[1]陆秋霖,陈明璐,胡勇林.玉林市两次冬季暴雨过程分析[J].气象研究与应用,2016,37(02):55-58,80.
 LU Qiu-lin,Chen Ming-lu,Hu Yong-lin.Analysis of two winter rainstorm processes in Yulin[J].Journal of Meteorological Research and Application,2016,37(02):55-58,80.
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玉林市两次冬季暴雨过程分析()
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气象研究与应用[ISSN:1673-8411/CN:45-1356/P]

卷:
第37卷
期数:
2016年02期
页码:
55-58,80
栏目:
天气气候
出版日期:
2016-12-21

文章信息/Info

Title:
Analysis of two winter rainstorm processes in Yulin
作者:
陆秋霖 陈明璐 胡勇林
玉林市气象局, 广西玉林 537000
Author(s):
LU Qiu-lin Chen Ming-lu Hu Yong-lin
Yulin Municipal meteorological Service, Yulin Guangxi, 537000
关键词:
玉林冬季暴雨水汽K指数
Keywords:
Yulinwinterrainstormwater vaporK index
分类号:
P458.1+21.1
摘要:
利用常规观测资料、自动站雨量资料以及6h一次的NECP FNL分析资料(水平分辨率为1°×1°)等,对2016年1月27日20时~28日20时和2013年12月13日20时~16日20时玉林市两次冬季暴雨过程进行诊断分析,结果表明:两次冬季暴雨过程均主要受南支槽东移和切变线的影响,西南气流为这两次过程提供了大量的水汽。低层辐合高层辐散促进上升运动发展,触发了大气层结的不稳定度,而K指数对暴雨的预报有一定的指示作用。
Abstract:
Based on the conventional observation data, the automatic stations rainfall data and NCEP FNL (Final) (1°×1°) every six hours, two winter rainstorm processes in Yulin of January 27th -28th in 2016 and December 13th to 16th in 2013 were analyzed. The results show that:the two winter rainstorm processes are mainly influenced by eastward southern trough and shear line, and the southwest wind provides large amount of water vapor. Low-level convergence and high-level divergence promoted the development of upward movement, and triggered the instability of the atmosphere. So the K index has certain indicative function in forecasting rainstorm.

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备注/Memo

备注/Memo:
收稿日期:2016-01-15。
作者简介:陆秋霖(1992-),女,广西北流人肋工,从事天气预报工作。
更新日期/Last Update: 1900-01-01