Lightning Alley
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Lightning Alley
The distribution of lightning, or the incidence of individual strikes, in any particular place is highly dependent on its location, climate, and time of year. Lightning does have an underlying spatial distribution. High quality lightning data has only recently become available, but the data indicates that lightning occurs on average times every second over the entire Earth, making a total of about 1.4 billion flashes per year. 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 in the ratio: (IC+CC):CG = 3:1. 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 9:1. In Norway, at latitude 60° N, where the freezing elevation is lower, the (IC+CC):CG ratio is about 1:1. Dis ...
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Lightning Flash Density 12
Lightning is a naturally occurring electrostatic discharge during which two electrically charged regions, both in the atmosphere or with one on the ground, temporarily neutralize themselves, causing the instantaneous release of an average of one gigajoule of energy. This discharge may produce a wide range of electromagnetic radiation, from heat created by the rapid movement of electrons, to brilliant flashes of visible light in the form of black-body radiation. Lightning causes thunder, a sound from the shock wave which develops as gases in the vicinity of the discharge experience a sudden increase in pressure. Lightning occurs commonly during thunderstorms as well as other types of energetic weather systems, but volcanic lightning can also occur during volcanic eruptions. The three main kinds of lightning are distinguished by where they occur: either inside a single thundercloud (intra-cloud), between two clouds (cloud-to-cloud), or between a cloud and the ground (cloud-to- ...
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