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THE
1966 TOPEKA TORNADO
37th
Anniversary
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| June 8th, 2003 will mark
the 37th anniversary of one of the most destructive and deadly tornadoes
in Kansas history. The massive 1966 Topeka tornado killed 16 people,
injured over 400 and caused $100 million damage; at the time, the
highest in America history. With modern day inflation factored in, the
tornado still ranks as one of the costliest on record.
The tornado formed about 7pm west of Auburn in
southwest Shawnee county, and cut a 22 mile long path, at times a half a
mile wide, across the heart of the city. Total devastation occurred
along an 8 block section in the center of Topeka. Every building on the
Washburn University campus was either destroyed or heavily damaged
producing $10 million damage, alone.
Citywide about 800 homes were completely destroyed
with nearly 3000 damaged. Even the state Capitol dome sustained damage
from the flying debris, as did many downtown buildings. The intense
destruction classified the tornado as an F5, the top of the Fujita
Intensity Scale, with winds estimated at over 250 mph.
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| The tornado held a northeast pace at about
35 mph, but weakened after leaving the downtown area, finally
dissipating just east Billard Airport on the city’s northeast side
after being on the ground for about a half an hour. Power and utilities
in many parts of the city were out for weeks, and hundreds were left
homeless.
Entering the southwest part of Topeka, the tornado
roared across Burnetts Mound, ending a longstanding Indian legend that
the Mound would deflect any tornadoes and spare the city. Although 42
tornadoes have struck Shawnee county since 1950, the infamous June 8th,
1966, is, by far, the worst.
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| Excellent watch, warning and storm spotter
activation prior to the storms development helped keep the death and
injury toll relatively low, especially when compared to the amount of
destruction and the storms path. In addition, the existence of an active
and longstanding community preparedness plan was also instrumental in
reducing potential casualties and injuries. Outstanding education,
cooperation and understanding between Topeka governmental agencies, the
media and public became a model for other cities to follow in the
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Research and examination of the destruction and debris
provided insights into tornado understanding, and improved safety rules
and information. For example, the longstanding advice about going to the
southwest corner of the basement and opening windows, was shown to be
incorrect from damage surveys in Topeka. We now know that you should
forget the windows, and head for the middle of the basement and get
under a table, stairway or something sturdy.
Often overshadowed by the Topeka destruction, a large
tornado also hit the city of Manhattan on June 8th causing 65
injuries and about $2 million damage. The Manhattan tornado hit shortly
before 6pm on the city’s northwest edge, destroying 11 homes and
damaging over 300 more. Public awareness of the Manhattan tornado,
likely alerted Topeka residents to volatile atmospheric conditions and
high potential for another tornado. In addition, shortly after the
Topeka tornado, and likely from the same thunderstorm, two other
tornadoes occurred in Leavenworth county, producing one fatality near
Jarbalo.
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A lot has changed since 1966, including weather technology that lets us
better understand, forecast and warn for deadly tornadoes, like the one
that devastated Topeka. Powerful computers, both table-top PC models and
large mainframe systems, have allowed quick and thoroughly analysis and
prediction of weather data. Small scale weather features unknown in
1966, are now scrutinized routinely for atmospheric evidence and clues.
Computers have also been
coupled to more powerful and sophisticated Doppler weather radars, to
look inside thunderstorms for areas of rotation, which are sometimes a
precursor to the tornado.
Weather radars used in 1966
were WWII surplus with small fuzzy black and white images. Today’s
National Weather Service Doppler radar present state-of-the-art high
detail color images of both reflectivity and velocity zoomed to city and
county level. Additional 3D interrogation of storms can pinpoint
critical areas for storm spotters to observe before tornado development.
Much smaller warning areas are
now selected on the radar screen using a cursor and movement vectors.
With another click of the mouse the complete warning text is generated
in seconds, and disseminated immediately, a fraction of the time it took
to hand type a warning in 1966.
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6 AM Surface Map

Surface Map at Noon shows the warm front had moved north of Topeka,
with a cold front and dry line moving in from the West.
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Slow speed manual teletypes and
paper facsimile charts have been replaced by ultra high speed satellite
computer driven communication circuits. These modern tools can bring
weather information and send warnings out to the media and public in a
fraction of a second. Direct broadcasts to the public by the NOAA
Weather Radio network allow the average citizen to receive warning
information anytime day or night, and at the same time as media outlets.
Internet popularity and connections have allowed a multitude of weather
data to be available to nearly everyone.
Can the devastation of June 8, 1966, happen again? Yes, and at
anytime! We can’t stop storms from forming. But through improved
atmospheric understanding, modern technology and high speed
communications, the death and injury toll, if any, will hopefully remain
small compared to the destruction caused.
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