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Calibration of Rainfall Runoff Models in Ungauged Catchments: Regionalization Relationships for a Rainfall Runoff Model

机译:疏ga集水区降雨径流模型的标定:降雨径流模型的区域关系。

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In many regions where rainfall runoff models are required, there is a lack of streamflowdata available to calibrate the model parameters. Along with streamflow data simply notbeing recorded, there are many reasons for a lack of a suitable data set for modelcalibration, such as significant modifications to catchment characteristics, or longperiods of unseasonable rainfall producing unrepresentative relationships. Generally, foran ungauged catchment, it is desirable to implement a model with as few free parametersas possible, provided the conceptualization of the model is suitable for the catchmentunder consideration. The Australian Water Balance Model (AWBM) is a rainfall runoffmodel that is commonly used in Australia. Typically it has 7 parameters, howevermethods are available to determine the storage size and capacity parameters for theAWBM based on an estimate of the average annual runoff. This is a great advantagewhen applying the model to ungauged catchments. However, there are two AWBMparameters which cannot be determined by this approach, namely the baseflow indexand baseflow recession constant. The aim of this paper is to develop regionalizationrelationships to allow these two parameters to be estimated for ungauged catchments,based on the characteristics of the catchment that can be easily identified. GeneralRegression Neural Networks are used to identify the relationships between modelparameters and catchment characteristics. The results indicate that by using only easilyidentifiable characteristics of an ungauged catchment, suitable estimates of the unknownAWBM parameter values can be obtained, thereby allowing reasonable rainfall-runoffmodels to be developed. While the relationships developed in this work are specific toAustralian catchments, the methodology used can be easily adapted to developrelationships for other regions.
机译:在许多需要降雨径流模型的地区,流量缺乏 可用于校准模型参数的数据。连同流数据根本不一样 被记录下来的原因很多,原因是缺少适用于模型的数据集 校准,例如对流域特性的重大修改,或长时间 降雨不足的时期会产生代表性的关系。通常,对于 在没有流域的集水区,希望实现具有最少自由参数的模型 只要模型的概念化适合于流域 在考虑中。澳大利亚水平衡模型(AWBM)是降雨径流 澳大利亚常用的模型。通常它有7个参数,但是 可用方法来确定存储的大小和容量参数 AWBM基于对年均径流量的估算。这是一个很大的优势 将模型应用于未受污染的集水区时。但是,有两个AWBM 用这种方法无法确定的参数,即基流索引 和基流衰退常数。本文的目的是发展区域化 关系,以允许针对未覆盖的集水区估算这两个参数, 根据可以轻松识别的集水区特征。一般的 回归神经网络用于识别模型之间的关系 参数和流域特征。结果表明,仅通过轻松使用 没流失的流域的可识别特征,对未知流域的适当估计 可以获得AWBM参数值,从而实现合理的降雨径流 待开发的模型。虽然在这项工作中建立的关系是特定于 澳大利亚流域,所使用的方法可以很容易地适应发展 其他地区的关系。

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