse of the left lateral moraine that consequently generated flood waves which breached the terminal moraine dam of the lake. We recommend monitoring land subsidence and calving events for large proglacial lakes to prevent the disastrous consequences of such GLOFs in the future.

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Publication Details

Journal
Scientific Reports
Published
2026-03-24
DOI
https://doi.org/10.1038/s41598-026-35895-7
Primary Topic
Cryospheric studies and observations
Type
article
Field-Weighted Citation Impact
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article

Sequence of events that led to the South Lhonak lake outburst flood in Sikkim, India

Scientific Reports
Cryospheric studies and observations
article

Sequence of events that led to the South Lhonak lake outburst flood in Sikkim, India

article en

Abstract

On October 4, 2023, a proglacial lake named the South Lhonak lake was the source of a catastrophic Glacier Lake Outburst Flood (GLOF) in the Teesta river basin area, resulting in 24 fatalities and leaving over 70 persons missing. The GLOF also destroyed 13 bridges and a major hydropower plant in the Chungthang region. Over 60,000 individuals in four districts of Sikkim were impacted by this GLOF event. This study examines the factors that led to the GLOF event. Our study shows that the cause of this GLOF was initiated by a landslide, that dumped a substantial amount (~ 38.31 million m3) of debris into the South Lhonak Lake. Furthermore, the glacier that was connected to the lake, lost a big chunk of ice mass (~ 7 million m3) due to calving. The combination of these two processes led to the collapse of the left lateral moraine that consequently generated flood waves which breached the terminal moraine dam of the lake. We recommend monitoring land subsidence and calving events for large proglacial lakes to prevent the disastrous consequences of such GLOFs in the future.

Scientific ReportsVol. 16(1)
Gangneung–Wonju National University (KR), Wadia Institute of Himalayan Geology (IN), Institute of Science and Technology Austria (AT), Cornell University (US), National Geophysical Research Institute (IN), Central Ground Water Board (IN), Singapore-MIT Alliance for Research and Technology (SG)
Openalex Percentile: Top 7%
Cryospheric studies and observations
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