Lidar Sounding of Atmospheric Temperature and Density Variability with a 2.5 Meter Telescope

P. Dao, J. Meriwether, R. McNutt, W. Klemetti, J. Servaites, W. Moskowitz, G. Davidson
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Abstract

In May 1989 the Geophysics Laboratory (GL) mobile lidar facility was moved to Wright Patterson AFB and combined with the WRDC 2.5 meter telescope. The objective was to merge Air Force resources in a campaign to obtain atmospheric density data in the altitude range from 20 to 100 km. GL has been performing high altitude density measurements since 1984. For density measurements, the lidar system typically consists of a pulsed laser and a medium quality optical telescope to collect backscattered radiation. For UV and visible lasers, the optical signal is detected with photomultiplier tubes and the electrical signal is recorded either with a transient recorder or a multichannel scaler. The latter is used with photon counting and considerably increases the detection sensitivity.
用2.5米望远镜激光雷达探测大气温度和密度变化
1989年5月,地球物理实验室(GL)移动激光雷达设备被转移到赖特帕特森空军基地,并与WRDC 2.5米望远镜结合。目标是合并空军资源,以获得海拔20至100公里范围内的大气密度数据。自1984年以来,GL一直在进行高海拔密度测量。对于密度测量,激光雷达系统通常由一个脉冲激光器和一个中等质量的光学望远镜组成,用于收集后向散射辐射。对于紫外和可见激光器,光信号用光电倍增管检测,电信号用瞬态记录器或多通道标度器记录。后者与光子计数一起使用,大大提高了探测灵敏度。
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