文章摘要
乔贤玲, 侯精明, 刘 园, 陈光照, 王 添, 郭庆元, 高徐军, 王 岩.降雨空间分辨率对城市内涝模拟敏感性研究Journal of Water Resources and Water Engineering[J].,2024,35(3):81-89
降雨空间分辨率对城市内涝模拟敏感性研究
Sensitivity of rainfall data spatial resolution to urban inundation simulation
  
DOI:10.11705/j.issn.1672-643X.2024.03.10
中文关键词: 降雨空间分辨率  城市雨洪模型  洛伦兹曲线  基尼系数  西安市小寨片区
英文关键词: rainfall spatial resolution  urban inundation model  Lorenz curve  Gini coefficient  the Xiaozhai area of Xi’an City
基金项目:国家自然科学基金项目( 52079106);中德合作交流项目( M-0427) ; 陕西省自然科学基础研究计划-引汉济渭联合基金重点项目(2022JC-LHJJ-09);宁夏回族自治区重点研发计划项目(2022BEG02020)
Author NameAffiliation
QIAO Xianling1, HOU Jingming1, LIU Yuan2, CHEN Guangzhao1, WANG Tian1, GUO Qingyuan3, GAO Xujun2, WANG Yan2 (1.西安理工大学 省部共建西北旱区生态水利国家重点实验室 陕西 西安 710048 2.中国电建集团西北勘测设计研究院有限公司 陕西 西安 710065 3.西安市气象局 陕西 西安 710014) 
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中文摘要:
      为研究降雨空间分辨率对城市内涝模拟的影响规律以及一、二维耦合的城市雨洪模型的敏感性降雨空间分辨率,本研究选取西安市小寨片区为研究区,以西安市气象局提供的3场降雨为基础,采用空间插值算法获取5种降雨(0.2、0.5、1.0、2.0和4.0 km)空间分辨率,引入洛伦兹曲线、基尼系数判断不同降雨空间分辨率的不均匀程度,驱动一、二维耦合的城市雨洪模型进行模拟分析。结果表明,3场降雨0.5 km降雨空间分辨率对应的基尼系数分别为0.163、0.201、0.165,评价结果均为均匀分布。随着降雨空间分辨率的降低,基尼系数逐渐减小,峰值积水面积相对误差、内涝积水水量相对变化范围、内涝淹没水深相对变化范围均逐渐增大。对于这3个水力要素评价指标,降雨空间分辨率为0.5 km对应的模拟误差最小,且该降雨空间分辨率为敏感性降雨空间分辨率。
英文摘要:
      To study the impact of rainfall spatial resolution on the simulation of urban inundation and the sensitivity of a one-two-dimensional coupled urban inundation model, this research selected the Xiaozhai area of Xi’an City as the study area. Based on three rainfall datasets provided by the Xi’an Meteorological Bureau, the spatial interpolation algorithm of inverse distance weighting was used to obtain five rainfall spatial resolutions: 0.2, 0.5, 1.0, 2.0, and 4.0 km. The Lorenz curve and Gini coefficient were introduced to assess the uniformity of different rainfall spatial resolutions, and they were used to drive the one-two-dimensional coupled urban inundation model for simulation analysis. The results indicate that for the three rainfall events, the Gini coefficients corresponding to the 0.5 km rainfall spatial resolution are 0.163, 0.201, and 0.165, indicating uniformly distributed evaluations. As the rainfall spatial resolution decreases, the Gini coefficient gradually decreases, while the relative errors of peak inundation area, relative changes in inundation volume, and relative changes in inundation depth all gradually increase. In terms of these three hydraulic evaluation indicators, the simulation error is the smallest for the rainfall spatial resolution of 0.5 km, and this resolution is identified as the sensitive rainfall spatial resolution.
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