A pileus (//; Latin for "cap"), also called scarf cloud or cap cloud, is a small, horizontal, lenticular cloud appearing above a cumulus or cumulonimbus cloud. Pileus clouds are often short-lived, with the main cloud beneath them rising through convection to absorb them. They are formed by strong updraft at lower altitudes, acting upon moist air above, causing the air to cool to its dew point. As such, they are usually indicators of severe weather, and a pileus found atop a cumulus cloud often foreshadows transformation into a cumulonimbus cloud, as it indicates a strong updraft within the cloud.
Sometimes several pileus clouds are observed above each other. The bright iridescent colors seen in pileus are sunlight diffracted in water vapor. Iridescent colors are strongest when the diffracting droplets are small and similar in size. The newly formed pileus droplet all of similar provenance are ideal for iridescence.
Pilei clouds indicate the parent cloud is growing rapidly, has plenty of moisture, and is highly unstable. This means the parent cloud could quickly grow to become a cumulonimbus cloud and continue to grow into a cumulonimbus incus cloud.
- 1965-, Hamblyn, Richard (2017-05-15). Clouds. London, UK. ISBN 9781780237701. OCLC 1000297560.CS1 maint: numeric names: authors list (link)
- Ulrike, Lohmann. An Introduction to Clouds : From the Microscale to Climate. Lüönd, Felix,, Mahrt, Fabian. Cambridge. p. 288. ISBN 9781139087513. OCLC 953455396.
- Holzmann, B. G.; Cumberledge, A. A. (October 1946). "Weather and The Atomic Bomb Tests at Bikini (II)". Bulletin of the American Meteorological Society. 27 (8): 435–437. Bibcode:1946BAMS...27..435H. doi:10.1175/1520-0477-27.8.435.
- "Pileus - AMS Glossary". glossary.ametsoc.org. Retrieved 2019-01-25.
- "Iridescent Pileus". Atmospheric Optics. Retrieved 2019-01-25.
- "Velum". Meteorological glossary. American Meteorological Society. Retrieved May 2, 2014.