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首页> 外文期刊>Journal of Hydrology >Experimental validation of two-dimensional depth-averaged models for forecasting rainfall–runoff from precipitation data in urban areas
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Experimental validation of two-dimensional depth-averaged models for forecasting rainfall–runoff from precipitation data in urban areas

机译:二维深度平均模型从城市降水数据预测降雨径流的实验验证

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摘要

This paper presents an experimental validation of two widely used numerical models in urban flood inundation studies, the two-dimensional dynamic and diffusive wave models. Instead of using the common approach in flood inundation modelling, which consists of computing the water depth and velocity fields for a given water discharge, in this study the rainfall intensity is imposed directly in the model, the surface runoff being generated automatically. Both the dynamic and diffusive wave models are implemented in the same unstructured finite volume code, removing in such a way any differences in the numerical discretisation other than the wave approximation used to compute the water velocity. Two different methods for representing buildings are used and compared, the so-called building-block and building-hole approaches. Experimental validation of the models is presented in several simplified laboratory configurations of urban catchments, in which the surface runoff has been measured for different hyetographs. For this purpose, 72 experiments were undertaken in a rainfall simulator, including eight catchment configurations and nine hyetographs. Numerical results show that the dynamic wave model is able to predict the peak discharge and its arrival time, as well as the shape of the outlet hydrograph, while the diffusive wave model gives less accurate results. The experimental validation confirms that, when the geometry of the problem is well defined, depth-averaged dynamic wave models may be used to predict rainfall–runoff from direct precipitation data in urban environments.
机译:本文提出了两种在城市洪水泛滥研究中广泛使用的数值模型,即二维动态和扩散波模型的实验验证。代替在洪水淹没模型中使用通常的方法来计算给定排水量的水深和速度场,在本研究中,降雨强度直接施加在模型中,地表径流自动生成。动态波模型和扩散波模型都在相同的非结构化有限体积代码中实现,以这种方式消除了数值离散中除用于计算水速的波逼近之外的任何差异。使用和比较了两种表示建筑物的不同方法,即所谓的“砌块法”和“孔洞法”。在城市流域的几种简化的实验室配置中对模型进行了实验验证,其中已针对不同的湿度记录仪测量了地表径流。为此,在降雨模拟器中进行了72个实验,包括8个集水区配置和9个Hyographs。数值结果表明,动态波模型能够预测峰值流量及其到达时间,以及出口水位图的形状,而扩散波模型的准确性较差。实验验证证实,当问题的几何形状得到明确定义时,深度平均动态波模型可用于根据城市环境中的直接降水数据预测降雨径流。

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