Lightning

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Lightning occurs when friction between ice particles within large clouds, (cumulonimbus) builds up a charge of electricity which is trapped. This is because there is a gap between the cloud & an other body, i.e. the ground or another cloud.

 Eventually this charge becomes so great that it can jump across this gap. This is when Lightning occurs, the sound of thunder is a result of this electrical discharge. Because the electrical discharge is so great, it can be detected over long distances, by a lightning detector & then plotted onto a map by computer.

 Cloud to ground lighting can be a negative or positive charge. Positive lightning usually comes from the top of the cloud and can develop six to ten times the amount of charge and voltage of a negative bolt,

Inter cloud lightning

Cloud to ground Lightning

To find out how far away a lightning strike is, count the time in seconds between the flash of lightning, and the sound thunder, every 5 seconds = 1 mile.

 
Microsferics Recent activity
 
Recent Western Europe Activity
Do not use for protection of life or property!

Map of UK Lightning

Image from Blitzortung.org


Recent European Activity

Map of europe Lightning

Image from Blitzortung.org

 

 

Recent Worldwide Activity

Map of world lightning

Image from Blitzortung.org

Note - During a thunderstorm you are advised to disconnect equipment from your telephone lines & your TV aerial.

Disclaimer Doncasterwx does not accept responsibility for any loss or injury resulting from use of this website.

Warning Don't stand under a tall tree or object during a thunder storm. The safest places are Indoors, in your vehicle or  on the ground.

 

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