This was not an isolated case, Coleman says. "There are a decent number of cases where there is some possible wave interaction with tornadoes."

Coleman is scheduled to present his preliminary research findings at the American Meteorological Society's Conference on Severe Local Storms in St. Louis on Monday.

In addition to their interaction with tornadoes, these atmospheric waves -- also called "gravity waves" -- may interact with fast-moving squall lines, might influence rain and snowfall, and can cause local high speed, straight-line wind damage.

While Coleman's National Science Foundation and NOAA-funded study of gravity waves is in its early stages, his long term goal is to develop tools to improve short range forecasts of violent weather, including tornadoes.

"If we can figure out how it works, our goal will be to teach the (National Weather Service) meteorologists and the TV meteorologists how to see when these things are coming so they can get warnings out in time," said Coleman, himself a former Birmingham TV weatherman. "There are still a lot of questions to answer, but I'm optimistic."

One of the first surprises the researchers found was that gravity waves "are really quite common," said Dr. Kevin Knupp, a professor of atmospheric science and the leader of UAH's severe weather research team. "A lot more common than we thought."

Gravity waves are caused by air flowing over mountains, by wind shear, thunderstorms and imbalances in the atmosphere. Air is a fluid, like water, and waves are created when the flow of fluid is interrupted. As wind blows toward a tall mountain, for instance, air that hits the mountain is forced upward. As this crest of air clears the mountain, it is cold and dense. Gravity pulls this cold, dense air mass downward, hence "gravity wave."

This up and down motion can set up gravity waves which continue through the atmosphere for hundreds of miles.

While much is not known about how these waves interact with powerful storms, Coleman and Knupp have discovered that the angle at which the two collide seems to have a strong influence: If the wave and the storm collide head on, there is little or no effect. If the gravity wave hits the storm front at an angle, however, that is when the waves seem to have their greatest influence on tornadoes.

Exactly how gravity waves amplify tornadoes is not known, but Coleman has theories that he will test.

"We think there are two processes at work here," he said. "Ahead of the crest of the wave you have a convergence of fluid, like water at the beach being drawn toward an approaching wave. This convergence might enhance the spin of anything that is already be spinning.

"Because it creates pressure between the wave moving in one direction and the air rushing toward the wave, the convergence might also squeeze a spin so it will be smaller but spin faster, like a skater tucking in her arms. It might make a rotating circulation smaller and more intense."

This pattern shows up in the Doppler radar images of a storm that hit Fayette County, Alabama, in January 1999.

"There are several of the major tornadoes in the south in the past decade that when we go back and look, there might have been a gravity wave involved," Coleman said. "The Dec. 16, 2000, Tuscaloosa storm was moving up I-59 without forming any tornadoes. Then it interacted with a gravity wave and it spun out a tornado."

In another case, Doppler radar picked up the signature of a tornado in storms going through Central Alabama on April 8, 1998.

"That tornado went from F1 to F4 within a couple of miles and a few minutes after a possible gravity wave went through," said Coleman. "You still don't know for sure that (the wave) caused it, but it did happen together."

That April 1998 tornado later grew into an F5 twister than killed more than 30 people in Birmingham.

Related Links
University of Alabama in Huntsville
A world of storm and tempest
The Air We Breathe at TerraDaily.com