In mountain snow basins, a change in climate will likely cause a chang
e 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 ca
n be used to generate snow covered area data in a new climate for inpu
t to runoff models such as the Snowmelt-Runoff Model (SRM). Second, it
could potentially be used to provide input to climate models that req
uire knowledge of the land area covered by snow at a given time. A com
puter program is now operational for use on real basins and is demonst
rated on the Rio Grande basin in Colorado and the Illecillewaet River
basin in British Columbia.