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Infiltration Losses Calculated for the Flash Flood in the Upper Catchment of Geru River, Gala?i County, Romania

机译:罗马尼亚加拉奇县格鲁河上游流域暴雨洪水的入渗损失计算

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MIKE software created by Danish Institute of Hydraulics can be used to perform mathematical modelling of rainfall-runoff process on the hillslopes, resulting in a runoff hydrograph in the closing section of a catchment. The software includes a unitary hydrograph method - UHM in the hydrological module Rainfall - Runoff. Excess rainfall is routed to the river and transited through unit hydrograph method. The model divides the flood generating precipitation in excess rainfall (net rainfall) and losses (infiltration). This paper analyzes data from the flash flood that occurred between the 11th and 13th of September 2013 in the upper catchment of the river Geru. The catchment chosen for study, is controlled by the hydrometric station located in the village Cudalbi. Simulations of this flash flood were performed with MIKE by DHI –UHM software, alternatively using as input data the precipitations recorded by AHSS (Automated Hydrological Sensor Station) Cudalbi and radar precipitations generated by ROFFG (Romanian Flash Flood Guidanc e) software system in ArcGIS module for determining the areas affected by flash floods. The Unitary Hydrograph Method - UHM from the hydrological module Rainfall – Runoff calculates excess rainfall and determines infiltration losses by four methods. For each set of input data, the four methods for calculating infiltration losses were subsequently used. The comparison between the results highlights that the amplitude and phase errors for the maximum discharge are smaller when the model uses for simulation radar precipitations as input data, and calculates infiltration losses with the Proportional Loss method. This method reproduces with a better accuracy the peaks of the discharge hydrograph. The model can be used in the future to forecast a discharge hydrograph based on estimated radar precipitations in the catchment.
机译:丹麦水利学会开发的MIKE软件可用于对山坡上的降雨-径流过程进行数学建模,从而在流域的关闭部分生成径流水位图。该软件在水文模块降雨-径流中包含单一的水文法-UHM。过多的降雨被引导到河流,并通过单位水位法进行过渡。该模型将洪灾产生的降水除以过量降雨(净降雨)和损失(入渗)。本文分析了2013年9月11日至13日在格鲁河上游流域发生的山洪暴发的数据。选择进行研究的流域由位于Cudalbi村的水文站控制。使用DHI –UHM软件通过MIKE对此次洪水进行了模拟,或者使用ArcGIS模块中的AHSS(自动水文传感器站)Cudalbi记录的降水和ROFFG(罗马尼亚洪水Guidanc e)软件系统生成的雷达降水作为输入数据。确定受山洪影响的区域。水文模块降雨-径流中的统一水文法-UHM通过四种方法计算过量降雨并确定入渗损失。对于每组输入数据,随后使用了四种计算渗透损失的方法。结果之间的比较表明,当模型将模拟雷达降水用作输入数据并使用比例损失法计算入渗损失时,最大流量的幅度和相位误差较小。该方法可以更好地再现放电水位图的峰值。该模型将来可用于基于流域内估计的雷达降水量来预测流量水位图。

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