Guizhou Air Traffic Control Bureau of CAAC,Guiyang 550012,China[J]. Journal of Yunnan University: Natural Sciences Edition, 2012, 34(S1): 39-42.
Citation: Guizhou Air Traffic Control Bureau of CAAC,Guiyang 550012,China[J]. Journal of Yunnan University: Natural Sciences Edition, 2012, 34(S1): 39-42.

Guizhou Air Traffic Control Bureau of CAAC,Guiyang 550012,China

  • 摘要: :利用贵阳机场航空器报告、常规资料等对贵阳机场低空风切变的气候特征及其环流背景进行统计分析,同时对低空风切变发生前及发生时的风场特征进行分析,得到如下结论:贵阳机场低空风切变主要发生在冬末和春季,3月和8月出现次数较多;一天中,低空风切变主要发生在上午10时以后,午后发生低空风切变的频率较高;其发生的环流背景分为冷锋型、高压后部型和热低压型,主要发生在冷锋型环流背景下.从风场特征来看,地面南风和北风均会产生低空风切变,但北风条件下出现频率较高;低空风切变发生时边界层风均为南风,且风速较大.冷锋型低空风切变发生前地面风常伴随南风转北风的转风过程,但低空风切变发生在风向完全转成北风后.高压后部型和热低压型低空风切变发生前后地面风均为较大南风.

     

    Abstract: Based on the routine datas and the airplane reports of Guiyang airport,the climatic characters and circulation background of low-level windshear of Guiyang airport are analysed,at the same time the wind field characters of low-level windshear are analysed.The result shows that the low-level windshear of Guiyang airport mainly take place in later winter and spring,March and August appear more times.In a day the low-level windshear often take place after 10 oclock at AM,the higher frequency appear in the afternoon.The circulation background of windshear include the cold-front type,high pressure rear type and thermal low pressure type,and the cold-front type is the main circulation background.From the wind field characters,when the ground wind are the South wind and North wind,the low-level windshear will occur,but it appears higher frequency on the north wind conditions.When the low-level windshear take place,the boundary wind are all the South wind,accompany with high wind speed.Before the cold-front type low-level windshear occur,the ground wind turn the South wind to the North wind,but when the ground wind become the North wind,the low-level windshear will occur.When the low-level windshear of high pressure rear type and the thermal low pressure type take place,the ground wind are the South wind.

     

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