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河西走廊一次强沙尘暴天气的螺旋度诊断

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应用NCEP再分析资料计算了螺旋度,通过总螺旋度、螺旋度的水平和垂直分布特征对河西走廊一次区域性强沙尘暴天气进行了诊断分析.结果表明:沙尘区位于总螺旋度负值区或零线附近;沙尘暴爆发区水平螺旋度高层300 hPa为负螺旋度控制,低层700 hPa为正螺旋度控制;在沙尘暴发生时,高层负螺旋度中心有一个明显增大的过程,沙尘暴爆发区对应高空低层螺旋度强梯度区内;沙尘暴爆发区的垂直螺旋度分布特征是上负下正;螺旋度对沙尘暴爆发区有较好的指示意义.
Diagnostic Analysis of the Helicity During a Heavy Dust Storm Weather Process in Hexi Corridor
Based on the reanalysis data of NCEP, a regional storng dust storm in Hexi corridor was analyzed from the horizontal and vertical distribution characteristics of the total helicity and helicity. The results showed that the dust storm occurred in the intensive isoline or the zeroline of the negative helicity area. There was the negative helicity at 300 hPa and the positive helicity at 700 hPa over dust-storm area. The negative center of the helicity was growing obviously with the outbreak of the duststorm. The vertical helicity distribution characteristic was negative at the high level and positive at the low level. The helicily indicated the outbreak area of dust storm very well.

dust stormtotal helicityhelicityHexi Corridor

程鹏、王宝鉴、孔祥伟、张静、伏晓红、宋秀玲

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甘肃省庆阳市气象局,甘肃西峰 745000

兰州中心气象台,甘肃兰州 730020

沙尘暴 总螺旋度 螺旋度 河西走廊

中国气象局预报员专项

CMAYBY2012-064

2013

干旱气象
中国气象局兰州干旱气象研究所 中国气象学会干旱气象学委员会

干旱气象

CSTPCD
影响因子:1.9
ISSN:1006-7639
年,卷(期):2013.31(1)
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