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Hadley cell
(redirected from Hadley circulation)

   Also found in: Wikipedia, Hutchinson 0.03 sec.
Hadley cell [′had·lē ‚sel]
(meteorology)
A direct, thermally driven, and zonally symmetric circulation first proposed by George Hadley as an explanation for the trade winds; it consists of the equatorward movement of the trade winds between about latitude 30° and the equator in each hemisphere, with rising wind components near the equator, poleward flow aloft, and finally descending components at about latitude 30° again.


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This so-called Hadley circulation ensures that most dust lofted into the atmosphere in the tropics doesn't travel to other parts of the world.
 
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