暴雨,环流形势,物理量场,诊断分析,对流云团,武威,甘肃," /> 暴雨,环流形势,物理量场,诊断分析,对流云团,武威,甘肃,"/> 2012年7月29日武威市大到暴雨天气过程分析
干旱区研究

干旱区研究 ›› 2013, Vol. 30 ›› Issue (5): 789-795.

• 气候与气候变化 • 上一篇    下一篇

2012年7月29日武威市大到暴雨天气过程分析

杨晓玲1,2, 丁文魁2, 钱沛泉3, 殷玉春2, 姚玉璧4   

  1. 1. 中国气象局兰州干旱气象研究所，甘肃省干旱气候变化与减灾重点实验室，中国气象局干旱气候变化与
    减灾重点开放实验室，甘肃 兰州 730020； 2. 甘肃省武威市气象局，甘肃武威 733099；
    3. 中盛国际保险经纪有限责任公司甘肃分公司，甘肃 兰州 730020； 4.甘肃省定西市气象局，甘肃 定西 743000
  • 收稿日期:2012-08-22 修回日期:2012-12-11 出版日期:2013-09-15 发布日期:2013-09-22
  • 作者简介:杨晓玲（1971-），女，学士，高级工程师，主要从事天气预报的研究工作.E-mail: wwqxj6150343@163.com
  • 基金资助:

    国家重点基础研究发展计划项目（973计划）（ 2012CB955903，2010CB428401）；石羊河流域干旱灾害风险评估及防御对策研究（IAM201205）共同资助

A Rainstorm Weather in Wuwei City on July 29, 2012  

 YANG  Xiao-Ling1,2,, DING  Wen-Kui2, QIAN  Pei-Quan3, YIN  Yu-Chun2, YAO  Yu-Bi4   

  1. 1. Lanzhou Institute of Arid Meteorology & Key Laboratory of Arid Climate Change and Disaster Reduction, 
    China Meteorological Administration, Lanzhou 730020, China;
    2. Wuwei Meteorological Bureau, Wuwei 733000, Gansu Province, China;
    3. Gansu Branch, Zhongsheng International Insurance Brokers Co., Ltd., Lanzhou 730020, China;
    4. Dingxi Meteorological Bureau, Dingxi 743000, Gansu Province, China
  • Received:2012-08-22 Revised:2012-12-11 Online:2013-09-15 Published:2013-09-22

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摘要： 利用常规天气图、FY-2D卫星云图、单站地面资料、物理量场等资料，对2012年7月29日下午到夜间武威市的对流性强降雨天气成因进行了系统分析。结果表明：该过程是在一定的大尺度环流背景下高低层天气系统共同作用发生的，地面气象要素的剧烈变化是强降雨天气能量的释放过程；大的湿度条件和水汽在本地辐合，为大到暴雨提供了丰沛的水汽；高层辐散、低层辐合以及强烈的上升气流是大到暴雨发生的动力条件；强烈的不稳定能量和不稳定层结是对流增强、雨强增大的必要条件；对流云团的发展和加强是降雨强度较大的直接原因。

关键词: font-family: 宋体, mso-bidi-font-family: 宋体, mso-font-kerning: 1.0pt, mso-ansi-language: EN-US, mso-fareast-language: ZH-CN, 暴雨')">mso-bidi-language: AR-SA">暴雨, 环流形势, 物理量场, 诊断分析, 对流云团, 武威, 甘肃

Abstract: The formation causes of convection rainstorm weather in Wuwei City from afternoon to night on July 29, 2012 were systematically analyzed using the conventional weather charts, FY-2D satellite images and meteorological data observed by a meteorological station, and physical quantity field data. The result showed that the rainstorm occurred under the interaction of multiple factors and a certain largescale circulation background. Dramatic change of surface meteorological factors was an energy release process of strong convection weather. Local high humidity and water vapor convergence provided an abundant water vapor source for the rainstorm. Highlevel divergence, lowlevel convergence and strong ascending motion were the dynamic conditions of the rainstorm. Strong unstable energy and unstable stratification were the necessary conditions of enhancing the convection and increasing the rainstorm intensity. Development and strengthening of convective cloud clusters were the direct causes of the rainstorm intensity.

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