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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 12 Sep 2018

Research article | 12 Sep 2018

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This discussion paper is a preprint. It is a manuscript under review for the journal Atmospheric Chemistry and Physics (ACP).

Free Tropospheric Aerosols at the Mt. Bachelor Observatory: More Oxidized and Higher Sulfate Content Compared to Boundary Layer Aerosols

Shan Zhou1, Sonya Collier1, Daniel A. Jaffe2,3, and Qi Zhang1 Shan Zhou et al.
  • 1Department of Environmental Toxicology, University of California, Davis, CA 95616, USA
  • 2School of Science, Technology, Engineering, and Mathematics, University of Washington Bothell, Bothell, WA, USA
  • 3Department of Atmospheric Sciences, University of Washington, Seattle, WA, USA

Abstract. Understanding the properties and lifecycle processes of aerosol particles in regional air masses is crucial for constraining the climate impacts of aerosols on a global scale. In this study, characteristics of aerosols in the boundary layer (BL) and free troposphere (FT) of a remote continental region in the western US were studied using a high-resolution time-of-flight aerosol mass spectrometer deployed at the Mount Bachelor Observatory (MBO; 2763ma.s.l.) in central Oregon in summer 2013. In the absence of wildfire influence, the average (±1σ) concentration of non-refractory submicrometer particulate matter (NR-PM1) at MBO was 2.8 (±2.8)µgm−3 and 84% of the mass was organic. The organic aerosol (OA) at MBO from these clean periods showed clear diurnal variations driven by the boundary layer dynamics with significantly higher concentrations occurring during daytime, upslope conditions. NR-PM1 contained a higher mass fraction of sulfate and was frequently acidic when MBO resided in the FT. In addition, OA in the FT was found to be highly oxidized (O/C ~ 1.17) with low volatility. In contrast, OA associated with BL air masses had an average O/C of 0.67 and appeared to be semivolatile. The significant compositional and physical differences observed between FT and BL aerosols may have important implications for understanding the climate effects of regional background aerosols.

Shan Zhou et al.
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Status: final response (author comments only)
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Shan Zhou et al.
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