Cumulus clouds are a type of cloud that is fluffy, white, and often described as having a "cotton-like" appearance. They are generally associated with fair weather, but can also develop into larger storm clouds under the right conditions.
Cumulus clouds form as a result of convection, which occurs when warm air rises and cools as it ascends. As the air cools, water vapor in the air condenses to form water droplets, which collect to create the puffy, billowy appearance of cumulus clouds.
Here are some key points to remember about cumulus clouds:
Studying the formation and characteristics of cumulus clouds can provide insight into the dynamic processes of Earth's atmosphere and contribute to a greater understanding of weather patterns and meteorology.