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Statistical analysis of error propagation from radar rainfall to hydrological models

机译:从雷达降雨到水文模型误差传播的统计分析

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This study attempts to characterise the manner with which inherent error inradar rainfall estimates input influence the character of the stream flowsimulation uncertainty in validated hydrological modelling. An artificialstatistical error model described by Gaussian distribution was developed togenerate realisations of possible combinations of normalised errors andnormalised bias to reflect the identified radar error and temporaldependence. These realisations were embedded in the 5 km/15 min UK Nimrodradar rainfall data and used to generate ensembles of stream flowsimulations using three different hydrological models with varying degreesof complexity, which consists of a fully distributed physically-based modelMIKE SHE, a semi-distributed, lumped model TOPMODEL and the unit hydrographmodel PRTF. Thesemodels were built for this purpose and applied to the Upper Medway Catchment(220 km2) in South-East England. The results show that the normalisedbias of the radar rainfall estimates was enhanced in the simulated streamflow and also the dominate factor that had a significant impact on streamflow simulations. This preliminary radar-error-generation model could bedeveloped more rigorously and comprehensively for the error characteristicsof weather radars for quantitative measurement of rainfall.
机译:这项研究试图表征在经过验证的水文模拟中,雷达降水估计输入的固有误差影响河流流量模拟不确定性特征的方式。开发了一种由高斯分布描述的人工统计误差模型,以生成归一化误差和归一化偏差的可能组合的实现,以反映所识别的雷达误差和时间相关性。这些实现被嵌入到5 km / 15分钟的英国Nimrodradar降雨数据中,并用于使用三种具有不同复杂程度的不同水文模型来生成河流模拟流,这些模型包括完全分布式的基于物理的模型MIKE SHE,半分布式,集总模型TOPMODEL和单位水文模型PRTF。这些模型是为此目的而构建的,并应用于英格兰东南部的上梅德韦集水区(220 km 2 )。结果表明,在模拟的水流中雷达雨量估计值的归一化偏斜得到了增强,并且对水流模拟产生重大影响的主导因素也得到了增强。可以针对雨量定量测量天气雷达的误差特性,更加严格和全面地开发这种初步的雷达误差产生模型。

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