Effect of mineral dust aerosol aspect ratio on polarized reflectance

The effects of dust particle aspect ratios on single- and multiple-scattering processes are studied using the spheroidal model in order to obtain a better understanding of the radiance and polarization signals at the top of the atmosphere (TOA) under various dust-aerosol-loading conditions. Specific...

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Bibliographic Details
Published in:Journal of quantitative spectroscopy & radiative transfer 2015-01, Vol.151, p.97-109
Main Authors: Huang, Xin, Yang, Ping, Kattawar, George, Liou, Kuo-Nan
Format: Article
Language:English
Subjects:
Anisotropy
Aspect ratio
Dust
Dust aerosol
Polarization
Polarization measurement
Polders
Radiance
Radiative transfer
Satellite
Satellites
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Summary:The effects of dust particle aspect ratios on single- and multiple-scattering processes are studied using the spheroidal model in order to obtain a better understanding of the radiance and polarization signals at the top of the atmosphere (TOA) under various dust-aerosol-loading conditions. Specifically, the impact of the particle aspect ratio on the polarization state of the TOA radiation field is demonstrated by comparing the normalized polarized radiances observed by the POLDER (POLarization and Directionality of the Earth׳s Reflectances) instrument on board the PARASOL (Polarisation et Anisotropie des Reflectances au sommet de l׳Atmosphère, couples avec un Satellite d׳Observation emportant un Lidar) satellite with the corresponding theoretical counterparts. Furthermore, presented are the aspect ratio values inferred from multi-angular polarized radiance measurements of Saharan and Asian dust by the POLDER/PARASOL. •The radiative effect of dust aerosol aspect ratio is investigated.•A computational efficient vector radiative transfer model is developed.•Spaceborne Polarimetric measurements are used to retrieve aerosol properties.•A case study of Saharan dust shows a mean aspect ratio of 2.5.•Asian dust exhibits two aspect ratio values, 2.5 and 1.25.
ISSN:0022-4073
1879-1352
DOI:10.1016/j.jqsrt.2014.09.014