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Which type of particles will gather near the bottom of the storm cloud if it releases electrical energy as lightning?
Wiki User
∙ 10y ago
positive and negative have the same change
Wiki User
∙ 10y ago
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Thunder is created by?
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.
How is electricity produced in lightning?
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.
How does the principle of opposite charges attracting help to produce lightning?
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.
Does lightning come from the clouds?
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.
In sedimentation what order do the layers settle in?
Oldest at the bottom, newest at the top. OR Largest particles first, finest particles last.
Thunder is created by?
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.
How are Subatomic Particles involved in 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
How is electricity produced in lightning?
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.
How does the principle of opposite charges attracting help to produce lightning?
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.
How was lightning created?
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.
How does lightning occur?
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.
What happens to the particles in a suspension if they are not being mixed?
These particles will settle to the bottom of the container.
Lightning forms when?
Lightning happens when the negative charges (electrons) in the bottom of the cloud are attracted to the positive charges (protons) in the ground.
Does lightning come from the clouds?
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.
Positive and negative charges in cumulonimbus clouds?
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.
What do you call a mixture that has little particles that settle in the bottom?
a suspension.
What particles in one of these will eventually settle out at the bottom?
bro what are you saying
