The Brule Watershed, located in western Alberta, covers an area of approximately 5,000 km². The hydrology of the watershed is dominated by the Brule River, which flows into the Athabasca River. The watershed experiences a continental climate, with cold winters and warm summers. Snowpack accumulation in the watershed varies from year to year, with the highest snowpack typically occurring in March. Surface water in the watershed is important for both recreational activities and agriculture. Reservoirs in the watershed contain water used for hydroelectric power generation. The region experiences some interesting climatic facts, including frequent Chinook winds in winter, and occasional severe thunderstorms in the summer. Trends in the watershed include changes in snowmelt timing, with earlier melt dates being observed in recent years, and an overall drying trend in the region due to climate change.