cirrifeathery

Cirrifeathery is a term used in meteorology to describe a type of cloud formation characterized by its wispy, feathery appearance. The term is derived from the Latin word "cirrus," meaning "curl of hair," and the Old English word "feathery," referring to the appearance of the clouds. Cirrifeathery clouds are typically high-altitude clouds, forming at altitudes above 20,000 feet (6,000 meters). They are composed of ice crystals and are often associated with fair weather conditions. The clouds can take various shapes, including thin, wavy strands, tufts, or patches, and are often seen in the sky during the day or night. Cirrifeathery clouds are a common sight in the sky and are often used as an indicator of atmospheric stability and the presence of high-altitude winds.