EGU25-2400, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-2400
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Monday, 28 Apr, 10:45–12:30 (CEST), Display time Monday, 28 Apr, 08:30–12:30
 
Hall X3, X3.1
Sediment disasters induced by the 26-28 September 2024 extreme rainfall event in Nallu Khola watershed of Central Nepal
Ching-Ying Tsou1, Zinky Bhusal2, Hayato Kakinuma1, Reona Kawakami3, Daisuke Higaki4, Jagat K. Bhusal5, Subodh Dhakal6, and Shanmukhesh Chandra Amatya7
Ching-Ying Tsou et al.
  • 1Hirosaki University, Faculty of Agriculture and Life Science, Aomori, Japan (tsou.chingying@hirosaki-u.ac.jp)
  • 2Department of Hydrology and Meteorology, Nepal
  • 3United Graduate School of Agricultural Sciences, Iwate University
  • 4Nippon Koei Co., Ltd.
  • 5(previous) Department of Hydrology and Meteorology, Nepal
  • 6Department of Geology, Tribhuvan University
  • 7Nepal Development Research Institute

From September 26 to 28, 2024, Nepal experienced exceptionally heavy rainfall, severely impacting large areas, particularly the Kathmandu Valley and its surrounding districts, triggering flash floods and landslides. This study presents preliminary findings from an assessment conducted approximately two months after the event, focusing on the upstream region of the Nallu Khola watershed in Lalitpur District, one of the areas most severely impacted. The event recorded a cumulative rainfall total of 518 mm at the Lele AWS Station (Department of Hydrology and Meteorology, Nepal), located approximately 2 km NW of the study area. This rainfall was about 4.3 times the total monthly rainfall for September 2023. The maximum hourly rainfall, observed at 5:00 AM on September 28, reached 39.8 mm, while the highest 24-hour rainfall was an extraordinary 441.2 mm. The rainfall triggered a series of compound sediment disasters, including raising the river level by approximately 3 m above the riverbed, along with numerous landslides and debris flows. The landslides predominantly consist of shallow failures, primarily occurring along roads and in areas associated with cultivated land, while areas covered with forest exhibit relatively few failures. Debris flows are predominantly concentrated in creeks, with a comparable event having occurred on September 30, 1981. Following that event, debris flow mitigation engineering measures (e.g. gabion check dams and channel works) were implemented in some creeks and the impacts of the 2024 event appear to have been largely confined to these mitigated creeks. This underscores the importance of implementing and maintaining effective mitigation measures to manage debris flow hazards in vulnerable areas.

How to cite: Tsou, C.-Y., Bhusal, Z., Kakinuma, H., Kawakami, R., Higaki, D., Bhusal, J. K., Dhakal, S., and Amatya, S. C.: Sediment disasters induced by the 26-28 September 2024 extreme rainfall event in Nallu Khola watershed of Central Nepal, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-2400, https://doi.org/10.5194/egusphere-egu25-2400, 2025.