1996-9 -- FOR IMMEDIATE RELEASE: May 10, 1996
Howard Bluestein, 303-497-8924 until August 15, 1996
-- and 405-325-3006, email@example.com
School of Meteorology, University of Oklahoma
Specialty: Observational studies of tornadoes and severe storms; synoptic and mesoscale meteorology. Note: Bluestein is on sabbatical at NCAR this spring and summer.
Harold Brooks, 405-366-0499, firstname.lastname@example.org
NOAA/National Severe Storms Laboratory
Specialty: Probabilistic forecasts of storms; short-range forecasts using ensembles of computer models
Tom Grazulis, 802-748-2505
The Tornado Project, St. Johnsbury, Vermont
Specialty: History of tornadoes; author of Significant Tornadoes 1680-1991 and producer of Tornado Video Classics (vols. I, II, III)
Morris Weisman, 303-497-8901, email@example.com
Specialty: thunderstorm modeling and observation; mesoscale convective systems
James Wilson, 303-497-8818, firstname.lastname@example.org
NCAR/Atmospheric Technology Division
Specialty: Short-period forecasting (nowcasting) of storms, microbursts, and related phenomena, using Doppler radar
Tornado and Storm Research Organization
This British entity provides statistics and other information on tornadoes and severe storms in the United Kingdom and throughout Europe.
Fatalities. Tornadoes have killed over 3,700 people since 1953. Though fatalities have been dropping in recent years, tornadoes killed 69 people in 1994, the most deaths since 1984, and 29 people in 1995.
What causes tornadoes? The strongest tornadoes occur from "supercells," long-lived thunderstorms with large-scale cyclonic circulations that can persist for hours and extend well beyond the storm itself. These strong circulations are often associated with the most violent twisters, yet only a small percentage of supercells produce tornadoes. Recent data indicate that gust fronts and other wind boundaries near the ground are important factors in a tornado's eventual formation.
Where? Tornadoes have been reported in every U.S. state, but they are most concentrated in Tornado Alley, which runs north from central Texas through Oklahoma and Kansas into eastern Nebraska, South Dakota, and Iowa. Other areas of high frequency include the Corn Belt of Illinois and Indiana and the Deep South states of Mississippi, Alabama, and Georgia.
When? Spring is tornado season, with about 50% of all reported tornadoes occurring from April through June. Most tornadoes strike between noon and sunset.
Path of destruction. The typical (median) track length is about one mile for all tornadoes and 23 miles for the strongest ones. The longest track length recorded for a single tornado is the 219-mile track of the Great Tri-State Tornado of March 18, 1925. The typical track width is only 48 yards, but it can range to more than a mile.
Direction and wind speed. Thunderstorms and their attendant tornadoes typically move northeast or east, but tornado tracks can be erratic. Tornadoes move forward at speeds ranging from nearly stationary to 60 mph or more and averaging 20 to 40 mph. Measurements from Doppler radar and estimates based on motion pictures give top speeds in the range of 250-300 mph. Most tornadic winds are below 150 mph.
UCAR manages NCAR under sponsorship of the National Science Foundation.