(Last updated May 12, 2002)
A series of tornadic thunderstorms wreaked havoc from central Texas
to southern Kansas on May 3-4, 1999. Over fifty tornadoes occurred, with central
Oklahoma the worst hit area. This page shows several images from the Twin Lakes,
OK, radar of the the tornadic storm that moved through the Oklahoma City area.
The first image (77K GIF) is a
reflectivity image at 6:31 PM CDT. Radar reflectivity is a measure of
how much of a radar pulse bounces off a target and returns to the radar. For
weather radar, the heavier the rain and hail, the greater the signal returned
to the radar and the hight the reflectivity. This images shows the
tornadic thunderstorm about the time the Oklahoma City/Moore tornado first
touched down. Notice the large area of yellow, orange, and red in the center
of the picture, and how these colors curve around an area of green just north
of the town of Amber. These are the areas of heavy rain and hail (higher
reflectivity), forming a hook echo around the lighter precipitation
(lower reflectivity) just north of Amber. This is a pattern characteristic of a
supercell thunderstorm. The area of lighter precipitation is caused by
the thunderstorm's updraft, which is so strong that little precipitation can
fall through it.
The second image (71K GIF) is a
storm-relative velocity image of the cell. The
National Weather Service's doppler radars
can seen the wind blowing toward (green colors) or away (red colors) from the
radar site. In a storm-relative velocity image, the motion of the storm has
been subtracted from the winds, making it easier to see any rotation in the
storm. Notice the couplet of bright green and bright red and pink near Amber.
This is the strong cyclonic circulation associated with the developing
tornado.
The reflectivity image (91K GIF)
on the left shows the storm at 6:56 PM. The hook echo has become even more
pronounced just west of Lancaster, with the blue colors in the hook showing
even lighter precipitation than before. The
storm-relative velocity image (71K GIF) on the right
shows winds greater than 75 mph blowing toward the radar (bright green) right
next to greater than 75 mph blowing away from the radar (pink). This sharp
change in the winds is a Tornado Vortex Signature, the signal that
appears when a tornado is large enough or strong enough to be directly
detected.
The
tornado
track map created by the
National Weather Service Forecast
Office in Norman, OK shows the tornado reached F5 (maximum intensity)
on the Fujita tornado
scale around this time. Eyewitness accounts indicate the tornado was about a
mile wide.
The reflectivity image (86K GIF)
on the left shows the storm at 7:32 PM PM. Notice the increased reflectivity
(the white pixels) at the end of the hook. The increase is mostly likely due
to the radar detecting the debris raised by the tornado as it moved through
the Oklahoma City metropolitan area. The
storm-relative velocity image (79K GIF) continues
to show the well-defined velocity couplet associated with the tornado, which
has been on the ground for an hour.
These images are used with the kind permission of
National Weather Service Forecast
Office in Norman, OK and can be found in the
May 3 tornado
outbreak section of their web site. Another National Weather Service office
with information on the outbreak is
Tulsa, OK.
There are numerous other on-line sources of information on this notorious event. Satellite imagery can be found at:
Other information is available from the National Severe Storms Laboratory, the Doppler on Wheels web site, and the Oklahoma Climate Survey. Last, but certainly not least, pictures and chase accounts of the May 3 tornadoes are available from Roger Edwards and Jim Leonard.
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