Mars aerosol optical thickness retrieved from measurements of the polarization inversion angle and the shape of dust particles.

Details Mars aerosol optical thickness retrieved from measurements of the polarization inversion angle and the shape of dust particles. Mars aerosol optical thickness retrieved from measurements of the polarization inversion angle and the shape of dust particles.

Dec 1999

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1999jqsrt..63..667p&link_type=abstract

Journal of Quantitative Spectroscopy and Radiative Transfer, vol. 63, issue 2-6, pp. 667-676

Physics

1

Mars Atmosphere: Aerosols, Mars Atmosphere: Scattering, Mars Atmosphere: Polarization, Dust Grains: Scattering, Dust Grains: Polarization

Scientific paper

Estimates of the optical thickness of the "clear" atmosphere of Mars obtained from ground-based polarimetric observations are characterized by very low values. The sensitivity of polarization to the size and shape of scatterers raises the question of the effect of the irregular shape of solid aerosol particles on the optical thickness retrieved from the spectral dependence of the polarization inversion angle for Mars (the phase angle at which the polarization of the scattered radiation changes sign). The Stokes scattering matrix for irregular dust particles is calculated using the T-matrix method. The model of randomly oriented oblate polydisperse spheroids used in this study indicates a weak dependence of the polarization inversion angle on the optical thickness of aerosols τd: an increase in τd from 0.05 to 0.15 results in an inversion angle increase of less than 1° whereas for spherical particles this change is about 5°. It is reasonable to expect that particles with more pronounced irregular shapes than spheroids may lead to more substantial depolarization and hence an even weaker sensitivity of the inversion angle to variations in the aerosol optical thickness. Thus, very low estimates of the optical thickness of the "clear" atmosphere of Mars retrieved from ground-based polarimetric observations using a spherical-shape approach for aerosol particles cannot be considered reliable. Ignoring the dust particle shape introduces similar uncertainties in the models of the Martian atmosphere as those caused by traditionally discussed errors in such parameters as refractive index or size distribution.

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