切變線降水系統微物理特征及隆水機制個例分析
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國家科研院所社會公益研究專項基金項目(2001DIB10084)資助


Analysis of MicroPhysical Structure Characteristics and Precipitation Mechanisms of a ShearLine Precipitation Case in Jilin Province
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    摘要:

    利用機載云粒子探測系統(PMS),對2004年7月1日影響吉林省的一次切變線降水過程進行了探測飛行,利用所獲取的宏微觀資料對此次降水過程的微物理結構、降水機制進行綜合分析。結果表明:此次切變線降水云系主要由高層云、雨層云、碎云構成,高層云和雨層云中間夾有1100 m左右的無云區;3類云中平均云滴濃度、平均云滴直徑各不相同;云水含量隨高度分布不均勻,云的不同部位云水含量起伏較大;冰晶濃度平均為17.3個/L;此次探測的降水云系符合Bergeron提出的催化云〖CD*2〗供水云相互作用導致降水的概念。根據云圖及其他探測資料綜合分析,冰晶主要產生于高層云上部或卷層云的冰晶播撒,供水云為高層云中下部和雨層云。

    Abstract:

    A composite sounding flight was made during a shearline precipitation process in Jilin Province on 1 July 2004. The microphysical structure, precipitation mechanisms of this precipitation process are analyzed by means of the airborne Particle Measuring System (PMS) data, and the microphysical structure characteristics of the shearline precipitation cloud system and the physical mechanisms of rainfall formation are analyzed compositely. The results show that this shearline rainfall clouds mainly consist of altostratus, nimbostratus, and fractus; the average cloud droplet concentration and average cloud droplet diameter are different in three kinds of clouds; the cloud water content is distributed unevenly with increasing height; and the different parts of the clouds have different cloud water contents. The precipitation cloud system measured by PMS conforms to the concept of Bergeron seederfeeder cloud mechanism. The comprehensive analysis of cloud pictures and other sounding data shows that ice crystals mainly appeared in the upper part of altostratus or resulted from the spreading of ice crystals in cirrostratus, and feeder clouds are the central and lower parts of altostratus and nimbostratus.

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劉健,齊彥斌,蔣彤,陳知新,米長樹,紀瑛英.切變線降水系統微物理特征及隆水機制個例分析[J].氣象科技,2008,36(4):396~399

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  • 收稿日期:2007-06-20
  • 定稿日期:2007-12-17
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