The 2011 Souris/Mouse River flood in Canada and the United States occurred in June and was greater than a hundred-year flooding event for the river. [1] [2] The US Army Corps of Engineers estimated the flood to have a recurrence interval of two to five centuries. [3]
The Souris River begins in southeastern Saskatchewan, flows southeast into North Dakota, then to southwestern Manitoba. It is a tributary of the Assiniboine River, which it meets near Treesbank, Manitoba, and flows east to meet the Red River of the North in Winnipeg.
The flooding affected Saskatchewan and North Dakota; notably in Minot, where it overtopped levees and caused the evacuation of about 11,000 residents. The flooding in Minot was worse than the 1969 and 1881 floods; many other towns along the river were affected and many acres of farmland were inundated.
Flooding in Saskatchewan the previous summer, [4] in addition to heavy snowfall and a thick snowpack from the previous La Niña winter added to overflow on rivers across North America. In May 2011, heavy rains and thunderstorms driven by a series of cut off lows migrating westward triggered more flooding on watersheds in the southern Prairie Provinces, as some communities received nearly the annual rainfall in less than two months.
In early May, flash flooding occurred between the Souris River source and the Assiniboine River, as Kingsley No. 124, Saskatchewan saw its worst flooding in over 50 years. [5] Towards late May, barely half Saskatchewan's agricultural crops had been seeded, while southeastern Saskatchewan, surrounding the Souris River was the worst-hit. [6] However, even as the flooding continued in northern Saskatchewan, Alberta, and the Northwest Territories, significant fires burned while the weather remained dry and lightning was able to spark new blazes. [7]
On June 17, Weyburn, Saskatchewan became one of 19 provincial communities to declare a state of emergency from the severe flooding, after a power outage caused the failure of the city's waste treatment plant; Saskatoon, surrounding the South Saskatchewan River, also experienced street-level floods. [8] The next day, more flash flooding resulted in flooded homes and basements from Regina to Weyburn, while Estevan declared a state of emergency from flooding. [9]
By June 19, a dike breach flooded the village of Roche Percee, Saskatchewan, forcing about 150 residents to evacuate. [10] A trailer park in downstream Estevan also evacuated about 400 people. [11] [12] Several major highways, including part of Highway 47, Saskatchewan Highway 56, and the Trans-Canada Highway near Sintaluta were closed due to flooding damage. [13]
By June 21, Estevan had recorded 324 mm (12.8 in) of rain since May 1, making it the wettest two-month May–June period on record, while the average annual rainfall in Estevan is 333 mm (13.1 in). Water was released from two area dams to ease the pressure on the local reservoirs. At the start of summer, the flood crest moved downstream into the United States.
This article needs to be updated.(August 2011) |
Forecasters and hydrologists anticipated a full dike breach on the Souris by June 25 or 26 after the river began overtopping it on June 22. Close to 12,000 residents were evacuated from their homes. [14] [15]
The flood was expected to exceed the 1969 levels, while residents seek relief in evacuation shelters nearby. [16] [17] [18]
On June 24, the Souris River exceeded record flood levels at Minot. By June 26, all hydrographs on the Souris from the North Dakota side had recorded record-breaking flood levels, with the exception of Lake Darling, which was less than 0.2 ft (6 cm) from record stage.
Manitoba officials began preparing for the third time in 2011 for Souris flooding in late June as communities were expecting record flooding, [19] after already experiencing flooding on the Red River and the Assiniboine River, which amounted to a 300-year flood. Also lake levels at Lake Manitoba will continue to be high or may even rise more due to the high flows on the Souris River that flows into the Assiniboine east of Brandon near Treesbank. The province has stated that the flood protection and the Portage Diversion will be pushed to their limits again.
At least 85 families were evacuated from Souris, Manitoba by June 27. On July 2, the army from CFB Shilo was sent in to help with the sandbagging and building up of dykes. The river crested at Melita on July 4, at Souris on July 5 and Wawanesa on July 6. With dry weather the peak levels were a little lower than forecast and the dikes held. See the record from Manitoba Water Stewardship's daily flood report for July 7.
A levee, dike, dyke, embankment, floodbank, or stop bank is a structure that is usually earthen and that often runs parallel to the course of a river in its floodplain or along low-lying coastlines.
