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Application of distributed KIneMatic wave STOrm Runoff Model (KIMSTORM) for flood simulation considering dam release in the NamHan river basin of Korea

机译:考虑韩国水坝释放的分布式KIneMatic波STOrm径流模型(KIMSTORM)在洪水模拟中的应用

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摘要

This study describes the application of distributed hydrologic model, KIneMatic wave STOrm Runoff Model (grid-based KIMSTORM) to simulate the flood discharge considering dam releases during storm event. The model adopts single flowpath algorithm, and simulates surface and subsurface water depth by routing the water balance of hydrologic components at each cell. For the 12,373 km 2 watershed having four dams (two multipurpose, one hydroelectric, and one flood regulation) of NamHan river in Korea, the model was calibrated and verified at five stream locations (two on main and three on tributary) for six flood events with the average Nash-Sutcliffe model efficiency of 0.77. The release amount from dam cell was successfully delivered to the next down cell as an inflow and propagated to the downstream because the model solves the flow routing with hydrologic approach. From the spatiotemporal model results, we could trace the growth of overland flow discharge, the flood flow progress, and the regulation effect by the dams.
机译:这项研究描述了应用分布式水文模型,KIneMatic Wave STOrm径流模型(基于网格的KIMSTORM)来模拟考虑暴雨过程中大坝释放的洪水流量。该模型采用单一流径算法,并通过路由每个单元中水文组分的水平衡来模拟地表和地下水深。对于韩国南汉河有四个水坝(两个多用途,一个水力发电和一个洪水调节)的12,373 km 2流域,在六个溪流事件的五个溪流位置(两个在主干河和三个在支流上)对模型进行了校准和验证。 Nash-Sutcliffe模型的平均效率为0.77。由于该模型通过水文方法解决了水流路径问题,因此从坝单元释放的水量作为流入量成功传递到了下一个向下的单元,并传播到下游。从时空模型结果中,我们可以追踪到陆上径流量的增长,洪水的流量以及大坝的调节作用。

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