Lidar signal model from remote aerosol formations in double scattering approach

V. Bryukhanova, I. V. Samokhvalov
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引用次数: 1

Abstract

Lidars are applied in many geophysics, meteorology and atmospheric optics research. However, the problem of lidar data interpretation is not solved yet. It is necessary to take into consideration the multiple scattering (MS) when laser radiation propagates in optically dense aerosol formations. The paper discusses the problem of numerical simulations of the lidar returns that account for contributions from single and double scattering from dense aerosol formations. We have analyzed the lidar equation that was obtained in Samokhvalov (1979) for an inhomogeneous atmosphere with account of single and double scattering. It is shown in the paper that double scattering "forward-backward" and "backward-backward" photon trajectories equally contribute to the backscattering intensity. This significantly simplifies the lidar equation, if the sounding pulse penetrates the cloud to the depth that is small compared with the diameter scattering volume at the cloud top.
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双重散射方法下远程气溶胶形成的激光雷达信号模型
激光雷达在许多地球物理、气象和大气光学研究中得到了应用。然而,激光雷达数据解释的问题尚未得到解决。激光辐射在光学密集气溶胶地层中传播时,有必要考虑多重散射。本文讨论了考虑稠密气溶胶形成的单散射和双散射对激光雷达回波贡献的数值模拟问题。我们分析了Samokhvalov(1979)在考虑单散射和双散射的非均匀大气下得到的激光雷达方程。结果表明,双散射“前向-后向”和“后向-后向”光子轨迹对后向散射强度的贡献是相等的。如果探测脉冲穿透云层的深度与云顶的直径散射体积相比较小,这将大大简化激光雷达方程。
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