The Hadley cell, named after George Hadley, is a tropical atmospheric circulation that is defined by the average over longitude, which features rising motion near the equator, poleward flow 10–15 kilometers above the surface, descending motion in the subtropics, and equatorward flow near the surface. This circulation is intimately related to the trade winds, tropical rainbelts & hurricanes, subtropical deserts and the jet streams.
There are three primary circulation cells. They are known as the Hadley cell, Ferrel cell, and Polar cell.
Read more about Hadley Cell: Mechanism, History of Discovery, Major Impacts On Precipitation By Latitude, Hadley Cell Expansion
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