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Monitoring and adjusting ground-based weather radar in Europe using TRMM space-borne radar

机译:使用TRMM星载雷达监测和调整欧洲地面气象雷达

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We show how the TRMM Precipitation Radar (TPR) can be used to monitor and adjust Ground-based Radar (GR) data as a function of the distance from the radar site. The analysis is based on the average, linear radar reflectivity in circular rings around the GR site, _(2π), as a function of the range from the GR site. The GR/TPR ratio varies for the Cyprus radar on average from 2 dB, at 10 km, to -10 dB at 100 km. The cause of the average departure at the average range is ascribed mainly to the calibration of the GR. The range dependence of GR/TPR is significant and similar in all the investigated cases. This is attributed to the increasing sampling volume of GR with range combined with non-homogeneous beam filling. For example, at longer ranges of GR, the lower part of the volume could be in rain, whereas the upper part of the same pulse is filled with snow, or even without echo.
机译:我们将展示TRMM降水雷达(TPR)如何根据距雷达站点的距离来监视和调整地面雷达(GR)数据。该分析基于GR站点周围圆环中的平均线性雷达反射率 _(2π),它是GR站点范围的函数。塞浦路斯雷达的GR / TPR比平均从10 km的2 dB到100 km的-10 dB变化。平均范围内平均偏离的原因主要归因于GR的校准。在所有调查的案例中,GR / TPR的范围相关性均显着且相似。这归因于GR的采样量随范围的增加以及不均匀的光束填充而增加。例如,在较长的GR范围内,体积的下部可能处于雨中,而同一脉冲的上部则充满了雪,甚至没有回声。

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