Minot is a city in and the county seat of Ward County, North Dakota, United States, in the state's north-central region. It is most widely known for the Air Force base approximately 15 miles (24 km) north of the city. With a population of 48,377 at the 2020 census, Minot is the state's fourth-most populous city and a trading center for a large part of northern North Dakota, southwestern Manitoba, and southeastern Saskatchewan. Founded in 1886 during the construction of James J. Hill's Great Northern Railway, Minot is also known as "Magic City", commemorating its remarkable growth in size over a short time.
Lake Agassiz was a large proglacial lake that existed in central North America during late Pleistocene, fed by meltwater from the retreating Laurentide Ice Sheet at the end of the last glacial period. At its peak, the lake's area was larger than all of the modern Great Lakes combined.
The Red River is a river in the north-central United States and central Canada. Originating at the confluence of the Bois de Sioux and Otter Tail rivers between the U.S. states of Minnesota and North Dakota, it flows northward through the Red River Valley, forming most of the border of Minnesota and North Dakota and continuing into Manitoba. It empties into Lake Winnipeg, whose waters join the Nelson River and ultimately flow into Hudson Bay.
Weyburn is the tenth-largest city in Saskatchewan, Canada. The city has a population of 11,019. It is on the Souris River 110 kilometres (68 mi) southeast of the provincial capital of Regina and is 70 kilometres (43 mi) north from the North Dakota border in the United States. The name is reputedly a corruption of the Scottish "wee burn," referring to a small creek. The city is surrounded by the Rural Municipality of Weyburn No. 67.
The Assiniboine River is a 1,070-kilometre (660 mi) river that runs through the prairies of Western Canada in Saskatchewan and Manitoba. It is a tributary of the Red River. The Assiniboine is a typical meandering river with a single main channel embanked within a flat, shallow valley in some places and a steep valley in others. Its main tributaries are the Qu'Appelle, Souris, and Whitesand Rivers. For early history and exploration see Assiniboine River fur trade.
The Red River flood of 1997 was a major flood that occurred in April and May 1997 along the Red River of the North in Minnesota, North Dakota, and southern Manitoba. It was the most severe flood of the river since 1826. The flood reached throughout the Red River Valley, affecting the cities of Fargo and Winnipeg, but none so greatly as Grand Forks and East Grand Forks, where floodwaters reached more than 3 miles (4.8 km) inland. They inundated virtually everything in the twin communities. Total damages for the Red River region were US$3.5 billion. The flood was the result of abundant snowfall and extreme temperatures.
The Souris River or Mouse River is a river in central North America. Approximately 435 miles (700 km) in length, it drains about 23,600 square miles (61,100 km2) in Canada and the United States.
Souris is an unincorporated urban community in the Municipality of Souris – Glenwood within the Canadian province of Manitoba that held town status prior to January 1, 2015. It is located within the municipality at the confluence of Plum Creek and Souris River, from which it takes its name. Before 1882, the town was called Plum Creek. The community is home to Canada's longest historic cable-stayed footbridge at 177 metres (581 ft) long, known as the Swinging Bridge, which spans the Souris River that divides the community. The Swinging Bridge was built in 1904 as a means of transportation over the Souris River, later floods destroyed the original swinging bridge and in 2013 a modern cable bridge was installed. Residents of Souris are referred to as Sourisites.
A levee breach or levee failure is a situation where a levee fails or is intentionally breached, causing the previously contained water to flood the land behind the levee.
Gainsborough is a village in the Canadian province of Saskatchewan within the Rural Municipality of Argyle No. 1 and Census Division No. 1. A farming community, the village is located on Highway 18 in the southeastern corner of Saskatchewan. Gainsborough is approximately 6 km (3.7 mi) from the Manitoba border, and 19 km (12 mi) from the North Dakota, United States border. The first post office was established on April 1, 1884 as the community of Antler. On September 1, 1885 the name of the community changed to Gainsborough, after Gainsborough, Lincolnshire in England, which was the former home of J. J. Sadler, an early settler.
Highway 39 is a provincial, paved, highway in the southern portion of the Canadian province of Saskatchewan connecting North Portal and Moose Jaw in the north. This is a primary Saskatchewan highway maintained by the provincial and national governments and providing a major trucking and tourism route between the United States via Portal, Burke County, North Dakota, and North Portal, Saskatchewan. On July 3, 2000, Highways and Transportation Minister Maynard Sonntag officiated at the ribbon cutting ceremony opening the new duty-free shop and the twinned highway at Saskatchewan's busiest border crossing. Highway 39 is one of Canada's busiest highways, facilitating transport for $6 billion in trade goods via approximately 100,000 trucks over the year. The entire length of highway 39 is paved. The CanAm Highway comprises Saskatchewan Highways Hwy 35, Hwy 39, Hwy 6, Hwy 3, as well as Hwy 2. 44.3 miles (71.3 km) of Saskatchewan Highway 39 contribute to the CanAm Highway between Weyburn and Corinne. Highway 39 is divided or twinned in two areas at North Portal as well as north of Weyburn for 1.7 kilometres (1.1 mi). The junction of Hwy 39 with the Trans–Canada divided four-lane highway is done via a "Parclo" or partial cloverleaf interchange.
