Snowmelt runoff in the Knob Lake basin at Schefferville, Quebec, passes through a complex drainage system composed of rough snow-covered slopes and a chain of lakes connected by poorly developed snow- and icefilled channels. This study examines the hydrographs of inflow, outflow, and storage for this complex system and identifies the roles of each of the above elements in the snowmelt
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FitzGibbon et al. (1981) studied this question.
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