![]() The Red River drainage basin, with the Red River highlighted | |
Date | April 1 - April 24 |
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The 1897 Red River flood took place in April 1897, along the Red River resulting in significant damage to the city of Fargo, North Dakota. The conditions which led to the flood of 1897 were similar to the conditions behind the 2009 flood, however the 1897 flood was different in terms of the human response to it. [1] Although the river gauge was not installed on the Red River until 1901, other sources indicate that the crest of the 1897 flood at a site 1.5 miles (2.4 km) downstream from the present Fargo gauge would have been 40.10 ft (with a discharge rate of 25,000 ft3/s) according to the present datum. [2]
Until the 2009 flood, the 1897 flood was the highest water recorded in the Fargo-Moorhead area and has since served as the benchmark for which many other floods of the Red River were measured against.
In the spring of 1897 R.M. Probesfield took a measurement of 5 feet (1.5 m) of snow on the ground in an area which was free from drifting; a value 2 feet (0.61 m) higher than one taken prior to the 1861 flood. [2] Due to the level of measured snowfall a flood in the spring was expected.
City | Crest | Date |
---|---|---|
Wahpeton, North Dakota | 2' 8" above the 1893 high [2] | 1897-03-31 |
Fargo, North Dakota | 40.10 ft (present datum) [2] 34.2 ft (1952 datum) [2] | 1897-04-07 - Early Morning |
Grand Forks, North Dakota | Line along 3rd Street [2] Covering Demers Ave in East Grand Forks [2] | 1897-04-10 - Noon |
Fargo is a city in and the county seat of Cass County, North Dakota, United States. According to the 2020 census, its population was 125,990, making it the most populous city in the state and the 216th most populous city in the United States. Fargo, along with its twin city of Moorhead, Minnesota, and the adjacent cities of West Fargo, North Dakota and Dilworth, Minnesota, form the core of the Fargo–Moorhead, ND-MN Metropolitan Statistical Area (MSA). The MSA had a population of 248,591 in 2020.
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.
The Red River Floodway is an artificial flood control waterway in Western Canada. It is a 47 km (29 mi) long channel which, during flood periods, takes part of the Red River's flow around the city of Winnipeg, Manitoba to the east and discharges it back into the Red River below the dam at Lockport. It can carry floodwater at a rate of up to 140,000 cubic feet per second (4,000 m3/s), expanded in the 2000s from its original channel capacity of 90,000 cubic feet per second (2,500 m3/s).
The Ouachita River is a 605-mile-long (974 km) river that runs south and east through the U.S. states of Arkansas and Louisiana, joining the Tensas River to form the Black River near Jonesville, Louisiana. It is the 25th-longest river in the United States.
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 Great Flood of 1993 was a flood that occurred in the Midwestern United States, along the Mississippi and Missouri rivers and their tributaries, from April to October 1993.
The Red River Valley is a region in central North America that is drained by the Red River of the North; it is part of both Canada and the United States. Forming the border between Minnesota and North Dakota when these territories were admitted as states in the United States, this fertile valley has been important to the economies of these states and to Manitoba, Canada.
In mid-July 1951, heavy rains led to a great rise of water in the Kansas River, Missouri River, and other surrounding areas of the Central United States. Flooding occurred in the Kansas, Neosho, Marais Des Cygnes, and Verdigris river basins. The damage in June and July 1951 across eastern Kansas and Missouri exceeded $935 million. The flooding killed 17 people and displaced 518,000.
The Blanco River is a river in the Hill Country of Texas in the United States.
The Ohio River flood of 1937 took place in late January and February 1937. With damage stretching from Pittsburgh to Cairo, Illinois, 385 people died, one million people were left homeless and property losses reached $500 million. Federal and state resources were strained to aid recovery as the disaster occurred during the depths of the Great Depression and a few years after the beginning of the Dust Bowl.
Interstate 94 (I-94) runs east–west for 352.4 miles (567.1 km) through the southern half of the US state of North Dakota, from the Montana state line east to the Red River at Fargo. The route generally follows the route of the Northern Pacific Railway.
North Dakota's climate is typical of a continental climate with cold winters and warm-hot summers. The state's location in the Upper Midwest allows it to experience some of the widest variety of weather in the United States, and each of the four seasons has its own distinct characteristics. The eastern half of the state has a humid continental climate with warm to hot, somewhat humid summers and cold, windy winters, while the western half has a semi-arid climate with less precipitation and less humidity but similar temperature profiles. The areas east of the Missouri River get slightly colder winters, while those west of the stream get higher summer daytime temperatures. In general, the diurnal temperature difference is prone to be more significant in the west due to higher elevation and less humidity.
The Red River flood of 1997 in the United States was a major flood that occurred in April 1997, along the Red River of the North in North Dakota and Minnesota. The flood reached throughout the Red River Valley, affecting the cities of Fargo, Moorhead, and Winnipeg, while Grand Forks and East Grand Forks received the most damage, where floodwaters reached over 3 miles (5 km) inland, inundating virtually everything in the twin communities. Total damages for the Red River region were US$3.5 billion.
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.
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 Fargo-Moorhead Toll Bridge is a former toll bridge on the Red River of the North between Fargo, North Dakota and Moorhead, Minnesota. It connects Moorhead's 15th Avenue N with Fargo's 12th Avenue N.
The Fargo-Moorhead (FM) Area Diversion project, officially known as the Fargo-Moorhead Metropolitan Area Diversion Flood Risk Management Project, is a large, regional flood control infrastructure project on the Red River of the North, which forms the border between North Dakota and Minnesota and flows north to Lake Winnipeg in Manitoba, Canada.
In April 2013, persistent heavy rains caused widespread flooding, primarily impacting the Midwestern and Great Lakes regions. In a span of two days on April 17 and 18, heavy rainfall associated with a slow-moving storm system caused widespread flooding across rivers and areas, where rainfall amounts over 8 inches (200 mm) caused rivers to swell and crest, including the Mississippi River and the Red River, with the latter river dealing with melting ice caps. The Grand River crested to a record level, prompting water rescues and evacuations in Grand Rapids, Michigan. A local state of emergency was declared for the city of Des Plaines, Illinois after the Des Plaines river swelled to 10.92 feet (3,330 mm). The governors of Illinois and Missouri declared state of emergencies, and the Federal Emergency Management Agency declared a federal emergency and a disaster declaration for 46 counties in Illinois. Five fatalities occurred: two each in Illinois and Indiana, with a fifth in Missouri. Three others were injured, all in Illinois.