Scattering, Absorption, and Emission of Light by Small Particles

By Larry Travis, M. I. Mishchenko, Andrew A. Lacis. 2002

2,160 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/0de9ede34c94f3d707393e4d4b816542233e109e

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Citations in the corpus

Light Scattering by a Dielectric Sphere: Perspectives on the Mie Resonances (2018, background): “commonly used as a reference for any kind of electromagnetic scattering theory [13] and applications, from the utilization on experimental setups [7] to the benchmarking of computational methods [14,15] and beyond.”
The impact of aerosols on polarized sky radiance: model development, validation, and applications (2009, unknown): “The Stokes parameters are defined as time averages of linear combinations of the electromagnetic field vector (Chandrasekhar , 1950; Hansen and Travis, 1974; Mishchenko et al., 2002): I = E l E * l + E r E * r , (1) Atmos.”
Three-Dimensional Dust Radiative Transfer ∗ (2013, unknown): “2006), MCMax (Min et al. 2009), or TORUS (Harries et al.”
Scattering and radiative properties of complex soot and soot-containing aggregate particles (2006, methodology): “The deviation of the ratio a2ðYÞ=a1ðYÞ from unity is a manifestation of the overall nonsphericity of the soot clusters [16].”
Polarimetric remote sensing of aerosols over land (2009, background): “The reason for this is that when particles are small compared with the measurement wavelength they act like Rayleigh scatterers [Hansen and Travis, 1974; Mishchenko et al., 2002], and any sensitivity to the refractive index is lost.”
A general database of hydrometeor single scattering properties at microwave and sub-millimetre wavelengths (2018, unknown): “…then re-set to the means of respective values for the purpose of consistency For example, M 34 is re-set Other elements in a and K , i.e. i (cid:54)= 1 in a and off-diagonal elements in K , are set to zero according to the theory for totally randomly oriented particles (Mishchenko et al., 2002).”
Scattering and absorption of light by ice particles: Solution by a new physical-geometric optics hybrid method (2011, background): “Over the past several decades, steady improvements have been made in the numerical modeling of the scattering and absorption of light by nonspherical particles [1–5].”
Application of spheroid models to account for aerosol particle nonsphericity in remote sensing of desert dust (2006, methodology): “For example, even the most advanced T-matrix code [Mishchenko et al., 2002] slows down and becomes numerically unstable for highly elongated and flattened spheroids (i.”
ARTS, the Atmospheric Radiative Transfer Simulator – version 2.2, the planetary toolbox edition (2017, methodology): “PyARTS uses the T-matrix codes by [24].”