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Copula-based assimilation of radar and gauge information to derive bias-corrected precipitation fields

机译:基于Copula的雷达和轨距信息同化,以得出经偏差校正的降水场

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摘要

This study addresses the problem of combining radar information and gaugemeasurements. Gauge measurements are the best available source of absoluterainfall intensity albeit their spatial availability is limited.Precipitation information obtained by radar mimics well the spatial patternsbut is biased for their absolute values.In this study copula models are used to describe the dependence structurebetween gauge observations and rainfall derived from radar reflectivity atthe corresponding grid cells. After appropriate time series transformation togenerate "iid" variates, only the positive pairs (radar >0,gauge >0) of the residuals are considered. As not each grid cellcan be assigned to one gauge, the integration of point information, i.e.gauge rainfall intensities, is achieved by considering the structure and thestrength of dependence between the radar pixels and all the gauges within theradar image. Two different approaches, namely Maximum Theta andMultiple Theta, are presented. They finally allow for generatingprecipitation fields that mimic the spatial patterns of the radar fields andcorrect them for biases in their absolute rainfall intensities. Theperformance of the approach, which can be seen as a bias-correction for radarfields, is demonstrated for the Bavarian Alps. The bias-corrected rainfallfields are compared to a field of interpolated gauge values (ordinarykriging) and are validated with available gauge measurements. The simulatedprecipitation fields are compared to an operationally corrected radarprecipitation field (RADOLAN). The copula-based approach performs similarlywell as indicated by different validation measures and successfully correctsfor errors in the radar precipitation.
机译:这项研究解决了将雷达信息与仪表测量相结合的问题。量规测量是绝对降雨强度的最佳可用来源,尽管其空间可用性有限。雷达获得的降水信息模拟了空间模式,但其绝对值存在偏差。 在本研究中,用copula模型描述了观测资料与降雨之间的相关性结构取决于相应网格单元的雷达反射率。经过适当的时间序列转换以生成“ iid”变量后,仅考虑残差的正对(雷达> 0,量规> 0)。由于不是每个网格单元都可以分配一个量规,因此通过考虑雷达像素与雷达图像内所有量规之间的结构和相依强度,可以实现点信息即量规降雨强度的积分。介绍了两种不同的方法,即最大Theta 和多个Theta 。最后,它们允许生成模拟雷达场空间模式的降水场,并对其绝对降雨强度的偏差进行校正。这种方法的性能可以看作是雷达场的偏差校正,已在巴伐利亚阿尔卑斯山得到了证明。将经过偏差校正的降雨场与内插仪表值(普通克里金法)字段进行比较,并通过可用仪表测量进行验证。将模拟的降水场与经操作校正的雷达降水场(RADOLAN)进行比较。基于copula的方法执行效果类似,如不同的验证措施所示,并且可以成功校正雷达降水中的误差。

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