Editing Wind speed

{{Short description|Rate at which air moves from high- to low-pressure areas}}
{{Distinguish|Airspeed (disambiguation){{!}}Airspeed}}

[[File:Weather Station at Feilding Waste Water Treatment Plant.JPG|thumb|240px|An [[anemometer]] is commonly used to measure wind speed.]]

[[File:Wind wiki.png|thumb|Global distribution of wind speed at 10m above ground averaged over the years 1981–2010 from the CHELSA-BIOCLIM+ data set<ref>Brun, P., Zimmermann, N.E., Hari, C., Pellissier, L., Karger, D.N. (preprint): Global climate-related predictors at kilometre resolution for the past and future. Earth Syst. Sci. Data Discuss. https://doi.org/10.5194/essd-2022-212</ref>]]

In [[meteorology]], '''wind speed''', or [[wind]] [[flow speed]], is a fundamental [[atmosphere|atmospheric]] quantity caused by air moving from [[high-pressure area|high]] to [[low-pressure area|low pressure]], usually due to changes in temperature. Wind speed is now commonly measured with an [[anemometer]].

Wind speed affects [[weather forecasting]], [[aviation]] and [[maritime transport|maritime]] operations, [[construction]] projects, growth and [[metabolism]] rates of many plant species, and has countless other implications.<ref>{{cite book |first=C. Michael |last=Hogan |year=2010 |url=http://www.eoearth.org/article/Abiotic_factor?topic=49461 |entry=Abiotic factor |title=Encyclopedia of Earth |editor1=Emily Monosson |editor2=C. Cleveland |publisher=[[National Council for Science and the Environment]] |archive-url=https://web.archive.org/web/20130608071757/http://www.eoearth.org/article/Abiotic_factor?topic=49461 |archive-date=2013-06-08 |location=Washington D.C.}}</ref> [[Wind direction]] is usually almost parallel to [[isobar (meteorology)|isobars]] (and not perpendicular, as one might expect), due to [[Earth's rotation]].

== Units ==
The [[metre per second|meter per second]] (m/s) is the [[SI unit]] for velocity and the unit recommended by the [[World Meteorological Organization]] for reporting wind speeds, and used amongst others in weather forecasts in the [[Nordic countries]].<ref>[http://www.whiteweather.com/wd/vind/Windspeed.htm Windspeed | Icelandic Meteorological office] "The Icelandic Meteorological Office now uses the SI (Systeme Internationale d'Unites) measurement metres per second (m/s) […] other Nordic meteorological institutes have used this system for years with satisfactory results"</ref> Since 2010 the [[International Civil Aviation Organization]] (ICAO) also recommends meters per second for reporting wind speed when approaching [[runway]]s, replacing their former recommendation of using [[kilometres per hour|kilometers per hour]] (km/h).<ref>[https://aerosavvy.com/wp-content/uploads/2014/08/an05_cons.pdf International Civil Aviation Organization – International Standards and Recommended Practices – Units of Measurement to be Used in Air and Ground Operations – Annex 5 to the Convention on International Civil Aviation]</ref>

For historical reasons, other units such as [[miles per hour]] (mph), [[Knot (unit)|knots]] (kn),<ref>[https://www.thoughtco.com/measuring-wind-speed-in-knots-3444011 Measuring Wind Speed in Knots] "The reason why sea winds are measured in knots at all has to do with maritime tradition"</ref> and [[feet per second]] (ft/s) are also sometimes used to measure wind speeds. Historically, wind speeds have also been classified using the [[Beaufort scale]], which is based on visual observations of specifically defined wind effects at sea or on land.

==Factors affecting wind speed==
Wind speed is affected by a number of factors and situations, operating on varying scales (from micro to macro scales). These include the [[pressure gradient]], [[Rossby wave]]s, [[jet stream]]s, and local weather conditions. There are also links to be found between wind speed and [[wind direction]], notably with the pressure gradient and terrain conditions.

The '''Pressure gradient''' describes the difference in air pressure between two points in the atmosphere or on the surface of the Earth. It is vital to wind speed, because the greater the difference in pressure, the faster the wind flows (from the high to low pressure) to balance out the variation. The pressure gradient, when combined with the [[Coriolis effect]] and [[friction]], also influences [[wind direction]].

