virga
(
Also called Fallstreifen, fallstreaks, precipitation trails.) Wisps or streaks of water or
ice particles falling out of a
cloud but vaporizing before reaching the earth's surface as
precipitation.
Virga is frequently seen trailing from
altocumulus and
altostratus clouds, but also is discernible below the bases of high-level
cumuliform clouds from which precipitation is falling into a dry
subcloud layer. It typically exhibits a hooked form in which the streaks descend nearly vertically just under the precipitation source but appear to be almost horizontal at their lower extremities. Such curvature of virga can be produced simply by effects of strong vertical
wind shear, but ordinarily it results from the fact that
droplet or
crystal vaporization decreases the
particle terminal
fall velocity near the ends of the streaks. Under some conditions, virga is associated with dry
microbursts, which are formed as a product of the
vaporization.
See cloud classification.
Term edited 14 April 2015.
Copyright 2022 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.