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A pileus (/ˈpaɪliəs/; 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, appearing for typically only a few minutes,[1] with the main cloud beneath them rising through convection to absorb them. Furthermore, the clouds are typically formed by drier air with a higher lifting condensation level, which often prevents vertical growth and leads to the smooth horizontal cap shape that the cloud is named for.[2]
They are formed by strong updraft at lower altitudes, acting upon moist air above, causing the air to cool to its dew point as it rises.[3][4] 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.[3][5]
Pilei can also form above mountains, ash clouds, and pyrocumulus clouds from erupting volcanoes.[6] Pilei form above some mushroom clouds of high-yield nuclear detonations.[7]
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