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甘肃河西走廊春季强沙尘暴与低空急流

Relationship of Low Level Jet and Severe Dust Storm over Hexi Corridor of Gansu in Spring

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【作者】 汤绪俞亚勋李耀辉张存杰

【Author】 TANG Xu~(1, 2),YU Ya-xun~2,LI Yao-hui~2,ZHANG Cun-jie~2 (1. Department of Atmospheric Sciences, Institute of Physics, Peking University, Beijing 100871, China; e, Lanzhou Institute of Arid Meteorology, China Meteorological Administration, Lanzhou 730020, China)

【机构】 北京大学物理学院大气科学系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 北京 100871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甘肃兰州 730020甘肃兰州 730020

【摘要】 使用NCEP/NCAR全球再分析网格点资料(2.5°×2.5°纬度/经度)和我国区域性沙尘暴过程历史资料,分析了春季大气环流特征及低空急流与甘肃河西走廊春季强沙尘暴的关系。结果表明,在东亚中纬度高空维持纬向强急流锋区的情况下,极易造成甘肃河西走廊春季强沙尘暴的低空急流产生。揭示了沙尘暴形成的大尺度环流动力影响因子的事实,指出可将产生这种低空急流特征的西风带大型环流的调整过程,作为甘肃河西走廊春季强沙尘暴天气的预警信号,而低空急流的位置及强度又可作为沙尘暴强度及沙尘暴发生和影响区的预报指标。

【Abstract】 Using the regional dust storm records in China and NCEP/NCAR reanalysis data (2.5°×2.5°lat/lon) in recent 48 years (1955\2002), the relations between the characteristics of atmospheric circulation and low-level jet with severe dust storm over North China in spring were analyzed. The results showed that the low-level jet of severe dust storm over Hexi Corridor of Gansu in spring was easily formed under the case of maintaining zonal jet front zone over the high-lever of the middle latitude of East Asia. The facts that the relevant dynamic and thermodynamic factors of large-scale circulation formed dust storms in Hexi Corridor of Gansu in spring was revealed, it indected that take the low-level jet with adjustment processes for large-scale circulations in westerly belt not only as the early warning signal of severe dust storm weather over Hexi Corridor of Gansu in spring, but also the location and indensity of low-level jet as the predictive index of dust storms intensity, occurrance and effect areas.

【基金】 科技部社会公益项目"西北干旱区沙尘暴预警、服务系统研究"项目(2000DIA10031)资助
  • 【文献出处】 高原气象 ,Plateau Meteorology , 编辑部邮箱 ,2004年06期
  • 【分类号】P445.4
  • 【被引频次】44
  • 【下载频次】199
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