烏魯木齊市邊界層日變化特征
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中國沙漠氣象科學研究基金(Sqj2015009)、中央級公益性科研院所基本科研業務費專項資金(IDM201505)資助


Diurnal Variation of Atmospheric Boundary Layer in Urumqi
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    摘要:

    利用烏魯木齊市晴天CFL03型風廓線雷達觀測資料,分析了邊界層日變化特征。得出結論如下:邊界層結構季節變化明顯。冬、春季300~600 m以下風速較小,小于3 m/s,且愈近地面風速愈?。灰陨巷L速大、風向恒定,基本為東南大風。夏季和秋季風速比冬季和春季小,流場特征較復雜,水平風速和風向變化較活躍,存在明顯的風切變。折射率結構常數春、秋和冬季比夏季分別小1個、3個和1~3個量級;夏季最大,集中在10-16~10-13m-2/3之間。春、夏和秋季晴天湍流動能耗散率量級分別在10-6~10-2m2〖DK〗·s-3、10-4~10-3m2〖DK〗·s-3、10-6~10-3m2〖DK〗·s-3之間;白天比夜間約大1個量級。晴天折射率結構常數和湍流動能耗散率日變化特征與風場日變化特征有較好地對應關系,即湍流發展旺盛的區域與風速較大的區域相一致。風廓線雷達資料反演的湍流動能耗散率對春季和夏季邊界層結構日變化演變特征的監測較好。夏季夜間穩定邊界層約400~500 m,殘余層可達到約1800 m,對流邊界層可發展到約2500 m,混合層約2200 m,夾卷層約300~400 m。

    Abstract:

    The clear day observation data of the CFL03 wind profiler radar (WPR) collected in Urumqi are used to analyze the characteristics of the diurnal variation of the atmospheric boundary layerThe results show that the seasonal variation of the boundary layer is obviousBelow the 300-600 m height, the wind speed is weak (<3 m/s), and the nearer the surface the smaller the wind speed is While wind speed is larger, the wind direction is constant in southeast above 300 to 600 mThe wind speeds in summer and autumn are smaller than those in winter and springThe characteristics of the flow field in summer and autumn are more complex, in which the horizontal wind speed and direction are more volatile, and there is obvious wind shearThe magnitude of structural parameter of turbulence reflectivity in spring (autumn or winter) is one magnitude (three magnitudes or 1 to 3 magnitudes) less than that in summer In summer, the structural parameter of turbulence reflectivity is maximum, which is 10-16 to 10-13m-2/3Under the condition of clear sky, the dissipation rate of turbulent kinetic energy is 10-6 to 10-2, 10-4 to 10-3 and 10-6 to 10-3m2〖DK〗·s-3, respectively, in spring, summer, and autumnThe magnitude of dissipation rate of turbulent kinetic energy in daytime is one magnitude more than that at nightThe diurnal variation of structural parameter of turbulence reflectivity and dissipation rate of turbulent kinetic energy is correlated well to wind field in clear daysThat is, the region of strong turbulence development is consistent with the larger wind velocityThe diurnal boundarylayer feature in spring and summer can be better monitored by the dissipation rate of turbulent kinetic energy using a new product of WPR In summer, under the condition of clear sky, the height of the stable boundary layer, residual layer, convective boundary layer, mixed layer, and entrainment layer are 400 to 500, 1800, 2500, 2200 and 300 to 400 m, respectivelyThe diurnal variation of the boundary layer height is positively related to surface temperature

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金莉莉,李振杰,何清,繆啟龍,買買提艾力·買買提依明.烏魯木齊市邊界層日變化特征[J].氣象科技,2017,45(4):686~697

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  • 收稿日期:2016-04-02
  • 定稿日期:2017-04-10
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  • 在線發布日期: 2017-08-30
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