Английская Википедия:Anticyclonic tornado

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Шаблон:Short description An anticyclonic tornado is a tornado which rotates in a clockwise direction in the Northern Hemisphere and a counterclockwise direction in the Southern Hemisphere. The term is a naming convention denoting the anomaly from normal rotation which is cyclonic in upwards of 98 percent of tornadoes.Шаблон:Citation needed Many anticyclonic tornadoes are smaller and weaker than cyclonic tornadoes, forming from a different process, as either companion/satellite tornadoes or nonmesocyclonic tornadoes.

Файл:2016-05-22 Anticyclonic tornado, Big Spring, Texas.jpg

An anticyclonic tornado near Big Spring, Texas on May 22, 2016 captured by storm chaser Aaron Jayjack.

Formation

Most strong tornadoes form in the inflow and updraft area bordering the updraft-downdraft interface (which is also near the mesoscale "triple point") zone of supercell thunderstorms. The thunderstorm itself is rotating, with a rotating updraft known as a mesocyclone, and then a smaller area of rotation at lower altitude the tornadocyclone (or low-level mesocyclone) which produces or enables the smaller rotation that is a tornado. All of these may be quasi-vertically aligned continuing from the ground to the mid-upper levels of the storm. All of these cyclones and scaling all the way up to large extratropical (low-pressure systems) and tropical cyclones rotate cyclonically. Rotation in these synoptic scale systems stems partly from the Coriolis effect, but thunderstorms and tornadoes are too small to be significantly affected. The common property here is an area of lower pressure, thus surrounding air flows into the area of less dense air forming cyclonic rotation. The rotation of the thunderstorm itself is induced mostly by vertical wind shear, specifically clockwise turning as altitude increases (called a veered vertical profile, although backed profiles can occur with anticyclonic supercells).

Various processes can produce an anticyclonic tornado. Most often they are satellite tornadoes of larger tornadoes which are directly associated with the tornadocyclone and mesocyclone. Occasionally anticyclonic tornadoes occur as an anticyclonic companion (mesoanticyclone) to a mesocyclone within a single storm. Anticyclonic tornadoes can occur as the primary tornado with a mesocyclone and under a rotating wall cloud. Also, anticyclonic supercells (with mesoanticyclone), which usually are storms that split and move to the left of the parent storm motion, though very rarely spawning tornadoes, spawn anticyclonic tornadoes. There is an increased incidence of anticyclonic tornadoes associated with tropical cyclones, and mesovortices within bow echoes may spawn anticyclonic tornadoes.

The first anticyclonic tornado associated with a mesoanticyclone was spotted on WSR-88D weather radar in Sunnyvale, California on May 4, 1998. The tornado was an F2 on the Fujita Scale.

