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a water withdrawal or terminate a registration.
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annual water use data.
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fees for registered water withdrawals.
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water use data and maps.
Learn
about water use in Wisconsin.
Contact information
For information on this page, contact:
Water Use Program
608-266-2299
WI Department of Natural Resources
Water Use Section DG/5
PO Box 7921
Madison WI 53707-7921

Groundwater levels and aquifer response

Monitoring groundwater levels can be used for:

  • understanding local water resources;
  • assessing aquifers in drought or wet conditions;
  • assessing groundwater divides and surface water impacts;
  • calibrating groundwater flow models and other decision-support tools; and
  • helping to determine the relationship between water resources and withdrawals.

Groundwater level monitoring

The DNR and its partners at the United States Geological Survey (USGS) and the Wisconsin Geological and Natural History Survey (WGNHS) collectively operate and maintain a statewide network of monitoring wells that provide necessary long-term data for Wisconsin's statewide water resources inventory. The groundwater monitoring network, started in 1946, now consists of 91 long-term monitoring wells that measure groundwater levels in aquifers across the state.

The DNR's water quantity data viewer shows the location and water levels associated with the statewide groundwater monitoring network.

Groundwater level fluctuations

The upper surface of groundwater, referred to as the water table, can fluctuate in response to precipitation events and water withdrawals. During times of drought, local water tables can decline due to decreased recharge and increased water use (e.g. watering lawns, irrigating farm fields, municipal water supply). The result is that the water table can fall below surface water resources or from wells that withdraw water from the aquifer (see diagram below).

The opposite can also occur, resulting in a high water table (too much groundwater). Groundwater flooding occurs when frequent, sustained rainfall leads to excessively fast recharge of local groundwater levels and the water table rises above the land surface. This type of flood may be pronounced near seepage lakes (see diagram below). This type of flood can be long-lasting because water table decline requires drainage from the entire aquifer above the flood level. For the time that it takes for this drainage to occur, flood waters can cause significant property loss, human displacement and disruption of transportation.

water level variation diagram

Water level variation diagram. Image credit: DNR.

Photo of seepage lake

Seepage lake: a natural lake fed by precipitation,
limited runoff and groundwater. It does not have
a stream outlet. Image credit: UW Stevens Point.

Seepage lakes may also experience flooding of shoreline beaches and buildings due to a rise in the water table elevation and the related long-term increase in lake levels. Floods and droughts are part of life in Wisconsin and elsewhere, but they come with significant economic, public health and environmental costs.

It may be difficult to determine if nearby flooding is due to surface water or groundwater flooding. For example, increased groundwater flow to nearby streams and rivers may cause the waterbodies to flood; or storm sewers that typically would drain to rivers don't work properly if too much inflow into the pipes from groundwater is occurring.

Over the past several years, Wisconsin has received a record-breaking amount of precipitation. The accumulation of above-average precipitation has resulted in many areas of Wisconsin experiencing high water and flooding issues. Information is available from the DNR to help residents cope with flooding.

Status of groundwater levels

Department staff track recent and historical precipitation and compare that data to long-term averages to characterize and identify trends. These precipitation patterns are compared to water level readings in monitoring wells statewide. As of June 2019, the charts below indicate that most of the state has received well above average precipitation in recent years and groundwater data reflects this trend. Groundwater levels are at or near historic highs throughout the state, which is consistent with groundwater flooding reports received by the department in recent years.

groundwater levels by region

Status of groundwater levels in each region of the state - detailed charts are available below.

View the regional charts to see the status of water levels as compared to the long-term average, as well as the relationship between precipitation and groundwater:

Note: reading the charts - probability of occurrence.

Last revised: Thursday July 25 2019