Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/35071
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Título : Snow cover response to climate change in a high alpine and half-glacierized basin in Switzerland
Autor : Magnusson, Jan, Jonas, Tobias, López-Moreno, Juan I., Lehning, Michael
Palabras clave : Glacier
Global warming
Modelling
Snow cover
Snow hydrology
Fecha de publicación : 2010
Editor: IWA Publishing
Resumen: In alpine areas, the accumulation and melting of snow controls the hydrological regime. Even in watersheds where glacier melt dominates, the snow pack strongly influences the stream-flow dynamics. Prognostic simulations of the response of the snow pack to climate change were conducted in a high alpine and half-glacierized basin in central Switzerland. The snow cover and glacier were simulated using a high-resolution alpine surface model. The simulations cover a reference period (1981–2007) and two predictions (2071–2100) where the measured records of temperature, precipitation and longwave radiation were modified using six regional climate model projections for two different emission scenarios of greenhouse gases. The results show that the snow season shortens by one month at the beginning of the winter and by one and a half months at the end of the season, compared to today. The maximum snow water equivalent decreases by 27% on average. The difference in the response of the snow pack to a change in climate between the emission scenarios is rather small. The most pronounced effects of a warming climate are simulated for the highest altitudes, where all snow completely melts during summer and no snow remains for glacier accumulation.
Descripción : 11 páginas.
Versión del editor: http://dx.doi.org/10.2166/nh.2010.115
URI : http://hdl.handle.net/10261/35071
ISSN: 0029-1277
DOI: 10.2166/nh.2010.115
Citación : Hydrology Research 41(3-4): 230-240 (2010)
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