Today is the 62nd anniversary of the first documented case of a tornado detected by radar. Illinois State Water Survey staff, at Willard Airport in Champaign, IL, captured the historic event on film on April 9, 1953. This discovery helped lead to the first national weather radar network in the United States.
The radar was located at Willard Airport, south of Champaign IL, and was being used along with a rain gauge network to relate radar signals with rain rates. Don Staggs, the radar technician, had stayed late to complete repairs on the radar. While testing the repairs, he noticed an interesting radar return and began recording the radar scope using the mounted 35 mm camera. As a result, he captured a well-defined hook echo on film. See photo below. The hook echo is best described by the National Severe Storm Laboratory:
A “hook echo” describes a pattern in radar reflectivity images that looks like a hook extending from the radar echo, usually in the right-rear part of the storm (relative to the motion of the storm). A hook is often associated with a mesocyclone and indicates favorable conditions for tornado formation. The hook is caused by the rear flank downdraft and is the result of precipitation wrapping around the back side of the updraft.
Afterwards, researchers related the radar data that Staggs recorded to detailed damage reports along the tornado’s path (see map and photos below).
I find this story fascinating for a variety of reasons. Some of the reasons are personal. It happened at my home institution (Illinois State Water Survey) and I knew several of the people involved (Don Staggs, Glen Stout, Floyd Huff, Stan Changnon). But beyond that there were several key ingredients to the story:
- The radar was on when it should have been off. If Don Staggs had not been working late to replace a piece of equipment on the radar, the discovery would have been missed. The storm occurred in the early evening hours when the radar was normally turned off. Don had the foresight to keep the radar running when he saw the unusual return on the radar.
- The tornado occurred near one of the few radars in the country at that time designed for weather research, as opposed to defense or air traffic control. There was no network of weather radars like we enjoy today. In addition, this radar set was equipped with a 35-mm camera to record what was on the scope.
- The thunderstorm was strong enough to produce a clear hook echo, and was located to the north of the radar so there was no attenuation (interference) from rain.
- The tornado was well-documented in terms of the location and timing of the damage. This allowed scientists to relate what happened on the radar scope with what happened on the ground.
The 1954 Water Survey report on the tornado stated, “It may be possible to establish radar storm warning systems in tornado areas to reduce loss of lives.” The April 9, 1953, event, along with subsequent events, helped provide the push in the US for developing a nationwide network of weather radars.
Additional information on this event:
- Water Survey page on the hook echo event
- History of the CHILL radar
- 1954 Water Survey report on the event (pdf)
- Dr. Fujita’s 1958 Journal of Meteorology article