A multi-source quantitative reconstruction of the 26 August 2026 Bhote Koshi rock-ice avalanche-debris-flow-flood cascade, Nepal
Abstract
On 26 August 2026, a catastrophic transboundary mass-flow and flood cascade originated in the upper Lhende Khola-Bhote Koshi headwaters and propagated through the Bhote Koshi, Trishuli, and Narayani river system in Nepal. Early public descriptions used the glacial lake outburst flood (GLOF) label, but subsequent seismic, satellite, video, field, hydrological, and damage-assessment evidence supported a more complex sequence of rock-ice avalanche, progressive entrainment and debris-flow transformation, followed by downstream flood-wave routing. This study aims to provide a reproducible, evidence-weighted quantitative reconstruction using publicly available data through 7 October 2026. Official hydrometeorological timelines, peer-reviewed source-process studies, preliminary satellite mapping, the Government of Nepal Rapid Damage and Needs Assessment, and dated human-impact snapshots were harmonized. Propagation and warning-time metrics, hydrological amplification, paired channel-width change at 22 sections, exposure and infrastructure severity ratios, and sectoral concentration of disaster effects and recovery needs were calculated. The source-to-border segment was reported at approximately 188 km/h (52.2 m/s), declining to 23-26 km/h in lower-river segments which was explained by a descriptive log-linear decay model at 80.1% of variation across six reported segment speeds. The public-warning anchor at 09:15 Nepal Standard Time occurred 38 minutes after the source seismic signal, after the flood had already passed or disabled upper-corridor stations, leaving only five minutes to the Betrawati station-failure proxy but 365 minutes to the reported Devghat flood-wave arrival. At Devghat, stage rose from 4.76 to 6.57 m, and discharge increased from approximately 2,600 to 5,850 m3/s where the reported 19.96 million m3 excess volume represented 34.8% of total flow volume during 14:10-18:00. All 22 mapped channel sections widened, from a mean of 66.1 to 266.5 m with the mean post/pre width ratio of 4.49 (bootstrap 95% CI 3.65-5.39; one-sided Wilcoxon p=1.99x10-5). The official assessment recorded USD 2.695 billion in disaster effects and USD 4.775 billion in recovery needs, with energy accounting for 54.0% of needs. The results showed that Nepalese cryospheric risk screening, early warning, and infrastructure design must expand from lake-centric hazard concepts to process-chain surveillance that connects unstable rock-ice source areas, entrainment-prone transport corridors, temporary blockages, and exposed downstream assets.
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BibTeX
@misc{pokhrel2026multisource,
title = {{A multi-source quantitative reconstruction of the 26 August 2026 Bhote Koshi rock-ice avalanche-debris-flow-flood cascade, Nepal}},
author = {Nischal Pokhrel and Tinisha Khatri},
howpublished = {EarthArXiv},
year = {2026},
month = oct,
doi = {10.31223/x5mb9v},
url = {https://eartharxiv.org/repository/view/15771/},
note = {CC BY 4.0},
}
RIS
TY - UNPB
TI - A multi-source quantitative reconstruction of the 26 August 2026 Bhote Koshi rock-ice avalanche-debris-flow-flood cascade, Nepal
AU - Nischal Pokhrel
AU - Tinisha Khatri
PY - 2026
DA - 2026/10/26
PB - EarthArXiv
DO - 10.31223/x5mb9v
UR - https://eartharxiv.org/repository/view/15771/
AB - On 26 August 2026, a catastrophic transboundary mass-flow and flood cascade originated in the upper Lhende Khola-Bhote Koshi headwaters and propagated through the Bhote Koshi, Trishuli, and Narayani river system in Nepal. Early public descriptions used the glacial lake outburst flood (GLOF) label, but subsequent seismic, satellite, video, field, hydrological, and damage-assessment evidence supported a more complex sequence of rock-ice avalanche, progressive entrainment and debris-flow transformation, followed by downstream flood-wave routing. This study aims to provide a reproducible, evidence-weighted quantitative reconstruction using publicly available data through 7 October 2026. Official hydrometeorological timelines, peer-reviewed source-process studies, preliminary satellite mapping, the Government of Nepal Rapid Damage and Needs Assessment, and dated human-impact snapshots were harmonized. Propagation and warning-time metrics, hydrological amplification, paired channel-width change at 22 sections, exposure and infrastructure severity ratios, and sectoral concentration of disaster effects and recovery needs were calculated. The source-to-border segment was reported at approximately 188 km/h (52.2 m/s), declining to 23-26 km/h in lower-river segments which was explained by a descriptive log-linear decay model at 80.1% of variation across six reported segment speeds. The public-warning anchor at 09:15 Nepal Standard Time occurred 38 minutes after the source seismic signal, after the flood had already passed or disabled upper-corridor stations, leaving only five minutes to the Betrawati station-failure proxy but 365 minutes to the reported Devghat flood-wave arrival. At Devghat, stage rose from 4.76 to 6.57 m, and discharge increased from approximately 2,600 to 5,850 m3/s where the reported 19.96 million m3 excess volume represented 34.8% of total flow volume during 14:10-18:00. All 22 mapped channel sections widened, from a mean of 66.1 to 266.5 m with the mean post/pre width ratio of 4.49 (bootstrap 95% CI 3.65-5.39; one-sided Wilcoxon p=1.99x10-5). The official assessment recorded USD 2.695 billion in disaster effects and USD 4.775 billion in recovery needs, with energy accounting for 54.0% of needs. The results showed that Nepalese cryospheric risk screening, early warning, and infrastructure design must expand from lake-centric hazard concepts to process-chain surveillance that connects unstable rock-ice source areas, entrainment-prone transport corridors, temporary blockages, and exposed downstream assets.
ER -