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Impact of an Extreme Flood Event on Streambank Retreat: Cedar River, Nebraska, USA
Author(s) -
Dave Naisargi,
Mittelstet Aaron,
Korus Jesse,
Waszgis Michele
Publication year - 2020
Publication title -
jawra journal of the american water resources association
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.957
H-Index - 105
eISSN - 1752-1688
pISSN - 1093-474X
DOI - 10.1111/1752-1688.12828
Subject(s) - flood myth , riparian zone , hydrology (agriculture) , erosion , environmental science , bank erosion , physical geography , geology , geography , geomorphology , ecology , archaeology , geotechnical engineering , habitat , biology
The 2010 dam breach and consequent anomalous flood event on the Cedar River in Nebraska, USA provided an opportunity to study the following objectives: (1) evaluate the impact of an extreme flood event on streambank retreat along a 45 km stretch relative to the average annual retreat; (2) quantify the changes in streambank retreat for each km segment downstream of the breach; and (3) examine the influence of riparian vegetation and radius of curvature on meander bank erosion rate. During the hydrologic event, discharge peaked at nearly three times greater than the next highest recorded rate and equated to a return period of 2,000 years. Aerial images and ArcGIS were utilized to calculate the average annual streambank retreat for each year during the preflood (2006–2010), flood (2010), and postflood (2010–2016) periods. The 2010 flood period had a significantly higher average annual streambank retreat of 2,820 m 2 /km/yr than the preflood and postflood periods, which, respectively, measured 576 and 384 m 2 /km/yr. From 2006 to 2016, 29% of all streambank erosion was from this one extreme flood event, thus demonstrating the impact that one extreme flood event can have on streambank retreat and the geomorphology of a stream system.