Open main menu
Home
Random
Recent changes
Special pages
Community portal
Preferences
About Wikipedia
Disclaimers
Incubator escapee wiki
Search
User menu
Talk
Dark mode
Contributions
Create account
Log in
Editing
Wall cloud
(section)
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
=== Associated features === [[File:Wall Cloud in NE Colorado.jpg|thumb|left|A wall cloud with '''tail cloud'''.]] Some wall clouds have a feature similar to an "eye", as in a [[mesoscale convective vortex]]. Attached to many wall clouds, especially in moist environments, is a '''cauda'''<ref name=ICA2017/> ('''tail cloud'''), a tail-like band of cloud extending from the wall cloud toward the [[precipitation]] core.<ref name=":0">{{Cite web |date=July 20, 2021 |title=Cauda | International Cloud Atlas |url=https://cloudatlas.wmo.int/en/clouds-supplementary-features-cauda.html |archive-url=https://web.archive.org/web/20210720112818/https://cloudatlas.wmo.int/en/clouds-supplementary-features-cauda.html |archive-date=2021-07-20}}</ref> It can be thought of as an extension of the wall cloud in that the tail cloud is connected to the wall cloud and condensation forms for a similar reason.{{Citation needed|date=July 2024}} Cloud elements may be seen to be moving into the wall cloud, as it is also an inflow feature.<ref name=":0" /> Most movement is horizontal, but some rising motion is also often apparent at the junction between the tail cloud and the wall cloud.<ref name=":0" /> Some wall clouds also have a band of cloud fragments encircling the top of the wall cloud where it meets the ambient cloud base; this feature is a '''collar cloud'''.<ref>{{cite book |last = Branick |first = Michael L. |title = NOAA Technical Memorandum NWS SR-145: A Comprehensive Glossary of Weather Terms for Storm Spotters |publisher = National Weather Service |date = 1996 |url = http://www.srh.noaa.gov/oun/?n=spotterglossary2#Collar%20Cloud |oclc = 39732655 }}</ref> Another accessory cloud is the '''flumen''', commonly known as the '''beaver's tail'''.<ref name="ICA2017" /> It is formed by the warm, humid [[inflow (meteorology)|inflow]] of a strong thunderstorm, and is often mistaken for tornadoes.<ref name="ICA2017" /> Although the presence of a flumen is associated with tornado risk,{{Citation needed|date=July 2024}} the flumen does not rotate.<ref name="ICA2017" />
Edit summary
(Briefly describe your changes)
By publishing changes, you agree to the
Terms of Use
, and you irrevocably agree to release your contribution under the
CC BY-SA 4.0 License
and the
GFDL
. You agree that a hyperlink or URL is sufficient attribution under the Creative Commons license.
Cancel
Editing help
(opens in new window)