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中文摘要: 通过对发生于长江中游地区两个中-β尺度对流云团引起的特大暴雨过程的分析,探讨中-β尺度对流云团产生强降水的条件,研究其变化规律,从而为暴雨预报提供一定的物理依据。
中文关键词: 中-β尺度，云团，对流回波，暴雨
Abstract:An analysis of the heavy rain over the Changjiang River basin during 21—22 July 1998 was made.It is mainly to inquire into the problems with the genesis and development of the meso-β scale convective systems which caused severe convective weather.The results show that the environmental conditions,especially the interaction between the upper-level and lower-level jets for the formation of deep convection is very important.
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基金项目:“我国重大天气灾害形成机理与预测理论研究”项目资助
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引用文本：
薛秋芳,梁海河,张沛源,2001.中-β尺度对流云团造成特大暴雨过程的分析[J].气象,27(2):39-43.
,2001.An Analysis of Meso-β-scale Convective Systems in a Heavy Rain Process[J].Meteor Mon,27(2):39-43.
薛秋芳,梁海河,张沛源,2001.中-β尺度对流云团造成特大暴雨过程的分析[J].气象,27(2):39-43.
,2001.An Analysis of Meso-β-scale Convective Systems in a Heavy Rain Process[J].Meteor Mon,27(2):39-43.