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.
Formation
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.
They are fluffy, white clouds with flat bases and rounded tops.
Cumulus clouds are generally associated with fair weather, but can develop into larger storm clouds under the right conditions.
They are often observed on sunnydays and can create picturesque skies.
Learning to identify different types of clouds, including cumulus clouds, can help in predicting weatherpatterns and understanding atmospheric processes.