Negative lightning occurs when negative charges at the base of the storm cloud travel toward the ground in a “stepped leader” and the positive charges in taller ground objects travel toward the negative charge in a “streamer.” When these channels connect, there is an electrical transfer. Negative lightning usually has two or more discharges, or strokes.
Positive lightning, which typically only has one stroke, originates in the more positive upper portion of the thunderstorm. In this case, the stepped leaders are positively charged, and the streamers are negatively charged when they collide. This leads to a net transfer of positive charge from cloud to ground. While positive lightning occurs less than 5% of the time, it is more dangerous than negative lightning because its electric fields are stronger, its flash duration is longer, and the peak charge is up to 10 times greater than negative cloud-to-ground strikes.