Abstract

Dammed lakes are an important secondary hazard caused by earthquakes. They can induce further damage to nearby humans. Current hydrology calculation research on dammed lakes usually lacks spatial expressive ability and cannot accurately conduct impact assessment without the support of remote sensing, which obtains important characteristic information of dammed lakes. The current study aims to address the issues of the potential impact area estimate of earthquake-induced dammed lakes by combining remote sensing (RS), a geographic information system (GIS), and hydrological modeling. The Tangjiashan dammed lake induced by the Wenchuan earthquake was selected as the case for study. The elevation-versus-reservoir capacity curve was first calculated using the seed-growing algorithm based on digital elevation model (DEM) data. The simulated annealing algorithm was applied to train the hydrological modeling parameters according to the historical hydrologic data. Then, the downstream water elevation variational process under different collapse capacity conditions was performed based on the obtained parameters. Finally, the downstream potential impact area was estimated by the highest water elevation values at different hydrologic sections. Results show that a flood with a collapse elevation of at least 680 m will impact the entire downstream region of Beichuan town. We conclude that spatial information technology combined with hydrological modeling can accurately predict and demonstrate the potential impact area with limited data resources. This paper provides a better guide for future immediate responses to dammed lake hazard mitigation.

Highlights

  • Dammed lakes formed by earthquake landslides are an important secondary hazard induced by earthquakes

  • Such floods will generate a second calamity to the people who have just suffered from an earthquake

  • Study a seriesareas of submerged areas corresponding to different levels in aThe short time.in this potential impact areas impact with scarce

Read more

Summary

Introduction

Dammed lakes formed by earthquake landslides are an important secondary hazard induced by earthquakes. Damming objects, sliding from mountain slopes, comprise rocks and weathered soil, which have strong penetrability, low stickiness, and high instability. Damming objects collapse and threaten human beings who live downstream [1,2]. Given that a high amount of rainfall falls upstream, the damming objects block the runoff and destroy the river function, thereby increasing the water level and the risk of the dam collapsing. A flood that develops under these extreme conditions after a dam collapses is more dangerous than the usual mountain torrent disasters. Such floods will generate a second calamity to the people who have just suffered from an earthquake

Objectives
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call