
Clouds develop from water vapour that cools within rising air. Collecting on dust particles and other cloud seeds, water coalesces into droplets and ice crystals that scatter sunlight so clouds appear white. The temperature, wind and moisture determine the size, shape and type of clouds. There are three main types: cumulus, stratus and cirrus.
Cumulus, meaning “heap”, are puffy clouds like cotton balls. They form in an unstable humid atmosphere where water condenses in bubbles of warm air. They float across the sky, a picturesque backdrop to a beautiful sunny day. Cumulus clouds can be as low as 1,000 feet (305 m) or as high as 15,000 feet (4,570 m). When the sky fills with cumulus clouds, it’s a sign the weather is changing. As they grow, they can become rain clouds.
Cloud names are combined to describe specific types. Altocumulus are mid-level clouds covering the sky. Cirrocumulus are high white patches with cloudlets hinting of rain. Cumulonimbus, or thunderheads, are threatening dark clouds that form on stormy days. These towering giants can be 10 miles (16 km) tall and cause severe rain, snow, hail and lightning.