'''Rossby waves''' are strong winds in the upper [[troposphere]]. These operate on a global scale and move from west to east (hence being known as [[westerlies]]). The Rossby waves are themselves a different wind speed from that experienced in the lower [[troposphere]].

'''Local weather conditions''' play a key role in influencing wind speed, as the formation of [[hurricanes]], [[monsoon]]s, and [[cyclones]] as freak weather conditions can drastically affect the flow velocity of the wind.{{Citation Needed | date= April 2021}}

==Highest speed==
[[File:The Big Wind Anemometer.JPG|thumb|upright|The original anemometer that measured The Big Wind in 1934 at [[Mount Washington Observatory]]]]
===Non-tornadic===
The fastest wind speed not related to [[tornado]]es ever recorded was during the passage of Tropical [[Cyclone Olivia]] on 10 April 1996: an [[automatic weather station]] on [[Barrow Island (Western Australia)|Barrow Island]], [[Australia]], registered a maximum [[wind gust]] of {{cvt|113.3|m/s|km/h mph kn ft/s}}<ref name="courtney"/><ref>{{cite web|url=https://public-old.wmo.int/en/media/news/new-world-record-wind-gust|archive-url=https://web.archive.org/web/20231218171508/https://public-old.wmo.int/en/media/news/new-world-record-wind-gust|url-status=dead|archive-date=December 18, 2023|publisher=World Meteorological Association|title=World record wind gust|date=5 November 2015 |access-date=12 February 2017}}</ref> The wind gust was evaluated by the WMO Evaluation Panel, who found that the anemometer was mechanically sound and that the gust was within statistical probability and ratified the measurement in 2010. The anemometer was mounted 10 m above ground level (and thus 64 m above sea level). During the cyclone, several extreme gusts of greater than {{cvt|83|m/s|km/h mph kn ft/s}} were recorded, with a maximum 5-minute mean speed of {{cvt|49|m/s|km/h mph kn ft/s}}; the extreme gust factor was on the order of 2.27–2.75 times the mean wind speed. The pattern and scales of the gusts suggest that a [[mesovortex]] was embedded in the already-strong [[eyewall]] of the cyclone.<ref name="courtney">{{cite web|url=http://www.bom.gov.au/amoj/docs/2012/courtney_hres.pdf|title=Documentation and verification of the world extreme wind gust record: 113.3 m s–1 on Barrow Island, Australia, during passage of tropical cyclone Olivia|publisher=Australian Meteorological and Oceanographic Journal}}</ref>

Currently{{As of when|date=June 2024}}, the second-highest surface wind speed ever officially recorded is {{cvt|103.266|m/s|km/h mph kn ft/s}} at the [[Mount Washington (New Hampshire)]] Observatory {{cvt|6288|ft|m|order=flip}} above sea level in the US on 12 April 1934, using a [[Hot-wire anemometry|hot-wire anemometer]]. The anemometer, specifically designed for use on Mount Washington, was later tested by the US [[National Weather Service|National Weather Bureau]] and confirmed to be accurate.<ref>{{cite web|url=http://www.mountwashington.org/about/visitor/recordwind.php|access-date=26 January 2010|title=The story of the world record wind|publisher=Mount Washington Observatory}}</ref>

