Facts about LIGHTNING

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By the founder of StormWarn!

The upward and downward motions within a thunderstorm causes air to rise above and fall below the freezing point, upon which moisture changes from water to ice and back to water again. There is something about this process that tends to create an electrostatic gradient in the thunderstorm cloud (called a CB for short). The top of the CB becomes positively charged and the bottom negatively. If the gradient is strong enough, electrons from the bottom of the cloud will discharge to the top in the form of lightning (called IC lightning or intracloud lightning). A negatively charged cloud base repels electrons on the surface and thus causes a positively charged surface. A discharge from the cloud to the ground is called CG lightning (cloud-to-ground lightning). The bottoms of adjust storms can discharge to the tops of others and vice versa, which is also deemed IC lightning. Lightning can occur in many forms - the most dangerous of which is called a Positive Giant, or "bolt from the blue". This is when a discharge occurs between the positive CB top and the relatively negative charge of outlying surface areas away from the thunderstorm. This is rare because of the great distances (sometimes up to 20 miles!) that such lightning has to travel, but when it occurs it is by far the most deadly. Positive giants have many times the destructive power of normal lightning and as its nickname denotes, strikes where no thunderstorm is overhead. You can get struck by lightning under a clear blue sky, by a thunderstorm twenty miles away! Contrary to popular belief, it is quite common for people to be struck by lightning, and in fact lightning is a very poor killer. While people do get killed by lightning, most survive it. Here are some facts about lightning taken from the Stormwise website, makers of very good and inexpensive lightning detection devices:

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