Thunderstorm

- Thunderstorm is the correct answer because it is the only option that involves the meeting of negative charge of electricity and positive charge of rain inside a cloud that leads to the sparking of electricity.
- Thunderstorms are weather phenomena characterized by the presence of lightning, thunder, and heavy rain. They typically occur when warm air rises rapidly in the atmosphere, forming tall clouds called cumulonimbus clouds.
- Within a thunderstorm cloud, there are different regions with varying electrical charges. The upper part of the cloud tends to have a positive charge, while the lower part has a negative charge.
- Raindrops in the cloud also acquire a positive charge due to a process called collision and separation. When water droplets collide with ice crystals in the cloud, they become positively charged, while the ice crystals acquire a negative charge.
- As the positive and negative charges separate within the cloud, an electric field is formed. This electric field becomes stronger as the charge separation increases.
- Eventually, the electric field becomes strong enough to overcome the resistance of the air and a discharge of electricity occurs. This discharge is what we perceive as lightning. It is the sudden flow of electrons from the negatively charged region to the positively charged region within the cloud or between the cloud and the ground.
- The discharge of electricity during a thunderstorm is accompanied by the release of intense heat, light, and sound energy. The heat causes the surrounding air to rapidly expand, creating a shock wave that we hear as thunder.
- Thunderstorms can be dangerous due to the potential for lightning strikes, strong winds, hail, and heavy rain. It is important to seek shelter indoors during a thunderstorm and avoid tall objects, open fields, and bodies of water.
- In conclusion, thunderstorms occur when the negative charge of electricity and positive charge of rain meet inside a cloud, leading to the sparking of electricity in the form of lightning and the subsequent production of thunder.

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