Atmos. Chem. Phys. Discuss., 13, 10395-10461, 2013
www.atmos-chem-phys-discuss.net/13/10395/2013/
doi:10.5194/acpd-13-10395-2013
© Author(s) 2013. 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.
Vertical profiling of aerosol particles and trace gases over the central Arctic Ocean during summer
P. Kupiszewski1,2, C. Leck1, M. Tjernström1, S. Sjogren3, J. Sedlar4, M. Graus5,6, M. Müller7, B. Brooks8, E. Swietlicki3, S. Norris9, and A. Hansel7
1Department of Meteorology and Bert Bolin Centre for Climate Research, Stockholm University, 10691 Stockholm, Sweden
2Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen PSI, Switzerland
3Department of Physics, Lund University, Lund, Sweden
4Swedish Meteorological and Hydrological Institute, Remote Sensing Division, Norrköping, Sweden
5Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado, Boulder, CO 80309, USA
6NOAA Earth Sciences Research Lab, Chemical Sciences Division, Boulder, CO 80305, USA
7Institute of Ion and Applied Physics, University of Innsbruck, 6020 Innsbruck, Austria
8National Centre for Atmospheric Science, Leeds, UK
9Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds, UK

Abstract. Unique measurements of vertical size resolved aerosol particle concentrations, trace gas concentrations and meteorological data were obtained during the Arctic Summer Cloud Ocean Study (ASCOS, http://www.ascos.se), an International Polar Year project aimed at establishing the processes responsible for formation and evolution of low-level clouds over the high Arctic summer pack ice. The experiment was conducted from onboard the Swedish icebreaker Oden, and provided both ship- and helicopter-based measurements. This study focuses on the vertical helicopter profiles and onboard measurements obtained during a three-week period when Oden was anchored to a drifting ice floe, and sheds light on the characteristics of Arctic aerosol particles and their distribution throughout the lower atmosphere.

Distinct differences in aerosol particle characteristics within defined atmospheric layers are identified. Near the surface (lowermost couple hundred meters), transport from the marginal ice zone (MIZ), if sufficiently short (less than ca. 2 days), condensational growth and cloud-processing develop the aerosol population. During two of the four representative periods defined in this study, such influence is shown. At altitudes above about 1 km, long-range transport occurs frequently. However, only infrequently does large-scale subsidence descend such air masses to become entrained into the mixed layer in the high Arctic, and therefore they are unlikely to directly influence low-level stratiform cloud formation. Nonetheless, long-range transport plumes can influence the radiative balance of the PBL by influencing formation and evolution of higher clouds, as well as through precipitation transport of particles downwards. New particle formation was occasionally observed, particularly in the near-surface layer. We hypothesize that the origin of these ultrafine particles can be from biological processes, both primary and secondary, within the open leads between the pack ice and/or along the MIZ. In general, local sources, in combination with upstream boundary layer transport of precursor gases from the MIZ, are suggested to constitute the origin of CCN particles and thus be of importance for the formation of interior Arctic low level clouds during summer, and subsequently, through cloud influences, on the melting and freezing of sea ice.


Citation: Kupiszewski, P., Leck, C., Tjernström, M., Sjogren, S., Sedlar, J., Graus, M., Müller, M., Brooks, B., Swietlicki, E., Norris, S., and Hansel, A.: Vertical profiling of aerosol particles and trace gases over the central Arctic Ocean during summer, Atmos. Chem. Phys. Discuss., 13, 10395-10461, doi:10.5194/acpd-13-10395-2013, 2013.
 
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