Gustando (gust + tornado) (1991)
Bapopik at AOL.COM
Bapopik at AOL.COM
Thu Apr 26 05:45:05 UTC 2007
A weather formation whipped through the Texas-Mexico border at Eagle
Pass/Piedras Negras last night. It was not pleasant at all in these parts, either.
...
OED doesn't have "gustnado"? Citations from at least 1992 come from Texas.
...
...
...
_http://www.barrypopik.com/index.php/texas/entry/gustnado_gust_tornado/_
(http://www.barrypopik.com/index.php/texas/entry/gustnado_gust_tornado/)
...
Gustnado (Gust + Tornado)
A “gustnado” is a portmanteau of the words “gust” and “tornado.”
Gustnadoes are short-lived, shallow mini-cylcone formations that develop on a gust
front along with thunderstorms or showers.
The word “gustnado” has been cited from at least 1991; its origin is
unknown, but the term is popular in Texas and other parts of _Tornado Alley._
(http://www.barrypopik.com/index.php/texas/entry/tornado_alley/)
_National Weather Service (Morristown, TN)_
(http://www.srh.noaa.gov/mrx/svrevnts/may15tornado/gustnadodef.htm)
Gustnado definition
A slang term for a short-lived, ground-based, shallow, vortex that develops
on a gust front associated with either thunderstorms or showers. They may
only extend to 30 to 300 feet above the ground with no apparent connection to
the convective cloud above. They may be accompanied by rain, but usually are ‘
wispy’, or only visible as a debris cloud or dust whirl at or near the ground.
Wind speeds can reach 60 to 80 mph, resulting in significant damage, similar
to that of a F0 or F1 tornado. However, gustnadoes are not considered to be
a tornado, and some cases, it may be difficult to distinguish a gustnado from
a tornado. Gustnadoes are not associated with storm-scale rotation (i.e.
mesocyclones) that is involved with true tornadoes; they are more likely to be
associated visually with a shelf cloud that is found on the forward side of a
thunderstorm.
_Wikipedia; Gustnado_ (http://en.wikipedia.org/wiki/Gustnado)
A gustnado is a colloquial expression for a type of short-lived, shallow,
cyclonic circulation that can form in a severe thunderstorm. While it derives
its name from the tornado, it has little in common with tornadoes structurally
in terms of vertical development, or in regard to intensity, longevity, and
formative process (classic tornadoes are associated with mesocyclones).
The average gustnado lasts no more than a few seconds to a few minutes each,
although there can be several generations and simultaneous swarms. Most have
the winds of a F0 or F1 tornado, and are commonly mistaken for tornadoes.
However, unlike tornadoes, the rotating column of air in a gustnado usually
does not extend all the way to the base of the thundercloud. Gustnadoes actually
have more in common with whirlwinds (which include dust devils, whirldwinds
that form due to superheated surface layers and stretched vorticity, most
commonly on sunny, warm days with light winds). They are not considered true
tornadoes (unless they connect the surface to the ambient cloud base) by most
meteorologists and are not included in tornado statistics. Sometimes referred
to as spin-up tornadoes, that term more correctly describes the rare tornadic
gustnado that connects the surface to the ambient cloued base, or to
relatively brief tornadoes associated with a mesovortex.
The most common setting for a gustnado is on the outflow from a severe
thunderstorm (58+ mph winds). They are triggered by gust fronts (hence the name)
in thunderstorms. The cool air in the gust front acts like a mesoscale cold
front, it slices under the warm air ahead of it, creating upward motions and
turbulent interactions. The friction from this interaction creates spinning
columns of air, or eddys, which can create a gustnado (to get the general idea
of this, picture an area of leaves swirling on a windy day, just on a much
larger scale).
_Google Groups: sci.geo.meteorology_
(http://groups.google.com/group/sci.geo.meteorology/browse_thread/thread/6cb1afede1138895/a1f3d0e8ac863f88?lnk=st&q=gu
stnadoes&rnum=69&hl=en#a1f3d0e8ac863f88)
Newsgroups: sci.geo.meteorology
From: _cur... at nsslsun.gcn.uoknor.edu_ (mailto:cur... at nsslsun.gcn.uoknor.edu)
(Brian Curran)
Date: 11 May 91 04:49:55 GMT
Local: Sat, May 11 1991 12:49 am
Subject: Re: willies willies/dust devils
“Greg Stumpf knows gustnadoes”
_Google Groups: sci.geo.meteorology_
(http://groups.google.com/group/sci.geo.meteorology/browse_thread/thread/1b625a2fb02cae31/d13457c24dd1a3ec?lnk=st&q=gu
stnado&rnum=113&hl=en#d13457c24dd1a3ec)
Newsgroups: sci.geo.meteorology
From: _mfos... at ALLIANT.BACKBONE.uoknor.edu_
(mailto:mfos... at ALLIANT.BACKBONE.uoknor.edu) (Marc Foster)
Date: Mon, 20 Jul 1992 15:38:48 GMT
Local: Mon, Jul 20 1992 11:38 am
Subject: DFW Gustnado
I saw my first gustnado in a long while yesterday at the north end of
Dallas/Fort Worth International Airport.
_Google Groups: sci.geo.meteorology_
(http://groups.google.com/group/sci.geo.meteorology/browse_thread/thread/cb2995973b14b477/dfd303d9ca23c355?lnk=st&q=gu
stnadoes&rnum=68&hl=en#dfd303d9ca23c355)
Newsgroups: sci.geo.meteorology
From: _stu... at nsslsun.nssl.uoknor.edu_
(mailto:stu... at nsslsun.nssl.uoknor.edu) (Greg Stumpf)
Date: Thu, 23 Jul 1992 15:29:48 GMT
Local: Thurs, Jul 23 1992 11:29 am
Subject: Re: Gustnadoes
>a definition/my best understanding of what a gustnado is…
>Gustnadoes form on the leading edge of thunderstorms, where the outflow
>boundary/gustfront is located. Now if you have a dust devil or some
>similar broad low power circulation ahead of the gust front, the
interaction
>of the front with the circulation stretches the vortex and narrows the
>diameter. Since energy must be conserved, the angular velocity is forced
>to increase (spinning figure skater bringing her arms close to the body).
>This is the basic form of the gustnado. They don’t normally have winds
>in excess of F0, and don’t derive their energy in the same manner as a
>tornado, and since the circulation is not pendant to the base of the storm,
>it is not a tornado (by definition). The only way they are visible from
>the dirt raised by the winds.
Good description. Many argue that a gustnado *is* a tornado beacuse it is a
violently rotating column of air on the ground, but seem to forget that the
definition of a true tornado says that this column of air is *pendant from
the cumulonimbus cloud*. This does not mean, however, that you can have very
damaging gustnadoes if conditions are met. Also, some gustnadoes can be
entrained into the thunderstorm updraft, becoming tornadoes (or hybrids).
8 October 1992, For Worth (TX) Star-Telegram (Google News Archives):
“We call it a ‘gustnado.’ It was a very small-scale tornado in northwest
Dallas County on the leading edge of the squall line.”
8 November 1994, Syracuse (NY) Herald-Journal, pg. C3:
Weather experts say the rare twister was formed by a “gust front” generated
from high winds flowing out of a nearby thunderstorm. This type of phenomena
is also referred to as a “gustnado.”
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