Advanced Intermediate Beginner Home English Spanish

Cirrus



Photograph of cirrus clouds
Click on image for full size version (64K JPG)
Courtesy of Lisa Gardiner

Cirrus (weather symbol - Ci) clouds are the most common of the High Cloud (5000-13000m) group. They are composed entirely of ice and consist of long, thin, wispy streamers. They are commonly known as "mare's tails" because of their appearance.

The reason for the long tails is primarily due to the wind. In the upper troposphere, the winds travel at very high speeds from west to east (in the Northern Hemisphere). The winds are so strong at these altitudes that they actually stretch the crystalline structure of the Cirrus cloud, creating a tail.

Cirrus clouds are usually white and predict fair weather.



Next Cloud Type
Back to Cloud Types

How Clouds Form

Cloud Formation Due to Weather Fronts


Credits Settings Sponsorship Membership Contact us About the site Site map Help Myths People News Arts, books and film Images and multimedia Tours Life Geology Physics Space weather Space Missions Solar system Astronomy and the Universe Shop for science stuff Games Ask a scientist Journal Comets Dwarfs Neptune Uranus Saturn Jupiter Asteroids Mars Earth Venus Mercury Sun Teacher resources Kids Space Search Home


Last modified September 24, 2007 by Becca Hatheway.
The source of this material is Windows to the Universe, at http://www.windows.ucar.edu/ at the University Corporation for Atmospheric Research (UCAR). © The Regents of the University of Michigan. Windows to the Universe® is a registered trademark of UCAR. All Rights Reserved. Site policies and disclaimer