Atmos. Chem. Phys. Discuss., 12, 14813-14836, 2012
www.atmos-chem-phys-discuss.net/12/14813/2012/
doi:10.5194/acpd-12-14813-2012
© Author(s) 2012. This work is distributed
under the Creative Commons Attribution 3.0 License.
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This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
Sources of anions in aerosols in northeast Greenland during late winter
M. Fenger1, L. L. Sørensen2, K. Kristensen1, B. Jensen2, Q. T. Nquyen1,2, J. K. Nøjgaard2, A. Massling2, H. Skov2,3, and M. Glasius1
1Department of Chemistry, Aarhus University, 8000 Aarhus, Denmark
2Department of Environmental Science, Aarhus University, 4000 Roskilde, Denmark
3Institute of Chemical Engineering, Biotechnology and Environmental Technology, University of Southern Denmark, 5230 Odense M, Denmark

Abstract. The knowledge of climate effects of atmospheric aerosols is associated with large uncertainty, and a better understanding of their physical and chemical properties is needed, especially in the Arctic environment. The objective of the present study is to improve our understanding of the processes affecting the composition of the aerosols in the high Arctic. Therefore size-segregated aerosols were sampled at a high Arctic site, Station Nord (Northeast Greenland), in March 2009 using a Micro Orifice Uniform Deposit Impactor. The aerosol samples were extracted in order to analyze the three water-soluble anions: chloride, nitrate and sulphate. The results are discussed based on possible chemical and physical transformations as well as transport patterns.

The total concentrations of the ions at Station Nord were 53–507 ng m−3, 2–298 ng m−3 and 535–1087 ng m−3 for chloride (Cl), nitrate (NO3-) and sulphate (SO42−), respectively. The aerosols in late winter/early spring, after polar sunrise, are found to be a mixture of long-range transported and regional to local originating aerosols. Fine particles, smaller than 1 μm, containing SO42−, Cl and NO3, are hypothesized to originate from long-range transport, where SO42− is by far the dominating anion accounting for 50–85% of the analyzed mass. The analysis suggests that Cl and NO3 in coarser particles (>1.5 μm) originate from local/regional sources. Under conditions where the air mass is transported over sea-ice at high wind speeds, very coarse particles (>18 μm) are observed and it is hypothesized that frost flowers on the sea ice is a source of very coarse chloride particles in the Arctic.


Citation: Fenger, M., Sørensen, L. L., Kristensen, K., Jensen, B., Nquyen, Q. T., Nøjgaard, J. K., Massling, A., Skov, H., and Glasius, M.: Sources of anions in aerosols in northeast Greenland during late winter, Atmos. Chem. Phys. Discuss., 12, 14813-14836, doi:10.5194/acpd-12-14813-2012, 2012.
 
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