Atmospheric turbulence measurements by angle of arrival fluctuations and intensity scintillations with large aperture

Y. Glick, R. Zaibel, G. Bar-Tal, Y. Bar-Sagi
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引用次数: 4

Abstract

Summary form only given. Atmospheric turbulence was measured using a one station scheme, over a flat beach parallel to the Mediterranean sea shore. A diffusive white target situated at a distance of 1500 m was illuminated with a 5 mJ Q-switched Nd:YAG laser beam at a rep-rate of 500 Hz. The laser spot on the target had a diameter of about 0.5 m and the height of the path was 1.2 m. The reflected beam was imaged near the laser by a Cassegrain lens system (f=1000 mm D=91 mm) onto a horizontal linear array detector with eight 50/spl times/250 /spl mu/m (width/spl times/height) elements. At the same time the system measures cross wind speeds, this is reported elsewhere. This scheme was used to measure the turbulence based on two separate principles. The first is based on the intensity scintillations measured on the detectors. The second principle is based on the angle of arrival (AOA) fluctuations of the beam, measured on the detector array as a linear displacement.
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用大孔径到达角波动和强度闪烁测量大气湍流
只提供摘要形式。在与地中海海岸平行的平坦海滩上,采用单站方案测量大气湍流。用5 mJ调q Nd:YAG激光束以500 Hz的重复频率照射1500 m处的漫射白色目标。目标上的激光光斑直径约0.5 m,路径高度为1.2 m。利用卡塞格伦透镜系统(f=1000 mm, D=91 mm)将反射光束在激光器附近成像到一个具有8个50/spl倍/250 /spl mu/m(宽/高)单元的水平线阵探测器上。与此同时,该系统测量横向风速,这在其他地方也有报道。该方案基于两个不同的原理用于测量湍流。第一种是基于探测器上测量到的闪烁强度。第二个原理是基于光束的到达角(AOA)波动,在探测器阵列上测量为线性位移。
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