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MOTIVATION
River Flooding

In the last several years, there have been numerous flooding events in the North Fish Creek basin. More intense rainfall events associated with climate change and land use changes had contributed to  more frequent flooding. These floods have caused damage to roads, property, and have threatened public safety and livelihoods.

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In marine environments, it is known that sea level fluctuations and tides influence estuary staging and flooding events (Eliot 2012). This relationship can be applied to Chequamegon Bay and one of its estuaries, North Fish Creek.

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June 2018 Storms

On June 29 and 30, 2018, ​complex convective storms hit Chequamegon Bay and the North Fish Creek basin. The storms produced flooding in North Fish Creek but also water level oscillations in the Bay. These water level oscillations were recorded at the Ashland Breakwater Lighthouse in the Bay. The storms produced water level oscillations of about 1 meter with a period of about 3 hours. The recorded data from these storm events will be used to study the influence of water level oscillations in the Bay on upstream flooding in the North Fish Creek basin.

Disclaimer

The research results published on this website are the Final Project for the course, CEE 411 Open Channel Hydraulics, at the University of Wisconsin–Madison. Access to the works and information contained herein is provided for public information with the understanding that the UW Department of Civil Engineering makes no warranties, either express or implied, concerning the accuracy, completeness, reliability, or suitability of the information. Any results do not imply any endorsement of or responsibility for the opinions, ideas, data, or products presented, or guarantee the validity of the information provided.​

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