Cirrus clouds are high-altitude clouds that are thin, wispy, and often appear feathery. They are composed mostly of ice crystals and are found at altitudes above 20,000 feet. Cirrus clouds are typically associated with fair weather but can also indicate approaching storms.
Cirrus clouds form when water vapor in the atmosphere condenses directly into ice crystals at high altitudes where the temperature is below freezing. These ice crystals then aggregate to form the thin, wispy structures characteristic of cirrus clouds.