Multiple Scattering of Light by Particles: Radiative Transfer and Coherent Backscattering

By M. I. Mishchenko, Larry Travis, Andrew A. Lacis. 2006

531 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/ff314c0bdf601846c8a81fcc7f53d12ff43ac1ed

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Citations in the corpus

Application of spheroid models to account for aerosol particle nonsphericity in remote sensing of desert dust (2006, methodology): “[10] Photometric and polarization parameters of atmospheric radiation can be modeled by solving the vector radiative transfer equation for a plane-parallel multilayered atmosphere [Hovenier et al., 2004; Mishchenko et al., 2006].”
Role of fluctuational electrodynamics in near-field radiative heat transfer (2007, background): “Mishchenko, M.I., Maxwell’s Equations, Radiative Transfer, and Coherent Backscattering: A General Perspective, Journal of Quantitative Spectroscopy and Radiative Transfer, Vol. 101, pp. 540-555, 2006.”
Comparison between discrete dipole implementations and exact techniques (2007, background): “[1], we can say that the RO and GO use only the ladder diagrams e.”
THE USE OF TRANSPORT APPROXIMATION AND DIFFUSION-BASED MODELS IN RADIATIVE TRANSFER CALCULATIONS (2012, methodology): “The VRTE is formulated for the Stokes column vector (instead of the radiation intensity), and the scattering matrix is used instead of the scattering phase function in the VRTE integral term (Mishchenko et al., 2006).”
Models for surface reflection of radiance and polarized radiance: Comparison with airborne multi-angle photopolarimetric measurements and implications for modeling top-of-atmosphere measurements (2011, methodology): “The coherent backscattering effect, which is caused by interference (see, for example, Litvinov et al., 2007; Mishchenko et al., 2006; Muinonen, 2004 and literature cited therein), depends on the wavelength of incident radiation and may give negative value of the degree of linear polarization of…”
A multiple sphere T-matrix Fortran code for use on parallel computer clusters (2011, methodology): “For a plane wave (PW), the coefﬁcients for the incident ﬁeld VSWF expansion, centered about the target origin, are given by where t mnp are derived from the vector spherical harmonic functions, and are given by with D ð n Þ mk denoting the generalized spherical function [15].”