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气象:2006,32(7):102-109
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河西走廊盛夏一次强沙尘暴天气综合分析
(兰州中心气象台, 730020)
Integrated Analysis of a Severe Sand-dust Storm in Hexi Corridor in Summer
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投稿时间:2006-01-10    修订日期:2006-03-29
中文摘要: 利用常规气象观测资料和NCEP/NCAR月平均再分析资料,对2003年7月20日甘肃河西走廊一次历史上少见的区域性夏季沙尘暴天气进行了分析。研究发现高空小槽、切变线、热低压是引发夏季沙尘暴的主要天气系统。夏季沙尘暴发生过程中,各测站出现了气压跃升、风速猛增、气温下降、湿度增加等现象,但变化幅度小于春季。夏季沙尘暴云图特征表现为中小尺度云团,TBB≤-35℃的云团在一定程度上能够反映沙尘暴天气的变化。诊断分析表明,沙尘暴爆发前散度场呈低层辐合高层辐散状态,沙尘暴发生在最大垂直速度出现以后,同时水平螺旋度对夏季沙尘暴预报有较好的指示意义,螺旋度正值越大,沙尘暴越强。
Abstract:Using the observational and NCEP/NCAR reanalysis data, the characteristics of an unusual severe summer sand-dust storm in Hexi corridor is analyzed. The results show that upper trough and shear line and thermal depression are main synoptic systems introducing summer sand-dust storm. The value of air pressure, wind speed and relative humidity increased, and the value of air temperature descended when the summer sand-dust storm occured, but the changing extents were less than that of meteorological elements in spring sand-dust storm. The summer sand-dust storm is as characteristics of middle-small scale cloud cluster on cloud image, the cloud cluster of TBB≤-35℃ can show the change of sandstorm in summer. The diagnostic analysis shows that there is convergence in low level and divergence in upper level, sandstorm happened after the appearance of max vertical velocity, and at the same time, the helicity in eve of sand-dust storm eruption has good indication in the forecasting of sand-dust storm. When the helicity is large, the sand-dust storm is severe.
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基金项目:国家自然科学基金“新一代天气雷达测量沙尘暴的能力和方法研究”(40475011),甘肃省气象局“夏季沙尘暴预报方法研究”(200602)共同资助
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引用文本:
王锡稳,刘治国,黄玉霞,张铁军,程鹏,2006.河西走廊盛夏一次强沙尘暴天气综合分析[J].气象,32(7):102-109.
,2006.Integrated Analysis of a Severe Sand-dust Storm in Hexi Corridor in Summer[J].Meteor Mon,32(7):102-109.