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首页> 外文期刊>Applied optics >Aerosol and cloud backscatter at 1.06, 1.54, and 0.53 mu m by airborne hard-target-calibrated Nd:YAG/methane Raman lidar
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Aerosol and cloud backscatter at 1.06, 1.54, and 0.53 mu m by airborne hard-target-calibrated Nd:YAG/methane Raman lidar

机译:机载硬目标校准的Nd:YAG /甲烷拉曼激光雷达在1.06、1.54和0.53μm处的气溶胶和云向后散射

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A lidar instrument was developed to make simultaneous measurements at three distinct wavelengths in the visible and near infrared at 0.532, 1.064, and 1.54 mu m with high cross-sectional calibration accuracy. Aerosol and cloud backscatter cross sections were acquired during November and December 1989 and May and June 1990 by the NASA DC-8 aircraft as part of the Global Backscatter Experiment. The instrument, methodology, and measurement results are described. A Nd:YAG laser produced 1.064- and 0.532-mu m energy. The 1.54-mu m transmitted pulse was generated by Raman-shifted downconversion of the 1.064-mu m pulse through a Raman cell pressured with methane gas. The lidar could be pointed in the nadir or zenith direction from the aircraft. A hard-target-based calibration procedure was used to obtain the ratio of the system calibration between the three wavelengths, and the absolute calibration was referenced to the 0.532-mu m lidar molecular backscatter cross section for the dearest scattering regions. From the relative wavelength calibration, the aerosol backscatter cross sections at the longer wavelengths are resolved for values as small as 1% of the molecular cross section. Backscatter measurement accuracies are better than 10(-9) (m sr)(-1) at 1.064 and 1.54 mu m. Results from the Pacific Ocean region of the multiwavelength backscatter dependence are presented. Results show extensive structure and variation for the aerosol cross sections.; The range of observed aerosol cross section is over 4 orders of magnitude, from less than 10(-9) (m sr)(-1) to greater than 10(-5) (m sr)(-1). (C) 1997 Optical Society of America.
机译:开发了一种激光雷达仪器,可同时在可见光和近红外中的三个不同波长下以0.532、1.064和1.54μm的波长进行同时测量,并具有很高的截面校准精度。作为全球反向散射实验的一部分,NASA DC-8飞机在1989年11月和12月以及1990年5月和1990年6月获得了气溶胶和云反向散射截面。描述了仪器,方法和测量结果。一盏Nd:YAG激光产生1.064和0.532微米的能量。 1.54微米的透射脉冲是通过将1.064微米的脉冲进行拉曼位移降频转换而产生的,该脉冲是通过用甲烷气体加压的拉曼电解池产生的。激光雷达可以从飞机指向天底或天顶方向。使用基于硬目标的校准程序来获得三个波长之间系统校准的比率,并且绝对校准是针对最散射区域的0.532微米激光雷达分子背向散射截面进行的。通过相对波长校准,可以解析较长波长的气溶胶反向散射截面,其值仅为分子截面的1%。背向散射测量精度在1.064和1.54μm时优于10(-9)(m sr)(-1)。给出了太平洋地区多波长反向散射依赖性的结果。结果表明,气溶胶横截面具有广泛的结构和变化。观测到的气溶胶横截面范围超过4个数量级,从小于10(-9)(m sr)(-1)到大于10(-5)(m sr)(-1)。 (C)1997年美国眼镜学会。

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