J4 ›› 2009, Vol. 27 ›› Issue (3): 239-244.

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Weather System Analysis of a Strong Dust Storm in Summ er of Hexi Corridor

 WANG Fu-Cun1,2, ZHANG De-Yu1, HAO Zhi-Yi3, FU Wei-Zhi1   

  1. (1.ZhangyeMeteorologicalBureau ofGansu Province; Zhangye734000,China;2.KeyLaboratory ofArid Climatic Change andReducingDisaster ofGansu Province, Institute ofAridMeteorology,CMA, Lanzhou730020, China;3. Gansu ProvincialMeteorologicalBureau, Lanzhou730020, China)
  • Received:2009-04-20 Revised:2009-07-27 Online:2010-09-30 Published:2009-09-30

河西走廊一次夏季强沙尘暴的影响系统分析

王伏村1,2张德玉郝志毅付有智   

  1. (1.甘肃省张掖市气象局,甘肃 张掖 734000; 2.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,甘肃 兰州 730020; 3.甘肃省气象局业务处,甘肃 兰州 730020)
  • 作者简介:王伏村(1969-),甘肃临泽县人,高级工程师,主要从事天气预报及多普勒雷达应用研究.E-mai:l wangfucun3@ yahoo. com. cn
  • 基金资助:

    中国气象局兰州干旱气象研究所干旱气象科学研究基金项目(IAM200713)资助
      

Abstract:

By using the reanalysis data ofNCEP( 1°×1°) and the radiosonde and surface observations aswell as the Doppler radar products, the features of a strong dust storm occurred on 13 June 2008 in theHexiCorridor are analyzed. Results show that the upper cold airmoved fast and overlapped on the surface cyclone resulted inmeso-scale convection system developing fast. The dry-warmlid at the level of500-540 hPawas advantageous to the instability energy accumulation at low level and itwas importantomen for the strong convection weather.The convection system took place firstat the low layerbefore the sandstorm outbreak, then quickly developed tomiddle layer. The sandstorm occurred in theweak echo areawhichwas in frontof the strong echo and in the adversewind region of radial velocity

Key words: strong dust storm, convection instability, Dopplerweather radar, adversewind region

摘要:

:使用NCEP再分析资料以及高空、地面观测资料和张掖CINRAD-CC天气雷达观测数据对2008年6月13日发生在河西走廊中部的一次强沙尘暴天气进行了连续监测和分析。结果表明:高空冷空气快速东移叠加到地面热低压之上形成对流不稳定,使得中尺度对流系统快速发展;T-LnP图上500~540 hPa干暖盖有利于对流层低层不稳定能量的存储和积累,干暖盖是强对流天气发生的重要征兆;沙尘暴发生前对流系统先从低层发展,然后迅速向中层发展;沙尘暴发生后中低层雷达回波减弱;中层回波开始增强,并向下发展,降水增大后,沙尘暴减弱消失;沙尘暴发生在紧邻强回波前面弱回波区域内;地面观测沙尘暴发生、发展、消亡时间与逆风区生消演变密切相关,沙尘天气发生在逆风区范围内,强沙尘暴天气发生在逆风区外层风速大值区的强辐合上升气流中。

关键词: 强沙尘暴, 对流不稳定, 多普勒天气雷达, 逆风区

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