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Wind is the movement of air – Fact Check

Question asked:

“Wind is the movement of air.”
True
Confidence: High Checked on October 24, 2026

Summary

Wind is defined as air in motion, the horizontal flow of air caused by pressure differences in the atmosphere. This definition is consistently given by authoritative meteorological sources.

Sources 60 searched

noaa.gov
  • Origin of Wind | National Oceanic and Atmospheric Administration

    Wind is simply air in motion. Usually in meteorology, when we are talking about the wind it is the horizontal speed and direction we are concerned about. For example, if you hear a report of a west wind at 15 mph (24 km/h) that means the horizontal winds will be coming FROM the west at that speed. ,

metoffice.gov.uk
osti.gov
weather.gov
  • Prevailing Winds

    Given a steep lapse rate caused by cool air aloft over a hot surface, little horizontal air movement, few or no clouds, and the noonday sun heating flat arid soil surfaces to high temperatures, the air in contact with the ground becomes super-heated and highly unstable.

scijinks.gov
  • Why Does Wind Blow? | NOAA SciJinks – All About Weather

    You might think that the warm air would lead to a higher pressure area, but actually the opposite is true. Because warm air rises, it leaves behind an area of low pressure behind it. ... Now we’re getting to the part where wind happens. Gases move from high-pressure areas to low-pressure areas.

pressbooks-dev.oer.hawaii.edu
manoa.hawaii.edu
  • Wind Formation | manoa.hawaii.edu/ExploringOurFluidEarth

    An air mass may be large enough to cover an entire continent while a small air mass might only cover a single building. An air mass can be described by properties such as its density, temperature, pressure, and movement. Winds are currents of air that move across the earth’s surface and develop ...

ces.fau.edu
scied.ucar.edu
  • Wind - UCAR Center for Science Education

    There is still air everywhere, but the air molecules are more widely spaced in some areas and more tightly packed in others. The places with more air molecules have higher pressure. The areas with fewer air molecules have lower pressure. Air whooshes into the area with lower pressure. That’s wind.

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