Hadley cell
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(meteorology) A global-scale tropical atmospheric circulation that features air rising near the Equator, flowing poleward at a height of 10 to 15 kilometers above the earth's surface, descending in the subtropics, and then returning equatorward near the surface. This circulation creates the trade winds, tropical rain-belts and hurricanes, subtropical deserts and the jet streams.
Hadley cell
Meteorologists study the Hadley cell to understand why the tropics have intense convection and why deserts form in the subtropics.
Meteorologists study the Hadley cell to understand why the tropics have intense convection and why deserts form in the subtropics.
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