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Thunderstorm Electrification and Lightning Experiment
TELEX 2004 Overview Video
There were two broad objectives to the 2004 TELEX project:
One was to try to understand better why storms tend to produce a lot
of positive cloud-to-ground flashes. The second part looked
at the electrification of mesoscale convective systems.
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Text transcript
Examples of Launches of Instrumented Balloons in Storms
The videos show the launch sequence used during the Severe
Thunderstorm Electrification and Precipitation Study, based in Goodland,
Kansas, in 2000. It is the same procedure being used in the Thunderstorm
Electrification and Lightning Experiment in Oklahoma. There are two types
of weather balloons used: latex (beige colored) and plastic (clear). The
plastic is used to minimize the effects of hail hitting the balloon, i.e,
the plastic does not burst instantly when punctured. The latex balloon
is used if hail is not expected, such as in stratiform rain of certain
areas of mesoscale convective systems.
The basic instrument train consists of a parachute; a radiosonde
for measuring temperature, relative humidity, pressure, and GPS-derived
winds and location; and an electric field meter for measuring the vector
electric field in the storm along the flight path. Prior to launch, a
balloon is encased in the launch tube and inflated with helium. The counting
you may hear in the videos is our keeping track of timers set for 30 seconds.
When the 30 seconds has elapsed, lines are melted and the electric field
meter is lowered gently away from the balloon. In the case of plastic
balloons, a second timer releases the bottom half of the balloon, which
may be seen in some of the videos. Our balloon-launch procedure allows
launches in strong winds, as may be seen in Flights 3 and 24.
MPG VIDEOS:
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