干旱气象 ›› 2015, Vol. 33 ›› Issue (1): 110-118.DOI: 10.11755/j.issn.1006-7639(2015)-01-0110

• 论文 • 上一篇    下一篇

河北盛夏2次大暴雨过程对比分析

王福侠1, 2, 张 南1赵玉广1段 浩1李宗涛1   

  1. 1. 河北省气象台, 河北 石家庄 050021;
    2. 河北省生态环境重点实验室, 河北 石家庄 050021
  • 出版日期:2015-02-28 发布日期:2015-02-28
  • 作者简介:王福侠(1971-),女,河北乐亭人,高级工程师,主要从事中短期短时预报技术和雷达资料应用研究.Email:hbqxtwfx@sina.com

Contrast Analysis of Two Torrential Rainfall Processes in Mid -summer of Hebei Province

WANG Fuxia 1, 2ZHANG Nan1ZHAO Yuguang1DUAN Hao1LI Zongtao1     

  1. 1. Hebei Meteorological Observatory,Shijiazhuang 050021,China;
    2. Key Laboratory of Ecological Environment of Hebei Province,Shijiazhuang 050021, China
  • Online:2015-02-28 Published:2015-02-28
  • Supported by:

    中国气象局预报员专项“7.01大暴雨落区与中尺度系统的关系研究”(GMAYBY2014-06)和社会公益行业(气象)专项“华北、东北暴雨发生发展特点及预报技术研究”(GYHY200906011)共同资助

摘要:

利用常规天气资料、NCEP再分析资料、地面区域站和多普勒天气雷达资料对比分析了2012年7月21~22日罕见特大暴雨和2011年7月24日大暴雨的天气形势、水汽条件、动力条件以及中尺度影响系统。分析发现:这2次暴雨过程都是低槽冷锋类暴雨过程,中尺度影响系统也基本相同,降水效率相当,但降水极值和暴雨范围相差很大;充足的水汽输送强的动力条件和高降水效率是2012年7月21~22日极端降水的原因之一,河北中部长达6 h列车效应是这次极端降水的关键原因;低层θse锋区和切变线南侧急流的有利配置是造成河北中部列车效应的关键原因,是低槽冷锋类暴雨强降水持续时间和能否出现极端降水的预报着眼点之一;锋面前侧的地面中尺度辐合线是主要中尺度影响系统,强降水落区沿地面中尺度辐合线分布,根据地面中尺度辐合线的演变预报暴雨的落区比依据低层低涡东南象限预报暴雨落区更精确。

 

关键词:
特大暴雨,
中尺度, 锋生, 对比, 预报着眼点

Abstract:

There was a rare rainstorm weather process in the North of China on July 21,2012,which led to the most severe flooding disasters.The weather system of the process was the cold front with the upper trough,but such a system would not lead to more than 200 mm rainfall in 24 hours according to the statistical results of the last decade ( 2000 - 2011) . After the precipitation in Beijing ,the torrential rain occurred in the middle of Hebei Province ( Langfang and the northeast of Baoding) ,where heavy rainfall occurred relatively less in the past. Thus,some reasons of the torrential rainfall in Hebei and the forecasting focus were analyzed in the article,based on the conventional observation data,reanalysis data from NCEP at 1° × 1° spatial resolution,regional automatic meteorological observation data and Doppler weather radar data. The comparative study of weather patterns,physics conditions and meso - and micro- scale systems were carried out with another rainstorm process which occurred on the 24th July 2011. The results show that there were great differences between two weather processes in extreme value of precipitation and rainfall area,although their precipitation efficiency and meso - and micro - scale systems which directly resulted  in two precipitation processes were similar under the same synoptic scale circulation situation ( low - cold front type) . The extreme precipitation in 7. 21 process had a closely relation to strong moisture transport,intense dynamic condition and high precipitation efficiency,but the train effect for 6 hours was the leading cause of the heavy rainfall. The configuration of low frontal zone of se and low - level jet on the south of shear line led to the train effect in the middle of Hebei Province,which was concluded as a forecast point of the kind heavy rain events. And,the ground mesoscale convergence line ahead of the cold front was a key point for accurately forecasting heavy rainfall area,which was better than based on the southeast quadrant of the lower vortex,because strong precipitation occurred along with lines.

Key words: torrential rainfall, mesoscale, frontogenesis, contrast analysis, forecast index

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