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Rain microstructure retrievals using 2-D video disdrometer and C-band polarimetric radar

机译:使用二维视频测速仪和C波段极化雷达检索雨水微结构

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Measurements using the 2-D video disdrometer (2DVD) taken during a heavyrainfall event in Huntsville, Alabama, are analysed. The 2DVD images wereprocessed to derive the rain microstructure parameters for each individualdrop, which in turn were used as input to the T-matrix method to compute theforward and back scatter amplitudes of each drop at C-band. The polarimetricradar variables were then calculated from the individual drop contributionover a finite time period, e.g., 1 min. The calculated co-polarreflectivity, differential reflectivity, specific differential propagationphase and the co-polar correlation coefficient were compared withmeasurements from a C-band polarimetric radar located 15 km away. Anattenuation-correction method based on the specific differential propagationphase was applied to the co-polar and differential reflectivity data fromthe C-band radar, after ensuring accurate radar calibration. Time seriescomparisons of the parameters derived from the 2DVD and C-band radar datashow very good agreement for all four quantities, the agreement beingsometimes better than the computations using the 1-min drop sizedistribution and bulk assumptions on rain microstructure (such as meanshapes and model-based assumptions for drop orientation). The agreement isparticularly improved in the case of co-polar correlation coefficient sincethis parameter is very sensitive to variation of shapes as well asorientation angles. The calculations mark the first attempt at utilizingexperimentally derived "drop- by-drop" rain microstructure information tocompute the radar polarimetric parameters and to demonstrate the value ofutilizing the 2-D video disdrometer for studying rain microstructure undervarious precipitation conditions. Histograms of drop orientation angles aswell as the most probable drop shapes and the corresponding variations werealso derived and compared with prior results from the 80 m fall "artificialrain" experiment.
机译:分析了在阿拉巴马州亨茨维尔大雨期间使用2-D视频测速仪(2DVD)进行的测量。对2DVD图像进行处理,以得出每个单个雨滴的雨水微结构参数,这些参数又被用作T矩阵方法的输入,以计算C波段每个雨滴的前向和后向散射幅度。然后根据有限时间内(例如1分钟)的单个液滴贡献计算出极化雷达变量。将计算出的同极化反射率,差分反射率,特定差分传播相位和同极化相关系数与位于15公里以外的C波段极化雷达的测量结果进行了比较。在确保精确的雷达校准之后,将基于特定差分传播相位的衰减校正方法应用于来自C波段雷达的同极化和差分反射率数据。从2DVD和C波段雷达数据得出的参数的时间序列比较对于所有四个量都显示出很好的一致性,该一致性有时比使用1-min液滴尺寸分布和雨水微观结构的总体假设(例如均值形状和模型-基于液滴方向的假设)。由于该参数对形状和取向角的变化非常敏感,因此在同极性相关系数的情况下,尤其可以改善一致性。这些计算标志着首次尝试利用实验得出的“逐滴”雨水微结构信息来计算雷达的极化参数,并证明了利用二维视频测速仪研究各种降水条件下雨水微结构的价值。还得出了液滴定向角的直方图以及最可能的液滴形状和相应的变化,并将其与80 m坠落“人工降雨”实验的先前结果进行了比较。

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