- 1BGC Engineering, Golden, CO, USA (mhille@bgcengineering.ca)
- 2BGC Engineering, Vancouver, British Columbia, Canada
- 3BGC Engineering, Golden, CO, USA
- 4BGC Engineering, Fredericton, New Brunswick, Canada
- 5Asian Development Bank, Manila, Philippines
- 6BGC Engineering, Nashville, TN, USA
- 7BGC Engineering, Inc., Kingston, Ontario, Canada
Glacial lake outburst floods (GLOFs) are devastating to downstream communities in high mountain Asia. GLOF hazards are difficult to characterize because of the complexity and variability in factors that control susceptibility, such as warming temperatures, rainfall, and slope instability. Compounding this uncertainty is the potential for downstream hazards such as landslide dam outburst floods. The August 16, 2024 Thame GLOF in the Himalaya illustrates how local geomorphology can influence a cascading hazard chain. Initiating in the Thyanbo Lakes near the Tashi Lapcha Pass in the Solukhumbu region of Nepal, the Thame GLOF destroyed at least houses, an elementary school, and a medical clinic in the village of Thame, as well as displacing 135 people due to the debris inundation and burial of a majority of the town’s farmland. As part of a regional project with the Asian Development Bank, BGC Engineering and partnering organizations including Nepal’s National Disaster Risk Reduction and Management Authority and the International Centre for Integrated Mountain Development, visited Thame in December 2024 to assess GLOF risk from the remaining lakes and to inform reconstruction of the village. The team observed several characteristics of the watershed’s geomorphology that affected the triggering conditions and amplified the consequences of this GLOF. First, the GLOF burst through the lower of two adjacent glacial lakes from rapid water displacement, but not outburst, from the upper lake. Second, debris fan and rock avalanche deposits on both sides of the valley floor formed a constriction which ponded during the event, resulting in increased knickpoint erosion, sediment supply, and inundation of Thame. Third, the GLOF down-cut up to 10 meters through glaciolacustrine deposits at the terminus of the valley, triggering retrogressive landsliding that now poses risk to the remaining buildings in Thame. The Thame GLOF highlights the importance of considering geomorphology in assessing the potential magnitude and humanitarian risks of GLOFs, as well as the cascading hazard chain that can develop. Site-specific geomorphic and geologic studies will continue to be valuable in building our understanding of GLOFs and how to assess risk to downstream communities.
How to cite: Hille, M., Mark, E., Strouth, A., Sharma, K., Dixit, A., Zubrycky, S., Scheip, C., and Carter, R.: Field insights from the August 16, 2024 Thame glacial lake outburst flood in Nepal: how geomorphology can affect a cascading hazard chain, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-14809, https://doi.org/10.5194/egusphere-egu25-14809, 2025.