Atmos. Chem. Phys. Discuss., 13, 2695-2723, 2013
www.atmos-chem-phys-discuss.net/13/2695/2013/
doi:10.5194/acpd-13-2695-2013
© Author(s) 2013. This work is distributed
under the Creative Commons Attribution 3.0 License.
Review Status
This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
Atmospheric processing of iron carried by mineral dust
S. Nickovic1, A. Vukovic2,3, and M. Vujadinovic2,3
1World Meteorological Organization, Geneva, Switzerland
2Faculty of Agriculture, University of Belgrade, Belgrade, Serbia
3South East European Virtual Climate Change Center, Belgrade, Serbia

Abstract. Nutrification of the open ocean originates mainly from deposited aerosol in which the bioavaliable iron is likely to be an important factor. The relatively insoluble iron in dust from arid soils becomes more soluble after atmospheric processing and could contribute to marine primary production. To numerically simulate the path of iron on its atmospheric route from desert sources to sinks in the ocean, we developed a regional atmospheric dust-iron model that included parameterization of the transformation of iron to a soluble form caused by dust mineralogy, cloud processes and solar radiation. When compared with sample data on the aerosol iron, which were collected during several Atlantic cruises, the results from the higher-resolution simulation experiments showed that the model was capable of reproducing the major observed patterns.

Citation: Nickovic, S., Vukovic, A., and Vujadinovic, M.: Atmospheric processing of iron carried by mineral dust, Atmos. Chem. Phys. Discuss., 13, 2695-2723, doi:10.5194/acpd-13-2695-2013, 2013.
 
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