2011 spring flooding, which altered the hydrology of many of our rivers and-2025

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The Actors Like most rivers fed by mountain snow, the Missouri experiences a surge every spring. So why was the 2011 spring flood so extreme? The lead actors were cold temperatures and heavy snowfall throughout the winter, followed by heavy rains during late spring.
The primary meteorological factors that led to the historic Mississippi River Flood of 2011 included above-normal snowfall over the Upper Mississippi Valley, elevated river levels from heavy rain events from February to April, and a very heavy rain event the end of April/beginning of May.
Rainfall Meteorology in South East Queensland During 8th to 12th January 2011. The flooding in southeast Queensland during the second week of January was caused by the interaction of a low-pressure system situated off the mid and south Queensland coasts, and upper level and monsoonal troughs [13].
ing to the National Weather Service, in the second half of the month of May 2011, almost a years 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.
When the snow that has accumulated over the winter begins to melt, it can create a significant amount of runoff that can overwhelm rivers and streams.
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In 2011, heavy winters and an extremely wet April in the upper Midwest with 600% more rain than normal in some southern states, turned the spring of 2011 into the spring of floods along the Mississippi River. The Mighty Mississippi reached a crest of 48.03 feet―14 feet past flood stage―on May 10.
The Great Flood of 1844 yielded the biggest water discharge in recorded history of the Missouri River and Upper Mississippi River in North America. The adjusted economic impact was not as great as subsequent floods because of the small population in the region at the time.

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