USGS Groundwater Information
Groundwater Resources Program
New & Noteworthy
Press Release: High Plains Aquifer Groundwater Levels Continue to Decline
USGS Groundwater Watch
USGS maintains a network of active wells to provide basic statistics about groundwater levels.
Other Water Topics
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USGS Water Science Centers are located in each state.
Water-Table Fluctuation (WTF) Method
Estimating the Water-Level Rise (DH(tj))
The water-level rise DH(tj) is estimated as the difference between the peak of a water-level rise and the value of the extrapolated antecedent recession curve at the time of the peak. The recession curve is the trace that the well hydrograph would have followed had there not been any recharge. Extrapolation of the recession curve is not always straightforward.
At least two approaches can be used to estimate DH(tj) in the WTF method: graphical extrapolation and calculation from a master recession curve (MRC). A third approach used to estimate DH(tj), made on the basis of the computer code from the RISE program (A. Rutledge, U.S. Geological Survey, written commun., 2005), does not extrapolate for continuation of a hypothetical recession while the water table is rising. Because of the need for daily water-level data, the MRC and RISE approaches can be applied only at sites where water levels were continuously monitored.