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Jianhua Sun and Sixiong Zhao

impacts in the continuous rain–snow process? To answer this question, infrared data for cloud-top temperatures from the Chinese Fēngyún ( FY-2C ) satellite have been used to analyze the activities of mesoscale systems propagating eastward from the Tibetan Plateau toward eastern China. Data with a horizontal resolution of 0.05° were available every hour and covered the whole of East Asia (20°–70°N, 70°–160°E). The temporal evolution of the hourly average cloud-top temperature and 6-h precipitation

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