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Lightning

During any given minute, there are more than a thousand thunderstorms around the Earth causing some 6,000 flashes of lightning. Every minute!

Friction Thunderstorlight showms are caused by rapidly rising and falling currents of air. The friction from this moving air creates electrical charges within a cloud. Water droplets and ice pellets fall, carrying charged electrons to the lower portion of the cloud, where a negative charge builds. A positive charge builds up near the top of a cloud.

Most of the electrical energy in a thunderstorm is dissipated within the clouds, as lightning hops between the positively and negatively charged areas. Lightning becomes dangerous, though, when it reaches for the Earth.

How lightning strikes

Charges When the negative charge in the cloud becomes great enough, it seeks an easy path to the positively charged ground below. The current looks for a good conductorLightning of electricity, or a tall structure anchored to the ground (such as a tree or a tall building). The negative charge sends out a feeler, called a stepped leader, which is a series of invisible steps of negative charges.

Lightning Strikes As the stepped leader nears the ground, a positive streamer reaches up for it. Only then, once this channel is made, does the visible lightning happen. A return stroke runs from the ground to the clouds in a spectacular flash.

Though the bolt appears continuous, it is actually a series of short bursts. Most lightning strikes occur in less than a half second and the bolt is usually less than 2 inches in diameter.

Thunder

The air around a lightning bolt is superheated to about 54,000 degrees Fahrenheit (five times hotter than the sun!). This sudden heating causes the air to expand faster than the speed of sound, which compresses the air and forms a shock wave; we hear it as thunder. Since the bolt is actually several short bursts strung together, multiple shock waves are created at different altitudes; this is why thunder seems to rumble — each shock wave takes a different amount of time to reach your ear.

Estimating distance

Because light travels faster than sound (186,291 miles per second vs. 1,088 feet per second) you see lightning before you hear the thunder. When you see it, count the seconds before the thunder arrives. Divide this number by 5, and you'll know approximately how many miles away the lightning was (5 seconds = 1 mile).

Lightning facts

lightning map

Although cloud-to-ground lightning strikes pose the most danger to people on the ground, they make up only about 20% of all lightning strikes. The most common type of lightning in a thunderstorm is in-cloud lightning, which occurs within the cloud itself.

Cloud-to-cloud lightning is a common occurrence in which opposite electrical charges in one cloud attract those in another.

An extremely rare form of lightning is called ball lightning. It is so rare that scientists often question its existence. Those who have witnessed ball lightning describe it as a round ball of fire seen on telephone wires or entering through windows and doors during a thunderstorm.

Then there's heat lightning. Heat lightning has nothing to do with how warm temperatures are on a summer's night. It is actually lightning seen from a distant thunderstorm too far away for the thunder to be heard.

A Warning Is Issued

You observe and/or hear lightning and thunder, or thunderstorms are in the forecast.

A severe thunderstorm warning is in effect — what should you do?

At home: If you are at home, protect yourself and your family following the safety tips below:

Away from home: There are times when storms come up suddenly. If you are away from home, protect yourself and your family by taking cover in the best shelter you can find.

 
 
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