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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 13, issue 7 | Copyright
Atmos. Chem. Phys., 13, 3733-3741, 2013
https://doi.org/10.5194/acp-13-3733-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 09 Apr 2013

Research article | 09 Apr 2013

Effective aerosol optical depth from pyranometer measurements of surface solar radiation (global radiation) at Thessaloniki, Greece

A. V. Lindfors1, N. Kouremeti2, A. Arola1, S. Kazadzis3, A. F. Bais2, and A. Laaksonen4,5 A. V. Lindfors et al.
  • 1Kuopio Unit, Finnish Meteorological Institute, Kuopio, Finland
  • 2Laboratory of Atmospheric Physics, Aristotle University of Thessaloniki, Thessaloniki, Greece
  • 3National Observatory of Athens, Athens, Greece
  • 4Climate Change Unit, Finnish Meteorological Institute, Helsinki, Finland
  • 5Department of Applied Physics, University of Eastern Finland, Kuopio, Finland

Abstract. Pyranometer measurements of the solar surface radiation (SSR) are available at many locations worldwide, often as long time series covering several decades into the past. These data constitute a potential source of information on the atmospheric aerosol load. Here, we present a method for estimating the aerosol optical depth (AOD) using pyranometer measurements of the SSR together with total water vapor column information. The method, which is based on radiative transfer simulations, was developed and tested using recent data from Thessaloniki, Greece. The effective AOD calculated using this method was found to agree well with co-located AERONET measurements, exhibiting a correlation coefficient of 0.9 with 2/3 of the data found within ±20% or ±0.05 of the AERONET AOD. This is similar to the performance of current satellite aerosol methods. Differences in the AOD as compared to AERONET can be explained by variations in the aerosol properties of the atmosphere that are not accounted for in the idealized settings used in the radiative transfer simulations, such as variations in the single scattering albedo and Ångström exponent. Furthermore, the method is sensitive to calibration offsets between the radiative transfer simulations and the pyranometer SSR. The method provides an opportunity of extending our knowledge of the atmospheric aerosol load to locations and times not covered by dedicated aerosol measurements.

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