The 2009 Red River flood along the Red River of the North in North Dakota and Minnesota in the United States and Manitoba in Canada brought record flood levels to the Fargo-Moorhead area. The flood was a result of saturated and frozen ground, spring snowmelt exacerbated by additional rain and snow storms, and virtually flat terrain. Communities along the Red River prepared for more than a week as the U.S. National Weather Service continuously updated the predictions for the city of Fargo, North Dakota, with an increasingly higher projected river crest. Originally predicted to reach a level of near 43 feet (13 m) at Fargo by March 29, the river in fact crested at 40.84 feet (12.45 m) at 12:15 a.m. March 28, and started a slow decline. The river continued to rise to the north as the crest moved downstream.
The US State of North Dakota experienced significant flooding in its major river basins in 2009, following abnormally heavy winter snows atop saturated and frozen ground.
Roche Percee is a village in the Canadian province of Saskatchewan within the Rural Municipality of Coalfields No. 4 and Census Division No. 1. The village is near the Canada–United States border just off of Highway 39. Roche Percee is 20 km (12 mi) east of Estevan in the valley of the Souris River.
The 2011 Red River flood took place along the Red River of the North in Manitoba in Canada and North Dakota and Minnesota in the United States beginning in April 2011. The flood was, in part, due to high moisture levels in the soil from the previous year, which meant that further accumulation would threaten the flood-prone region. Flood predictors in Winnipeg were worried that a dual crest of both the Assiniboine River and the Red might crest at the city at the same time. Beginning around April 8, 50 homes were evacuated and two more were flooded after an ice jam in St. Andrews, Manitoba caused the river to flood over its banks.
The 2011 Assiniboine River flood was caused by above average precipitation in Western Manitoba and Saskatchewan. This was a 1 in 300 year flood that affected much of Western Manitoba. The flooding in Manitoba was expected to mostly involve the 2011 Red River Flood but instead the more severe flooding was found on the Assiniboine in the west.
The 2011 flooding event on the Missouri River in the United States was triggered by record snowfall in Rocky Mountains of Montana and Wyoming along with near-record spring rainfall in central and eastern Montana. All six major dams along the Missouri River released record amounts of water to prevent overflow which led to flooding threatening several towns and cities along the river from Montana to Missouri; in particular Bismarck, North Dakota; Pierre, South Dakota; Dakota Dunes, South Dakota; South Sioux City, Nebraska, Sioux City, Iowa; Omaha, Nebraska; Council Bluffs, Iowa; Saint Joseph, Missouri; Kansas City, Missouri; Jefferson City, Missouri, and St. Louis, Missouri. Many smaller towns were also at risk, suffering the same fate as the larger cities if not worse. According to the National Weather Service, in the second half of the month of May 2011, almost a year's worth of rain fell over the upper Missouri River basin. Extremely heavy rainfall in conjunction with an estimated 212 percent of normal snowpack in the Rocky Mountains contributed to this flooding event.
Downtown Minot is the central business district of Minot, North Dakota, located south of the Souris River in the Souris Valley. Downtown is the site of the first permanent settlement in Minot in 1886. Downtown is home to many of Minot's cultural sites of interest. It is also home to numerous galleries, stores and restaurants. The Minot Riverwalk traverses the downtown.
The 2014 Assiniboine River flood was caused by above average precipitation in western Manitoba and Saskatchewan. Unlike most prior floods, this flood was not due to spring runoff, but rather significant rainfall. Flooding and high water involved both the main stem of the Assiniboine River and many of its tributaries including the Qu'Appelle River and the Souris River. The flood came just 3 years after the 2011 Assiniboine River Flood which was considered a 1 in 300 year event. Peak flows along the river for the first crest were generally slightly less than in 2011. However, the second peak on the river has exceeded 2011 levels starting near St. Lazare, Manitoba up to Brandon, Manitoba so far.