1970
DOI: 10.1086/150296
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Multiple Scattering in a Plane-Parallel Atmosphere. I. Successive Scattering in a Semi-Infinite Medium

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Cited by 43 publications
(13 citation statements)
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“…(5) is very slow when ω is very close to 1. In order to solve this problem, the asymptotic form of ) ( * n R is proposed for higher-order scattering (refer to [9,10] …”
Section: Methods Of the Successive Orders Of Scatteringmentioning
confidence: 99%
“…(5) is very slow when ω is very close to 1. In order to solve this problem, the asymptotic form of ) ( * n R is proposed for higher-order scattering (refer to [9,10] …”
Section: Methods Of the Successive Orders Of Scatteringmentioning
confidence: 99%
“…[159][160][161][162] The equation of radiative transfer is separated in azimuth and the integrals replaced by sums. [167][168][169][170][171] The intensity is expressed as aseries developed for the number of seattering proeesses to be eonsidered. [163][164][165][166] The atmosphere is divided into layers and the unit sphere into a set of solid angle inerements.…”
Section: Monte Carlo Methodsmentioning
confidence: 99%
“…As mentioned above, the atmosphere of AOT (0.46  μ m) > 4 is optically semi-infinite. We propose calculating the reflectance R as a sum of the n th-order of reflection function R *( n ) [21, 22]: R(Ω,Ωnormal0)=false∑n=normal1ωnR(n:Ω,Ωnormal0), where n is the number of times of scattering, and ω represents single-scattering albedo. The n th-order reflection function R *( n : Ω , Ω 0 ) describes radiation emerging at the TOA after scattering n times within the atmosphere.…”
Section: Algorithmsmentioning
confidence: 99%