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There is much confusion over the "up" or "down" motion of lightning bolts, but in most cases it is initiated by the flow of negative ions in clouds to a positively charged point at another point (cloud or ground). What is referred to as "lightning" is a luminous path of superheated air caused by repeated current flows from the ground and the air. In certain cloud types, the interaction of ice and water (and possibly the Earth's magnetic field) creates a surplus of negatively charged particles, usually near the bottom of the cloud. Where the ground and objects below have accumulated positive charges, an electric discharge can occur. This is preceded by "step leaders" moving down from the clouds and "positive leaders" moving up from the ground. Where these streams come in contact, the negative ions flow to the ground, followed by a return flow of positive ions. This can occur multiple times in the same lightning strike.

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