J4 ›› 2009, Vol. 27 ›› Issue (3): 245-249.

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Diagnostic Analysis of a RegionalHeavy Dust Storm Caused by Cold Front in HexiCorridor

 CHENG  Feng1, LI Guang-Lin2, LIU  Gang1, ZHANG Pei-Yan1, YANG Xiao-Jun1, SONG Xiu-Ling1   

  1. 1.Lanzhou CentralMeteorologicalObservatory, Lanzhou730020,China;2.DunhuangMeteorologicalBureau ofGansu Province, Dunhuang736200, China
  • Received:2009-07-06 Revised:2009-08-11 Online:2010-09-30 Published:2009-09-30

河西走廊一次区域性大风强沙尘暴天气诊断

程 鹏李光林刘 抗张培燕杨晓军宋秀玲   

  1. 1.兰州中心气象台,甘肃 兰州 730020;2.甘肃敦煌市气象局,甘肃 敦煌 736200
  • 作者简介:程鹏(1981-),男,甘肃临泽人,工程师,主要从事中短期天气预报及研究.E-mail:tfreefish@163.com
  • 基金资助:

    兰州中心气象台创新基金项目(200901c)资助

Abstract:

Based on the basic observationaldata and automaticweather station data, a regionalheavy dust storm occurred onApril29,2009 inHexiCorridorwas analyzed from the causes of the synopticmeteorology, physics quantity fields and so on.The results show that itwas a duststorm thatcaused by the gale behind the cold front, and ithappened in the zone ofstrong pressure gradient. Groundmeteorological elements had a strong response to the outbreak of the dust storm, which can be used as a reference for forecast of dust storms. Therewas an obvious upwardmotion in the outbreak area ofduststorm with the lower level convergence and the high-leveldivergence. The frontogenesis function and helicity indicated the area of dust storm verywel.l

Key words: dust storm, physical quantity, cold front, diagnostic analysis

摘要:

应用常规和自动加密站观测资料,对2009年4月29日发生在河西走廊的一次区域性强沙尘暴天气过程,从天气学成因、物理量要素等方面进行了诊断分析。结果表明:这是一次冷锋后大风引发的沙尘暴;沙尘暴发生在强气压梯度区;地面气象要素对冷锋过境及沙尘暴爆发有强烈反应,可以在沙尘暴预报中作为一个参考依据;沙尘暴爆发区低层辐合,高层辐散,有明显的上升运动;锋生函数和螺旋度对沙尘暴爆发区有较好的指示意义。

关键词: 沙尘暴, 物理量, 冷锋, 诊断分析

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