Journal of Geoscience and Environment Protection

Volume 10, Issue 5 (May 2022)

ISSN Print: 2327-4336   ISSN Online: 2327-4344

Google-based Impact Factor: 0.72  Citations  

Regionalization and the Method for Risk Grading for Flash Flood Disaster in Tibet Region

HTML  XML Download Download as PDF (Size: 16689KB)  PP. 84-93  
DOI: 10.4236/gep.2022.105007    93 Downloads   411 Views  
Author(s)

ABSTRACT

Flash flood is one of the major meteorological disasters on the Tibet Plateau (TP). Flash flood risk regionalization based on the theory of flash flood occurrence risk is the essential basis for relative risk management. The flash flood risk regionalization and the high-resolution grid mountain flood risk level in TP is carried out by using ArcGIS with the indicators of rainfall, days of heavy rain, vegetation cover, slope, relative elevation difference, river network density, population density, average GDP and traffic density. The areas with high mountain flood risk are mainly located in the middle and downstream of Yarlung, the Nujiang River Valley, the Jinsha River and Lancang River Basin. Besides, the results of flash flood disaster risk regionalization were tested by using historical flash flood disaster data and calamity census data. The disasters occurred in high-risk and sub-high-risk regions are accounted for 73%. Flash floods that cause casualties and economic losses of more than 100,000 CNY (Chinese Yuan) occurred in high-risk areas. Flash flood risk assessment may provide reference for the prevention and control of geological disasters in TP, improve disaster prevention and mitigation capabilities, reduce the hazards of flash floods to social development.

Share and Cite:

Ciren, Y. and Ji, N. (2022) Regionalization and the Method for Risk Grading for Flash Flood Disaster in Tibet Region. Journal of Geoscience and Environment Protection, 10, 84-93. doi: 10.4236/gep.2022.105007.

Cited by

No relevant information.

Copyright © 2024 by authors and Scientific Research Publishing Inc.

Creative Commons License

This work and the related PDF file are licensed under a Creative Commons Attribution 4.0 International License.