What forms on the forward edge of a fully developed cumulonimbus cloud?

In a fully developed cumulonimbus cloud, what primarily forms on the forward edge is a thunderstorm. Cumulonimbus clouds are associated with intense weather phenomena, and when they are fully developed, they can produce severe thunderstorms that often include heavy rainfall, lightning, and strong updrafts.

The forward edge of a mature cumulonimbus cloud is characterized by the outflow boundary where cool air from precipitation downdrafts pushes ahead of the storm. This action can enhance the existing lift from the updrafts, leading to the development of new storm cells, which can result in further thunderstorm activity.

While tornadoes can occasionally occur in conjunction with severe thunderstorms, they specifically develop from supercell thunderstorms rather than being a direct product of all cumulonimbus clouds. Hurricanes and blizzards are also not formed directly from these clouds but are separate storm systems with very different characteristics and formation processes.