In stormy conditions, strong winds in a cloud can lead to a separation of charges, with the top acquiring a positive charge and the bottom a negative charge.
When strong winds occur in a cloud, they can cause the displacement of electrons from the top to the bottom of the cloud. This results in the top acquiring a positive charge and the bottom acquiring a negative charge.
The movement of electrons causes charge imbalances within the cloud, leading to distinct distributions of positive and negative charges. This phenomenon is crucial in understanding lightning strikes and cloud electrification processes.
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