Articles | Volume 13, issue 7
Atmos. Chem. Phys., 13, 3793–3810, 2013

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

Atmos. Chem. Phys., 13, 3793–3810, 2013

Research article 10 Apr 2013

Research article | 10 Apr 2013

Spectral albedo of seasonal snow during intensive melt period at Sodankylä, beyond the Arctic Circle

O. Meinander1, S. Kazadzis2, A. Arola3, A. Riihelä1, P. Räisänen1, R. Kivi4, A. Kontu4, R. Kouznetsov1, M. Sofiev1, J. Svensson1, H. Suokanerva4, V. Aaltonen1, T. Manninen1, J.-L. Roujean5, and O. Hautecoeur5 O. Meinander et al.
  • 1Finnish Meteorological Institute, P.O. Box 503, 00101 Helsinki, Finland
  • 2Institute for Environmental Research and Sustainable Development, National Observatory of Athens, Greece
  • 3Finnish Meteorological Institute, Kuopio Unit, P.O. Box 1627, 70211 Kuopio, Finland
  • 4Finnish Meteorological Institute, Arctic Research Centre, Tähteläntie 62, 99600 Sodankylä, Finland
  • 5Meteo-France/Centre National de la Recherche Scientifique (CNRS), Toulouse, France

Abstract. We have measured spectral albedo, as well as ancillary parameters, of seasonal European Arctic snow at Sodankylä, Finland (67°22' N, 26°39' E). The springtime intensive melt period was observed during the Snow Reflectance Transition Experiment (SNORTEX) in April 2009. The upwelling and downwelling spectral irradiance, measured at 290–550 nm with a double monochromator spectroradiometer, revealed albedo values of ~0.5–0.7 for the ultraviolet and visible range, both under clear sky and variable cloudiness. During the most intensive snowmelt period of four days, albedo decreased from 0.65 to 0.45 at 330 nm, and from 0.72 to 0.53 at 450 nm. In the literature, the UV and VIS albedo for clean snow are ~0.97–0.99, consistent with the extremely small absorption coefficient of ice in this spectral region. Our low albedo values were supported by two independent simultaneous broadband albedo measurements, and simulated albedo data. We explain the low albedo values to be due to (i) large snow grain sizes up to ~3 mm in diameter; (ii) meltwater surrounding the grains and increasing the effective grain size; (iii) absorption caused by impurities in the snow, with concentration of elemental carbon (black carbon) in snow of 87 ppb, and organic carbon 2894 ppb, at the time of albedo measurements. The high concentrations of carbon, detected by the thermal–optical method, were due to air masses originating from the Kola Peninsula, Russia, where mining and refining industries are located.

Final-revised paper