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Characteristics of raindrop spectra as normalized gamma distribution from a Joss-Waldvogel disdrometer

机译:Joss-Waldvogel测干仪测得的雨滴光谱作为归一化伽玛分布的特征

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The raindrop spectra observed in a precipitation system is a complex phenomenon that can help to explain the underlying physical processes of rainfall. This paper explores the characteristics of raindrop spectra in terms of drop size distributions (DSD) using seven years of Joss-Waldvogel disdrometer data within the mid-latitude UK region climatology. A total of 162,415 one-minute "filtered" raindrop spectra obtained from the disdrometer are fitted into a normalized gamma DSD model describing DSDs by the concentration parameter (N_w), the drop diameter (D_m and D_o), and the shape parameter (μ). The results show that the rain rates retrieved from the normalized gamma DSD model are in good agreement with the disdrometer measured rain rates, implying the appropriateness of the raindrop spectra as normalized gamma distributions. The DSD characteristics are studied in different seasonal ("cold" and "warm"), atmospheric ("dry" and "wet") as well as rain type ("stratiform" and "convective") contexts in a long-term perspective. It has been revealed that the normalized gamma DSD parameters are very sensitive to the rain intensities. The mass weighted mean drop diameter D_m clearly increases exponentially with respect to the rain intensities. Variation of the DSDs in different contexts is also exposed reflecting seasonal, atmospheric and rain type consequence on raindrop spectra. Particularly, the scatterplot between the concentration parameter log_(10)N_w and the median drop diameter D_o exhibits clear separation index between stratiform and convective DSDs. There is a large difference in averaged mass weighted mean drop diameters among stratiform and convective segments (stratiform =0.988 mm versus convective =1.99 mm). The DSD inconsistency in different contexts have been further examined in terms of the Z-R relationships (Z=aR~b) variability. Additionally, 10 selected events taken place during the study period are also investigated, in which each of the events has shown unique DSD characteristics.
机译:在降水系统中观察到的雨滴光谱是一个复杂的现象,可以帮助解释潜在的降雨物理过程。本文使用英国中纬度地区气候学中七年的Joss-Waldvogel测雨仪数据,以液滴尺寸分布(DSD)的方式探索了雨滴光谱的特征。从测风仪获得的总共162,415个一分钟的“过滤”雨滴光谱拟合到归一化伽玛DSD模型中,该模型通过浓度参数(N_w),液滴直径(D_m和D_o)和形状参数(μ)描述了DSD。 。结果表明,从归一化的伽玛DSD模型中获得的降雨率与测得的雨量仪吻合得很好,这表明雨滴谱作为归一化的伽玛分布是适当的。从长远的角度来看,在不同季节(“冷”和“暖”),大气(“干”和“湿”)以及降雨类型(“层状”和“对流”)环境中研究了DSD特性。已经发现,归一化的伽马DSD参数对雨强度非常敏感。质量加权平均液滴直径D_m相对于雨强度明显呈指数增长。 DSD在不同环境下的变化也被暴露出来,这反映了雨滴谱图上季节性,大气和降雨类型的后果。特别地,浓度参数log_(10)N_w和中值液滴直径D_o之间的散点图在层状和对流DSD之间显示出清晰的分离指数。在层状和对流段之间,平均质量加权平均液滴直径存在较大差异(层状 = 0.988 mm与对流 = 1.99 mm)。根据Z-R关系(Z = aR〜b)的可变性,进一步研究了DSD在不同情况下的不一致。此外,还研究了在研究期间发生的10个选定事件,其中每个事件都显示出独特的DSD特性。

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