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ShareApr. 22, 2002 — Lightning. It avoids the ocean, but likes Florida. It's likely to strike in the Himalayas and even more so in central Africa. And lightning almost never strikes the North or South Poles.
These are just a few of the things NASA scientists at the National Space Science and Technology Center (NSSTC) in Huntsville, Ala., have learned using satellites to monitor worldwide lightning.
"For the first time, we've been able to map the global distribution of lightning, noting its variation as a function of latitude, longitude and time of year," said Hugh Christian, a scientist from NASA's Marshall Space Flight Center in Huntsville, Ala. and project leader for the lightning team at the NSSTC's Global Hydrology and Climate Center.
This new perspective on lightning is possible thanks to two satellite-based detectors: the Optical Transient Detector (OTD) and the Lightning Imaging Sensor (LIS).
"These are two optical sensors that we've flown in lower Earth orbit," said Christian, whose team developed the sensors. "The Optical Transient Detector was launched in 1995 and we got five good years out of it, compared to the two years expected, before it stopped transmitting data. The Lightning Imaging Sensor was launched on the Tropical Rainfall Measuring Mission satellite in 1997, and it's still going strong."
"Basically, these optical sensors use high-speed cameras to look for changes in the tops of clouds, changes your eyes can't see," he explained. By analyzing a narrow wavelength band around 777 nanometers -- which is in the near-infrared region of the spectrum -- they can spot brief lightning flashes even under daytime conditions.
Before the Optical Transient Detector and Lightning Imaging Sensor, only approximate global lightning patterns were known. Ground-based lightning detectors employing radio-frequency sensors provide high-quality local measurements. But because such sensors have a limited range, oceans and low-population areas had been poorly sampled.
The development of space-based optical detectors was a major advance, giving researchers their first complete picture of planet-wide lightning activity. The new maps show that Florida, for example, is one place where the rate of strikes is unusually high.
Dennis Boccippio, an atmospheric scientist with the NSSTC lightning team, explained why: "Florida experiences two sea breezes: one from the East Coast and one from the West Coast." The "push" between these two breezes forces ground air upward and triggers thunderstorms.
Within thunderclouds, turbulence spawned by updrafts causes tiny ice crystals and water droplets, called "hydrometeors," to bump around and collide. For reasons not fully understood, positive electric charge accumulates on smaller particles -- that is, on hydrometeors smaller than about 100 micrometers -- while negative charges grow on the larger ones. Winds and gravity separate the charged hydrometeors and produce an enormous electrical potential within the storm.
"Lightning is one of the mechanisms to relax this build-up," said Boccippio.
Another lightning hot spot is in the Himalayas, where the extreme local topography forces the convergence of air masses from the Indian Ocean.
And where does lightning strike most frequently? Central Africa. "There you get thunderstorms all year 'round," Christian said. "It's a result of weather patterns, air flow from the Atlantic Ocean, and enhancement by mountainous areas."
The satellite data also track patterns of lightning intensity over time. In the Northern Hemisphere, for example, most lightning happens during the summer months. But in equatorial regions, lightning appears more often during the fall and spring.
Meanwhile, areas such as the Arctic and Antarctic have very few thunderstorms and, therefore, almost no lightning at all.
"Oceanic areas also experience a dearth of lightning," Christian said. "People living on some of the islands in the Pacific don't describe much lightning in their language." The ocean surface doesn't warm up as much as land does during the day because of water's higher heat capacity. Heating of low-lying air is crucial for storm formation, so the oceans don't experience as many thunderstorms.
According to Boccippio these global patterns probably aren't much influenced by human activity. Some people have suggested that buildings and metal communications towers increase the overall frequency of lightning strikes. But, "lightning that does make it to the ground is pretty much creating its own channels," Boccippio said.
"The likelihood that we are changing the amount of cloud-to-ground strikes with construction of towers is very slim." He cautions, however, that this has not been verified experimentally.
To answer such questions, a new lightning detector -- the Lightning Mapper Sensor or "LMS" -- is on the drawing board at the National Space Science and Technology Center. The proposed instrument would circle our planet in a geostationary orbit over the United States, detecting all forms of lightning with a high spatial resolution and detection efficiency.
The LMS, or something like it, could provide valuable -- even life-saving -- data to weather forecasters. "The same updrafts that drive severe weather often cause a spike in the lightning rate at the onset of a storm," explained Boccippio. So, measuring the rate of lightning flashes in real time might offer a way to identify potentially deadly storms before they become deadly.
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The above story is reprinted from materials provided by NASA/Marshall Space Flight Center.
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