Mi. Mishchenko et al., ERRORS INDUCED BY THE NEGLECT OF POLARIZATION IN RADIANCE CALCULATIONS FOR RAYLEIGH-SCATTERING ATMOSPHERES, Journal of quantitative spectroscopy & radiative transfer, 51(3), 1994, pp. 491-510
Although neglecting polarization and replacing the rigorous vector rad
iative transfer equation by its approximate scalar counterpart has no
physical background, it is a widely used simplification when the incid
ent light is unpolarized and only the intensity of the reflected light
is to be computed. In this paper we employ accurate vector and scalar
multiple-scattering calculations to perform a systematic study of the
errors induced by the neglect of polarization in radiance calculation
s for a homogeneous, plane-parallel Rayleigh-scattering atmosphere (wi
th and without depolarization) above a Lambertian surface. Specificall
y, we calculate percent errors in the reflected intensity for various
directions of light incidence and reflection, optical thicknesses of t
he atmosphere, single-scattering albedos, depolarization factors, and
surface albedos. The numerical data displayed can be used to decide wh
ether or not the scalar approximation may be employed depending on the
parameters of the problem. We show that the errors decrease with incr
easing depolarization factor and/or increasing surface albedo. For con
servative or nearly conservative scatter-ing and small surface albedos
, the errors are maximum at optical thicknesses of about 1. The calcul
ated errors may be too large for some practical applications, and, the
refore, rigorous vector calculations should be employed whenever possi
ble. However, if approximate scalar calculations are used, we recommen
d to avoid geometries involving phase angles equal or close to 0-degre
es and 90-degrees, where the errors are especially significant. We pro
pose a theoretical explanation of the large vector/scalar differences
in the case of Rayleigh scattering. According to this explanation, the
differences are caused by the particular structure of the Rayleigh sc
attering matrix and come from lower-order (except first-order) light s
cattering paths involving right scattering angles and right-angle rota
tions of the scattering plane.