2010年湖南汛期13次暴雨过程的力子天气学分析 |
| |
引用本文: | 姜海泉,张剑明.2010年湖南汛期13次暴雨过程的力子天气学分析[J].安徽农业科学,2011,39(32):19863-19866. |
| |
作者姓名: | 姜海泉 张剑明 |
| |
作者单位: | 湖南省株洲市气象局,湖南株洲,412003 |
| |
摘 要: | 采用力子天气学方法,通过对2010年4月以来出现在湖南的13次区域性暴雨天气过程进行合成分析。结果表明,2010年湖南汛期的13次暴雨均与自组织的辐合水汽流密切相关,暴雨是自组织辐合水汽流爆发后所产生的必然结果;自组织辐合水汽流的孕育区对应未来12~36 h出现暴雨的区域,自组织辐合水汽流孕育区一旦消失,则未来12~36 h不会有区域性暴雨出现;自组织辐合水汽流孕育区产生在大尺度南北力子偶的交汇域。南北力子偶是否存在可以作为汛期区域性暴雨的短期预报模式。
|
关 键 词: | 汛期暴雨 自组织辐合水汽流 力子天气学 南北力子偶 |
Analysis on Lizi Synoptic Meteorology of 13 Rainstorm Processes during the Flood Season of Hunan Province in 2010 |
| |
Institution: | JIANG Hai-quan et al(Zhuzhou Meteorological Bureau,Zhuzhou,Hunan 412003) |
| |
Abstract: | By lizi synoptic method,we analyzed the synthesis of 13 regional rainstorm weather processes occurring since April 2010 in Hunan.Results indicated that,all rainstorm was closely related to the self-organization convergence airflow,storm was the inevitable result of the self-organization convergence airflow;the initiation zone attributing to self-organization of convergent airflow corresponded to rainstorm area at next 12-36 hours;Once the self-organization of convergent airflow disappeared,there was no regional rainstorm at next 12-36 hours;the self-organization of convergent airflow in the breeding areas generated in the large-scale north and south of lizi intersection domain,therefore a new model of rainstorm forecast were formed. |
| |
Keywords: | Rainstorm during flood season Self-organization convergent airflow Lizi synoptic meteorology Lizi between North and South |
本文献已被 CNKI 维普 万方数据 等数据库收录! |
|