1Finnish Geospatial Research Institute (FGI), Geodeetinrinne 2, Masala, Finland
2Department of Physics, University of Helsinki, P.O. Box 64, Helsinki, Finland
3Finnish Meteorological Institute, P.O. Box 503, Helsinki, Finland
4Finnish Meteorological Institute Arctic Research Centre, Tähteläntie 62, Sodankylä, Finland
5Agricultural University of Iceland, Faculty of Environmental Sciences, Hvanneyri, Iceland
6University of Iceland, Faculty of Physical Sciences and Faculty of Earth Sciences, Reykjavik, Iceland
7Czech University of Life Sciences Prague, Faculty of Environmental Sciences, Department of Ecology, Prague, Czech Republic
8Ural Federal University, Institute of Physics and Technology, Ekaterinburg, Russia
9Department of Environmental Science, University of Helsinki, Helsinki, Finland
Received: 24 Apr 2015 – Discussion started: 03 Jun 2015
Abstract. In order to quantify the effects of absorbing contaminants on snow, a series of spectral reflectance measurements were conducted. Chimney soot, volcanic sand, and glaciogenic silt were deposited on a natural snow surface in a controlled way as a part of the Soot on Snow (SoS) campaign. The bidirectional reflectance factors of these soiled surfaces and untouched snow were measured using the Finnish Geodetic Institute's Field Goniospectropolariradiometer, FIGIFIGO.
Revised: 26 Oct 2015 – Accepted: 16 Nov 2015 – Published: 11 Dec 2015
A remarkable feature is the fact that the absorbing contaminants on snow enhanced the metamorphism of snow under strong sunlight in our experiments. Immediately after deposition, the contaminated snow surface appeared darker than the natural snow in all viewing directions, but the absorbing particles sank deep into the snow in minutes. The nadir measurement remained the darkest, but at larger zenith angles, the surface of the contaminated snow changed back to almost as white as clean snow. Thus, for a ground observer the darkening caused by impurities can be completely invisible, overestimating the albedo, but a nadir-observing satellite sees the darkest points, underestimating the albedo. Through a reciprocity argument, we predict that at noon, the albedo perturbation should be lower than in the morning or afternoon. When sunlight stimulates sinking more than melting, the albedo should be higher in the afternoon than in the morning, and vice versa when melting dominates. However, differences in the hydrophobic properties, porosity, clumping, or size of the impurities may cause different results than observed in these measurements.
Peltoniemi, J. I., Gritsevich, M., Hakala, T., Dagsson-Waldhauserová, P., Arnalds, Ó., Anttila, K., Hannula, H.-R., Kivekäs, N., Lihavainen, H., Meinander, O., Svensson, J., Virkkula, A., and de Leeuw, G.: Soot on Snow experiment: bidirectional reflectance factor measurements of contaminated snow, The Cryosphere, 9, 2323-2337, doi:10.5194/tc-9-2323-2015, 2015.