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Volume 14, issue 22
Atmos. Chem. Phys., 14, 12167-12179, 2014
https://doi.org/10.5194/acp-14-12167-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Interactions between climate change and the Cryosphere: SVALI,...

Atmos. Chem. Phys., 14, 12167-12179, 2014
https://doi.org/10.5194/acp-14-12167-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 19 Nov 2014

Research article | 19 Nov 2014

Aerosol indirect effects on continental low-level clouds over Sweden and Finland

M. K. Sporre1, E. Swietlicki1, P. Glantz2, and M. Kulmala3 M. K. Sporre et al.
  • 1Department of Physics, Lund University, Box 118, 222 11 Lund, Sweden
  • 2Department of Applied Environmental Science, Stockholm University, 114 18 Stockholm, Sweden
  • 3Department of Physics, University of Helsinki, P. O. Box 64, 00014 Helsinki, Finland

Abstract. Aerosol effects on low-level clouds over the Nordic Countries are investigated by combining in situ ground-based aerosol measurements with remote sensing data of clouds and precipitation. Ten years of number size distribution data from two aerosol measurement stations (Vavihill, Sweden and Hyytiälä, Finland) provide aerosol number concentrations in the atmospheric boundary layer. This is combined with cloud satellite data from the Moderate Resolution Imaging Spectroradiometer and weather radar data from the Baltic Sea Experiment. Also, how the meteorological conditions affect the clouds is investigated using reanalysis data from the European Centre for Medium-Range Weather Forecasts.

The cloud droplet effective radius is found to decrease when the aerosol number concentration increases, while the cloud optical thickness does not vary with boundary layer aerosol number concentrations. Furthermore, the aerosol–cloud interaction parameter (ACI), a measure of how the effective radius is influenced by the number concentration of cloud active particles, is found to be somewhere between 0.10 and 0.18 and the magnitude of the ACI is greatest when the number concentration of particles with a diameter larger than 130 nm is used. Lower precipitation intensity in the weather radar images is associated with higher aerosol number concentrations. In addition, at Hyytiälä the particle number concentrations is generally higher for non-precipitating cases than for precipitating cases. The apparent absence of the first indirect effect of aerosols on low-level clouds over land raises questions regarding the magnitude of the indirect aerosol radiative forcing.

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