By Alexander A. Kokhanovsky
Light Scattering experiences (vol. nine) is aimed toward the outline of recent advances in radiative move and lightweight scattering. the next issues may be thought of: mild scattering through atmospheric airborne dirt and dust debris and likewise through inhomogeneous scatterers, the overall - goal discrete - ordinate set of rules DISORT for radiative move, the radiative move code RAY in accordance with the adding-doubling answer of the radiative move equation, aerosol and cloud distant sensing, use of polarization in distant sensing, direct aerosol radiative forcing, ideas of the Mueller matrix measurements, mild reflectance from a variety of land surfaces. This quantity can be a helpful addition to already released volumes 1-8 of sunshine Scattering Reviews.
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Extra info for Light Scattering Reviews 9: Light Scattering and Radiative Transfer
Ellipsoids have also been applied to investigate the radiative eﬀects of atmospheric dust by Yi et al. (2011). The application of ellipsoids to mineral dust is facilitated by the pre-computed lookup tables in the form of an optical database made available by Meng et al. (2010). The close similarity of spheroids and ellipsoids suggests that ellipsoids probably suﬀer from the same ﬂaws. Even though no studies apparently exist to test the applicability of ellipsoids for predicting the spectral dependence of dust particle single-scattering properties, Merikallio et al.
8d), deﬁned by two shape parameters: the aspect ratio and the number of corners in the polygonal cross-section. The number of corners was varied from four to seven, while the aspect ratios were varied roughly within a factor of two, with diﬀerent sets for polyhedra with diﬀerent cross-sections. A T -matrix code speciﬁcally tailored for diﬀerent types of polyhedra was used for light-scattering computations; recently, this code has been made publicly available (Kahnert, 2013). To test the performance of polyhedra as model particles for mineral dust, the simulations were compared against a scattering matrix for a feldspar sample measured by Volten et al.
The size parameter is also an important parameter when considering the suitability and applicability of diﬀerent light-scattering methods. The composition speciﬁes the complex refractive index m(λ) of a particle, or, in the case of anisotropic materials, the dielectric tensor. These describe how the material responds to the time-harmonic electric and magnetic ﬁelds of the incident radiation. The imaginary part of m is related to the absorptivity of the material. 2 Models with simple homogeneous particles For light-scattering purposes, dust particles are often modeled using simple geometries, assuming internal homogeneity, even though real dust particles are very complex targets.