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A grid-based rainfall-runoff model for flood simulation including paddy fields

机译:基于网格的包括稻田在内的洪水模拟降雨径流模型

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A grid-based, KIneMatic wave STOrm Runoff Model (KIMSTORM) is described. The model adopts the single flow-path algorithm and routes the water balance during the storm period. Manning's roughness coefficient adjustment function of the paddy cell was applied to simulate the flood mitigation effect of the paddy fields for the grid-based, distributed rainfall-runoff modeling. The model was tested in 2296 km2 dam watershed in South Korea using six typhoon storm events occurring between 2000 and 2007 with500 m spatial resolution, and the results were tested through the automatic model evaluation functions in the model. The average values of the Nash-Sutc-liffe model efficiency (ME), the volume conservation index (VCI), the relative error of peak runoffrate (EQ_p), and the absolute error of peak runoff (ET_p) were 0.974, 1.016, 0.019, and 0.45 h for calibrated storm events and 0.975, 0.951, 0.029, and 0.50 h for verified storm events, respectively. In the simulation of the flood mitigation effect of the paddy fields, the average values of the percentagechanges for peak runoff, total runoff volume, and time to peak runoff were only -1.95, -0.93, and 0.19%, respectively.
机译:描述了一种基于网格的KIneMatic波STOrm径流模型(KIMSTORM)。该模型采用单一流径算法,并在暴风雨期间路由水平衡。应用Manning的稻谷糙率系数调整功能,以基于网格的分布式降雨-径流模型模拟稻田的防洪效果。该模型在韩国2296 km2大坝流域进行了测试,使用了2000年至2007年之间发生的六次台风风暴事件,空间分辨率为500 m,并通过模型中的自动模型评估功能对结果进行了测试。 Nash-Sutc-liffe模型效率(ME),体积守恒指数(VCI),峰值径流率的相对误差(EQ_p)和峰值径流的绝对误差(ET_p)的平均值分别为0.974、1.016、0.019 ,对于经过校准的暴风雨事件分别为0.45小时和0.95、0.951、0.029和0.50小时,对于已验证的暴风雨事件而言。在水田减洪效果的模拟中,峰值径流量,总径流量和到峰值径流时间的百分比变化平均值分别仅为-1.95,-0.93和0.19%。

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