In mountain snow basins, a change in climate will likely cause a change in the basin snow cover extent. A procedure for evaluating whether a given climate change scenario will speed up or slow down the seasonal decrease of snow covered area is outlined with hypothetical examples for a simple basin. This procedure has two main purposes. First, it can be used to generate snow covered area data in a new climate for input to runoff models such as the Snowmelt-Runoff Model (SRM). Second, it could potentially be used to provide input to climate models that require knowledge of the land area covered by snow at a given time. A computer program is now operational for use on real basins and is demonstrated on the Rio Grande basin in Colorado and the Illecillewaet River basin in British Columbia.
Research Article|August 01 1994
Areal Extent of Seasonal Snow Cover in a Changed Climate
A. Rango, J. Martinec; Areal Extent of Seasonal Snow Cover in a Changed Climate. Hydrology Research 1 August 1994; 25 (4): 233–246. doi: https://doi.org/10.2166/nh.1994.0006
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