Groundwater flood of a river terrace in southwest Wisconsin, USA

• Published in: Hydrogeology journal Vol. 22; no. 6; pp. 1421 - 1432
• Main Authors: Gotkowitz, Madeline B., Attig, John W., McDermott, Thomas
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Springer Berlin Heidelberg 01.09.2014; Springer Nature B.V
• Subjects: Aquatic Pollution; Aquifers; Climate change; Earth and Environmental Science; Earth Sciences; Economics; Emergency preparedness; Extreme weather; Flooding; Floodplains; Floods; Floodwater; Freshwater; Geology; Geomorphology; Geophysics/Geodesy; Gravel; Groundwater; Groundwater discharge; Groundwater recharge; Hydrogeology; Hydrology/Water Resources; Land use; Land use planning; Outwash; Rain; Rainstorms; Recharge; Rivers; Runoff; Surface runoff; Surface water; Terraces; Waste Water Technology; Water Management; Water Pollution Control; Water Quality/Water Pollution; Water table; USA, Wisconsin, Wisconsin R; USA, Wisconsin; USA; Rainfall/runoff; Groundwater recharge; Groundwater flood
• ISSN: 1431-2174; 1435-0157
• DOI: 10.1007/s10040-014-1129-x

Intense rainstorms in 2008 resulted in wide-spread flooding across the Midwestern United States. In Wisconsin, floodwater inundated a 17.7-km 2 area on an outwash terrace, 7.5 m above the mapped floodplain of the Wisconsin River. Surface-water runoff initiated the flooding, but results of field investigation and modeling indicate that rapid water-table rise and groundwater inundation caused the long-lasting flood far from the riparian floodplain. Local geologic and geomorphic features of the landscape lead to spatial variability in runoff and recharge to the unconfined sand and gravel aquifer, and regional hydrogeologic conditions increased groundwater discharge from the deep bedrock aquifer to the river valley. Although reports of extreme cases of groundwater flooding are uncommon, this occurrence had significant economic and social costs. Local, state and federal officials required hydrologic analysis to support emergency management and long-term flood mitigation strategies. Rapid, sustained water-table rise and the resultant flooding of this high-permeability aquifer illustrate a significant aspect of groundwater system response to an extreme precipitation event. Comprehensive land-use planning should encompass the potential for water-table rise and groundwater flooding in a variety of hydrogeologic settings, as future changes in climate may impact recharge and the water-table elevation.