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Rainfall estimation improvements using polarization data from Monte Lema C-band weather radar in the southern European alps

机译:使用来自欧洲南部阿尔卑斯山的蒙特勒玛C波段天气雷达的极化数据改进降雨估算

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Simple improvements in C-band weather radar data processing are performed based on radar polarimetry. The starting point is the estimation of the differential propagation phase ΦDP from the measured total differential phase ΨDP. The main topics are (ground) clutter removal and quantitative precipitation estimation (QPE). For the former, a new test which checks some polarimetric quantities is added (as a trial) in a pre-existing clutteron-clutter bin classification system For the latter, three ‘state-of-the-art’ ΦDP-based precipitation attenuation correction procedures are considered to correct ZH for precipitation attenuation. In addition, since the specific differential phase KDP proves to be a better rainfall rate estimator in heavy rain, some hybrid formulas R(ZH, KDP) are developed so that they result practically unbiased.
机译:基于雷达极化仪对C波段天气雷达数据处理进行了简单的改进。起点是从测量的总差分相位phase DP 估算差分传播相位Φ DP 。主要主题是(地面)杂波去除和定量降水估计(QPE)。对于前者,在预先存在的杂物/非杂物箱分类系统中添加了(作为试验)一项新的检查极化量的测试。对于后者,使用了三个“最新技术”Φ基于DP 的降水衰减校正程序被认为可以校正Z H 的降水衰减。另外,由于在大雨中特定的微分相位K D P被证明是更好的降雨率估算器,因此一些混合公式R(Z H ,K D P)被开发出来,因此它们几乎没有偏见。

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