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Oceanographic lidar attenuation coefficients and signal fluctuations measured from a ship in the Southern California Bight

机译:从南加州海岸线的一艘船测得的海洋激光雷达衰减系数和信号波动

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摘要

We measured the attenuation coefficient of the National Oceanic and Atmospheric Administration lidar from a ship in the Southern California Bight in September 1995. The region from approximately 5 to 30 m in depth was covered. The laser was linearly polarized, and the receiver was operated with the same polarization and the orthogonal polarization. The measured values were between 0.08 and 0.12 m~(-1) and were highly correlated with in situ measurements of the beam attenuation coefficient. Fluctuations of the lidar signal were found to be induced primarily by surface waves whose wavelengths are approximately three times the lidar spot size at the surface.
机译:我们从1995年9月在南加利福尼亚湾的一艘船上测量了美国国家海洋和大气管理局激光雷达的衰减系数。覆盖了大约5至30 m的区域。激光是线性偏振的,并且接收机在相同的偏振和正交偏振下工作。测量值在0.08至0.12 m〜(-1)之间,与光束衰减系数的原位测量高度相关。发现激光雷达信号的波动主要是由表面波引起的,该表面波的波长大约是表面激光雷达光斑尺寸的三倍。

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