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Impact of urbanization on rainfall-runoff processes: case study in the Liangshui River Basin in Beijing, China

机译:城市化对降雨径流过程的影响:以北京凉水河流域为例

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China is undergoing rapid urbanization during the past decades. For example, the proportion of urban population in Beijing has increased from 57.6a?ˉ% in 1980 to 86.3a?ˉ% in 2013. Rapid urbanization has an adverse impact on the urban rainfall-runoff processes, which may result in the increase of urban flood risk. In the present study, the major purpose is to investigate the impact of land use/cover change on hydrological processes. The intensive human activities, such as the increase of impervious area, changes of river network morphology, construction of drainage system and water transfer, were considered in this study. Landsat TM images were adopted to monitor urbanization process based on Urban Land-use Index (ULI). The SWMM model considering different urbanized scenarios and anthropogenic disturbance was developed. The measured streamflow data was used for model calibration and validation. Precipitation with different return periods was taken as model input to analyse the changes of flood characteristics under different urbanized scenarios. The results indicated that SWMM provided a good estimation for storms under different urbanized scenarios. The volume of surface runoff after urbanization was 3.5 times greater than that before urbanization; the coefficient of runoff changed from 0.12 to 0.41, and the ratio of infiltration decreased from 88 to 60a?ˉ%. After urbanization, the time of overland flow concentration increased while the time of river concentration decreased; the peak time did not show much difference in this study. It was found that the peak flow of 20-year return-period after urbanization is greater than that of 100-year return-period before urbanization. The amplification effect of urbanization on flood is significant, resulting in an increase of the flooding risk. These effects are especially noticeable for extreme precipitation. The results in this study will provide technical support for the planning and management of urban storm water and the evaluation on Low Impact Development (LID) measures.
机译:在过去的几十年中,中国正在经历快速的城市化进程。例如,北京的城市人口比例从1980年的57.6a%上升到2013年的86.3a%。快速的城市化对城市降雨径流过程有不利影响,这可能导致城市降雨径流增加。城市洪水风险。在本研究中,主要目的是调查土地利用/覆盖变化对水文过程的影响。本研究考虑了人类的密集活动,如不透水面积的增加,河网形态的变化,排水系统的建设和输水等。采用Landsat TM影像,根据城市土地利用指数(ULI)监测城市化进程。建立了考虑不同城市化情景和人为干扰的SWMM模型。测得的流量数据用于模型校准和验证。以回归期不同的降水为模型输入,分析了不同城市化情景下洪水特征的变化。结果表明,SWMM为不同城市化情景下的风暴提供了很好的估计。城市化后的地表径流量是城市化前的3.5倍。径流系数从0.12变为0.41,入渗率从88降低到60a?%。城镇化后,陆流集中时间增加,河流集中时间减少。在这项研究中,高峰时间没有太大差异。研究发现,城市化后20年回报期的峰值流量大于城市化前100年回报期的峰值流量。城市化对洪水的放大作用非常显着,导致洪水风险增加。这些影响对于极端降水尤为明显。这项研究的结果将为城市雨水的规划和管理以及对低影响发展(LID)措施的评估提供技术支持。

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