Cirrus clouds are high-altitude clouds that are thin, wispy, and often have a feathery appearance. They are composed of ice crystals and are found at altitudes of 20,000 to 40,000 feet. Cirrus clouds are typically associated with fair weather, but they can also indicate the approach of a storm.
Cirrus clouds are formed when water vapor in the atmosphere condenses directly into ice crystals at high altitudes where temperatures are very cold. These ice crystals then combine to form the thin, wispy appearance of cirrus clouds.
Use the following study guide to review and reinforce your understanding of cirrus clouds: