Atmos. Chem. Phys. Discuss., 8, 4155-4198, 2008
www.atmos-chem-phys-discuss.net/8/4155/2008/
doi:10.5194/acpd-8-4155-2008
© Author(s) 2008. This work is distributed
under the Creative Commons Attribution 3.0 License.
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This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
UV albedo of arctic snow in spring
O. Meinander1, A. Kontu1, K. Lakkala1, A. Heikkilä1, L. Ylianttila2, and M. Toikka3
1Finnish Meteorological Institute, P.O. BOX 503, 00101 Helsinki, Finland
2Radiation and Nuclear Safety Authority, P.O. Box 14, 00881, Helsinki, Finland
3Toikka Engineering Ltd., Hannuntie 18, 02360 Espoo, Finland

Abstract. The relevance of snow for climate studies is based on its physical properties, such as high surface reflectivity. Surface ultraviolet (UV) albedo is an essential parameter for various applications based on radiative transfer modeling. Here, new continuous measurements of the local UV albedo of natural Arctic snow were made at Sodankylä (67.37° N, 26.63° E, 179 m a.s.l.) during the spring of 2007. The data were logged at 1-min intervals. The accumulation of snow was up to 68 cm. The surface layer thickness varied from 0.5 to 35 cm with the snow grain size between 0.2 and 2.5 mm. The midday erythemally weighted UV albedo ranged from 0.6 to 0.8 in the accumulation period and 0.5–0.7 during melting. During the snow melt period, under cases of an almost clear sky and variable cloudiness, an unexpected diurnal decrease of 0.05 in albedo soon after midday, and recovery thereafter, was detected. This diurnal decrease in albedo was found to be asymmetric with respect to solar midday, thus indicating a change in the properties of the snow. Independent UV albedo results with two different types of instruments confirm these findings. The measured temperature of the snow surface was below 0°C on the following mornings. Hence, the reversible diurnal change, evident for ~1–2 h, could be explained by the daily metamorphosis of the surface of the snowpack, in which the temperature of the surface increases, melting some of the snow to liquid water, after which the surface freezes again.

Citation: Meinander, O., Kontu, A., Lakkala, K., Heikkilä, A., Ylianttila, L., and Toikka, M.: UV albedo of arctic snow in spring, Atmos. Chem. Phys. Discuss., 8, 4155-4198, doi:10.5194/acpd-8-4155-2008, 2008.
 
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