
Yearly fluctuations in groundwater levels are normal, but the end of summer in drier years can lead to concerns about reduced well yields.
Groundwater levels tend to be highest during March and April because of winter snowmelt and spring rainfall. The movement of rain and snowmelt into groundwater is known as groundwater recharge. Groundwater levels usually begin to fall in May and continue to decline during the summer.
The natural fluctuation of groundwater levels tends to be most pronounced in shallow wells. As a result, shallow wells are usually more susceptible to drought than deeper wells. Shallow, hand-dug wells, for example, are often the first wells to dry up during drought. Although deeper wells may be slower to suffer from drought conditions, they may also take longer to recover after a drought has occurred.
If you are concerned about dry conditions affecting your well, some changes in habits can help reduce your water use. Not watering lawns or washing cars, only doing full loads of laundry, and taking shorter showers can all add up to conserve water.
Some counties in PA are currently under a drought watch for some conditions. To help citizens monitor conditions, the U.S. Geological Survey (USGS) provides a simple website that compiles the various drought measurements (precipitation, surface water, groundwater, and the Palmer Drought Index) into one county-based graphic at the USGS website. The circular graphic in each county provides more information about the current status of drought indicators in that county.
For more information on managing your well during drought conditions, visit Managing your well during drought

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