Atmos. Chem. Phys. Discuss., 7, 15805-15851, 2007
www.atmos-chem-phys-discuss.net/7/15805/2007/
doi:10.5194/acpd-7-15805-2007
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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.
Cloud condensation nuclei activity at Jeju Island, Korea in spring 2005
M. Kuwata1, Y. Kondo1, Y. Miyazaki1, Y. Komazaki1, J. H. Kim2, S. S. Yum2, H. Tanimoto3, and H. Matsueda4
1Research Center for Advanced Science and Technology, University of Tokyo, Tokyo, Japan
2Department of Atmospheric Science, Yonsei University, Seoul, Korea
3Atmospheric Environmental Div., National Inst. for Environmental Studies, Tsukuba, Japan
4Geochemical Research Department, Meteorological Research Institute, Tsukuba, Japan

Abstract. We measured the number concentrations of cloud condensation nuclei (CCN) and the size distributions of CCN/CN (CN: condensation nuclei) ratios at supersaturations (SSs) of 0.097, 0.27, 0.58, and 0.97% at Jeju-Island, Korea during March-April 2005. Measurements of aerosol inorganic ions, water-soluble organic carbon (WSOC), organic carbon (OC), and elemental carbon (EC) in PM2.5 were simultaneously made. The CCN/CN ratios increased with increasing particle diameter, and the diameter at CCN/CN=0.5 was defined as D50. D50 represents the activation dry diameter of atmospheric particles. The average D50 at SS=0.097% and 0.97% was 136 nm and 31 nm, respectively. The temporal variation of D50 at SS=0.097% was correlated with the mass fraction of water-soluble components (inorganic ions + WSOC), indicating that the temporal variation of CCN activity was mainly controlled by changes in the water-soluble components fraction. The critical dry diameter (Dcrit), which is the threshold dry diameter for CCN activation, was calculated from the observed aerosol chemical compositions by K√∂hler theory for comparison with D50. The D50 at SS=0.097% was correlated (r2=0.48) with calculated Dcrit, although Dcrit were larger than D50 by 20–29% on average. The systematic difference between D50 and Dcrit could be caused by the size dependence of the aerosol chemical compositions or surface tension lowering caused by the mixing of water-soluble organic compounds. This difference corresponds to a 27±14% uncertainty in the CCN number concentration estimated from the observed particle number size distribution.

Citation: Kuwata, M., Kondo, Y., Miyazaki, Y., Komazaki, Y., Kim, J. H., Yum, S. S., Tanimoto, H., and Matsueda, H.: Cloud condensation nuclei activity at Jeju Island, Korea in spring 2005, Atmos. Chem. Phys. Discuss., 7, 15805-15851, doi:10.5194/acpd-7-15805-2007, 2007.
 
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