After lightning strikes, electrons from the cloud discharge into the Earth, neutralizing the charge imbalance, but the upper part of the cloud retains its positive charge. The mechanism of charge acquisition in clouds is still debated in the scientific community. Lightning typically occurs between the cloud and the Earth rather than within the cloud due to the potential energy favoring discharge to the ground. The Earth's vast charge density allows it to absorb the extra electrons without significant long-term imbalance. Overall, while the cloud loses electrons, the positive charges remain, and the system does not need to return to a complete circuit.