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WEATHER
Lesson 5 - Page 2

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Lightning during a thurderstorm

Thunderstorms are generated by temperature imbalances in the atmosphere and a violent example of convection. Instability causes convective overturning of the layers of air, with heavier, denser layers sinking to the bottom and the lighter, warmer air rising rapidly.

Lightning is a build up of electrons concentrating and discharging static electricity during a thunderstorm. As the thunderstorm develops, interactions of charged particles produce an intense electrical field within the cloud. A large positive charge is usually concentrated in the frozen upper layers of the cloud, and a large negative change, along with a smaller positive area, is found in the lower portions.

Thunder is the sound produced by explosive expansion of air super heated by a lightning stroke. When lightning is close by, the thunder sounds like a sharp crack. More distant strokes produce growling and rumbling noises. Because the speed of light is about a million times that of sound, a lightning bolt is seen before the sound of the thunder. 

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