Coniferous trees in Germany damaged by windthrow
Conifers in Germany are damaged by windthrow
Diagram displaying Europe's mistral wind
Wind diagram displaying the mistral wind
Wind as portrayed in the Tacuinum Sanitatis

Wind is the flow of gases on a large scale. On the surface of the Earth, wind consists of the bulk movement of air. In outer space, solar wind is the movement of gases or charged particles from the Sun through space, while planetary wind is the outgassing of light chemical elements from a planet's atmosphere into space. Winds are commonly classified by their spatial scale, their speed, the types of forces that cause them, the regions in which they occur, and their effect. The strongest observed winds on a planet in the Solar System occur on Neptune and Saturn. Winds have various aspects, an important one being its velocity (wind speed); another the density of the gas involved; another its energy content or wind energy. Wind is also a great source of transportation for seeds and small birds; with time things can travel thousands of miles in the wind.

In meteorology, winds are often referred to according to their strength, and the direction from which the wind is blowing. Short bursts of high-speed wind are termed gusts. Strong winds of intermediate duration (around one minute) are termed squalls. Long-duration winds have various names associated with their average strength, such as breeze, gale, storm, and hurricane. Wind occurs on a range of scales, from thunderstorm flows lasting tens of minutes, to local breezes generated by heating of land surfaces and lasting a few hours, to global winds resulting from the difference in absorption of solar energy between the climate zones on Earth. The two main causes of large-scale atmospheric circulation are the differential heating between the equator and the poles, and the rotation of the planet (Coriolis effect). Within the tropics, thermal low circulations over terrain and high plateaus can drive monsoon circulations. In coastal areas the sea breeze/land breeze cycle can define local winds; in areas that have variable terrain, mountain and valley breezes can dominate local winds.

In human civilization, the concept of wind has been explored in mythology, influenced the events of history, expanded the range of transport and warfare, and provided a power source for mechanical work, electricity and recreation. Wind powers the voyages of sailing ships across Earth's oceans. Hot air balloons use the wind to take short trips, and powered flight uses it to increase lift and reduce fuel consumption. Areas of wind shear caused by various weather phenomena can lead to dangerous situations for aircraft. When winds become strong, trees and human-made structures are damaged or destroyed.

Winds can shape landforms, via a variety of aeolian processes such as the formation of fertile soils, such as loess, and by erosion. Dust from large deserts can be moved great distances from its source region by the prevailing winds; winds that are accelerated by rough topography and associated with dust outbreaks have been assigned regional names in various parts of the world because of their significant effects on those regions. Wind also affects the spread of wildfires. Winds can disperse seeds from various plants, enabling the survival and dispersal of those plant species, as well as flying insect populations. When combined with cold temperatures, wind has a negative impact on livestock. Wind affects animals' food stores, as well as their hunting and defensive strategies.


Surface analysis of the Great Blizzard of 1888. Areas with greater isobaric packing indicate higher winds.

Wind is caused by differences in the atmospheric pressure. When a difference in atmospheric pressure exists, air moves from the higher to the lower pressure area, resulting in winds of various speeds. On a rotating planet, air will also be deflected by the Coriolis effect, except exactly on the equator. Globally, the two major driving factors of large-scale wind patterns (the atmospheric circulation) are the differential heating between the equator and the poles (difference in absorption of solar energy leading to buoyancy forces) and the rotation of the planet. Outside the tropics and aloft from frictional effects of the surface, the large-scale winds tend to approach geostrophic balance. Near the Earth's surface, friction causes the wind to be slower than it would be otherwise. Surface friction also causes winds to blow more inward into low-pressure areas.[1][2]

Winds defined by an equilibrium of physical forces are used in the decomposition and analysis of wind profiles. They are useful for simplifying the atmospheric equations of motion and for making qualitative arguments about the horizontal and vertical distribution of winds. The geostrophic wind component is the result of the balance between Coriolis force and pressure gradient force. It flows parallel to isobars and approximates the flow above the atmospheric boundary layer in the midlatitudes.[3] The thermal wind is the difference in the geostrophic wind between two levels in the atmosphere. It exists only in an atmosphere with horizontal temperature gradients.[4] The ageostrophic wind component is the difference between actual and geostrophic wind, which is responsible for air "filling up" cyclones over time.[5] The gradient wind is similar to the geostrophic wind but also includes centrifugal force (or centripetal acceleration).[6]

