Optical and microphysical properties of natural mineral dust and anthropogenic soil dust near dust source regions over northwestern China

Mineral dust aerosols (MDs) not only influence the climate by scattering and absorbing solar radiation but also modify cloud properties and change the ecosystem. From 3 April to 16 May 2014, a ground-based mobile laboratory was deployed to measure the optical and microphysical properties of MDs n...

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Bibliographic Details
Main Authors: X. Wang, H. Wen, J. Shi, J. Bi, Z. Huang, B. Zhang, T. Zhou, K. Fu, Q. Chen, J. Xin
Format: Article
Language:English
Published: Copernicus Publications 2018-02-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/18/2119/2018/acp-18-2119-2018.pdf
Description
Summary:Mineral dust aerosols (MDs) not only influence the climate by scattering and absorbing solar radiation but also modify cloud properties and change the ecosystem. From 3 April to 16 May 2014, a ground-based mobile laboratory was deployed to measure the optical and microphysical properties of MDs near dust source regions in Wuwei, Zhangye, and Dunhuang (in chronological order) along the Hexi Corridor over northwestern China. Throughout this dust campaign, the hourly averaged (±standard deviation) aerosol scattering coefficients (<i>σ</i><sub>sp</sub>, 550 nm) of the particulates with aerodynamic diameters less than 2.5 µm (PM<sub>2.5</sub>) at these three sites were sequentially 101.5 ± 36.8, 182.2 ± 433.1, and 54.0 ± 32.0 Mm<sup>−1</sup>. Correspondingly, the absorption coefficients (<i>σ</i><sub>ap</sub>, 637 nm) were 9.7 ± 6.1, 6.0 ± 4.6, and 2.3 ± 0.9 Mm<sup>−1</sup>; single-scattering albedos (<i>ω</i>, 637 nm) were 0.902 ± 0.025, 0.931 ± 0.037, and 0.949 ± 0.020; and scattering Ångström exponents (Å<sub>sp</sub>, 450–700 nm) of PM<sub>2.5</sub> were 1.28 ± 0.27, 0.77 ± 0.51, and 0.52 ± 0.31. During a severe dust storm in Zhangye (i.e., from 23 to 25 April), the highest values of <i>σ</i><sub>sp</sub><sup>2.5</sup> ( ∼  5074 Mm<sup>−1</sup>), backscattering coefficient (<i>σ</i><sub>bsp</sub><sup>2.5</sup>,  ∼  522 Mm<sup>−1</sup>), and <i>ω</i><sub>637</sub> ( ∼  0.993) and the lowest values of backscattering fraction (<i>b</i><sub>2.5</sub>,  ∼  0.101) at 550 nm and Å<sub>sp</sub><sup>2.5</sup> ( ∼  −0.046) at 450–700 nm, with peak values of aerosol number size distribution (appearing at the particle diameter range of 1–3 µm), exhibited that the atmospheric aerosols were dominated by coarse-mode dust aerosols. It is hypothesized that the relatively higher values of mass scattering efficiency during floating dust episodes in Wuwei and Zhangye are attributed to the anthropogenic soil dust produced by agricultural cultivations.
ISSN:1680-7316
1680-7324