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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 14, issue 1
Atmos. Chem. Phys., 14, 143–157, 2014
https://doi.org/10.5194/acp-14-143-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 14, 143–157, 2014
https://doi.org/10.5194/acp-14-143-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 06 Jan 2014

Research article | 06 Jan 2014

Single scattering by realistic, inhomogeneous mineral dust particles with stereogrammetric shapes

H. Lindqvist1, O. Jokinen2, K. Kandler3, D. Scheuvens3, and T. Nousiainen1,4 H. Lindqvist et al.
  • 1University of Helsinki, Department of Physics, Helsinki, Finland
  • 2Aalto University, Department of Real Estate, Planning and Geoinformatics, Espoo, Finland
  • 3Technische Universität Darmstadt, Inst. für Angewandte Geowissenschaften, Darmstadt, Germany
  • 4Finnish Meteorological Institute, Helsinki, Finland

Abstract. Light scattering by single, inhomogeneous mineral dust particles was simulated based on shapes and compositions derived directly from measurements of real dust particles instead of using a mathematical shape model. We demonstrate the use of the stereogrammetric shape retrieval method in the context of single-scattering modelling of mineral dust for four different dust types – all of them inhomogeneous – ranging from compact, equidimensional shapes to very elongated and aggregate shapes. The three-dimensional particle shapes were derived from stereo pairs of scanning-electron microscope images, and inhomogeneous composition was determined by mineralogical interpretation of localized elemental information based on energy-dispersive spectroscopy. Scattering computations were performed for particles of equal-volume diameters, from 0.08 μm up to 2.8 μm at 550 nm wavelength, using the discrete-dipole approximation. Particle-to-particle variation in scattering by mineral dust was found to be quite considerable and was not well reproduced by simplified shapes of homogeneous spheres, spheroids, or Gaussian random spheres. Effective-medium approximation results revealed that particle inhomogeneity should be accounted for even for small amounts of absorbing media (here up to 2% of the volume), especially when considering scattering by inhomogeneous particles at size parameters 3<x<8. When integrated over a log-normal size distribution, the linear depolarization ratio and single-scattering albedo were also found to be sensitive to inhomogeneity. The methodology applied is work-intensive and the light-scattering method used quite limited in terms of size parameter coverage. It would therefore be desirable to find a sufficiently accurate but simpler approach with fewer limitations for single-scattering modelling of dust. For validation of such a method, the approach presented here could be used for producing reference data when applied to a suitable set of target particles.

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