Atmos. Chem. Phys. Discuss., 10, 14993-15022, 2010
www.atmos-chem-phys-discuss.net/10/14993/2010/
doi:10.5194/acpd-10-14993-2010
© Author(s) 2010. 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.
Saharan dust and ice nuclei over Central Europe
H. Klein1, S. Nickovic2, W. Haunold1, U. Bundke1, B. Nillius1, M. Ebert3, S. Weinbruch3, L. Schuetz4, Z. Levin5, L. A. Barrie2, and H. Bingemer1
1Institute for Atmospheric and Environmental Sciences, Goethe-University, Frankfurt am Main, Germany
2World Meteorological Organization, Geneva, Switzerland
3Institute for Applied Geosciences, Technical University of Darmstadt, Darmstadt, Germany
4Institute for Atmospheric Physics, Gutenberg-University, Mainz, Germany
5Dept. of Geophysics, Tel Aviv University, Tel Aviv, Israel

Abstract. Surface measurements of aerosol and ice nuclei (IN) at a Central European mountain site during an episode of dust transport from the Sahara are presented. Transport is simulated by the Eulerian regional dust model DREAM. Ice nuclei and mineral dust are significantly correlated. The highest correlation is found between IN concentration and aerosol surface area. The ice nucleating characteristics of the aerosol with respect to temperature and supersaturation are similar during the dust episode than during the course of the year. This suggests that dust is always a dominant constituent of ice nucleating aerosols in Central Europe.

Citation: Klein, H., Nickovic, S., Haunold, W., Bundke, U., Nillius, B., Ebert, M., Weinbruch, S., Schuetz, L., Levin, Z., Barrie, L. A., and Bingemer, H.: Saharan dust and ice nuclei over Central Europe, Atmos. Chem. Phys. Discuss., 10, 14993-15022, doi:10.5194/acpd-10-14993-2010, 2010.
 
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