1Department of Meteorology, Stockholm University, Stockholm, Sweden
2Bert Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
3Institute for Climate & Atmospheric Science, School of Earth and Environment, University of Leeds, Leeds, UK
4Environment Canada, Toronto, Canada
5Department of Chemistry, University of Toronto, Toronto, Canada
6Finnish Meteorological Institute, Helsinki, Finland
7Department of Physics, University of Helsinki, Helsinki, Finland
8TNO Environment and Geosciences, Dept. of Air Quality and Climate, Utrecht, the Netherlands
9Institute of Atmospheric Sciences and Climate (ISAC) of the Italian National Research Council, Rome, Italy
10Nansen Environmental and Remote Sensing Center, Bergen, Norway
11Geophysical Institute, University of Bergen, Bergen, Norway
12Institute of Ion Physics and Applied Physics, University of Innsbruck, Innsbruck, Austria
13Leibniz Institute for Tropospheric Research, Leipzig, Germany
14University of Bayreuth, Bayreuth Center of Ecology and Environmental Research, Bayreuth, Germany
15Bigelow Laboratory for Ocean Sciences, East Boothbay, ME, USA
16Cooperative Institute for Research in Environmental Science (CIRES), University of Colorado, Boulder, CO, USA
17National Oceanic and Atmospheric Administration, Physical Sciences Division, Boulder, CO, USA
18BNR Ecotour Consulting AB, Lammhult, Sweden
19Institute for Atmospheric and Climate Science, ETH Zürich, Zürich, Switzerland
20Max Planck Institute for Meteorology, Hamburg, Germany
21Institute for Systems Biology, Seattle, WA, USA
22School of Physical and Chemical Sciences, Queensland University of Technology, Brisbane, Australia
23Swedish Meteorological and Hydrological Institute, Norrköping, Sweden
24Bjerknes Centre for Climate Research, Bergen, Norway
25Division of Nuclear Physics, Lund University, Lund, Sweden
26Rosenstiel School of Marine and Atmospheric Sciences, University of Miami, Miami, FL, USA
27Department of Applied Physics, University of Eastern Finland, Kuopio, Finland
Received: 15 Mar 2013 – Published in Atmos. Chem. Phys. Discuss.: 23 May 2013
Abstract. The climate in the Arctic is changing faster than anywhere else on earth. Poorly understood feedback processes relating to Arctic clouds and aerosol–cloud interactions contribute to a poor understanding of the present changes in the Arctic climate system, and also to a large spread in projections of future climate in the Arctic. The problem is exacerbated by the paucity of research-quality observations in the central Arctic. Improved formulations in climate models require such observations, which can only come from measurements in situ in this difficult-to-reach region with logistically demanding environmental conditions.
Revised: 14 Nov 2013 – Accepted: 13 Jan 2014 – Published: 19 Mar 2014
The Arctic Summer Cloud Ocean Study (ASCOS) was the most extensive central Arctic Ocean expedition with an atmospheric focus during the International Polar Year (IPY) 2007–2008. ASCOS focused on the study of the formation and life cycle of low-level Arctic clouds. ASCOS departed from Longyearbyen on Svalbard on 2 August and returned on 9 September 2008. In transit into and out of the pack ice, four short research stations were undertaken in the Fram Strait: two in open water and two in the marginal ice zone. After traversing the pack ice northward, an ice camp was set up on 12 August at 87°21' N, 01°29' W and remained in operation through 1 September, drifting with the ice. During this time, extensive measurements were taken of atmospheric gas and particle chemistry and physics, mesoscale and boundary-layer meteorology, marine biology and chemistry, and upper ocean physics.
ASCOS provides a unique interdisciplinary data set for development and testing of new hypotheses on cloud processes, their interactions with the sea ice and ocean and associated physical, chemical, and biological processes and interactions. For example, the first-ever quantitative observation of bubbles in Arctic leads, combined with the unique discovery of marine organic material, polymer gels with an origin in the ocean, inside cloud droplets suggests the possibility of primary marine organically derived cloud condensation nuclei in Arctic stratocumulus clouds. Direct observations of surface fluxes of aerosols could, however, not explain observed variability in aerosol concentrations, and the balance between local and remote aerosols sources remains open. Lack of cloud condensation nuclei (CCN) was at times a controlling factor in low-level cloud formation, and hence for the impact of clouds on the surface energy budget. ASCOS provided detailed measurements of the surface energy balance from late summer melt into the initial autumn freeze-up, and documented the effects of clouds and storms on the surface energy balance during this transition. In addition to such process-level studies, the unique, independent ASCOS data set can and is being used for validation of satellite retrievals, operational models, and reanalysis data sets.
Citation: Tjernström, M., Leck, C., Birch, C. E., Bottenheim, J. W., Brooks, B. J., Brooks, I. M., Bäcklin, L., Chang, R. Y.-W., de Leeuw, G., Di Liberto, L., de la Rosa, S., Granath, E., Graus, M., Hansel, A., Heintzenberg, J., Held, A., Hind, A., Johnston, P., Knulst, J., Martin, M., Matrai, P. A., Mauritsen, T., Müller, M., Norris, S. J., Orellana, M. V., Orsini, D. A., Paatero, J., Persson, P. O. G., Gao, Q., Rauschenberg, C., Ristovski, Z., Sedlar, J., Shupe, M. D., Sierau, B., Sirevaag, A., Sjogren, S., Stetzer, O., Swietlicki, E., Szczodrak, M., Vaattovaara, P., Wahlberg, N., Westberg, M., and Wheeler, C. R.: The Arctic Summer Cloud Ocean Study (ASCOS): overview and experimental design, Atmos. Chem. Phys., 14, 2823-2869, doi:10.5194/acp-14-2823-2014, 2014.