Markov chain formalism for generalized radiative transfer in a plane-parallel medium, accounting for polarization

被引:17
作者
Xu, Feng [1 ]
Davis, Anthony B. [1 ]
Diner, David J. [1 ]
机构
[1] CALTECH, Jet Prop Lab, Pasadena, CA 91125 USA
关键词
Generalized radiative transfer; Polarized radiative transfer; Markov chain formalism; Stochastic optical media; Angular reciprocity; Clouds; BOLTZMANN-EQUATION; OPTICAL MEDIA; SCATTERING; CLOUDS; RECIPROCITY; PARAMETERIZATION; PROPAGATION; EXTINCTION; DERIVATION; LIGHT;
D O I
10.1016/j.jqsrt.2016.06.004
中图分类号
O43 [光学];
学科分类号
070207 ; 0803 ;
摘要
A Markov chain formalism is developed for computing the transport of polarized radiation according to Generalized Radiative Transfer (GRT) theory, which was developed recently to account for unresolved random fluctuations of scattering particle density and can also be applied to unresolved spectral variability of gaseous absorption as an improvement over the standard correlated-k method. Using Gamma distribution to describe the probability density function of the extinction or absorption coefficient, a shape parameter a that quantifies the variability is introduced, defined as the mean extinction or absorption coefficient squared divided by its variance. It controls the decay rate of a power-law transmission that replaces the usual exponential Beer-Lambert-Bouguer law. Exponential transmission, hence classic RT, is recovered when a ->infinity. The new approach is verified to high accuracy against numerical benchmark results obtained with a custom Monte Carlo method. For a < infinity, angular reciprocity is violated to a degree that increases with the spatial variability, as observed for finite portions of real-world cloudy scenes. While the degree of linear polarization in liquid water cloudbows, supernumerary bows, and glories is affected by spatial heterogeneity, the positions in scattering angle of these features are relatively unchanged. As a result, a single-scattering model based on the assumption of subpixel homogeneity can still be used to derive droplet size distributions from polarimetric measurements of extended stratocumulus clouds. (C) 2016 Elsevier Ltd. All rights reserved.
引用
收藏
页码:14 / 26
页数:13
相关论文
共 57 条
[1]   Accuracy assessments of cloud droplet size retrievals from polarized reflectance measurements by the research scanning polarimeter [J].
Alexandrov, Mikhail D. ;
Cairns, Brian ;
Emde, Claudia ;
Ackerman, Andrew S. ;
van Diedenhoven, Bastiaan .
REMOTE SENSING OF ENVIRONMENT, 2012, 125 :92-111
[2]  
[Anonymous], COMPUTATIONAL METHOD
[3]  
[Anonymous], 1973, IZV ACAD SCI USSR AT
[4]  
Barker HW, 1996, J ATMOS SCI, V53, P2304, DOI 10.1175/1520-0469(1996)053<2304:APFCGA>2.0.CO
[5]  
2
[6]   Cloud droplet effective radius from spaceborne polarization measurements [J].
Breon, FM ;
Goloub, P .
GEOPHYSICAL RESEARCH LETTERS, 1998, 25 (11) :1879-1882
[7]   Bounded cascade clouds: albedo and effective thickness [J].
Cahalan, R. F. .
NONLINEAR PROCESSES IN GEOPHYSICS, 1994, 1 (2-3) :156-167
[8]  
CAHALAN RF, 1994, J ATMOS SCI, V51, P3776, DOI 10.1175/1520-0469(1994)051<3776:IPAMCE>2.0.CO
[9]  
2
[10]  
Cairns B, 2000, J ATMOS SCI, V57, P700, DOI 10.1175/1520-0469(2000)057<0700:AWICAI>2.0.CO