prevailing wind direction

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(pri′vāl·iŋ ′wind di′rek·shən)

(meteorology) The wind direction most frequently observed during a given period; the periods most often used are the observational day, month, season, and year. Also known as prevailing wind.


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The most frequent winds within a specified period. In mid-latitudes, for example, most winds are westerly, with an azimuthal bearing of between 181 and 359°.

The winds produced by the global patterns of barometric pressure, both at the surface and aloft. The prevailing winds are influenced by the earth’s rotation (Coriolis effect). The prevailing winds are the polar high, polar easterlies, subpolar lows, westerlies, subtropical high-horse latitudes, and tradewinds in both the Northern and Southern Hemispheres. These northern and southern prevailing wind bands are mirror images of each other. The equatorial low doldrums are found along a belt near the equator. See planetary winds.

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