Other Languages
Afrikaans: Wind
Alemannisch: Wind
አማርኛ: ነፋስ
Ænglisc: Wind
العربية: ريح
aragonés: Viento
armãneashti: Vimtu
asturianu: Vientu
Avañe'ẽ: Yvytu
azərbaycanca: Külək
تۆرکجه: یئل
Bahasa Banjar: Ribut
Bân-lâm-gú: Hong
башҡортса: Ел
беларуская: Вецер
беларуская (тарашкевіца)‎: Вецер
भोजपुरी: हवा
български: Вятър
Boarisch: Wind
བོད་ཡིག: རླུང་།
bosanski: Vjetar
brezhoneg: Avel
буряад: Һалхин
català: Vent
Чӑвашла: Çил
čeština: Vítr
chiShona: Mhepo
Cymraeg: Gwynt
dansk: Vind
Deutsch: Wind
dolnoserbski: Wětš
eesti: Tuul
Ελληνικά: Άνεμος
español: Viento
Esperanto: Vento
euskara: Haize
فارسی: باد
français: Vent
Frysk: Wyn (waar)
Gaeilge: Gaoth
Gaelg: Geay
Gàidhlig: Gaoth
galego: Vento
ГӀалгӀай: Мух
客家語/Hak-kâ-ngî: Fûng
한국어: 바람
հայերեն: Քամի
हिन्दी: पवन
hornjoserbsce: Wětr
hrvatski: Vjetar
Ido: Vento
Bahasa Indonesia: Angin
íslenska: Vindur
italiano: Vento
עברית: רוח
Basa Jawa: Angin
ಕನ್ನಡ: ಗಾಳಿ/ವಾಯು
ქართული: ქარი
қазақша: Жел
Kiswahili: Upepo
Kreyòl ayisyen: Van
kurdî: Ba (hewa)
Кыргызча: Шамал
Latina: Ventus
latviešu: Vējš
lietuvių: Vėjas
Limburgs: Windj
lingála: Mompɛpɛ
lumbaart: Vent
magyar: Szél
македонски: Ветар
മലയാളം: കാറ്റ്
मराठी: वारा
მარგალური: ბორია
Bahasa Melayu: Angin
Mìng-dĕ̤ng-ngṳ̄: Hŭng
Mirandés: Biento
монгол: Салхи
မြန်မာဘာသာ: လေတိုက်ခတ်ခြင်း
Nāhuatl: Ehecatl
Nedersaksies: Wiend
नेपाल भाषा: फय्
нохчийн: Мох
Nordfriisk: Winj
norsk: Vind
norsk nynorsk: Vind
Nouormand: Vent
occitan: Vent
олык марий: Мардеж
oʻzbekcha/ўзбекча: Shamol
ਪੰਜਾਬੀ: ਹਵਾ
پنجابی: نیری
Picard: Vint
polski: Wiatr
português: Vento
Qaraqalpaqsha: Samal
română: Vânt
Runa Simi: Wayra
русский: Ветер
саха тыла: Тыал
Scots: Wind
shqip: Era
sicilianu: Ventu
සිංහල: සුළඟ
Simple English: Wind
slovenčina: Vietor
slovenščina: Veter
ślůnski: Wjater
Soomaaliga: Dabeyl
کوردی: با
српски / srpski: Ветар
srpskohrvatski / српскохрватски: Vetar
suomi: Tuuli
svenska: Vind
Tagalog: Hangin
தமிழ்: காற்று
татарча/tatarça: Җил
తెలుగు: పవనం (విండ్)
ไทย: ลม
тоҷикӣ: Бод
Türkçe: Rüzgâr
українська: Вітер
اردو: باد
Vahcuengh: Rumz
vepsän kel’: Tullei
Tiếng Việt: Gió
Võro: Tuul
walon: Vint
Winaray: Hangin
ייִדיש: ווינט
Zazaki: Va
žemaitėška: Vies