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Assessment and tuning of the behaviour of a microphysical characterisation scheme

机译:评估和调整微物理表征方案的行为

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The correct classification of prevailing bulk hydrometeor type within aradar resolution volume is a challenge task even if a full set ofpolarimetric radar observables is available. Indeed scattering andpropagation effects from the variety of hydrometeors present interact eachothers and sometimes, if not often, tend to obscure the characteristicsignature of each weather radar target type. This consideration is enforcedwhen the atmospheric volume is sampled with a wavelength where both Miescattering effects and attenuation start to become relevant.

In this paper, we utilize the hydrometeor classification scheme developed atthe National Severe Storms Laboratory (USA). Briefly, the scheme uses afuzzy logic approach to combine different polarimetric variables andenvironmental temperature in order to determine the most likely type ofprevalent hydrometeor in the radar volume. This means that the resultingclassification is based on two characteristics: the volume polarimetricresponses and the thermal value. The relative balance between these two ismanaged through the coefficients in the fuzzy scheme. We have observed thatthese parameters are crucial in order to get "physical reasonable result",independently from the meteorological character of the event investigated.

Our work is based on a reduced set of polarimetric variables (Z andZDR) as input. Data used in this study were collected by a C-band radar over weather events ranging from convective to stratiform.

机译:即使有全套极化极化雷达可观测物,如何在雷达分辨率范围内正确地确定主流水生气象子类型的分类也是一项艰巨的任务。实际上,来自各种水凝物的散射和传播效应相互影响,有时(如果不是经常的话)往往会掩盖每种天气雷达目标类型的特征特性。当以一定的波长采样大气体积时,考虑了米斯散射效应和衰减,因此必须考虑到这一点。

在本文中,我们采用了美国国家气象局开发的水流星分类方案风暴实验室(美国)。简而言之,该方案使用模糊逻辑方法来组合不同的极化变量和环境温度,以便确定雷达体积中最有可能的普遍水凝物类型。这意味着最终的分类基于两个特性:体积极化响应和热值。通过模糊方案中的系数来管理这两者之间的相对平衡。我们已经观察到,这些参数对于获得“物理上合理的结果”至关重要,独立于所调查事件的气象特征。

我们的工作基于减少的极化率集变量( Z 和 Z DR )作为输入。这项研究中使用的数据是通过C波段雷达收集的,涉及从对流到层状的天气事件。

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