positive and negative have the same change
Lightning is formed by particles in the clouds, that on the top forms a Positive charge, and on the bottom a Negative charge, these particles continue to form, and when there are to many particles in the clouds, some need to go, and when they go, they come out as Static electricity, which this is called Lightning, and the more particles there are, the more will need to be given, and that means the more lightning there is.
Positively charged particles in a storm cloud float near the top, while negatively charged particles stay near the bottom. If the negatively charged particles clump up too much, they 'jump' somewhere else, to help spread out again. This results in lightning from the attracted particles.
Lightning occurs when electrical charges build up in the atmosphere, usually during a thunderstorm. The negative charges gather at the bottom of the cloud, while positive charges accumulate on the ground below. When the difference in charge becomes strong enough, a channel of ionized air forms, allowing the electrical discharge of lightning to travel from the cloud to the ground.
In storm clouds, tiny particles in the cloud move around picking up positive or negative energy charges, like when shoes scuff a rug. The positive charged particles stay light, and rise to the top of the cloud. The negative charged particles get heavier, and collect at the bottom of the cloud.As more particles become charged, they divide into opposing groups in the cloud. When the power of attraction between them gets too great, the particles discharge their energy at each other, completing a path for electricity to travel through the air. We call this flow of electricity lightning.It's the negative charges in the bottom of the cloud that cause lightning to strike the ground. When the negatively charged particles group together, they begin to seek out positive charges from the ground below. The excess electrons create a channel of charged air called a leader that reaches down to the ground below. The leaders attract other charged ground-based channels called streamers.When the stepped leader from the cloud meets a returning streamer from the ground, the path is ready. An electrical current called the return stroke, travels back up the path. This return stroke releases tremendous energy, bright light and thunder.The typical stroke can last only 30 milliseconds, so four to five strokes may happen in the blink of an eye. Despite the old saying, lightning does strike the same place twice.In storm clouds, tiny particles in the cloud move around picking up positive or negative energy charges, like when shoes scuff a rug. The positive charged particles stay light, and rise to the top of the cloud. The negative charged particles get heavier, and collect at the bottom of the cloud.As more particles become charged, they divide into opposing groups in the cloud. When the power of attraction between them gets too great, the particles discharge their energy at each other, completing a path for electricity to travel through the air. We call this flow of electricity lightning.It's the negative charges in the bottom of the cloud that cause lightning to strike the ground. When the negatively charged particles group together, they begin to seek out positive charges from the ground below. The excess electrons create a channel of charged air called a leader that reaches down to the ground below. The leaders attract other charged ground-based channels called streamers.When the stepped leader from the cloud meets a returning streamer from the ground, the path is ready. An electrical current called the return stroke, travels back up the path. This return stroke releases tremendous energy, bright light and thunder.The typical stroke can last only 30 milliseconds, so four to five strokes may happen in the blink of an eye. Despite the old saying, lightning does strike the same place twice.To review, lightning is created by the attraction between opposite charges, the same force that creates static electricity. But lightning uses huge opposite charges to produce an electrical current that's nothing like what you'd get from static electricity.
The source of lightning in thunderhead clouds is when there is a significant amount of ice in the cloud, most likely hail and there are 2 differing charges in 2 areas. The negative charge is at the bottom of the cloud, while the positive charge is at the top of the cloud. The ground is positively charge until there is an electrical discharge between the negatively charged cloud base and the positively charged ground, then it becomes mostly negative which then can open up the opportunity for a lightning bolt to jump from the top of the cloud, all the way down to the ground in another electrical discharge that is of greater electrical potential (voltage) than the first electrical discharge between the cloud base and the ground. This is because it takes more voltage to have a visible electrical discharge over a longer distance. There has to be 30,000 volts/cm of distance for a visible electrical discharge to occur.
the answer is both positive and negitive charges and that is because to make lighting it has to be positive and negitive charges because if there is both 2 negitive charges will both repel and the same thing will happen to positive charges but when positive and negitive charges and positive charges will attract
Lightning is a natural discharge of static electricity that occurs during a thunderstorm. When a storm cloud builds up an excess of negative electrical charges at the bottom and positive charges at the top, they seek to balance out, resulting in a powerful discharge of electricity in the form of lightning. This discharge is what creates the electrical currents of lightning.
