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NCAR News Release
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| 2000-18 | FOR IMMEDIATE RELEASE: May 19, 2000 |
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BOULDER -- Scientists are scanning the skies for lightning and supercell storms from a host of high-tech platforms in the High Plains near Goodland, Kansas, from May 22 to July 15. Their tools include storm-chasing vehicles, radars, and an armored research aircraft. The Severe Thunderstorm Electrification and Precipitation Study (STEPS-2000) is the largest effort to date to study lightning and low-precipitation storms. The National Center for Atmospheric Research (NCAR) is one of the project's leaders, with funding from the National Science Foundation, NCAR's primary sponsor.
Besides NCAR, participating institutions include the National Weather Service (NWS), NOAA's National Severe Storms Laboratory (NSSL), Colorado State University (CSU), Los Alamos National Laboratory, the New Mexico Institute of Mining and Technology (NMIMT), the South Dakota School of Mines and Technology (SDSMT), Stanford University, and the University of Oklahoma. NCAR researchers Morris Weisman and Jay Miller and CSU's Steve Rutledge will direct field operations.
Low-precipitation storms have many of the earmarks of other intense supercells-- including hail, strong updrafts, and rotation--but they produce little rain. "We can't now differentiate between low-precipitation and other storms," explains Weisman. "With the newer technology we're focusing on these storms, we expect to observe features we've only theorized about until now."
STEPS-2000 is based at the NWS office in Goodland, Kansas, and at an operations center near Burlington, Colorado. The study area-- along the semipermanent dry line that marks the west edge of Tornado Alley--has one of the nation's highest frequencies of positive cloud-to-ground lightning, a primary research focus during STEPS.
Researchers know little about low-precipitation supercells, except that they seldom produce tornadoes or flooding. Sorting out the microphysics of downdraft generation and precipitation in these "dry storms" could improve forecasters' ability to predict what happens to supercells as they evolve.
"We want to know how and why low-precipitation storms don't produce much rain, even when they contain as much water vapor as classic storms," says Weisman. Miller, Weisman, and colleagues will replicate STEPS data in computer models. They will look for differences between low- and high-precipitation storms and track the growth and movement of precipitation in three dimensions. According to Miller, the modeling will help to unravel how storms transport electrical charge and "grow" precipitation, especially hail.
STEPS-2000 will be the largest research effort to date focused on lightning, and tornado forecasters may benefit from the effort. Low-precipitation storms produce more than their share of positive cloud-to-ground strikes. Recent studies at NSSL have found several cases in which a storm's predominant cloud-to-ground strikes suddenly shifted from positive to negative within minutes of tornado formation. A shift may be a good indicator of when a violent tornado might appear in some storms. If scientists can follow a storm as it produces a tornado, the link between a storm's electrical behavior and microphysics should become clearer, and that knowledge could translate in the future into better tornado forecasting.
NCAR is managed by the University Corporation for Atmospheric Research, a consortium of more than 60 universities offering Ph.D.s in atmospheric and related sciences.
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| A low-precipitation storm near Grover, Colorado, July 10, 1996. Photographers love LP storms because of their spectacular cloud formations and sparse rainfall, but little is known about them. STEPS-2000 is bringing high tech to the High Plains this summer to probe their mysteries. (Morris Weisman, NCAR.) |
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| A non-tornadic downdraft in a rotating supercell near Wray, Colorado, June 2, 1999. (Bob Henson, NCAR.) |
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| Low-precipitation storm in Texas panhandle. (Tegtmeier.) |
Note to Editors: STEPS investigators will be available to speak with reporters from 9:00 a.m. to 2:00 p.m. on Thursday, June 1, in Goodland, Kansas. For more information, contact David Hosansky (303-497-8611).
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