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对流风暴
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对流风暴
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对流动力学
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convective storm
对流风暴
通常是指由一个或多个对流单体组成的强烈发展的中小尺度天气系统。其水平尺度可从1~2千米的积云塔,到几十千米甚至几百千米的积雨云系,内部存在强烈的垂直运动并足以激发深对流的产生。
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