A Rapid Forecast Method for the Process of Flash Flood Based on Hydrodynamic Model and KNN Algorithm-Reference-Cited by-同舟云学术

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A Rapid Forecast Method for the Process of Flash Flood Based on Hydrodynamic Model and KNN Algorithm

Published:2024-02-29 Issue:6 Volume:38 Page:1903-1919
ISSN:0920-4741
Container-title:Water Resources Management
language:en
Short-container-title:Water Resour Manage

Author:

Zhou Nie,Hou Jingming^ORCID,Chen Hua,Chen Guangzhao,Liu Bingyi

Funder

Numerical Simulation of Flood Process in Urban Areas with Fine Terrain and Lack of Pipe Network Data

High Resolution Numerical Simulation of Sediment Carrying Capacity Mechanism and Erosion Process of Over surface Flow on Whole Sand Slope

Chinesisch-Deutsches Mobilit taprogramm: High-Resolution Numerical Simulating and Predicting Methods for Urban Floods

Publisher

Springer Science and Business Media LLC

Link

https://link.springer.com/content/pdf/10.1007/s11269-023-03664-0.pdf

Reference22 articles.

1. Berardi L, Laucelli D, Simeone V et al (2013) Simulating floods in ephemeral streams in Southern Italy by full-2D hydraulic models. Int J River Basin Manag 11(1):1–17. https://doi.org/10.1080/15715124.2012.746975

2. He BS, Ma MH, Li Q et al (2017) Summary and analysis of my country's mountain flood disaster prevention in 2016. China Flood Control and Drought Relief (01):95–98. https://doi.org/10.16867/j.cnki.cfdm.2017.01.016

3. Hou JM, Liang QH, Zhang HB et al (2015) An efficient unstructured MUSCL scheme for solving the 2D shallow water equations. Environ Model Softw 66:131–152. https://doi.org/10.1016/j.envsoft.2014.12.007

4. Hou JM, Wang JH, Tong Y et al (2021a) High-efficiency and high-precision flood process simulation based on non-uniform grid. Eng Sci Technol 53(04):53–62. https://doi.org/10.15961/j.jsuese.202000760

5. Hou JM, Zhang ZA, Zhang DW et al (2021b) Study on the influence of infiltration on flood propagation with different peak shape coefficients and duration. Water Policy 23:1059–1074. https://doi.org/10.2166/wp.2021.193

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