ESTIMATION OF LEVEE FAILURE POINTS BASED ON LEVEE VULNERABILITY INDEX AND FLOOD RISK ANALYSIS BY INTEGRATING SIMULATION OF FLOOD FLOW AND INUNDATION

Kosuke Tabata, S. Fukuoka
{"title":"ESTIMATION OF LEVEE FAILURE POINTS BASED ON LEVEE VULNERABILITY INDEX AND FLOOD RISK ANALYSIS BY INTEGRATING SIMULATION OF FLOOD FLOW AND INUNDATION","authors":"Kosuke Tabata, S. Fukuoka","doi":"10.2495/RBM190081","DOIUrl":null,"url":null,"abstract":"ABSTRACT To examine the flood risk management measures, it is important to estimate the levee breach points, inundation discharge hydrograph and motion of the inundation water in the basin as precisely as possible. The purpose of this paper is to conduct the above series of studies on the Kinu River (Japan) suffered from inundation in the range of 40 km2 due to overflowing and levee breach during the 2015 large flood. First, a simulation model integrating flood flow and inundation is developed. The inundation discharge hydrographs due to the overflowing and levee breach are estimated by the flood flow analysis based on observed temporal changes in water surface profiles in the Kinu River. The inundation is calculated by a two-dimensional model. The mesh of the inundation analysis model is generated by regular grid with 5 m size in order to express the microtopography obtained by DSM (Digital Surface Model). Manning’s roughness coefficients are given according to the situation of the land use and inundation depth. It is confirmed that the developed model is useful by the inundation arrival time read from camera images and the spread of the actual inundation water in the basin. Next, the suitability of the levee vulnerability index t* which has been derived by the authors is examined for the levees of the Kinu River. Finally, the inundation flow analysis is conducted under the actual and hypothetical levee breach conditions based on the value of t*. It is concluded that the difference in the location and time of the levee breach influences on the motion of the inundation water and inundation areas in the Kinu River basin.","PeriodicalId":390754,"journal":{"name":"River Basin Management X","volume":"55 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2019-07-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"River Basin Management X","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.2495/RBM190081","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

Abstract

ABSTRACT To examine the flood risk management measures, it is important to estimate the levee breach points, inundation discharge hydrograph and motion of the inundation water in the basin as precisely as possible. The purpose of this paper is to conduct the above series of studies on the Kinu River (Japan) suffered from inundation in the range of 40 km2 due to overflowing and levee breach during the 2015 large flood. First, a simulation model integrating flood flow and inundation is developed. The inundation discharge hydrographs due to the overflowing and levee breach are estimated by the flood flow analysis based on observed temporal changes in water surface profiles in the Kinu River. The inundation is calculated by a two-dimensional model. The mesh of the inundation analysis model is generated by regular grid with 5 m size in order to express the microtopography obtained by DSM (Digital Surface Model). Manning’s roughness coefficients are given according to the situation of the land use and inundation depth. It is confirmed that the developed model is useful by the inundation arrival time read from camera images and the spread of the actual inundation water in the basin. Next, the suitability of the levee vulnerability index t* which has been derived by the authors is examined for the levees of the Kinu River. Finally, the inundation flow analysis is conducted under the actual and hypothetical levee breach conditions based on the value of t*. It is concluded that the difference in the location and time of the levee breach influences on the motion of the inundation water and inundation areas in the Kinu River basin.
查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
基于堤防易损性指数和洪水风险综合模拟的堤防破坏点估算
为了检验洪水风险管理措施,必须尽可能准确地估计堤防决口点、淹没流量线和流域淹没水运动。本文的目的是在2015年大洪水期间,日本基努河因溢流和堤防决口而遭受40 km2范围内淹没的情况下进行上述系列研究。首先,建立了洪水与淹没相结合的模拟模型。根据观测到的基努河水面剖面的时间变化,通过洪水流量分析,估算了基努河因溢流和决口引起的洪涝流量曲线。洪水是用二维模型计算的。淹没分析模型的网格采用5 m大小的规则网格生成,以表达DSM (Digital Surface model)获得的微地形。曼宁粗糙度系数根据土地利用情况和淹没深度给出。从相机图像中读取的淹没到达时间和实际淹没水在流域内的扩散情况证实了所建立的模型的有效性。其次,对基努河堤防脆弱性指数t*的适用性进行了检验。最后,根据t*的值进行了实际溃坝和假设溃坝条件下的淹没流量分析。结果表明,基努河流域决口位置和决口时间的差异对淹没水量和淹没面积的运动有影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 去求助
来源期刊
自引率
0.00%
发文量
0
期刊最新文献
ADEQUACY OF GEOTEXTILE TUBE DEWATERING IN THREE RIVER REMEDIATION SCENARIOS UNDERGROUND WATERS: CHANGES IN GROUNDWATER POLICIES CRITICAL ROLE OF BRIDGING ORGANIZATIONS IN RIVER BASIN MANAGEMENT IN ALBERTA, CANADA TURBULENT KINETIC ENERGY IN FISH PASSES OF VARIOUS TYPES OF CONSTRUCTION CALIBRATION AND VALIDATION OF ET0 THROUGH AN R-CRAN CODE IN AGRICULTURAL LANDS OF SOUTH-EAST SPAIN
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1