4.6 Article

Effects of climate change and high-capacity wells pumping on streamflow and groundwater elevation in Northeastern Wisconsin

Journal

ENVIRONMENTAL EARTH SCIENCES
Volume 82, Issue 6, Pages -

Publisher

SPRINGER
DOI: 10.1007/s12665-023-10818-1

Keywords

SWAT; MODFLOW; High-capacity wells; Streamflow; Climate change

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The number of high-capacity wells in Wisconsin has increased, causing concerns about their impact on groundwater levels and streamflow. This study uses simulation models to demonstrate the combined effects of climate change and groundwater withdrawal on the state's water resources. The models predict that future increases in precipitation will lead to higher groundwater recharge and streamflow, but higher temperatures will result in deficits in both streamflow and groundwater recharge, exacerbating the impacts of climate change. The study also highlights the significant decrease in groundwater levels due to climate and increased withdrawal rates from high-capacity wells.
The number of high-capacity wells has increased substantially in the state of Wisconsin, United States, and concerns have been raised about their impact on both groundwater levels and streamflow. At the same time, Wisconsin's annual precipitation and temperature have been trending upward over the last 30 years and both are predicted to increase into the middle of the twenty-first century. The study demonstrates the simultaneous effects of climate change and groundwater withdrawal from high-capacity wells by employing two simulation models: the Soil & Water Assessment Tool (SWAT) and the USGS Modular Hydrologic Model (MODFLOW). SWAT was used to simulate the change in the recharge rate, and MODFLOW was then used to simulate the change in hydraulic head. The SWAT model predicted that future increases in Wisconsin's annual precipitation (5%) will cause increases in both groundwater recharge (16.7%) and streamflow (14.1%). The future increases in temperature (approximate to 3 degrees C), however, are predicted to leave the state with a net deficit in both streamflow (- 23.4%) and groundwater recharge (- 19.6%). In addition, the MODFLOW model predicted a mean head elevation decrease of over 2 m due to changes in the climate and an additional decrease (approximate to 3 m) in groundwater elevation surrounding high-capacity wells due to predicted increases in annual withdrawal rate.

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