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首页> 外文期刊>Natural hazards and earth system sciences >Daytime identification of summer hailstorm cells from MSG data
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Daytime identification of summer hailstorm cells from MSG data

机译:从味精数据中白天识别夏季雹暴细胞

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Identifying deep convection is of paramount importance, as it may be associated with extreme weather phenomena that have significant impact on the environment, property and populations. A new method, the hail detection tool (HDT), is described for identifying hail-bearing storms using multispectral Meteosat Second Generation (MSG) data. HDT was conceived as a two-phase method, in which the first step is the convective mask (CM) algorithm devised for detection of deep convection, and the second a hail mask algorithm (HM) for the identification of hail-bearing clouds among cumulonimbus systems detected by CM. Both CM and HM are based on logistic regression models trained with multispectral MSG data sets comprised of summer convective events in the middle Ebro Valley (Spain) between 2006 and 2010, and detected by the RGB (red-green-blue) visualization technique (CM) or C-band weather radar system of the University of León. By means of the logistic regression approach, the probability of identifying a cumulonimbus event with CM or a hail event with HM are computed by exploiting a proper selection of MSG wavelengths or their combination. A number of cloud physical properties (liquid water path, optical thickness and effective cloud drop radius) were used to physically interpret results of statistical models from a meteorological perspective, using a method based on these "ingredients". Finally, the HDT was applied to a new validation sample consisting of events during summer 2011. The overall probability of detection was 76.9% and the false alarm ratio 16.7 %.
机译:识别深度对流至关重要,因为它可能与对环境,财产和人口产生重大影响的极端天气现象有关。描述了一种新方法,即冰雹检测工具(HDT),用于使用多光谱气象卫星第二代(MSG)数据来识别冰雹风暴。 HDT被认为是一种两阶段方法,其中第一步是设计用于检测深对流的对流遮罩(CM)算法,第二步是用于识别积雨云中带冰雹云的冰雹遮罩算法(HM) CM检测到的系统。 CM和HM均基于logistic回归模型,该模型使用多光谱MSG数据集训练而成,该数据集由2006年至2010年之间的西班牙埃布罗河谷中部夏季对流事件组成,并通过RGB(红绿蓝)可视化技术(CM )或莱昂大学的C波段天气雷达系统。借助逻辑回归方法,通过适当选择味精波长或其组合,可以计算出使用CM识别积雨或使用冰雹识别冰雹事件的概率。使用多种云物理特性(液态水路径,光学厚度和有效云滴半径),使用基于这些“成分”的方法,从气象角度对统计模型的结果进行物理解释。最后,将HDT应用于一个新的验证样本,该样本由2011年夏季的事件组成。总的检测概率为76.9%,错误警报率为16.7%。

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