WW2010
University of Illinois

WW2010
 
welcome
 
online guides
 
archives
 
educational cd-rom
 
current weather
 
about ww2010
 
index

Online Guides
 
introduction
 
meteorology
 
remote sensing
 
reading maps
 
projects, activities

Meteorology
 
introduction
 
air masses, fronts
 
clouds, precipitation
 
el nino
 
forces, winds
 
hurricanes
 
hydrologic cycle
 
light, optics
 
midlatitude cyclones
 
severe storms
 
weather forecasting

Clouds, Precipitation
 
introduction
 
mechanisms
 
precip processes
 
high level clouds
 
mid level clouds
 
low level clouds
 
vertically developed
 
other cloud types

Other Cloud Types
 
contrails
 
billow clouds
 
mammatus
 
orographic
 
pileus

User Interface
 
graphics
text

.
Pileus Clouds
smooth capping clouds

Pileus (Latin for "skullcap") is a smooth cloud found either at the top of or attached to a mountain or a growing cumulus tower. Pileus clouds form when air at higher levels is forced to rise. In the photograph below, a pileus cloud is attached to the top of a cumuliform cloud.

[Image: pileus attached to cumuliform cloud top (88K)]


The air that is lifted to form the pileus clouds is drier and consequently has a much higher lifting condensation level than does the moist air from lower levels often responsible for cumulus clouds. Therefore, there is little tendency for any significant vertical growth in pileus clouds, which is why the cloud takes on a smoother horizontal shape.


Terms for using data resources. CD-ROM available.
Credits and Acknowledgments for WW2010.
Department of Atmospheric Sciences (DAS) at
the University of Illinois at Urbana-Champaign.