Lightning Forked cloudtoground lightning over an urban area Lightning occurs when a large electrical charge builds up in a cloud This is probably due to the rapid movement of water droplets and ice particles in the turbulent interior of the cloud Cloudtoground lightning occurs between a negatively charged cloud base and the positively charged ground Leader electrons leave the cloud and when contact is made there is a huge backflow of energy along the path of the electrons This produces a bright flash of light and temperatures of up to degrees Celsius Photographed in Finland
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Product ID: 22109993013A