Known "anticyclonic tornado" events

Date	F#/EF# Rating	Location	Notes and References
8 June 1951	bgcolor=#Шаблон:Storm colour | F3	Corn, Oklahoma	First known tornado filmed in the US, a companion or cyclic tornado to another significant tornado. It is officially listed as one tornado event by the CDNS report and the NCDC.
6 June 1975	bgcolor=#Шаблон:Storm colour | F1	Freedom, Oklahoma	One of three tornadoes to touch down in the area.
13 June 1976	bgcolor=#Шаблон:Storm colour | F3	Jordan, Iowa	Tornadoes of 1976#June 13 – A satellite tornado to the F5 Jordan, Iowa tornado.
3 June 1980	bgcolor=#Шаблон:Storm colour | F1	Grand Island, Nebraska	1980 Grand Island tornado outbreak – First of three anticyclonic tornadoes in the area that night.
3 June 1980	bgcolor=#Шаблон:Storm colour | F3	Grand Island, Nebraska	1980 Grand Island tornado outbreak – Second of three anticyclonic tornadoes in the area that night.
3 June 1980	bgcolor=#Шаблон:Storm colour | F1	Grand Island, Nebraska	1980 Grand Island tornado outbreak – Last of three anticyclonic tornadoes in the area that night.
4 April 1981	bgcolor=#Шаблон:Storm colour | F4	West Bend, Wisconsin	1981 West Bend tornado – Strongest anticyclonic tornado ever recorded.
13 June 1998	bgcolor=#Шаблон:Storm colour | F2	North Oklahoma City, Oklahoma	Tornado outbreak of June 13, 1998 – Sixth of seven tornadoes to touch down from the same supercell.
19 April 2002	bgcolor=#Шаблон:Storm colour | F0	Lubbock, Texas	"The tornado was produced by an antimesocyclone, which was located on the north flank of a left-split storm."
6 September 2004	bgcolor=#Шаблон:Storm colour | F?	Chek-Lap-Kok International Airport, Hong Kong	Described as a marginal tornado.
24 April 2006	bgcolor=#Шаблон:Storm colour | F1	El Reno, Oklahoma	Second of two F1 tornadoes in the area.
20 June 2006	bgcolor=#Шаблон:Storm colour | F1	Rushville, Nebraska	A house, sheds, and outbuildings were destroyed on a farmstead.
2 October 2007	bgcolor=#Шаблон:Storm colour | EF0	Bussey, Iowa	Tornadoes of 2007#October 2 – This brief anticyclonic touched down in an open field southeast of Bussey, doing no damage.
10 May 2010	bgcolor=#Шаблон:Storm colour | EF0	Nardin, Oklahoma	Tornado outbreak of May 10–13, 2010 – First of five anticyclonic on this day.
10 May 2010	bgcolor=#Шаблон:Storm colour | EF1	Bray, Oklahoma	Tornado outbreak of May 10–13, 2010 – Second of five anticyclonic tornadoes on this day; was very large at times.
10 May 2010	bgcolor=#Шаблон:Storm colour | EF1	Southern Norman, Oklahoma	Tornado outbreak of May 10–13, 2010 – Third of five anticyclonic tornadoes on this day; it was likely a satellite tornado to the Norman–Little Axe, Oklahoma EF4 tornado.
10 May 2010	bgcolor=#Шаблон:Storm colour | EF1	Wayne, Oklahoma	Tornado outbreak of May 10–13, 2010 – Fourth of five anticyclonic tornadoes on this day; was up to a Шаблон:Convert wide and was briefly accompanied by a cyclonic EF0 satellite tornado.
10 May 2010	bgcolor=#Шаблон:Storm colour | EF1	Lake Eufaula, Oklahoma	Tornado outbreak of May 10–13, 2010 – Last of five anticyclonic tornadoes on this day; was up to a Шаблон:Convert wide.
31 May 2013	bgcolor=#Шаблон:Storm colour | EF2	Yukon, Oklahoma	Tornado outbreak of May 26–31, 2013 – A long-lived strong satellite tornado that was southeast of the record-breaking EF3 El Reno tornado.
4 June 2015	bgcolor=#Шаблон:Storm colour | EF0	Simla, Colorado	Tornadoes of 2015#June 4 – A brief anticyclonic tornado caused no damage.
4 June 2015	bgcolor=#Шаблон:Storm colour | EF0	Kutch, Colorado	Tornadoes of 2015#June 4 – A brief anticyclonic tornado caused no damage.
31 March 2016	bgcolor=#Шаблон:Storm colour | EF0	Hohenwald, Tennessee	Tornadoes of 2016#March 30–April 1 – A brief anticyclonic tornado snapped and uprooted trees, downed several large tree branches and inflicted minor roof damage to a home and barn.
5 April 2017	bgcolor=#Шаблон:Storm colour | EF1	Shelbyville, Tennessee	Tornadoes of 2017#April 4–6 – A landspout anticyclonic tornado snapped damaged trees, cars, and structures.
15 June 2019	bgcolor=#Шаблон:Storm colour | EF0	Johnsonville, South Dakota	Tornadoes of 2019#June 15–16 – This tornado lasted approximately 45 seconds and damaged about seven trees.
29 July 2021	bgcolor=#Шаблон:Storm colour | EF0	Bustleton, Philadelphia, Pennsylvania	Tornado outbreak of July 28–29, 2021 – A weak tornado damaged buildings and trees.
27 August 2021	bgcolor=#Шаблон:Storm colour | EF0	Dougherty, Iowa	"This very brief track was found in Sentinel satellite imagery and stayed in fields for its existence. Based on the location in the supercell, inflow wind trajectories along the left side of the track, and striation patterns in the fields, there is a high likelihood that this was an anti-cyclonic tornado."

See also

• Vortex
• Vorticity
• Pressure-gradient force (PGF)
• Rossby number
• Anticyclonic storm

External links

• Tornadic Meso-anticyclonic supercell in Sunnyvale California (NSSL)