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Characteristics of Raindrop Size Distribution in Seoul, South Korea According to Rain and Weather Types

机译:雨水和天气类型韩国首尔雨滴大小分布的特点

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The raindrop size distribution (RSD) is useful in understanding various precipitation-related processes. Here, we analyze disdrometer data collected in Seoul, South Korea from May 2018 to July 2019 to characterize the RSD according to rain and weather types. Rain types are categorized into stratiform, mixed, and convective rain, and weather types into the Changma front (type CF) and low-pressure system (type L). The slope parameter ? decreases and the intercept parameterN(0)fluctuates with rain rate. Among the rain types, the RSD of stratiform (convective) rain shows the steepest (mildest) slope and the smallest (largest) mean diameter. The logarithm of generalized intercept parameter log(10)N(w)and ? for stratiform rain have considerably dispersed distributions, which may be attributed to the diversity within the stratiform rain type in Seoul. Mixed-type rain has a larger mean value of log(10)N(w)compared to stratiform and convective rain. Regarding the weather types, the RSD of type CF exhibits a milder slope, a larger mass-weighted mean diameter, and a larger radar reflectivity than type L. These differences between the weather types can be explained by the larger convective proportion in type CF (33%) compared to type L (9%). Possible causes for the differences between the RSD characteristics of the two weather types are examined using reanalysis and satellite data. Type CF has a larger convective available potential energy, a higher cloud top, and more active ice microphysical processes than type L, which can lead to different RSD characteristics.
机译:雨滴尺寸分布(RSD)可用于理解各种降水相关过程。在这里,我们分析了从2018年5月到2019年5月在韩国首尔收集的Discrometer数据,以便根据雨水和天气类型来表征RSD。雨型分为层状,混合和对流雨,以及天气类型进入Changma Front(CF)和低压系统(L型)。斜率参数?减少,拦截参数(0)波动与雨率。在雨季中,层状(对流)雨的RSD显示陡峭(最温和的)斜坡和最小(最大)平均直径。广义拦截参数日志(10)n(w)的对数和?对于层状雨,具有大幅分散的分布,这可能归因于首尔的层状雨型内的多样性。与层状和对流雨量相比,混合型雨具有更大的对数(10)N(w)的平均值。关于天气类型,CF型RSD表现出更升高的斜面,较大的质量加权平均直径和比L型更大的雷达反射率。天气类型之间的这些差异可以通过CF型较大的对流比例来解释( 33%)与L型(9%)相比。使用重新分析和卫星数据检查两个天气类型的RSD特性之间的可能原因。 CF型具有更大的对流可用潜在能量,更高的云顶,更具有比L型更高的活性冰微微物理过程,这可能导致不同的RSD特性。

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