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投稿时间:2009-12-10 修订日期:2010-03-24
投稿时间:2009-12-10 修订日期:2010-03-24
中文摘要: 利用观测资料和ECMWF分析资料,对广西2006—2008年发生的雷暴大风强天气45次个例进行统计分析,并应用天气学方法进行影响模型分析,从雷暴大风发生的条件入手,探讨了一些稳定度指数和动力参数的物理意义,及雷暴大风发生区域的环境场特征,统计归纳出了:(1)造成广西雷暴大风强天气过程可分为高原深槽型、台风低槽型、副高西部型和华北低槽型等四种天气模型;(2)雷暴大风多发生在午后,峰值出现在16时左右;7月和8月出现的最多;(3)局地雷暴大风的出现与地形作用有密切关系;(4)雷暴大风产生前,四种天气影响型广西大部地区大气层结均有不稳定能量聚集,低层有强的水汽辐合,相对湿度大;高原深槽、华北低槽和副高西部影响型强的垂直上升运动和正涡度中心位于广西北部,台风低槽影响型则位于广西东南部;(5)出现雷暴大风的区域大气层结不稳定性更显著,低层水汽辐合和中低层气旋性辐合也偏强。
中文关键词: 雷暴大风, 环流特征, 物理量, 诊断分析
Abstract:Based on the observation data and ECMWF analysis data, the 45 samples of thunderstorm gales occurring during 2006 to 2008 in Guangxi have been statistically analyzed and the influence model is analyzed by using the synoptic meteorology method. The physical significance of stability index and dynamic parameters, and the environment characteristics of the thunderstorm gale occurring area have been discussed in terms of the thunderstorm gale occurrence conditions. The results show: (1) There are 4 weather model types that can cause thunderstorm gales in Guangxi, including the type of plateau trough, the type of typhoon trough, the type of western subtropical high, and the type of North China trough; (2) Thunderstorm gale occurs mostly in July and August especially in the afternoon, whose peak appears at about 16 p.m. (3) The terrain is important for local thunderstorm gale occurring; (4) Before the thunderstorm gale occurring, the unstable energy in the atmospheric stratification congregates in most areas of Guangxi, the moisture convergence in lower layers and the relative humidity are powerful. The vertical ascending movement and the positive vorticity center of the plateau trough type, the western subtropical high type and the North China trough type are located in northern Guangxi, while the type of typhoon trough is located in southeastern Guangxi; (5) The atmospheric stratification is more unstable in the thunderstorm gale occurring, moisture convergence in lower layers and the cyclonic convergence in the middle and lower layers are also stronger.
文章编号: 中图分类号: 文献标志码:
基金项目:中国气象科学研究院项目“基于GRAPES的广西城市(群)强对流预报系统”资助
作者 | 单位 |
钟利华 | 广西气象科技服务中心, 南宁 530022 |
曾鹏 | 广西气象科技服务中心, 南宁 530022 |
李勇 | 广西气象科技服务中心, 南宁 530022 |
熊文兵 | 广西气象科技服务中心, 南宁 530022 |
胡宗煜 | 广西气象科技服务中心, 南宁 530022 |
引用文本:
钟利华,曾鹏,李勇,熊文兵,胡宗煜,2011.广西雷暴大风环流特征和物理量诊断分析[J].气象,37(1):59-65.
ZHONG Lihua,ZENG Peng,LI Yong,XIONG Wenbing,HU Zongyu,2011.Diagnostic Analysis of the Circulation and Physical Quantities of Thunderstorm Gales in Guangxi[J].Meteor Mon,37(1):59-65.
钟利华,曾鹏,李勇,熊文兵,胡宗煜,2011.广西雷暴大风环流特征和物理量诊断分析[J].气象,37(1):59-65.
ZHONG Lihua,ZENG Peng,LI Yong,XIONG Wenbing,HU Zongyu,2011.Diagnostic Analysis of the Circulation and Physical Quantities of Thunderstorm Gales in Guangxi[J].Meteor Mon,37(1):59-65.