#CARS FAST AS LIGHTNING WEEKLY EVENT CRACK#

Scientists think the two largest charge regions in most storms are caused mainly by graupel carrying negative charge in the middle of the storm and ice particles carrying gained positive charge in the upper part of the storm. Laboratory studies suggest that graupel gains positive charge at temperatures a little colder than 32 degrees Fahrenheit, but gains negative charge at colder temperatures a little higher in the storm. Because the smaller ice particles rise faster in updrafts than the graupel particles, the charge on ice particles separates from the charge on graupel particles, and the charge on ice particles collects above the charge on graupel.

When these graupel particles collide and bounce off of smaller ice particles, the graupel gains one sign of charge and the smaller ice particle gains the other sign of charge.

Scientists think that the initial process for creating charge regions in thunderstorms involves small hail particles called graupel that are roughly one quarter millimeter to a few millimeters in diameter and are growing by collecting even smaller supercooled liquid droplets. We generally know what conditions are needed to produce lightning, but there is still debate about exactly how a cloud builds up electrical charges, and how lightning forms. What causes lightning? The creation of lightning is a complicated process. Lightning can strike the ground in an open field even if the tree line is close by. However, this does not always mean tall objects will be struck. Tall objects such as trees and skyscrapers are more likely than the surrounding ground to produce one of the connecting sparks and so are more likely to be struck by lightning. When one of the sparks connects the downward developing channel, a huge electric current surges rapidly down the channel to the object that produced the spark. When it gets less than roughly a hundred yards of the ground, objects like trees and bushes and buildings start sending up sparks to meet it. If a lightning flash is going to strike ground, a channel develops downward toward the surface. Where does lightning strike? Most, if not all, lightning flashes produced by storms start inside the cloud. Sound travels approximately one fifth of a mile per second or one third of a kilometer per second, so dividing the number of seconds by 5 gives the number of miles to the flash and dividing by 3 gives the number of kilometers. Just count the number of seconds from the time you see a flash until you hear thunder.

#CARS FAST AS LIGHTNING WEEKLY EVENT CRACK#

A few seconds later, you hear a sharp click or loud crack from lightning channels a little farther away, and several tens of seconds later the thunder from the most distant part of a flash has quieted to low frequency rumbling.īecause light travels through the air roughly a million times faster than sound does, you can use thunder to estimate the distance to lightning. Very close to lightning, the first thunder you hear is from the closest channels,which produce a tearing sound, because that thunder contains high frequencies. Thunder can be heard up to 25 miles away from the lightning discharge, but the frequency of the sound changes with distance from the lightning channels that produce it, because higher frequencies are more quickly absorbed by the air. The huge pressure in the initial outward shock wave decreases rapidly with increasing distance and within ten yards or so has become small enough to be perceived as the sound we call thunder. What causes thunder? Lightning causes thunder! Energy from a lightning channel heats the air briefly to around 50,000 degrees Fahrenheit, much hotter than the surface of the sun. What we do: Read more about NSSL's lightning research here. It can be seen in volcanic eruptions, extremely intense forest fires, surface nuclear detonations, heavy snowstorms, in large hurricanes, and obviously, thunderstorms. Lightning is one of the oldest observed natural phenomena on earth. Lightning can occur between opposite charges within the thunderstorm cloud (intra-cloud lightning) or between opposite charges in the cloud and on the ground (cloud-to-ground lightning). The flash of lightning temporarily equalizes the charged regions in the atmosphere until the opposite charges build up again. When the opposite charges build up enough, this insulating capacity of the air breaks down and there is a rapid discharge of electricity that we know as lightning. In the early stages of development, air acts as an insulator between the positive and negative charges in the cloud and between the cloud and the ground. Watch on the NOAA Weather Partners YouTube Channel» What is lightning? Lightning is a giant spark of electricity in the atmosphere between clouds, the air, or the ground.

Cars fast as lightning weekly event