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A successive order of scattering model for solving vector radiative transfer in the atmosphere

TLDR
In this article, a full vector radiative transfer model for vertically inhomogeneous plane-parallel media has been developed by using the successive order of scattering approach, where a fast analytical expansion of Fourier decomposition is implemented and an exponent-linear assumption is used for vertical integration.
Abstract
A full vector radiative transfer model for vertically inhomogeneous plane–parallel media has been developed by using the successive order of scattering approach. In this model, a fast analytical expansion of Fourier decomposition is implemented and an exponent-linear assumption is used for vertical integration. An analytic angular interpolation method of post-processing source function is also implemented to accurately interpolate the Stokes vector at arbitrary angles for a given solution. It has been tested against the benchmarks for the case of randomly orientated oblate spheroids, illustrating a good agreement for each stokes vector (within 0.01%). Sensitivity tests have been conducted to illustrate the accuracy of vertical integration and angle interpolation approaches. The contribution of each scattering order for different optical depths and single scattering albedos are also analyzed.

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Radiative transfer through terrestrial atmosphere and ocean: Software package SCIATRAN

TL;DR: SCIATRAN as discussed by the authors is a comprehensive software package for the modeling of radiative transfer processes in the terrestrial atmosphere and ocean in the spectral range from the ultraviolet to the thermal infrared including multiple scattering processes, polarization, thermal emission and ocean-atmosphere coupling.
Journal ArticleDOI

A successive order of scattering code for solving the vector equation of transfer in the earth's atmosphere with aerosols

TL;DR: In this article, the vector equation of radiative transfer is solved by a code based on the successive orders of scattering and on the expansion into Fourier series of the azimuth; it includes polarizing effects of aerosol scattering and of reflectance by water or terrestrial surfaces.
Journal ArticleDOI

A vector radiative transfer model for coupled atmosphere and ocean systems with a rough interface

TL;DR: In this article, an exact vector (polarized) radiative transfer (VRT) model for coupled atmosphere and ocean systems is presented, which takes all the multiple scattering processes into account, including atmospheric scattering, oceanic scattering, reflection and transmission through the rough ocean surface.
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A vector radiative transfer model for coupled atmosphere and ocean systems based on successive order of scattering method

TL;DR: A vector radiative transfer model for coupled atmosphere and ocean systems based on the Successive Order of Scattering (SOS) method has been developed for easy-to-use and computationally efficient as mentioned in this paper.
References
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Journal ArticleDOI

Light Scattering by Small Particles

H. C. Van de Hulst, +1 more
- 18 Jul 1957 - 
TL;DR: Light scattering by small particles as mentioned in this paper, Light scattering by Small Particle Scattering (LPS), Light scattering with small particles (LSC), Light Scattering by Small Parts (LSP),
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Light Scattering by Small Particles

TL;DR: Light scattering by small particles as mentioned in this paper, Light scattering by Small Particle Scattering (LPS), Light scattering with small particles (LSC), Light Scattering by Small Parts (LSP),
Journal ArticleDOI

The Delta–M Method: Rapid Yet Accurate Radiative Flux Calculations for Strongly Asymmetric Phase Functions

TL;DR: The delta-M method as discussed by the authors is a natural extension of the delta-Eddington approximation to all orders M of angular approximation, which relies essentially on matching the first 2M phase function moments and using a Dirac delta-function representation of forward scattering.
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