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These are just a few of the things NASA scientists 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," says Hugh Christian, project leader for the National Space Science and Technology Center's (NSSTC's) lightning team at NASA's Marshall Space Flight Center. Left: A lightning bolt strikes the Atlantic Ocean near Florida. According to a new NASA map of global lightning rates, such strikes over open ocean waters are rare. Image courtesy NOAA.
"Basically, these optical sensors use high-speed cameras to look for changes in the tops of clouds, changes your eyes can't see," he explains. 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 OTD and LIS, global lightning patterns were known only approximately. 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.  Above: Data from space-based optical sensors reveal the uneven distribution of worldwide lightning strikes. Units: flashes/km2/yr. Image credit: NSSTC Lightning Team. 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, explains 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.
Right: Lightning is a sudden discharge of electricity between charged regions of thunderclouds and the ground. Only about 25 percent of lightning strikes are cloud-to-ground. The rest are either cloud-to-cloud or intracloud. [more information] 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 says. "[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. This seasonal variation contributes to a curious north-south asymmetry: Lightning ignites many of North America's late-summer wildfires, while some studies find that wildfires in South America are sparked more often by humans. Why the difference? It's simply because lightning in South America happens during a season when the ground is damp. Summertime lightning bolts in North America strike when the ground is dry and littered with fuel for fires.
"Oceanic areas also experience [a dearth of lightning]," Christian says. "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. Left: Relax. Lightning rarely strikes Pacific Islands. 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 says. "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 NSSTC. 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," explains Boccippio. So, measuring the rate of lightning flashes in real time might offer a way to identify potentially deadly storms before they become deadly. Clearly, lightning research is a field truly crackling with potential. You can learn more about it from the Global Hydrology and Climate Center's web site: Lightning and Atmospheric Electricity. |
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"Lightning is one of the mechanisms
to relax this build-up," says Boccippio.
Meanwhile,
areas such as the Arctic and Antarctic have very few thunderstorms
and, therefore, almost no lightning at all.
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