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Atmospheric Measurement Techniques An interactive open-access journal of the European Geosciences Union
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Volume 4, issue 8
Atmos. Meas. Tech., 4, 1603–1616, 2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Arctic Summer Cloud Ocean Study (ASCOS) (ACP/AMT/OS inter-journal...

Atmos. Meas. Tech., 4, 1603–1616, 2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 18 Aug 2011

Research article | 18 Aug 2011

Near-surface profiles of aerosol number concentration and temperature over the Arctic Ocean

A. Held1, D. A. Orsini2, P. Vaattovaara3, M. Tjernström4,5, and C. Leck4,5 A. Held et al.
  • 1University of Bayreuth, Bayreuth Center of Ecology and Environmental Research, 95440 Bayreuth, Germany
  • 2Leibniz Institute for Tropospheric Research, 04318 Leipzig, Germany
  • 3University of Eastern Finland, Department of Applied Physics, 70211 Kuopio, Finland
  • 4Stockholm University, Department of Meteorology, 10691 Stockholm, Sweden
  • 5Bert Bolin Center for Climate Research, Stockholm University, 10691 Stockholm, Sweden

Abstract. Temperature and particle number concentration profiles were measured at small height intervals above open and frozen leads and snow surfaces in the central Arctic. The device used was a gradient pole designed to investigate potential particle sources over the central Arctic Ocean. The collected data were fitted according to basic logarithmic flux-profile relationships to calculate the sensible heat flux and particle deposition velocity. Independent measurements by the eddy covariance technique were conducted at the same location. General agreement was observed between the two methods when logarithmic profiles could be fitted to the gradient pole data. In general, snow surfaces behaved as weak particle sinks with a maximum deposition velocity vd = 1.3 mm s−1 measured with the gradient pole. The lead surface behaved as a weak particle source before freeze-up with an upward flux Fc = 5.7 × 104 particles m−2 s−1, and as a relatively strong heat source after freeze-up, with an upward maximum sensible heat flux H = 13.1 W m−2. Over the frozen lead, however, we were unable to resolve any significant aerosol profiles.

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