[1]李宜爽,刘蕾,李家文.2014年5月10-11日柳州强降水过程诊断分析[J].气象研究与应用,2015,36(03):34-38,44.
 Li Yi-shuang,Liu Lei,Li Jiawen.An Analysis on the Heavy Precipitation on May 10 to 11th, 2014 in Liuzhou[J].Journal of Meteorological Research and Application,2015,36(03):34-38,44.
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2014年5月10-11日柳州强降水过程诊断分析()
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气象研究与应用[ISSN:1673-8411/CN:45-1356/P]

卷:
第36卷
期数:
2015年03期
页码:
34-38,44
栏目:
天气气候
出版日期:
2015-12-22

文章信息/Info

Title:
An Analysis on the Heavy Precipitation on May 10 to 11th, 2014 in Liuzhou
作者:
李宜爽 刘蕾 李家文
柳州市气象局, 广西柳州 545001
Author(s):
Li Yi-shuang Liu Lei Li Jiawen
Liuzhou Municipal Meteorological Service, Liuzhou Guangxi 545001
关键词:
锋面暴雨低涡切变线地面辅合线急流
Keywords:
frontal rainstormlow vortex shear linesurface convergence linejet stream
分类号:
P458.1
摘要:
利用Micaps资料、地面加密自动观测资料、NCEP/NCAR的1°×1°每6h再分析资料,对2014年5月10-11日发生在柳州的一次强降水过程进行了诊断分析。结果表明:500hPa南支槽、850hPa低涡切变线及低空急流、地面冷锋为此次降雨过程提供了有利的天气尺度背景场;近地层冷空气入侵是本次过程的触发机制,高层强辐散以及低层辐合的有利配置为此次强降水的产生提供了较好的动力条件;强盛的西南急流提供了较好的水汽及能量条件;水汽通量散度、涡度中心值的强弱变化及移动均与强降水中心有着很好的对应关系。
Abstract:
In this paper, the analysis of a heavy precipitation on May 10 to 11th, 2014 in Liuzhou is performed by using Micaps data, surface intensive observations data, and NCEP/NCAR 1.0x1.0 degree reanalysis (every 6 hours) data. The results show that 500hPa south branch groove, 850hPa low vortex shear line, and surface cold front provided a favorable synoptic scale background field for the heavy precipitation; the invasion of the cold air of surface layer is the triggering mechanism of the precipitation, and the assemblage of upper-level divergence and lower-level convergence created a suitable dynamic environment for its occurrence; the strong southwest jet stream provided a preferable vapor and energy condition for the heavy rainfall; the vapor flux divergence and the change of the intensity of the center of vorticity as well as its movement correspond well with the heavy precipitation center.

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备注/Memo

备注/Memo:
收稿日期:2015-5-17。
作者简介:李宜爽(1991-),女,助工,从事预报服务工作。
更新日期/Last Update: 1900-01-01