News Release Reston, VA – U.S.
Geological Survey (USGS) scientists have identified nationwide trends toward
increasing streamflow in many areas of the nation since 1940 based on data
collected from long-term USGS streamgages. This conclusion and several more
interesting trends in our nation’s streamflows can be found in four new fact
sheets recently issued by the agency. ·
Of the nearly 22,700 streamgages
for which the USGS has records, 435 monitor natural basins and have records of
sufficient length to analyze climatic trends. ·
The date when half of the total
volume of streamflow for winter/spring (January 1 to May 31) now arrives earlier
than it did in the first half of the 20th century at 14 of 27 streamgages in New
England.
USGS Scientists Document Widespread Increases in
Streamflow and Changes in the Timing of Snowmelt Over the Past 50 Years
U.S. Department of the Interior
U.S Geological Survey
Release Date: May 5, 2005
Contact: A.B. Wade
703-648-4483
abwade@usgs.gov
“Understanding streamflow trends is
essential to effective management of the nation’s water supply and is critical
to developing strategies that mitigate the potential negative impacts of floods
and droughts,” said USGS Associate Director for Water Robert Hirsch.
In the first study, USGS scientists
identified a nationwide trend that streamflow has been increasing in the United
States since at least 1940. Most of the increases were during
low-and-moderate streamflows. This means that, during typically dry periods,
more water is now available in the stream.
In the second study, scientists discovered
that over the last 30 years, winter/spring streamflows occurred one to two weeks
earlier than in previous decades in northern or mountainous areas of New
England. Similarly, in the third study, scientists found that streamflows
in most western rivers occur almost one to three weeks earlier now than they did
in the middle of the 20th century.
The fourth study shows that the streamflow
of the Mississippi River was influenced by both climate and human activities
such as construction of water reservoirs, agricultural irrigation and
groundwater pumping. Streamflow of the Mississippi River increased at a rate of
4.5 percent per decade largely because of an increase in precipitation.
The USGS has been measuring and recording
streamflow in the United States since the late 1800’s. Today, the USGS
monitors streamflow at 7,400 locations nationwide. The USGS streamflow
information is used for many purposes such as water resource appraisal and
allocation, design of the nation’s infrastructure such as bridges and water
treatment plants, flood hazard planning, National Weather Service flood
forecasting, reservoir operations, water-quality management, habitat assessment
and protection, recreational enjoyment and safety, and understanding changes in
streamflow due to land-use and climate changes. USGS streamflow data are
available at http://water.usgs.gov/waterwatch/.
Summary of the Fact Sheets:
Streamflow Trends in the United
States (http://pubs.water.usgs.gov/fs2005-3017/)
Streamflow has been increasing in the
United States since at least 1940. Regions that experienced the most widespread
increases were the Upper Mississippi, Ohio Valley, Texas-Gulf, and the Mid
Atlantic.
· Streamflow
increased across most of the United States during the 20th century at 40-45
percent of these 435 stations.
· Increases
were most prevalent in low to moderate streamflows (seen at 40 percent of the
stations), with relatively few decreases (seen at 8 percent of stations).
· Comparatively
few stations (10 percent) had increases in annual maximum streamflow.
· Streamflow
increases occurred as a sudden rather than gradual change around 1970,
suggesting the climate shifted to a new regime.
Changes in Streamflow Timing in New
England During the 20th Century http://pubs.water.usgs.gov/fs2005-3019/)
During the last 30 years, the timing of
winter/spring streamflow has shifted earlier by one to two weeks in northern and
mountainous New England streams.
·
· Only
4 of the 27 streamgages exhibited shifts in the timing of fall/winter streamflow
(October 1 to December 31), and all of these tended toward earlier streamflow.
Changes in Streamflow Timing in the
Western United States in Recent Decades http://pubs.water.usgs.gov/fs2005-3018)
As much as three-quarters of water
supplies in the western United States are derived from snowmelt. Trends toward
earlier snowmelt and streamflow need to be considered in the water-resource and
flood-management systems and procedures in many western settings.
·
The average streamflow
center-of-volume date (the date on which one-half of the total annual flow
volume passes a streamgage) in the western United States is about nine days
earlier now than in the 1950s.
· These
shifts in timing result both from late winter and early spring temperature
increases, and from changes in the form of precipitation (increasing liquid
precipitation, smaller percentage of snow) in late winter and early spring.
Trends in the Water Budget of the
Mississippi River Basin, 1949-1997 (http://pubs.water.usgs.gov/fs2005-3020/)
This study involved analysis of trends in
precipitation, streamflow, evapotranspiration, depletion of ground water, and
the filling of reservoirs. This study describes the influences of both climate
trends and human alterations on streamflow from 1949 to 1997.
·
Streamflow in the Mississippi River
basin increased at a rate of 4.5 percent per decade during the second half of
the 20th century.
· This
increase resulted primarily from an increase in precipitation offset by
increases in evaporation from reservoirs and irrigated cropland in the basin.
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