Dubinsky R H, Carswell A I, Pal S R
York University, Downsview, Ontario, M3J 1P3.
Appl Opt. 1985 Jun 1;24(11):1614-22. doi: 10.1364/ao.24.001614.
The extinction and backscattering of 514-nm laser radiation in polydisperse water droplet clouds have been studied in the laboratory. Three cloud size distributions with modal diameters of 0.02, 5, and 12 microm have been investigated. The relationships between the cloud optical parameters (attenuation coefficient sigma and volume backscattering coefficient beta(pi)) and the cloud water content C have been measured for each size distribution. It has been found that a linear relationship exists between sigma and C and between beta(pi) and C for cloud water content values up to 3 g/m3. The linear relationships obtained, however, have slopes which depend on the droplet size distribution. For a given water content both sigma and beta(pi) increase as the modal diameter decreases. The measured data are compared with existing theoretical analyses and discussed in terms of their application to lidar measurements of atmospheric clouds. It is concluded that the empirical information obtained can serve as a basis for quantitative lidar measurements.
在实验室中研究了514纳米激光辐射在多分散水滴云中的消光和后向散射。研究了模态直径分别为0.02、5和12微米的三种云滴尺寸分布。对每种尺寸分布测量了云光学参数(衰减系数σ和体积后向散射系数β(π))与云水含量C之间的关系。已发现,对于云水含量值高达3克/立方米的情况,σ与C以及β(π)与C之间存在线性关系。然而,所得到的线性关系的斜率取决于液滴尺寸分布。对于给定的含水量,σ和β(π)都随着模态直径的减小而增加。将测量数据与现有的理论分析进行了比较,并就其在大气云激光雷达测量中的应用进行了讨论。得出的结论是,所获得的经验信息可作为定量激光雷达测量的基础。