Special Clouds > Pileus Clouds
Learning Goal 1b. Recognize special clouds (e.g. castellanus,
billow, lenticular, rotor, banner, fractus, etc.)
Pileus is a scarf cloud that forms
above a rapidly rising cumulus cloud such as a cumulus
congestus cloud. It is very short lived (minutes).
NOTE: The pileus cloud is
not a thunderstorm anvil cloud.
When a cumulus congestus cloud rises through the ambient
environment, it pushes the environmental air out of the way. Some of
this air is pushed off to the sides of the rising cumulus; some, just
above the top of the cumulus, are pushed upward, just ahead of the
rising cumulus top. If this environmental air has thin layers of humid
and dry air, then when this sandwich of air is pushed upward, the humid
air layers can make a thin cloud layer — the pileus cloud.
But very quickly the rising top of the cumulus congestus cloud
pushes up through the pileus cloud, causing the pileus to disappear.
Here is a sequence of photos showing the evolution of a thin, curved
pileus cloud forming just above the top of the tallest cumulus
congestus cloud. The photos were taken at roughly 30 second intervals.
Although pileus are interesting, their existence does not tell you
anything useful that can help your flying, sailing, or snowboarding.
However, the cumulus congestus cloud implies strong updrafts and
turbulence, and can possibly grow into a thunderstorm later.
For more photos of pileus, do a web search on images of "pileus
clouds".
Keywords: cumulus congestus, pileus clouds
Extra info for experts;
Not Needed for this
Course.
Use this expert_resources link to find all the items
listed below:
- Item
- Topic
- World.A.1. - World Meteorological Organization (WMO)
"International Cloud Atlas"
- USA.B.1. - Wikipedia list
of cloud types
- World.A.2. - WMO: Manual on Cloud Observations (an old,
outdated document)
- USA.A.1. - American Meteorological Society (AMS): Glossary of
Meteorology
- USA.C.1. - Practical Meteorology (PrMet): Chapter 6, Clouds
Image credits. All figures copyright by Roland Stull.