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首页> 外文期刊>International Journal of Disaster Risk Science >Different Flooding Behaviors Due to Varied Urbanization Levels within River Basin: A Case Study from the Xiang River Basin, China
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Different Flooding Behaviors Due to Varied Urbanization Levels within River Basin: A Case Study from the Xiang River Basin, China

机译:流域内城市化水平变化导致的不同洪水行为-以湘江流域为例

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Booming urbanization due to a fast-growing population results in more impervious areas, less infiltration, and hence greater flood peak and runoff. Clear understanding of flood responses in regions with different levels and expansions of urbanization is of great importance for regional urban planning. In this study, comparison of flooding responses to urbanization processes in terms of flood peak and runoff volume in the upper, middle, and lower Xiang River Basin (XRB), China, was carried out using the Hydrologic Engineering Center-Hydrologic Modeling System (HEC-HMS) model. From 2005 to 2015, urbanization level and intensity were higher in the lower XRB compared to the upper and middle XRB, and the overall expansion rate of urban areas was 112.8%. Modeling results by the HEC-HMS model indicate elevated flood peak discharges and volumes due to fast urbanization in the XRB from the 1980s to 2015. This rapid increase is particularly the case in the lower XRB. The study also revealed different hydrological responses of flood regimes—urbanization tends to have larger impacts on peak flood flow rather than on flood volume in the lower XRB, which further corroborated urbanization-induced intensifying flood processes in terms of peak flood flow. Urbanization has increasing impacts on flood volume from the upper to the lower XRB, which can be attributed to accumulated runoff down the river system. This study provides a reference for basin-wide land use and urban planning as well as flood hazard mitigation.
机译:由于人口的快速增长,城市化的蓬勃发展导致了更不透水的地区,更少的渗透,从而导致更大的洪峰和径流量。清楚了解不同水平和城市化程度不断扩大的地区的洪水响应对区域城市规划具有重要意义。在这项研究中,利用水文工程中心-水文模拟系统(HEC),根据中国上,中,下游湘江流域(XRB)的洪峰和径流量比较了洪水对城市化过程的响应。 -HMS)模型。从2005年到2015年,低XRB地区的城市化水平和强度高于高XRB地区和中XRB地区,城市地区的总体扩张率为112.8%。 HEC-HMS模型的建模结果表明,由于1980年代至2015年XRB的快速城市化,洪水高峰流量和流量都增加了。这种快速增长尤其是XRB较低的情况。该研究还揭示了洪水制度的不同水文响应-城市化往往会对洪峰流量产生更大的影响,而不是对下游XRB的洪水量产生更大的影响,这进一步证实了城市化导致的洪峰过程加剧。城市化对高XRB到低XRB的洪水量的影响越来越大,这可以归因于河流系统下游的累积径流。该研究为流域范围的土地利用和城市规划以及减轻洪灾灾害提供了参考。

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