===Tornadic===
Wind speeds within certain atmospheric phenomena (such as [[tornado]]es) may greatly exceed these values but have never been accurately measured. Directly measuring these tornadic winds is rarely done, as the violent wind would destroy the instruments. A method of estimating speed is to use [[Doppler on Wheels]] or mobile [[Doppler weather radar]]s to measure the wind speeds remotely.<ref>{{cite news|title=Massive Okla. tornado had windspeed up to 200 mph|url=http://www.cbsnews.com/news/massive-okla-tornado-had-windspeed-up-to-200-mph/|access-date=17 May 2014|newspaper=CBS News|date=20 May 2013}}</ref> Using this method, a mobile radar ([[RaXPol]]) owned and operated by the [[University of Oklahoma]] recorded winds up to {{convert|150|m/s|mph km/h}} inside the [[2013 El Reno tornado]], marking the fastest winds ever observed by radar in history.<ref name="2024RadarPaper">{{cite journal |last1=Lyza |first1=Anthony W. |last2=Flournoy |first2=Matthew D. |last3=Alford |first3=A. Addison |title=Comparison of Tornado Damage Characteristics to Low-Altitude WSR-88D Radar Observations and Implications for Tornado Intensity Estimation |journal=[[Monthly Weather Review]] |date=19 March 2024 |volume=152 |issue=8 |page=1689 |doi=10.1175/MWR-D-23-0242.1 |url=https://journals.ametsoc.org/view/journals/mwre/aop/MWR-D-23-0242.1/MWR-D-23-0242.1.xml |access-date=19 March 2024 |publisher=[[National Oceanic and Atmospheric Administration]] and [[University of Oklahoma]] via the [[American Meteorological Society]]|bibcode=2024MWRv..152.1689L }}</ref> In 1999, a mobile radar measured winds up to {{cvt|135|m/s|km/h mph kn ft/s}} during the [[1999 Bridge Creek–Moore tornado]] in [[Oklahoma]] on 3 May,<ref>{{cite web|url=http://www.spc.noaa.gov/faq/tornado/#History|title=Historical Tornadoes|publisher=National Weather Service}}</ref> although another figure of {{cvt|142|m/s|km/h mph kn ft/s}} has also been quoted for the same tornado.<ref name=worldrecordacademy>{{cite news|title=Highest surface wind speed-Tropical Cyclone Olivia sets world record|url=http://www.worldrecordacademy.com/weather/highest_surface_wind_speed_Tropical_Cyclone_Olivia_sets_world_record_101519.htm|access-date=17 May 2014|newspaper=World Record Academy|date=26 January 2010}}</ref> Yet another number used by the Center for Severe Weather Research for that measurement is {{cvt|135|+/-|9|m/s|km/h mph kn ft/s}}.<ref>{{cite web|last=Wurman|first=Joshua|author-link=Joshua Wurman|title=Doppler On Wheels|publisher=Center for Severe Weather Research|year=2007|url=http://www.cswr.org/dow/DOW.htm|url-status=dead|archive-url=https://web.archive.org/web/20110719102124/http://www.cswr.org/dow/DOW.htm|archive-date=2011-07-19}}</ref> However, speeds measured by [[Weather radar#Velocity|Doppler weather radar]] are not considered official records.<ref name=worldrecordacademy/>

===On other planets===
Wind speeds can be much higher on [[exoplanet]]s. Scientists at the University of Warwick in 2015 determined that [[HD 189733 b|HD 189733b]] has winds of {{convert|2,400|m/s|km/h kn|abbr=on}}. In a press release, the University announced that the methods used from measuring HD 189733b's wind speeds could be used to measure wind speeds on Earth-like exoplanets.<ref>{{Cite web|title=5400mph winds discovered hurtling around planet outside solar system|url=https://warwick.ac.uk/newsandevents/pressreleases/5400mph_winds_discovered/|access-date=2020-08-08|website=warwick.ac.uk}}</ref>

== Measurement ==
{{main|Anemometer}}
[[File:Anemometer-Animation.gif|thumb|Modern day anemometer used to capture wind speed]]
[[File:FT742-DM_Acoustic_resonance_wind_sensor.jpg|thumb|left|FT742-DM acoustic resonance wind sensor, one of the instruments now used to measure wind speed at Mount Washington Observatory]]An anemometer is one of the tools used to measure wind speed.<ref>{{Cite web|url=http://www.ciese.org/curriculum/weatherproj2/en/docs/anemometer.shtml|title=Make and Use an Anemometer to measure Wind Speed|last=Koen|first=Joshua|website=www.ciese.org|access-date=2018-04-18}}</ref> A device consisting of a vertical pillar and three or four concave cups, the anemometer captures the horizontal movement of air particles (wind speed).

