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Volume 11, issue 16
Atmos. Chem. Phys., 11, 8703–8719, 2011
https://doi.org/10.5194/acp-11-8703-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 11, 8703–8719, 2011
https://doi.org/10.5194/acp-11-8703-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 25 Aug 2011

Research article | 25 Aug 2011

Aerosol particle number size distributions and particulate light absorption at the ZOTTO tall tower (Siberia), 2006–2009

J. Heintzenberg1, W. Birmili1, R. Otto1, M. O. Andreae2, J.-C. Mayer2, X. Chi2, and A. Panov3 J. Heintzenberg et al.
  • 1Leibniz-Institute for Tropospheric Research, Permoserstrasse 15, 04318 Leipzig, Germany
  • 2Max-Planck-Institute for Chemistry, P.O. Box 3020, 55020 Mainz, Germany
  • 3VN Sukachev Institute of Forest, Siberian Branch of the Russian Academy of Science, Akademgorodok, P.O. Box 26695, 660036 Krasnoyarsk, Russia

Abstract. This paper analyses aerosol particle number size distributions, particulate absorption at 570 nm wavelength and carbon monoxide (CO) measured between September 2006 and January 2010 at heights of 50 and 300 m at the Zotino Tall Tower Facility (ZOTTO) in Siberia (60.8° N; 89.35° E). Average number, surface and volume concentrations are broadly comparable to former studies covering shorter observation periods. Fits of multiple lognormal distributions yielded three maxima in probability distribution of geometric mean diameters in the Aitken and accumulation size range and a possible secondary maximum in the nucleation size range below 25 nm. The seasonal cycle of particulate absorption shows maximum concentrations in high winter (December) and minimum concentrations in mid-summer (July). The 90th percentile, however, indicates a secondary maximum in July/August that is likely related to forest fires. The strongly combustion derived CO shows a single winter maximum and a late summer minimum, albeit with a considerably smaller seasonal swing than the particle data due to its longer atmospheric lifetime. Total volume and even more so total number show a more complex seasonal variation with maxima in winter, spring, and summer. A cluster analysis of back trajectories and vertical profiles of the pseudo-potential temperature yielded ten clusters with three levels of particle number concentration: Low concentrations in Arctic air masses (400–500 cm−3), mid-level concentrations for zonally advected air masses from westerly directions between 55° and 65° N (600–800 cm−3), and high concentrations for air masses advected from the belt of industrial and population centers in Siberia and Kazakhstan (1200 cm−3). The observational data is representative for large parts of the troposphere over Siberia and might be particularly useful for the validation of global aerosol transport models.

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