新疆百里風區風廓線觀測分析
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鐵道部科技研究開發計劃項目(2008X012B),公益性行業(氣象)科研專項(GYHY201006012)、新疆氣象局業務新技術項目(YX200912)、新疆維吾爾自治區科技攻關項目(200833119)、中央級科研院所基本科研業務費專項(IDM200809)共同資助


Observational Study of Wind Profiles in Gale Area in Xinjiang
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    摘要:

    利用2009年3月25日至4月8日在新疆百里風區十三間房氣象站觀測取得的風廓線資料,分析了該地區低空風場的平均日變化、逐日變化以及強風天氣條件下大氣風場特征。研究表明:①十三間房地區觀測期間緯向風主要盛行西風氣流,經向風以北風為主,在大風天氣條件下經向北風氣流明顯大于同時間緯向西風氣流。②受七角井山口狹管效應的影響,該地區1500 m高度以下水平風速總體大于其上風速。③日、夜平均廓線分析表明,夜間風速大于白天,但二者隨高度的變化趨勢基本相同,1500 m以下,水平風速隨高度的升高呈減小趨勢,1500 m以上,隨高度升高呈增大趨勢。④Airda3000Q型邊界層風廓線雷達可獲得時間和空間分辨率較高的風場資料,通過分析其探測到的水平風廓線資料,可清晰地監測大風天氣的發生和變化過程。

    Abstract:

    To study the atmospheric wind field characteristics in the 100km Gale Area in Xinjiang, the Institute of Urumqi Desert Meteorology of the China Meteorological Administration carried out an observation experiment from 25 March to 8 April 2009 at Shisanjianfang Station, which is within the 100km Gale Area in Xinjiang. The diurnal and daytoday variations of the lowerlevel wind fields are analyzed by using the wind profile data from the Airda3000Q windprofiler radar system. The results show:(1) in this area, west and north winds prevailed, and longitudedirection winds were evidently greater than latitudedirection winds on the same time; (2) the horizontal wind speeds below 1500 meters were in general obviously greater that those above 1500 meters, influenced by the funneling effect of the Qijiaojing pass; (3) the analysis of the average profiles in day and night time shows that the nighttime wind speed was greater than that of the whole day, but the change trends with height were basically same for both, with the wind speed being decreasing with the increasing height below 1500 meters and increasing above 1500 meters; (4) the high temporalspatial resolution data of wind profiles were obtained by means of the Airda3000Q boundary layer wind profiler radar, which can be used to monitor the occurrence and change processes of gale weather.

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王敏仲,何清,魏文壽,趙勇,張廣興.新疆百里風區風廓線觀測分析[J].氣象科技,2010,38(5):640~644

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  • 收稿日期:2009-06-16
  • 定稿日期:2010-06-23
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