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Influence of rainfall observation network on model calibration and application

机译:降雨观测网络对模型标定和应用的影响

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摘要

The objective in this study is to investigate the influence of the spatial resolution of the rainfall input on the model calibration and application. The analysis is carried out by varying the distribution of the raingauge network. A meso-scale catchment located in southwest Germany has been selected for this study. First, the semi-distributed HBV model is calibrated with the precipitation interpolated from the available observed rainfall of the different raingauge networks. An automatic calibration method based on the combinatorial optimization algorithm simulated annealing is applied. The performance of the hydrological model is analyzed as a function of the raingauge density. Secondly, the calibrated model is validated using interpolated precipitation from the same raingauge density used for the calibration as well as interpolated precipitation based on networks of reduced and increased raingauge density. Lastly, the effect of missing rainfall data is investigated by using a multiple linear regression approach for filling in the missing measurements. The model, calibrated with the complete set of observed data, is then run in the validation period using the above described precipitation field. The simulated hydrographs obtained in the above described three sets of experiments are analyzed through the comparisons of the computed Nash-Sutcliffe coefficient and several goodness-of-fit indexes. The results show that the model using different raingauge networks might need re-calibration of the model parameters, specifically model calibrated on relatively sparse precipitation information might perform well on dense precipitation information while model calibrated on dense precipitation information fails on sparse precipitation information. Also, the model calibrated with the complete set of observed precipitation and run with incomplete observed data associated with the data estimated using multiple linear regressions, at the locations treated as missing measurements, performs well.
机译:本研究的目的是研究降雨输入的空间分辨率对模型校准和应用的影响。通过改变雨量计网络的分布来进行分析。这项研究选择了位于德国西南部的中尺度流域。首先,使用从不同雨量计网络的可用观测降水量内插的降水量对半分布式HBV模型进行校准。提出了一种基于组合优化算法模拟退火的自动标定方法。分析了水文模型的性能与雨量计密度的关系。其次,使用来自用于校准的相同雨量计密度的内插降水以及基于减小和增加的雨量计密度网络的内插降水来验证校准模型。最后,通过使用多元线性回归方法填充缺失的测量值来研究缺失的降雨数据的影响。然后,使用上述降水场在验证期内运行用完整的观测数据集校准的模型。通过比较计算出的纳什-萨克利夫系数和几个拟合优度指标,分析了上述三组实验中获得的模拟水文图。结果表明,使用不同雨量计网络的模型可能需要对模型参数进行重新校准,特别是在相对稀疏的降水信息上校准的模型可能在密集降水信息上表现良好,而在密集降水信息上校准的模型在稀疏降水信息上失败。同样,在观察到的降水的完整集合上校准的模型以及在与被视为缺失测量值的位置上使用不完整的观察到的数据(与使用多个线性回归估算的数据相关联)一起运行时,模型效果很好。

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