Cumulus clouds appear as cotton ball-like clouds formed by convection, while cumulonimbus clouds are tall and linked to thunderstorms. The vertical development of cumulus clouds aids in weather predictions through infrared observations.
Cumulus clouds are significant due to their appearance as small, cotton ball-like clouds formed by convection. They are known as 'fair-weather' clouds, indicating pleasant conditions. On the other hand, cumulonimbus clouds are the tallest clouds, reaching the stratosphere and associated with thunderstorms.
Vertically developed clouds, such as cumulus clouds, exhibit vertical growth, differing from layered clouds. Cumulus clouds are categorized as cumulo-form clouds due to their vertical development. The height of cumulus clouds plays a role in weather prediction, as infrared observations can help indicate rain rate and cloud top temperature.
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