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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 13, issue 17 | Copyright
Atmos. Chem. Phys., 13, 8543-8550, 2013
https://doi.org/10.5194/acp-13-8543-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 02 Sep 2013

Research article | 02 Sep 2013

Possible effect of extreme solar energetic particle events of September–October 1989 on polar stratospheric aerosols: a case study

I. A. Mironova1 and I. G. Usoskin2 I. A. Mironova and I. G. Usoskin
  • 1Institute of Physics, St. Petersburg State University, St. Petersburg, Russia
  • 2Sodankylä Geophysical Observatory (Oulu unit and Dept. of Physics), University of Oulu, Finland

Abstract. The main ionization source of the middle and low Earth's atmosphere is related to energetic particles coming from outer space. Usually it is ionization from cosmic rays that is always present in the atmosphere. But in a case of a very strong solar eruption, some solar energetic particles (SEPs) can reach middle/low atmosphere increasing the ionization rate up to some orders of magnitude at polar latitudes. We continue investigating such a special class of solar events and their possible applications for natural variations of the aerosol content. After the case study of the extreme SEP event of January 2005 and its possible effect upon polar stratospheric aerosols, here we analyze atmospheric applications of the sequence of several events that took place over autumn 1989. Using aerosol data obtained over polar regions from two satellites with space-borne optical instruments SAGE II and SAM II that were operating during September–October 1989, we found that an extreme major SEP event might have led to formation of new particles and/or growth of preexisting ultrafine particles in the polar stratospheric region. However, the effect of the additional ambient air ionization on the aerosol formation is minor, in comparison with temperature effect, and can take place only in the cold polar atmospheric conditions. The extra aerosol mass formed under the temperature effect allows attributing most of the changes to the "ion–aerosol clear sky mechanism".

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