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
 
development
 
cloud types
 
precipitation

Development
 
states of water
 
relative humidity
 
rising air
 
convection
 
convergence
 
topography
 
fronts
 
rain or snow

User Interface
 
graphics
text

.
Lifting Due To Topography
produces orographic clouds

When air is confronted by a mountain, it is lifted up and over the mountain, cooling as it rises. If the air cools to its saturation point, the water vapor condenses and a cloud forms.

These types of clouds are called "orographic clouds", which develop in response to lifting forced by the topography the earth.

[Image: lee mountain wave clouds (78K)]
Photograph by: Holle

The exact type of cloud that develops depends upon the moisture content and stability of the air.



convergence
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.

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