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Fluvial Systems

Floods and Flooding

stream gaugeA flood occurs when a stream channel can no longer contain the water moving through it. Floods usually are local, short-lived events, others can be catastrophic, happening with little or no warning. Floods are most often caused by prolonged rainfall that saturates the ground causing surface runoff into nearby streams increasing their discharge. Flooding occurs when the water spills out of the channel and on to the adjacent terrain. Though viewed as a "natural hazard" to humans, flooding is a natural, rejuvenating process.

Figure FS.19 Flooded USGS gage, Lamprey River near Newmarket, NH.
Courtesy USGS (Source )


Causes and Conditions

Generally speaking there are two types of floods, 1) where water slowly rises and spills over the banks of a stream or river and 2) flash floods. Floods can occur at anytime of year, but particular seasonal weather patterns are more conducive to the creation of floods than others in different geographic regions. In the United States, cyclonic storms roaring off the ocean and into the Pacific coast states during the winter and early spring can cause flooding. In the southwest, summer and fall thunderstorms release torrents of water that rush down dry stream beds or arroyos as flash floods. Flooding can occur in the north central states during the winter as rain fall or snow melt runs off the frozen ground surface, or ice jams rivers causing them to flood. Flooding in the mid portion of the United States tends to occur in spring and summer as polar front cyclones march across the North American continent. Hurricanes and large convective complexes create flooding in the late summer and fall along the Gulf coast of the United States.

flood season

Figure FS.20 Flood Season in the United States Courtesy USGS (Source )

In tropical regions like Bangla Desh, monsoon rains saturate the ground causing severe flooding.  Europe floods from the sea may occur as a result of Atlantic storms pushing water to the coast and can be particularly damaging when occurring at high tide. Deforestation greatly increases the risk for flooding.


Rochester Flood

Figure FS.21 Flooding in Rochester, MN (Source: :cjohnson7 on Flickr)

During August of 2007, widespread flooding occurred in the midwest causing damaged exceeding $115 million. A warm front advanced northward into Iowa and Illinois during mid-August where it stalled and became a stationary front. Warm, moist air overrunning the front provided the ingredients for showers and thunderstorms. Moisture from Tropical Storm Erin to the south enhanced the stormy conditions.

Some of the worst flooding in decades also occurred during the summer of 2007. The flooding in Britain was caused by a persistent jet stream sitting further south than usual during this time of the year. System after system pounded the British Isles.

Flood Frequency

100-year flood plainFigure FS.22 100- Year Flood Plain. Courtesy USGS (Source )

Using frequency analysis, one can estimate the probability of the occurrence of a given flood event  The recurrence interval, also known as the return period, is based on the probability that the100-year flood plain plan given event will be equaled or exceeded in any given year. For instance, a one hundred year flood has a 1% chance of occurring in any given year. One hundred year floods are rare but can be devastating. The 100-year flood plain is used for flood plain management and insurance purposes. Those living within this zone are often required to have flood insurance in addition to their regular home owner's insurance.

Figure FS.23 Development of flood plains increases risk of floods. Courtesy USGS (Source )

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For Citation: Ritter, Michael E. The Physical Environment: an Introduction to Physical Geography.
2006. Date visited.  http://www.uwsp.edu/geo/faculty/ritter/geog101/textbook/title_page.html

© 2003-2009
Michael Ritter (tpeauthor@mac.com)
Last revised 09/2/07