Shape of atmospheric mineral particles collected in three Chinese arid‐regions

By K. Okada, J. Heintzenberg, K. Kai, Yu Qin. 2001

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Modeling of the scattering and radiative properties of nonspherical dust-like aerosols (2007, background): “Sokolik et al. (1998) showed that the refractive indices in the infrared region are quite different for dust particles originating from different sources.”
Modeling the radiative properties of nonspherical soil-derived mineral aerosols (2004, methodology): “Aspect ratio of a sphere is equal to one; Circularity (CIR): Perimeter2=(4 ∗ Area) [21] (or as (4 ∗ Area)=Perimeter2 [22]).”
Optical properties of terrestrial clouds (2004, background): “This is due to different morphology of ice crystals (Magano and Lee, 1966) as compared to mineral aerosol (Okada et al., 2001).”
Ability of multiangle remote sensing observations to identify and distinguish mineral dust types : Optical models and retrievals of optically thick plumes : Quantifying the radiative and biogeochemical impacts of mineral dust (2005, methodology): “Recent field and laboratory work [Clarke et al., 2004; Huebert et al., 2000; Okada et al., 2001; Reid et al., 2003a, 2003b; Wang et al., 2002] provide new information about the physical properties of mineral dust originating in various regions.”