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Gradient Wind

   Also found in: Wikipedia 0.01 sec.
gradient wind [′grād·ē·ənt ‚wind]
(meteorology)
A wind for which Coriolis acceleration and the centripetal acceleration exactly balance the horizontal pressure force.

Gradient Wind 

a horizontal, uniform motion of air in the absence of frictional force in a linear (geostrophic wind) or circular path that coincides with the isobars. The gradient wind blows when there is a balance between the active force of pressure gradient and inertial forces: centrifugal force and deflective force owing to the earth’s rotation—the Coriolis force. The gradient wind is the best approximation of the actual state of wind in a free atmosphere above the layer of friction (approximately 1,000 m above the earth’s surface).



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Examples of specific topics covered include aircraft electrification, airmass, anabatic wind, boundary layer, convection, Dansgaard-Oeschger event, Dobson spectrophotometer, gradient wind, katabatic wind, meteorology, noble gases, pollution control, temperature scales, waterspout, and Venturi effect.
NEW YORK, East NYZ053>054-063-084 Western Rensselaer--Eastern Rensselaer--Western Ulster--Southern Washington 01 1624EST 1900EST Trees were reported down in Hensonville from strong gradient winds.
ARKANSAS, Northwest ARKANSAS, Southeast NONE REPORTED ARZ074>075 Ashley--Chicot 01 0000CST 16 0000CST ARZ075 Chicot 16 1455CST 1505CST Strong gradient winds developed across southeast Arkansas as a strong low pressured area moved across central Arkansas.
 
 
 
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