Unlike traditional cup-and-vane anemometers, ultrasonic wind sensors have no moving parts and are therefore used to measure wind speed in applications that require maintenance-free performance, such as atop wind turbines. As the name suggests, ultrasonic wind sensors measure the wind speed using high-frequency sound. An ultrasonic anemometer has two or three pairs of sound transmitters and receivers. Each transmitter constantly beams high-frequency sound to its receiver. Electronic circuits inside measure the time it takes for the sound to make its journey from each transmitter to the corresponding receiver. Depending on how the wind blows, some of the sound beams will be affected more than the others, slowing it down or speeding it up very slightly. The circuits measure the difference in speeds of the beams and use that to calculate how fast the wind is blowing.<ref>Chris Woodford. Ultrasonic anemometers. https://www.explainthatstuff.com/anemometers.html</ref>

Acoustic resonance wind sensors are a variant of the ultrasonic sensor. Instead of using time of flight measurement, acoustic resonance sensors use resonating acoustic waves within a small purpose-built cavity. Built into the cavity is an array of [[ultrasonic transducers]], which are used to create the separate standing-wave patterns at ultrasonic frequencies. As wind passes through the cavity, a change in the wave's property occurs (phase shift). By measuring the amount of phase shift in the received signals by each transducer, and then by mathematically processing the data, the sensor is able to provide an accurate horizontal measurement of wind speed and direction.<ref>Kapartis, Savvas (1999) "Anemometer employing standing wave normal to fluid flow and travelling wave normal to standing wave" {{US Patent|5877416}}</ref>

Another tool used to measure wind velocity includes a GPS combined with [[pitot tube]].{{citation needed|date=February 2019}} A fluid flow velocity tool, the [[Pitot tube]] is primarily used to determine the air velocity of an aircraft.

==Design of structures==
{{main|Wind engineering}}
[[File:Anemometer_on_stage_set.JPG|thumb|right|Anemometer on an outdoor stage set, to measure wind speed]]

Wind speed is a common factor in the design of structures and buildings around the world. It is often the governing factor in the required lateral strength of a structure's design.

In the United States, the wind speed used in design is often referred to as a "3-second gust", which is the highest sustained gust over a 3-second period having a probability of being exceeded per year of 1 in 50 (ASCE 7-05, updated to ASCE 7-16).<ref>{{Cite web|url=http://www.koreascience.or.kr/journal/AboutJournal.jsp?kojic=KJKHCF|title=Wind and Structures |website=Korea Science|language=ko|access-date=2018-04-18}}</ref> This design wind speed is accepted by most building codes in the United States and often governs the lateral design of buildings and structures.

In Canada, reference wind pressures are used in design and are based on the "mean hourly" wind speed having a probability of being exceeded per year of 1 in 50. The reference [[dynamic pressure|wind pressure]] {{Mvar|q}} is calculated using the equation {{Math|1=''q'' = ''&rho;v''<sup>2</sup> / 2}}, where {{Mvar|&rho;}} is the air density and {{Mvar|v}} is the wind speed.<ref>NBC 2005 Structural Commentaries – Part 4 of Div. B, Comm. I</ref>

Historically, wind speeds have been reported with a variety of averaging times (such as fastest mile, 3-second gust, 1-minute, and mean hourly) which designers may have to take into account. To convert wind speeds from one averaging time to another, the Durst Curve was developed, which defines the relation between probable maximum wind speed averaged over some number of seconds to the mean wind speed over one hour.<ref>ASCE 7-05 commentary Figure C6-4, ASCE 7-10 C26.5-1</ref>

==See also==
* [[American Society of Civil Engineers]] (promulgator of ASCE 7-05, current version is ASCE 7-16)
* [[Beaufort scale]]
* [[Fujita scale]] and [[Enhanced Fujita Scale]]
* [[International Building Code]] (promulgator of NBC 2005)
* [[International Civil Aviation Organization#Use of the International System of Units|ICAO recommendations – International System of Units]]
* [[Knot (unit)]]
* [[Prevailing wind]]
* [[Saffir–Simpson Hurricane Scale]]
* [[TORRO scale]]
* [[Wind direction]]

==References==
{{Reflist}}

== External links ==
* {{Commons-inline|Wind speed}}

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{{DEFAULTSORT:Wind Speed}}
[[Category:Wind]]
[[Category:Airspeed]]
[[Category:Meteorological quantities]]
[[Category:Wind power]]
[[Category:Weather extremes of Earth]]

[[es:Viento#Características físicas de los vientos]]