Hanson S G, Churnside J H, Wilson J J
Appl Opt. 1994 Sep 1;33(25):5859-68. doi: 10.1364/AO.33.005859.
Wind velocity across an optical path and refractive turbulence strength can be measured by observing a light source through the atmosphere with a receiver that contains two spatial filters. The frequency of the detected signal gives the transverse velocity of the turbulent structure, whereas signal intensity is proportional to refractive turbulence strength. The size of turbulent eddies that produce signals is determined by the optical setup. The position along the detector's field of view at which the measurement is made depends on the separation of the filters, and profiles can be made by varying the separation and using a telescope. The system requires longer integration times than one which uses a spatial filter at each end of the optical path, but it has the advantage of being able to use a natural source such as the Sun or a planet. An analysis of the system is presented along with numerical simulations and results from a short-range (several meters) laboratory experiment. The analysis assumes a single layer of refractive turbulence. Scales of the refractive turbulence in the inertial subrange from 5 to 20 cm will be of primary interest for this method.
通过一个包含两个空间滤波器的接收器在大气中观测光源,可以测量光路上的风速和折射湍流强度。检测信号的频率给出了湍流结构的横向速度,而信号强度与折射湍流强度成正比。产生信号的湍流涡旋大小由光学装置决定。沿探测器视场进行测量的位置取决于滤波器的间距,通过改变间距并使用望远镜可以绘制出剖面图。该系统比在光路两端各使用一个空间滤波器的系统需要更长的积分时间,但它具有能够使用自然光源(如太阳或行星)的优势。本文给出了该系统的分析,以及数值模拟和短程(几米)实验室实验的结果。该分析假设为单层折射湍流。对于这种方法,惯性子区内5至20厘米的折射湍流尺度将是主要关注对象。