大气与环境光学学报

• 大气光学 • 上一篇    下一篇

近地面层湍流大气中光传输到达角起伏实验研究

梅杰1,袁仁民1,王显1,吴徐平2   

  1. 1中国科学技术大学地球和空间科学学院,安徽合肥 230026;
    2安徽建筑大学数理学院,安徽合肥230601
  • 出版日期:2019-09-28 发布日期:2019-09-26

Experimental Investigation of Angle-of-Arrival Fluctuation of Light Propagating in Near Surface Layer Turbulent Atmosphere

MEI Jie1, YUAN Renmin1, WANG Xian1, WU Xuping2   

  • Published:2019-09-28 Online:2019-09-26

摘要: 为研究不同气象条件下近地面层湍流大气对光传输到达角起伏的影响,在校园内一块较平坦草地上开展了光传输实验。
采用半导体激光器作为光源,传输60 m至接收端,使用焦距为1300 mm的望远镜接收后由CCD相机采集光点灰度图片。
根据灰度图片上光点位置计算传输路径上的大气湍流折射结构常数$C_n^2$以及垂直、水平两个方向到达角
(Angle of arrival, AoA)起伏方差的比值。同时测量了传输路径附近的温度、风速等气象数据,计算稳定
度参数Richardson数。结果表明, Richardson数大于临界值0.25时,垂直、水平到达角起伏方差比值均
大于1.0; Richardson 数小于0.25时,垂直、水平到达角起伏方差比值在1.0左右起伏。由此可以看到,
稳定层结条件下,湍流表现为各向异性特征;不稳定层结条件下,湍流表现为各向同性特征。

关键词: 近地面层, 湍流大气, 到达角起伏, 大气稳定度, 各向同性, 各向异性

Abstract: In order to study the influence of turbulent atmosphere in the surface layer on the fluctuation of the
angle of arrival(AoA) of light propagation under different meteorological conditions, an optical
transmission experiment was carried out on a flat grass in the campus. A semiconductor laser
was used as the light source, and the light signal was received by a telescope with  focal length
of 1300 mm after transmitting 60 m to the receiving location, then a CCD camera was used to
shoot grayscale pictures of the light spot. Ratio of the AoA fluctuations in  vertical and
horizontal directions was calculated based on the position of the light spot on the photo.
The atmospheric turbulent refractive structure constant on the transmission path was also
calculated. Simultaneously, meteorological parameters near the transmission path, such as
temperature and wind speed, were measured so as to calculate the Richardson number as a
stability parameter. The results showed that when the Richardson number is greater
than 0.25, the ratio of vertical and horizontal AoA variances is greater
than 1.0; when the Richardson number is less than 0.25, the ratio of vertical and horizontal
AoA variances fluctuates around 1.0. Thus, it can be seen that atmospheric
turbulence is anisotropic under stable stratification conditions and isotropic under
unstable stratification conditions.

Key words: surface layer, turbulent atmosphere, AoA fluctuation, atmospheric stability, isotropy, anisotropy

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