Evaluation of Microphysical Retrievals from Polarimetric Radar with Wind Profiler Data

P. May, T. Keenan
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引用次数: 59

Abstract

Abstract Polarimetric radar data have been used to produce microphysical classifications. This kind of analysis is run in a real-time mode from several research radars, including the C-band polarimetric (C-Pol) radar in Darwin, Australia. However, these classifications have had very little systematic evaluation with independent data. Using surface data is often difficult because of sampling issues, particularly for hail. The approach taken here is to use a combination of 50- and 920-MHz wind profiler estimates of rain and hail to provide validation data for the radar pixels over the profiler. The profilers also observe signals associated with lightning, and some comparisons are made between lightning occurrence and the radar measurements of graupel. The retrievals of hail–rain mixtures are remarkably robust; there are some issues regarding other microphysical classes, however, including difficulties in detecting melting snow layers in stratiform rain. These difficulties are largely due to the resampling o...
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利用风廓线资料评价极化雷达微物理反演结果
极化雷达数据已被用于产生微物理分类。这种分析是在几个研究雷达的实时模式下运行的,包括澳大利亚达尔文的c波段偏振(C-Pol)雷达。然而,这些分类很少有独立数据的系统评价。由于采样问题,使用地面数据通常很困难,特别是对于冰雹。这里采用的方法是结合使用50 mhz和920 mhz风廓线仪对降雨和冰雹的估计,为廓线仪上的雷达像素提供验证数据。廓线仪还观测到与闪电有关的信号,并将闪电的发生与雷达测量的霰进行了比较。冰雹雨混合物的反演结果非常稳定;然而,还有一些关于其他微物理类的问题,包括在层状雨中探测融化的雪层的困难。这些困难主要是由于……的重采样。
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