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SOURIS RIVER

River Levels • Streamflow • Hydrology

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Total streamflow across the Souris River was last observed at 123 cfs, and is expected to yield approximately 244 acre-ft of water today; about 52% of normal. River levels are low and may signify a drought. Average streamflow for this time of year is 238 cfs, with recent peaks last observed on 2011-06-29 when daily discharge volume was observed at 125,600 cfs.

Maximum discharge along the river is currently at the Souris River Nr Westhope reporting a streamflow rate of 44.1 cfs. This is also the highest stage along the Souris River, with a gauge stage of 6.07 ft at this location. This river is monitored from 6 different streamgauging stations along the Souris River, the highest being situated at an altitude of 1,615 ft, the Souris River Nr Sherwood.

The Souris River is a 700-mile-long river that flows through Saskatchewan, North Dakota, and Manitoba. The river is named after the French word for mouse because of its winding path. The river has a long history of being used for transportation, fishing, and farming, but it also causes occasional flooding. The Souris River Basin is home to several reservoirs, including Lake Darling and Lake Darling Dam in North Dakota, which were constructed to manage water levels and prevent flooding. These reservoirs provide recreational opportunities, such as fishing and boating, and also support agricultural irrigation. The Souris River is an important water source for the region and is managed by various government agencies to balance the needs of agriculture, recreation, and flood control.

November 21, 2024

Last Updated	2024-11-20
Discharge Volume	244 ACRE-FT
Streamflow	123.02 cfs +3.48 cfs (+2.91%)
Percent of Normal	51.74%
Maximum	125,600.0 cfs 2011-06-29
Seasonal Avg	238 cfs

History of the River

The Souris River (French: rivière Souris) or Mouse River (as it is alternatively known in the U.S., a direct translation from its French name) is a river in central North America. It is about 700 km (435 mi) in length and drains about 23,600 square miles (61,100 km2). It rises in the Yellow Grass Marshes north of Weyburn, Saskatchewan. It wanders south through North Dakota beyond Minot to its most southern point at the city of Velva, and then back north into Manitoba. The river passes through the communities of Melita, Hartney, Souris and Wawanesa and on to its confluence with the Assiniboine River at Treesbank, about 25 miles (40 km) south east of Brandon. The main tributaries which flow into the Souris in Manitoba are the Antler River, the Gainsborough and Plum Creeks. Much of its drainage basin is fertile silt and clay deposited by former glacial Lake Souris.
The channel capacity of the river in Manitoba varies from about 150 cubic feet per second (4.2 m3/s) near the border, to about 1,400 cubic feet per second (40 m3/s) through Melita, to about 1,100 cubic feet per second (31 m3/s) near Lauder and 1,700 cubic feet per second (48 m3/s) near Hartney. North of Hartney the capacity increases to more than 3,000 cubic feet per second (85 m3/s). The drop between the border and Hartney is only about 6 inches per mile (9.5 cm/km).
During the period from 1930 to 1941 severe drought conditions prevailed and PFRA constructed four stock watering dams. In 1937 the Snyder and Ross Dams were built near Melita. In 1938 the Napinka Dam was built and the Hartney Dam was built in 1941. These were all stop log dams with a total capacity of 2,400 acre feet (3,000,000 m3). The Souris Dam was originally built in 1911 and was rebuilt in 1935. The Wawanesa Dam was completed in 1951 storing about 320 acre feet (390,000 m3) of water.
Most of the annual flow of the Souris River comes from snow melt and spring rains. The annual flow volume varies dramatically from 3,400 acre feet (4,200,000 m3) in 1937 to 2,100,000 acre feet (2.59 km3) in 1976. It is expected that the total runoff for 2011 at Wawanesa will exceed 3,800,000 acre feet (4.69 km3) about a one in 500 year event. The average annual runoff is equivalent to 3 mm over the entire Souris River watershed.Two large dams in Saskatchewan, Rafferty Dam and Alameda Dam were built, in part, to reduce flood peaks on the Souris River.
In summer 2011, a historic flood affected much of the Souris River basin, overtopping levees and causing the evacuation of about 11,000 residents in Minot as well as significant damage to farmland and other property along the length of the river.