Pyrocumulonimbus

From Glossary of Meteorology
Revision as of 04:36, 1 March 2021 by Rbrandt (talk | contribs) (→‎Pyrocumulonimbus)
(diff) ← Older revision | Latest revision (diff) | Newer revision → (diff)

Pyrocumulonimbus

An extreme manifestation of a pyrocumulus (pyroCu) cloud, generated by the heat of a wildfire, that often rises to the upper troposphere or lower stratosphere. Often abbreviated “pyroCb.” The pyroCb is distinctive owing to the presence of smoke, giving the cloud an off-white color and peculiar signatures at certain infrared wavelengths. The distinguishing characteristics of pyroCb, as opposed to pyroCu, are production of lightning, thunder, or hail or a fibrous or diffuse upper portion. The discovery of hemisphere-scale stratospheric smoke plumes traceable to pyroCbs reveals their buoyant energy and potential to inject smoke into the lower stratosphere. A pyrocumulonimbus cloud is also known as a pyrocumulonimbus flammagenitus cloud (CbFg).

World Meteorological Organization, 2017. International Cloud Atlas. Available at https://cloudatlas.wmo.int/en/home.html.



Term edited 1 March 2021


Copyright 2024 American Meteorological Society (AMS). For permission to reuse any portion of this work, please contact permissions@ametsoc.org. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act (17 U.S. Code § 107) or that satisfies the conditions specified in Section 108 of the U.S.Copyright Act (17 USC § 108) does not require AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a website or in a searchable database, or other uses of this material, except as exempted by the above statement, require written permission or a license from AMS. Additional details are provided in the AMS Copyright Policy statement.