USGS - science for a changing world

USGS Groundwater Information

*  Home *  Data & Information *  Publications *  Methods & Modeling *  Selected Topics *  Programs *  Contact Us

New & Noteworthy

Press Releases RSS

USGS in Your State

USGS Water Science Centers are located in each state.

 [Map: There is a USGS Water Science Center office in each State.] Washington Oregon California Idaho Nevada Montana Wyoming Utah Colorado Arizona New Mexico North Dakota South Dakota Nebraska Kansas Oklahoma Texas Minnesota Iowa Missouri Arkansas Louisiana Wisconsin Illinois Mississippi Michigan Indiana Ohio Kentucky Tennessee Alabama Pennsylvania West Virginia Georgia Florida Caribbean Alaska Hawaii and Pacific Islands New York Vermont New Hampshire Maine Massachusetts South Carolina North Carolina Rhode Island Virginia Connecticut New Jersey Maryland-Delaware-D.C.

Other USGS Water Science Areas


Groundwater and Drought

Groundwater is among the Nation's most important natural resources. It provides half our drinking water and is essential to the vitality of agriculture and industry, as well as to the health of rivers, wetlands, and estuaries throughout the country. Droughts can significantly impact the Nation's groundwater resources while the drought is occurring and for some time afterward. Understanding groundwater, surface water, and the integrated nature of the hydrologic system enables resource managers and policy makers to better prepare for and respond to drought. The USGS provides groundwater data and information that resource managers and policy makers can use to prepare for and respond to drought.

Learn more:

What is Drought?

 [Photo: Pool and dry river bed]

Sample graph of daily groundwater level data. Daily groundwater levels (bottom line) for the period shown are below the historical daily median (top line). (View the latest statistics for this well.)

A drought is a period of drier-than-normal conditions that results in water-related problems. When rainfall is less than normal for several weeks, months, or years, the flow of streams and rivers declines, water levels in lakes and reservoirs fall, and the depth to water in wells increases. If dry weather persists and water-supply problems develop, the dry period can become a drought.

The term "drought" can have different meanings to different people, depending on how a water deficiency affects them. Droughts have been classified into different types such as:

  • meteorological drought - lack of precipitation
  • agricultural drought - lack of soil moisture, or
  • hydrologic drought -reduced streamflow or groundwater levels

It is not unusual for a given period of water deficiency to represent a more severe drought of one type than another type. For example, a prolonged dry period during the summer may substantially lower the yield of crops due to a shortage of soil moisture in the plant root zone but have little effect on groundwater storage replenished the previous spring.


What is a groundwater drought?

A groundwater drought typically refers to a period of decreased groundwater levels that results in water-related problems. The amount of groundwater decline that would be considered a drought varies regionally and locally due to differences in groundwater conditions and groundwater needs for humans and the environment.

How is groundwater important during drought?

Groundwater is important during all hydrologic droughts:

  • Groundwater may be an alternative or supplemental source of water during periods of surface-water drought, if sufficient groundwater resources exist.
  • Reduced groundwater levels due to drought or increased pumping during drought can result in decreased water levels and flows in lakes, streams, and other water bodies. (On average, greater than 50 percent of stream flow is contributed by groundwater. Groundwater also is a major source of water to lakes and wetlands. Source: Circular 1139, p. 12)
  • Changes in groundwater/surface-water exchange can result in changes in water quality.
  • Decreased groundwater flow to surface waters can affect aquatic ecosystems that rely on a continuous supply of groundwater to sustain aquatic habitats and stream flow.
  • Reduced heads in aquifers can result in land subsidence.

 [Photo: Pool and dry river bed]

Pool and dry river bed along the Ipswich River, Reading, Massachusetts, September 2005. Groundwater withdrawals for primarily domestic and commercial uses in the Ipswich River Basin in eastern Massachusetts have caused substantial depletions of streamflow. Credit: USGS/Photograph by David Armstrong (Source: Circular 1376)

 [Photos: reach of the Santa Cruz River south of Tucson, Arizona.]

A 1942 photograph (left photograph) of a reach of the Santa Cruz River south of Tucson, Arizona, shows stands of mesquite and cottonwood trees along the river. A replicate photograph of the same site in 1989 (right photograph) shows that the riparian trees have largely disappeared. Data from nearby wells indicate that the groundwater levels declined more than 100 feet due to pumping, and this pumping appears to be the principal reason for the decrease in vegetation. Credit: USGS/Photograph by Robert H. Webb (Source: Circular 1186)


For more background on drought:

For additional USGS background on drought, see:

USGS Home Water Climate and Land Use Change Core Science Systems Ecosystems Energy and Minerals Environmental Health Natural Hazards

Accessibility FOIA Privacy Policies and Notices

Take Pride in America logo USA.gov logo U.S. Department of the Interior | U.S. Geological Survey
URL: http://water.usgs.gov/ogw/drought/index.html
Page Contact Information: Contact the USGS Office of Groundwater
Page Last Modified: Thursday, 06-Mar-2014 16:57:30 EST