Cirrus clouds are high-altitude clouds that are thin, wispy, and often have a feathery appearance. They are composed of ice crystals and are commonly found at altitudes above 20,000 feet.
Cirrus clouds form in the upper troposphere when water vapor condenses directly into ice crystals. They can be created by the lifting of air masses, often associated with the approach of a front, or by the presence of high-altitude wind patterns.