This study is concerned with the water cycle of the Mackenzie River Basin o
f northwestern Canada. The analysis of water vapour, clouds, precipitation,
snow cover, discharge and temperature shows that the region is subject to
substantial interannual variability and strong seasonal cycles. A number of
processes unique to cold climate regions, such as the impacts of various p
recipitation types, affect the water cycle of the basin. As well, this basi
n is experiencing a strong warming trend that is linked with an enhancement
of some water variables, and an apparent reduction in atmospheric recyclin
g. The Mackenzie Basin also exhibits some overall characteristics which dif
fer from other high latitude regions due to its unique geography.