首页|基于SWMM与LISFLOOD-FP耦合模型的城市街区内涝模拟研究

基于SWMM与LISFLOOD-FP耦合模型的城市街区内涝模拟研究

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为了评估高度城市化建设背景下暴雨侵袭时城市街区内涝灾害的演变过程,以北京市海淀区清河流域某典型排水分区为研究对象,构建了基于SWMM与LISFLOOD-FP模型的水文水动力耦合模型。选择P20210712、P20210718和P20210823 3场实测降雨率定和验证模型参数,并应用于P20210703实测降雨的预测,同时选取降雨重现期分别为10、20、30、50 a的长历时(24 h)设计降雨情景进行内涝模拟分析。结果表明:3场实测降雨条件下模型的纳什效率系数分别为0。76、0。68、0。71,模型参数设置合理;P20210703实测降雨条件下,模型模拟所得淹没范围、淹没水深与实际观测情况较为吻合,耦合模型精度较高;4种不同降雨重现期的长历时设计降雨情景下,溢流节点数和溢流总量均随降雨重现期的增大而增加,淹没深度大于1。00m的淹没面积从降雨重现期为10a的0。024 km2,增大到降雨重现期为50 a的0。345 km2,主要集中在上地下凹桥区、安宁庄西路、安宁庄中街、安宁庄路等位置,与观测情况吻合较好。
Research on urban block waterlogging simulation based on coupling model of SWMM and LISFLOOD-FP
In order to evaluate the evolution process of urban block waterlogging disaster when encountering rainstorm under the highly urbanized construction,a typical drainage division of the Qinghe River Basin in Haidian District of Beijing was selected as the research object,and a hydrological-hydrodynamic coupling model based on SWMM and LISFLOOD-FP model was constructed.Three measured rainfall events,P20210712,P20210718,and P20210823,were selected for model parameter calibration and validation.P20210703 measured rainfall was selected for model application,and long-term(24 h)rainfall scenarios with rainfall return periods of 10,20,30,and 50 a were selected for waterlogging simulation analysis.The results show that the Nash-Sutcliffe efficiency coefficients of the model under three measured rainfall conditions are 0.76,0.68,and 0.71,respectively,indicating that the model parameters are set reasonably.Under the condition of P20210703 measured rainfall,the simulated inundation range and depth of the model are in good agreement with the actual observation,indicating that the coupled model has high accuracy.Under long-term design rainfall scenarios with four different rainfall return periods,the number of overflow nodes and the total amount of overflow both increase with the increase of rainfall return period.The submerged area with a depth greater than 1.00 m increased from 0.024 km2 with a rainfall return period of 10 a to 0.345 km2 with a rainfall return period of 50a,mainly concentrated in lower concave bridge areas of Shangdi Road,Anningzhuang West Road,Anningzhuang Middle Street,Anningzhuang Road,etc.,which are in good agreement with the observation results.

urban stormwaterlogging modelhydrologic-hydrodynamic coupling modeloverflow volumeinundation depth

卢兴超、徐宗学、李永坤、胡小红、唐清竹、宋鹏越

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北京师范大学水科学研究院,北京 100875

城市水循环与海绵城市技术北京市重点实验室,北京 100875

北京市水科学技术研究院,北京 100048

城市暴雨 内涝模型 水文水动力耦合模型 溢流总量 淹没深度

国家自然科学基金重点项目

52239003

2024

水资源保护
河海大学 中国水利学会环境水利研究会

水资源保护

CSTPCD北大核心EI
影响因子:0.827
ISSN:1004-6933
年,卷(期):2024.40(3)
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