Lightning is formed by particles in the clouds, that on the top forms a Positive charge, and on the bottom a Negative charge, these particles continue to form, and when there are to many particles in the clouds, some need to go, and when they go, they come out as Static electricity, which this is called Lightning, and the more particles there are, the more will need to be given, and that means the more lightning there is.
Positively charged particles in a storm cloud float near the top, while negatively charged particles stay near the bottom. If the negatively charged particles clump up too much, they 'jump' somewhere else, to help spread out again. This results in lightning from the attracted particles.
During a storm small particles are propelled towards the top of the cloud by strong internal winds. The larger particles fall to the bottom of the cloud. This causes the top of the cloud to develop a strong positive charge, while the bottom of the cloud has a strong negative charge. This induces a positive charge on the ground. This combination is where there is a massive very rapid transfer of electrons, also known as lightning.
Electrons are negatively charged subatomic particles. When you have a cloud that at the top of it is most negativity charged and the bottom is positively charged and it rolls over a point in the ground that is negatively charged this causes lightening and actually lightening goes from the ground up to the clouds not from the clouds to the ground as believed - the lightning is composed of a stream of electrons
Lightning occurs when electrical charges build up in the atmosphere, usually during a thunderstorm. The negative charges gather at the bottom of the cloud, while positive charges accumulate on the ground below. When the difference in charge becomes strong enough, a channel of ionized air forms, allowing the electrical discharge of lightning to travel from the cloud to the ground.
Lightning typically travels from the clouds to the ground. It is formed when negative charges accumulate in the bottom of the cloud and positive charges build up on the ground, creating an electrical discharge.
As the bottom part of the cloud is lifted higher in an up drift, the water particles freeze as the air is colder. Down drifts then push those particles back down passing the water going up and in that passing electrons are stripped of their charge resulting in the bottom of the cloud being negatively charged.
Lightning may not seem much like static electricity, but it's actually very similar. Both are sparks of electricity created through the attraction of unlike charges. The difference is that static electricity creates a small spark, while lightning is a huge spark of electricity. In storm clouds, tiny particles in the cloud move around picking up positive or negative energy charges, like when shoes scuff a rug. The positive charged particles stay light, and rise to the top of the cloud. The negative charged particles get heavier, and collect at the bottom of the cloud.As more particles become charged, they divide into opposing groups in the cloud. When the power of attraction between them gets too great, the particles discharge their energy at each other, completing a path for electricity to travel through the air. We call this flow of electricity lightning.It's the negative charges in the bottom of the cloud that cause lightning to strike the ground. When the negatively charged particles group together, they begin to seek out positive charges from the ground below. The excess electrons create a channel of charged air called a leader that reaches down to the ground below. The leaders attract other charged ground-based channels called streamers.When the stepped leader from the cloud meets a returning streamer from the ground, the path is ready. An electrical current called the return stroke, travels back up the path. This return stroke releases tremendous energy, bright light and thunder.The typical stroke can last only 30 milliseconds, so four to five strokes may happen in the blink of an eye. Despite the old saying, lightning does strike the same place twice.To review, lightning is created by the attraction between opposite charges, the same force that creates static electricity. But lightning uses huge opposite charges to produce an electrical current that's nothing like what you'd get from static electricity.
Yes, thunder and lightning can occur in a cyclone due to the intense convection and strong winds within the storm. The lightning is caused by the collision of ice particles in the clouds, and the thunder is the sound waves produced by the rapid heating and cooling of the air around the lightning strike.
Lightning is a powerful electrical discharge produced during a thunderstorm. The electric current is very hot and causes thunder. Sometimes it happens between clouds. Sometimes (in the rain) it goes from cloud to ground. If it goes from cloud to ground, it can strike a person. Around 2000 people are struck by lightning each year.