Hadley cell


Hadley cell
Hadley cell [had′lē]
n.
after George Hadley (1685-1768), Eng meteorologist
Meteorol. an atmospheric convection pattern in which a current of hot equatorial air rises, divides, cools as it moves toward the poles, descends, and warms as it returns to the equator

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      model of the Earth's atmospheric circulation that was proposed by George Hadley (1735). It consists of a single wind system in each hemisphere, with westward and equatorward flow near the surface and eastward and poleward flow at higher altitudes. The tropical regions receive more heat from solar radiation than they radiate back into space, and the polar regions radiate more than they receive; because both areas have nearly constant temperatures, Hadley theorized that warm air must therefore rise near the Equator, flow poleward at high altitudes, and lose heat to the cold air present near the poles. This cooler and denser air then descends and flows equatorward at low levels until it nears the Equator, where it is warmed and rises again.

      Hadley devised this model in an attempt to explain the westward- and equatorward-flowing trade winds, but he ignored the Coriolis effect (Coriolis force) of the Earth's rotation, which deflects moving objects (including air) sideways and precludes a simple north-south circulation from the Equator to the poles. The Ferrel cell, a model with a statistically averaged circulation opposite to that of the Hadley cell, was subsequently proposed to account for the midlatitude westerly winds. The Hadley cell remains an excellent explanation of the Earth's atmospheric circulation occurring in both hemispheres equatorward of approximately 30° latitude.

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Universalium. 2010.

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