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Precipitation Type Classification of Micro Rain Radar Data Using an Improved Doppler Spectral Processing Methodology

机译:利用改进的多普勒光谱处理方法,微雨雷达数据的降水型分类

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摘要

This paper describes a methodology for processing spectral raw data from Micro Rain Radar (MRR), a K-band vertically pointing Doppler radar designed to observe precipitation profiles. The objective is to provide a set of radar integral parameters and derived variables, including a precipitation type classification. The methodology first includes an improved noise level determination, peak signal detection and Doppler dealiasing, allowing us to consider the upward movements of precipitation particles. A second step computes for each of the height bin radar moments, such as equivalent reflectivity (Ze), average Doppler vertical speed (W), spectral width (σ), the skewness and kurtosis. A third step performs a precipitation type classification for each bin height, considering snow, drizzle, rain, hail, and mixed (rain and snow or graupel). For liquid precipitation types, additional variables are computed, such as liquid water content (LWC), rain rate (RR), or gamma distribution parameters, such as the liquid water content normalized intercept (Nw) or the mean mass-weighted raindrop diameter (Dm) to classify stratiform or convective rainfall regimes. The methodology is applied to data recorded at the Eastern Pyrenees mountains (NE Spain), first with a detailed case study where results are compared with different instruments and, finally, with a 32-day analysis where the hydrometeor classification is compared with co-located Parsivel disdrometer precipitation-type present weather observations. The hydrometeor classification is evaluated with contingency table scores, including Probability of Detection (POD), False Alarm Rate (FAR), and Odds Ratio Skill Score (ORSS). The results indicate a very good capacity of Method3 to distinguish rainfall and snow (PODs equal or greater than 0.97), satisfactory results for mixed and drizzle (PODs of 0.79 and 0.69) and acceptable for a reduced number of hail cases (0.55), with relatively low rate of false alarms and good skill compared to random chance in all cases (FAR 0.70). The methodology is available as a Python language program called RaProM at the public github repository.
机译:本文描述了一种用于从微雨雷达(MRR),一个K波段垂直指向多普勒雷达旨在观察沉淀轮廓处理的频谱的原始数据的方法。其目的是提供一组雷达积分参数与导出变量,包括一个沉淀类型分类。该方法首先包括一个改进的噪声电平判定,峰值信号的检测和多普勒去混叠,使我们能够考虑沉淀颗粒的向上运动。对于每个高度仓雷达时刻,比如等效反射率(ZE),平均多普勒垂直速度(W),光谱宽度(σ)的第二步骤单位计算,偏度和峰度。第三步骤执行用于每个箱高度的析出型的分类,考虑雪,毛毛雨,雨,冰雹,并混合(雨,雪或霰)。对于液体沉淀类型,附加变量被计算,例如液体水含量(LWC),雨率(RR),或者伽马分布参数,例如液体水含量归截距(NW),或平均质量加权的雨滴直径( DM)分类层状或对流性降雨的制度。该方法被应用到记录在东比利牛斯山(NE西班牙)的数据,首先用一个详细的案例研究,其中的结果与不同的仪器,最后相比,具有32天的分析,其中所述水凝分类与协同定位的相比Parsivel disdrometer沉淀型目前的气象观测。该水汽凝结分类与列联表的分数,包括检测(POD)的概率,虚警率(FAR),和赔率比率技能分数(ORSS)进行评估。结果表明非常良好的容量方法3来区分降雨和雪(POD中等于或大于0.97),用于混合和毛毛雨和可接受的(0.79和0.69的POD)为冰雹案件数量减少(0.55)令人满意的结果,与假警报和良好的技能相对较低的速度相比,在所有情况下(FAR 0.70)随机的机会。该方法可作为在公共GitHub的仓库称为RaProM一个Python语言程序。

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