By Alexander A. Kokhanovsky
Light Scattering reports (vol. nine) is aimed toward the outline of contemporary advances in radiative move and light-weight scattering. the subsequent themes can be thought of: gentle scattering through atmospheric airborne dirt and dust debris and likewise through inhomogeneous scatterers, the final - function discrete - ordinate set of rules DISORT for radiative move, the radiative move code RAY according to the adding-doubling resolution of the radiative move equation, aerosol and cloud distant sensing, use of polarization in distant sensing, direct aerosol radiative forcing, rules of the Mueller matrix measurements, mild reflectance from numerous land surfaces. This quantity could be a important addition to already released volumes 1-8 of sunshine Scattering Reviews.
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Extra resources for Light Scattering Reviews 9: Light Scattering and Radiative Transfer
As the size-parameter range of the simulated particles does not cover more than about half of the total scattering cross-section of the sample particles, quantitatively good ﬁts cannot be expected, but comparisons still give qualitative information about the performance of the shape models. For example, irregular rhombohedra produce stronger depolarization and thus smaller P22 /P11 values than ﬂakes, matching the measured values much better, whereas ﬂakes produce linear polarization (−P12 /P11 ) with the same kind of angular dependency as the measurements, but with too high an amplitude, while for rhombohedra the values are too small.
2011). The monomers in the aggregates are overlapping, deformed spheroids. Example shapes of these particles are shown in Fig. 9, panels (c) and (d). The study compared simulated scattering properties against lidar measurements, but only in such a way that model ensembles always included multiple model particle types. It is therefore not possible to judge how well each shape model performs individually. It is noteworthy, however, that Gasteiger et al. 4) resulted in too strong backscattering compared to 1 Light scattering by atmospheric mineral dust particles 29 the measured values.
1 Light scattering by atmospheric mineral dust particles 31 The GRS geometry with internal inhomogeneity has been considered a model for large Saharan dust by Nousiainen et al. (2003, 2011a) and Mu˜ noz et al. (2007). Of these, Nousiainen et al. (2003) and Mu˜ noz et al. (2007) incorporated the inhomogeneity by a simple, phenomenological ad hoc scheme where internal Lambertian screens were put inside the model particles, while Nousiainen et al. (2011a) applied a more physical approach where the particle interiors were ﬁlled with a cloud of independent scatterers with pre-deﬁned single-scattering properties.