4.6 Article

Flash Flood Susceptibility Assessment and Zonation by Integrating Analytic Hierarchy Process and Frequency Ratio Model with Diverse Spatial Data

期刊

WATER
卷 14, 期 19, 页码 -

出版社

MDPI
DOI: 10.3390/w14193069

关键词

remote sensing; GIS; AHP; FR; sentinel-2; DEM

资金

  1. National Key Research and Development Program of China [2021YFC3200301]
  2. National Natural Science Foundation of China Youth Fund [52209068]
  3. Postdoctoral Research Foundation of China [2020M682477]
  4. Fundamental Research Funds for the Central Universities [2042021kf0053]

向作者/读者索取更多资源

This study generates flash flood maps using the Analytical Hierarchy Process (AHP) and Frequency Ratio (FR) models. It identifies high-risk zones based on eight flash flood-causative physical parameters and provides policy guidelines.
Flash floods are the most dangerous kinds of floods because they combine the destructive power of a flood with incredible speed. They occur when heavy rainfall exceeds the ability of the ground to absorb it. The main aim of this study is to generate flash flood maps using Analytical Hierarchy Process (AHP) and Frequency Ratio (FR) models in the river's floodplain between the Jhelum River and Chenab rivers. A total of eight flash flood-causative physical parameters are considered for this study. Six parameters are based on remote sensing images of the Advanced Land Observation Satellite (ALOS), Digital Elevation Model (DEM), and Sentinel-2 Satellite, which include slope, elevation, distance from the stream, drainage density, flow accumulation, and land use/land cover (LULC), respectively. The other two parameters are soil and geology, which consist of different rock and soil formations, respectively. In the case of AHP, each of the criteria is allotted an estimated weight according to its significant importance in the occurrence of flash floods. In the end, all the parameters were integrated using weighted overlay analysis in which the influence value of drainage density was given the highest weight. The analysis shows that a distance of 2500 m from the river has values of FR ranging from 0.54, 0.56, 1.21, 1.26, and 0.48, respectively. The output zones were categorized into very low, low, moderate, high, and very high risk, covering 7354, 5147, 3665, 2592, and 1343 km(2), respectively. Finally, the results show that the very high flood areas cover 1343 km(2), or 6.68% of the total area. The Mangla, Marala, and Trimmu valleys were identified as high-risk zones of the study area, which have been damaged drastically many times by flash floods. It provides policy guidelines for risk managers, emergency and disaster response services, urban and infrastructure planners, hydrologists, and climate scientists.

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