The Pileus cloud (or Cap Cloud) is a lenticular formation that appears like a “hat” atop developing cumulonimbus clouds. Discover its origin, characteristics, and meteorological significance.
Among the most spectacular and short-lived cloud formations is the Pileus cloud (also called Cap Cloud), a peculiar smooth “hat” that crowns developing convective towers. These clouds are visual indicators of rapid vertical growth in the atmosphere.
In this article, you’ll explore:
✔ What a Pileus cloud is and how it forms
✔ Differences from other lenticular clouds
✔ What it reveals about atmospheric conditions
✔ Where and when to observe them
The Pileus (Latin for “hat”) is an accessory cloud that forms when a rising current of moist air (from a developing cumulus or cumulonimbus) is forced to condense upon encountering a stable air layer above.
A Pileus cloud indicates:
Pileus Cloud | Standard Lenticular Cloud |
---|---|
Always attached to cumulus/cumulonimbus | Forms independently over mountains |
Hat-shaped over convective tower | Isolated saucer shape |
Short lifespan (minutes) | Can persist for hours |
✅ Accessory cloud shaped like a smooth hat over convective towers.
✅ Sign of rapid vertical growth and potential storms.
✅ Ephemeral: lasts only minutes before being pierced.
✅ Don’t confuse with classic lenticular clouds (which are stationary).
Q: Can a Pileus produce precipitation?
A: No, it’s just temporary condensation. Rain (if any) comes from the cumulonimbus below it.
Q: Are they visible from satellites?
A: Rarely, due to their small size and brief existence.
Q: Are they dangerous for aviation?
A: Not directly, but their associated cumulonimbus can be.