Abstract
A hydrological model applied to the Turkey Lakes Watershed at different locations produced results which agreed closely with observed stream flow, groundwater flow, snowpack, and snowpack chemistry. The model results are consistent with many of the episodic events that have occurred in the watershed. The snowpack sulphate concentration is simulated with a simple sulphate model linked to the hydrological model. The different calibrated hydrological coefficients were found to vary with the geology and geomorphology at several locations in he watershed. The general applicability of these coefficients was confirmed by comparing model results with a new set of data from subsequent years.
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