Xu Feng, Davis Anthony B, West Robert A, Esposito Larry W
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109, USA.
Opt Express. 2011 Jan 17;19(2):946-67. doi: 10.1364/OE.19.000946.
Building on the Markov chain formalism for scalar (intensity only) radiative transfer, this paper formulates the solution to polarized diffuse reflection from and transmission through a vertically inhomogeneous atmosphere. For verification, numerical results are compared to those obtained by the Monte Carlo method, showing deviations less than 1% when 90 streams are used to compute the radiation from two types of atmospheres, pure Rayleigh and Rayleigh plus aerosol, when they are divided into sublayers of optical thicknesses of less than 0.03.
基于标量（仅强度）辐射传输的马尔可夫链形式，本文给出了垂直非均匀大气中偏振漫反射和透射的解决方案。为了进行验证，将数值结果与通过蒙特卡罗方法获得的结果进行比较，结果表明，当使用90个流来计算两种类型大气（纯瑞利大气和瑞利加气溶胶大气）的辐射时，若将它们划分为光学厚度小于0.03的子层，则偏差小于1%。
