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thumb|upright=1.35|Cherry tree moving with the wind blowing about 22 m/sec (about 79 km/h or 49 mph) thumb|Sound of wind blowing in a pine forest at around 25 m/sec, with Wind gust|gust alterations Wind is the natural movement of air or other gases relative to a planet's surface. Winds occur 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 study of wind is called anemology.

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Wind is the natural movement of air across a planet's surface, occurring at many different scales—from brief thunderstorm gusts to local breezes lasting hours to large global wind patterns. Winds matter because they're driven by differences in how much solar energy different parts of Earth absorb, making them a fundamental part of how our planet's atmosphere and weather systems work.

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Article

35 sections
Contents
  • Causes
  • Measurement
  • Models
  • Wind force scale
  • Enhanced Fujita scale
  • Station model
  • Global climatology
  • Tropics
  • Westerlies and their impact
  • Polar easterlies
  • Local considerations
  • Sea and land breezes
  • Near mountains
  • Shear
  • In civilization
  • Religion
  • History
  • Transportation
  • Power source
  • Metallurgy
  • Recreation
  • In the natural world
  • Erosion
  • Desert dust migration
  • Effect on plants
  • Effect on animals
  • Related damage
  • In outer space
  • Planetary wind
  • Solar wind
  • On other planets
  • See also
  • References
  • Further reading
  • External links

thumb|upright=1.35|Cherry tree moving with the wind blowing about 22 m/sec (about 79 km/h or 49 mph) thumb|Sound of wind blowing in a pine forest at around 25 m/sec, with Wind gust|gust alterations Wind is the natural movement of air or other gases relative to a planet's surface. Winds occur 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 study of wind is called anemology.

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, which is called the Coriolis effect. Within the tropics and subtropics, 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 prevail.

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