Ice crystals inside cumulonimbus clouds rub against one another due to the strong updrafts in these clouds, thus building up a strong static charge. Positively charged crystals tend to rise to the top causing the cloud top to build up a positive static charge and negatively charged crystals and hail stones drop to the middle and bottom layers of the cloud building up a negative static charge. Cumulonimbus clouds that do not produce enough ice crystals usually fail to produce enough static electricity to cause lightning.
Lightning can also occur as a result of volcanic eruptions, which generate sufficient dust to create a static charge.
The earth is normally negatively charged with respect to the atmosphere. But as the thunderstorm passes over the ground, the negative charges at the bottom of the cumulonimbus cloud cause the positive charges on the ground to gather along the surface for several miles around the storm. When the negatives and positives gather in this way, an electrical discharge occurs, producing the bolt. This discharge usually occurs within the clouds or between the clouds and the ground. If you feel your hair stand up on end in a lightning storm beware. The negative charges from the cloud are pulling the positive charges inside your body to the top of your head and you could be in danger of being struck.
A bolt of lightning usually begins when a stepped leader stroke is sent out from the cloud. This leader is invisible to the naked eye. The electrical charge follows this leader from the ground back to the cloud. The return stroke is the most luminous part of the strike, and the part that is really visible. Most lightning strikes usually last about a quarter of a second. Sometimes several strokes will travel up and down the same leader strike, causing a flickering effect. Thunder is caused when the discharge rapidly super heats the air around the strike, causing a shockwave to be sent out.
All lightning is formed in the same fashion, as stated above, but some strikes take on particular characteristics, and scientists and the public have given names to these various types of lightning.
Intracloud lightning is the most common type of lightning which occurs completely inside one cumulonimbus cloud, jumping between different charged regions within the cloud. Intracloud lightning is commonly known as sheet lightning because it lights up the cloud and the surrounding sky with a sheet of light. One special type of intracloud lightning is commonly called an anvil crawler. Discharges of electricity in anvil crawlers travel up the sides of the cumulonimbus cloud branching out at the anvil top.
Cloud-to-ground lightning is a lightning discharge between a cumulonimbus cloud and the ground initiated by the downward-moving leader stroke. This is the second most common type of lightning. One special type of cloud-to-ground lightning is anvil lightning, which is sometimes called positive charge lightning, since it emanates from the anvil top of a cumulonimbus cloud where the ice crystals are positively charged. In anvil lightning, the leader stroke issues forth in a nearly horizontal direction till it veers toward the ground. These usually occur miles ahead of the main storm and will strike without warning on a sunny day. They are signs of an approaching storm. Another special type of cloud-to-ground lightning is bead lightning. This is a regular cloud-to-ground stroke that contains a higher intensity of luminosity. When the discharge fades it leaves behind a string of beads effect for a brief moment in the leader channel. A third special type of cloud-to-ground lightning is ribbon lightning. These occur in thunderstorms where there are high cross winds and multiple return strokes. The winds will blow each successive return stroke slightly to one side of the previous return stoke, causing a ribbon effect. The last special type of cloud-to-ground lightning is staccato lightning which is nothing more than a leader stroke with only one return stroke.
Cloud-to-cloud lightning is a somewhat rare type of discharge lightning between two or more completely separate cumulonimbus clouds.
Ground-to-cloud lightning is a lightning discharge between the ground and a cumulonimbus cloud from an upward-moving leader stroke. Most ground-to-cloud lightning occurs off of tall buildings, mountains and towers.
Heat lightning is nothing more than the faint flashes of lightning on the horizon from distant thunderstorms. Heat lightning was named because it often occurs on hot summer nights. Heat lightning can be an early warning sign that thunderstorms are approaching.
Ball lightning is described as a floating, illuminated ball that occurs during thunderstorms. They can be fast moving, slow moving or nearly stationary. Some make hissing or crackling noises or no noise at all. Some have been known to pass through windows and even dissipate with a bang. Ball lightning is a phenomenon only described by those who have witnessed it occurring.
However, the engineer Nikola Tesla wrote in Electrical World and Engineer, March 5, 1904 "I have succeeded in determining the mode of their formation and producing them artificially."
Sprites and jets are electrical discharges that occur high above a cumulonimbus cloud. They have been found to occur jointly or as a reaction to a normal discharge lightning. They are only visible for a split second, making them hard to detect with the naked eye. Photographs of them have been taken through telescopes mounted on high mountains or buildings aimed at distant thunderstorms. The most recent pictures and observations of sprites and jets have been from space aboard the space shuttles and unmanned satellites mounted with cameras pointed at the Earth's atmosphere.
All lightning is streak lighting. This is nothing more than the return stroke, the visible part of the lightning stroke. Because most of these strokes occur inside a cloud, we do not see many of the individual return strokes in a thunderstorm.
A bolt of lightning can reach temperatures approaching 50,000 degrees Fahrenheit (or about 28000 Kelvin) in a split second. This is hot enough to cause lightning strikes that hit a loose soil or sandy region of the ground to fuse the soil or sand into channels called fulgurites. These fulgurites are sometimes found under the sandy surfaces of beaches and golf courses or in desert regions. It is one evidence that lightning spreads out into branching channels when it strikes the ground.
Lightning is responsible for approximately 100 deaths a year in the United States alone. Lightning ranks second only to floods for storm related casualties in the U.S. every year. Many of these deaths could be prevented if basic precautions are taken when thunderstorms are expected in an area. Listening to a radio to keep up to date on storms in the area is the best way to prepare for safety.
One way to prepare for lightning safety is to install a device known as lightning conductor (commonly known as a lightning rod) for preventing injury by lightning to an individual or an instrument. Lightning rods consists of a short circuit to the ground that interrupt lightning by a thin nonconductor over which it jumps.
No place is truly 100% safe in a thunderstorm, but some places are more safe than others. Larger, better constructed structures are better than smaller or more open structures. Fully enclosed metal vehicles with the windows rolled up are good shelters, providing that no contact is made with any exposed metal inside or outside the vehicle.
When outside, avoid the following:
When inside avoid the following:
Lightning is often considered a divine or supernatural phenomenon. In many mythologies, it plays a role, and often have an affiliation with a certain god.
How Lightning is Formed
Various Types of Lightning
Intracloud Lightning, Sheet Lightning, Anvil Crawlers
Cloud-to-Ground Lightning, Anvil Lightning, Bead Lightning, Ribbon Lightning, Staccato Lightning
Cloud-to-Cloud Lightning
Ground-to-Cloud Lightning
Heat Lightning
Ball Lightning
Sprites and Jets
Streak Lightning
Lightning Facts
Lightning Safety
Safer Locations
If you find yourself trapped in an open area during a storm, position yourself close to the ground by squatting with your feet close together. Since lightning spreads when it hits the ground, you want to minimize as much surface area between you and the ground. Remember, humans are good conductors of electricity, and lightning tends to strike at the highest thing in an area, because electricity will always try to find the shortest pathway to the ground.
(basically anything to do with water)
Lightning in Cultures and Media
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