Look up and read the sky like a meteorologist.
Clouds form when air becomes saturated and water vapor condenses onto microscopic particles. Their shapes reflect rising air, stable layers, wind, moisture, and temperature.




Cumulus clouds look like puffy heaps.
Learn MoreStratus clouds form broad low layers.
Learn MoreCirrus clouds form high in the troposphere and are made mainly of ice crystals.
Learn MoreCumulonimbus clouds are thunderstorms.
Learn MoreAltostratus and altocumulus occupy middle levels.
Learn MoreCloud droplets are extremely small.
Learn MoreCloud base height depends partly on humidity and temperature.
Learn MoreChanging cloud patterns can reveal changing weather.
Learn MoreSmall fair-weather cumulus clouds form in rising bubbles of warm air.
They can produce gray skies, mist, drizzle, or light precipitation.
They can appear long before an approaching weather system.
Strong updrafts can build towers reaching near the top of the troposphere.
They can signal moisture spreading ahead of a storm system.
They can remain suspended until collision, freezing, or ice processes create larger precipitation particles.
When rising air cools to its dew point, condensation begins.
Meteorologists combine clouds with radar, satellite, pressure, wind, and model data rather than relying on clouds alone.