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First results on a process-oriented rain area classification technique using Meteosat Second Generation SEVIRI nighttime data

机译:使用Meteosat第二代SEVIRI夜间数据的面向过程的雨区分类技术的初步结果

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A new technique for process-oriented rain area classification using Meteosat SecondGeneration SEVIRI nighttime data is introduced. It is based on a combination of theAdvective Convective Technique (ACT) which focuses on precipitation areas connected toconvective processes and the Rain Area Delineation Scheme during Nighttime (RADS-N) a newtechnique for the improved detection of stratiform precipitation areas (e.g. in connection with mid-latitude frontal systems).The ACT which uses positive brightness temperature differences between the water vapour(WV) and the infrared (IR) channels (ΔTWV-IR) for the detection ofconvective clouds and connected precipitating clouds has been transferred from Meteosat FirstGeneration (MFG) Metesoat Visible and Infra-Red Imager radiometer (MVIRI) to MeteosatSecond Generation (MSG) Spinning Enhanced Visible and InfraRed Imager (SEVIRI).RADS-N is based on the new conceptual model that precipitating cloud areas are characterised by alarge cloud water path (cwp) and the presence of ice particles in the upper part of the cloud. Thetechnique considers information about both parameters inherent in the channel differencesΔT3.9-10.8, ΔT3.9-7.3, ΔT8.7-10.8, andΔT10.8-12.1, to detect potentially precipitating cloud areas. All fourchannel differences are used to gain implicit knowledge about the cwp. ΔT8.7-10.8 and ΔT10.8-12.1 are additionally considered to gain information about the cloud phase.First results of a comparison study between the classified rain areas and corresponding ground basedradar data for precipitation events in connection with a cold front occlusion show encouragingperformance of the new proposed process-oriented rain area classification scheme.
机译:介绍了一种使用Meteosat SecondGeneration SEVIRI夜间数据进行面向过程的雨区分类的新技术。它基于对流技术(ACT)(专注于与对流过程相关的降水区域)和夜间雨区划定方案(RADS-N)的组合,该技术是一种改进的层状降水区域检测新技术(例如,与中层降水有关) -纬度额叶系统)。ACT使用水蒸气(WV)和红外(IR)通道之间的正亮度温差(ΔT WV-IR )来检测对流云和相连的降水云已从气象卫星第一代(MFG)气象卫星可见光和红外成像仪(MVIRI)转移到气象卫星第二代(MSG)旋转增强型可见光和红外成像仪(SEVIRI)。RADS-N基于沉淀云区域的新概念模型其特点是云水路径较大( cwp )且云层上部存在冰粒。该技术考虑有关信道差异内在的两个参数的信息:ΔT 3.9-10.8 ,ΔT 3.9-7.3 ,ΔT 8.7-10.8 和ΔT 10.8-12.1 ,以检测可能有降水的云区域。所有四个通道的差异都用于获取有关 cwp 的隐式知识。另外还考虑了ΔT 8.7-10.8 和ΔT 10.8-12.1 来获取有关云相的信息。分类雨区与相应的地面雷达数据的比较研究的第一项结果是对于与冷锋闭塞有关的降水事件,显示了新的以过程为导向的雨区分类方案的令人鼓舞的性能。

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