Cumulonimbus clouds are large, dense, towering clouds that are associated with thunderstorms and severe weather. They are known for their distinctive anvil shape at the top and can extend high into the atmosphere.
Cumulonimbus clouds form through the convection process, where warm, moist air rises and cools, leading to condensation and cloud formation. These clouds can develop vertically, reaching heights of 20 kilometers or more, due to strong updrafts.
Cumulonimbus clouds play a crucial role in the Earth's water cycle, as they are responsible for producing intense rainfall and are essential for replenishing freshwater sources. Additionally, they contribute to the redistribution of heat in the atmosphere through the release of latent heat during condensation.