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Using Satellite Data to Analyze the Initiation and Evolution of Deep Convective Clouds

机译:利用卫星数据分析深对流云的形成和演化

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In this study, two deep convective cloud cases were analyzed in detail to study their initiation and evolution. In both cases, all deep convective clouds were posi-tioned at the rear of the cold front cloud bands and propagated backward. Satellite data showed that prior to initiation of the deep convective clouds, thermodynamic and moist conditions were favorable for their formation. In the morning, a deep convective cloud at the rear of cold front cloud band propagated backward, the outflow boundary of which created favorable conditions for initiation. An additional deep convective cloud cluster moved in from the west and interacted with the outflow boundary to develop a mesoscale convective system (MCS) with large, ellipse-shaped deep convective clouds that brought strong rainfall. The initiation and evolution of these clouds are shown clearly in satellite data and provide significant information for nowcasting and short-term forecasting.
机译:在这项研究中,详细分析了两个深对流云实例,以研究它们的形成和演化。在这两种情况下,所有深对流云都位于冷锋云带的后部,并向后传播。卫星数据显示,在深对流云开始之前,热力学和潮湿条件有利于它们的形成。早晨,冷锋云带后方的深对流云向后传播,其出流边界为起爆创造了有利条件。另外一个深对流云团从西部进入并与流出边界相互作用,形成了中尺度对流系统(MCS),该系统具有大的椭圆形深对流云,带来了强降雨。这些云的启动和演化在卫星数据中清晰显示,并为临近预报和短期预报提供了重要信息。

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