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Unit hydrographs to model quick and slow runoff components of streamflow

机译:单位水位图可模拟流量的快速和缓慢径流分量

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This article derives the unit pulse response functions (unit hydrographs (UHs)) for the quick and slow runoff components of streamflow (quick runoff: direct or surface runoff; slow runoff: the sum of rapid subsurface, delayed subsurface, and groundwater runoffs) using the model of three serial tanks with a parallel tank. The interdependence between the tanks is described by exponential functions of the model's parameters. The parameters are identified using the Simplex method. Ln comparison to traditional unit hydrograph (TUH) methods, the proposed UH method has the following advantages: (1) it can be used to separate quick and slow streamflow components; (2) it is appropriate for forecasting streamflow hydrographs produced by various storms such as single-peak storms and multi-peak storms without resorting to changing model's parameters; and (3) it does not require either an a priori calculation of rainfall excess or baseflow separation for deriving the UH. The TUH models such as the Sherman model and the Nash model with three cascade reservoirs are particular cases of the proposed model. The applicability and validity of the proposed model are verified using observed rainfall-streamflow data from an actual basin. The resulting computed streamflows show a good correspondence with observed ones. (C) 2000 Elsevier Science B.V. All rights reserved. [References: 26]
机译:本文使用以下公式推导了水流的快速和缓慢径流分量的单位脉冲响应函数(单位水位图(UHs))(快速径流:直接径流或地表径流;缓慢径流:快速地下径流,延迟地下径流和地下水径流之和)三个串联水箱与一个平行水箱的模型。储罐之间的相互依赖性通过模型参数的指数函数来描述。使用Simplex方法识别参数。与传统的单位水位线图法相比,本文提出的UH法具有以下优点:(1)可用于分离快,慢水流。 (2)适用于在不求助于模型参数变化的情况下,对单峰风暴和多峰风暴等各种风暴产生的水文水位进行预报的方法; (3)不需要事先计算降雨过量或基流分离来得出UH。 TUH模型(例如具有三个级联储层的Sherman模型和Nash模型)是该模型的特例。利用从实际流域观察到的降雨流数据验证了该模型的适用性和有效性。所得的计算出的流量与观察到的流量显示出良好的对应关系。 (C)2000 Elsevier Science B.V.保留所有权利。 [参考:26]

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