Articles | Volume 10, issue 1
The Cryosphere, 10, 329–339, 2016
The Cryosphere, 10, 329–339, 2016

Research article 10 Feb 2016

Research article | 10 Feb 2016

Snow and albedo climate change impacts across the United States Northern Great Plains

S. R. Fassnacht et al.

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Cited articles

Arola, A., Kaurola, J., Koskinen, L., Tanskanen, A., Tikkanen, T., Taalas, P., Herman, J. R., Krotkov, N., and Fioletov, V.: A new approach to estimating the albedo for snow-covered surfaces in the satellite UV method, J. Geophys. Res., 108, 4531,, 2003
Boon, S.: Snow ablation energy balance in a dead forest stand, Hydrol. Process., 23, 2600–2610, 2009.
Brown, R., Bartlett, P., MacKay, M., and Verseghy, D.: Evaluation of snowcover in CLASS for SnowMIP, Atmos. Ocean, 44, 223–238, 2006.
Brown, R. D. and Mote, P.: The response of Northern Hemisphere snow cover to a changing climate, J. Climate, 22, 2124–2145, 2009.
Brown, R. D. and Robinson, D. A.: Northern Hemisphere spring snow cover variability and change over 1922–2010 including an assessment of uncertainty, The Cryosphere, 5, 219–229,, 2011.
Short summary
We used 60 years of daily meteorological data from 20 stations across the US Northern Great Plains to examine climate trends, focusing on the winter climate. Besides standard climate trends, we computed trends in snowfall amounts, days with precipitation, days with snow, and modelled winter albedo (surface reflectivity). Daily minimum temperatures and days with precipitation increased at most locations, while winter albedo decreased at many stations. There was much spatial variability.