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Numerical simulation study on the severe convective weather over chengdu by three-dimension convective cloud model

机译:三维对流云模型对成都地区强对流天气的数值模拟研究

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In order to learn more about the severe convective weather occurred over Chengdu on Sep. 23rd of 2008, it is simulated by utilizing three-dimension convective cloud model. The results show as follows. The model can simulate macroscopic characteristics of severe convective weather in major developing sections, as well as microscopic ones of evolution of hydrometeor particles in cloud rather well. The strong updraft and sufficient vapor are essential conditions for the developing convective cells. Accumulating and melting of solid hydrometeor particles are contributed to the precipitation distinctly.
机译:为了进一步了解2008年9月23日在成都发生的强对流天气,利用三维对流云模型进行了模拟。结果如下。该模型可以很好地模拟主要发展地区的强对流天气的宏观特征,以及云中水凝物颗粒演变的微观特征。强烈的上升气流和足够的蒸汽是发展对流细胞的必要条件。固体水凝物颗粒的积累和熔化明显地促进了沉淀。

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