Distribution of lightning
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The incidence of individual lightning strikes in any particular place is highly variable, but lightning does have an underlying spatial distribution. Previously[when?], the frequency of lightning over the entire surface of the Earth was estimated to be 100 times a second. In 1997 NASA and National Space Development Agency (NASDA) of Japan launched the first Lightning Imaging Sensor (LIS)-equipped satellite to detect and record lightning.
Ratios of lightning types
The lightning flash rate averaged over the earth for intra-cloud (IC) + cloud-to-cloud (CC) to cloud-to-ground (CG) is at the ratio: (IC+CC):CG = 75:25. The base of the negative region in a cloud is normally at roughly the elevation where freezing occurs. The closer this region is to the ground, the more likely cloud-to-ground strikes are. In the tropics where the freeze zone is higher the (IC+CC):CG ratio is about 90:10. At the latitude of Norway (60° lat.) where the freezing elevation is lower the (IC+CC):CG ratio is about 50:50.
The map on the right shows that lightning is not distributed evenly around the planet. About 70% of lightning occurs on land in the Tropics, where the majority of thunderstorms occur. The north and south poles and the areas over the oceans have the fewest lightning strikes. The place where lightning occurs most often (according to the data from 2004 to 2005) is near the small village of Kifuka in the mountains of eastern Democratic Republic of the Congo, where the elevation is around 975 metres (3,200 ft). This region received 158 lightning strikes per 1 square kilometer (409 per sq mi) a year.
Above the Catatumbo river, which feeds Lake Maracaibo in Venezuela, Catatumbo lightning flashes several times per minute, 140 to 160 nights per year, accounting for about 25% of the world's production of upper-atmospheric ozone. Singapore has one of the highest rates of lightning activity in the world. The city of Teresina in northern Brazil has the third-highest rate of occurrences of lightning strikes in the world. The surrounding region is referred to as the Chapada do Corisco ("Flash Lightning Flatlands").
In the United States, the west coast has the fewest lightning strikes, but Central Florida sees more lightning than any other area. Florida has the largest number of recorded strikes during summer. Much of Florida is a peninsula, bordered by the ocean on three sides. The result is the nearly daily development of clouds that produce thunderstorms. For example, in what is called "Lightning Alley", an area from Tampa to Orlando, there are as many as 50 strikes per square mile (about 20 per km2) per year. The Empire State Building in New York City is struck by lightning on average 23 times each year, and was once struck 8 times in 24 minutes.
Lightning all over the world is observed by the LIS satellite system. In the US lightning monitoring is done by the National Lightning Detection Network, part of NASA’s National Severe Storms Laboratory. Maps of the U.S. lightning strike density/km2yr averaged from 1997-2010 are available from the National Lightning Detection Network (NLDL)--VAISALA More detailed U.S. regional lightning maps based on the National Oceanic and Atmospheric Administration (NOAA) and the National Weather Service (NWS) data centered on different cities are put out by the Cooperative Institute for Applied Meteorological Studies at Texas A&M University.
NASA scientists have found that electromagnetic radiation created by lightning in clouds only a few miles high can create a safe zone in the Van Allen radiation belts that surround the earth. This zone, known as the "Van Allen Belt slot", may be a safe haven for satellites in medium Earth orbits (MEOs), protecting them from the Sun's intense radiation.
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