Answer: Sahara Desert in Africa
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Which desert is caused by a Hadley cell?
Hadley cell | meteorology | Britannica
Hadley Cells
Hadley cell - Wikipedia
How Are Deserts Formed? Why Are Deserts Hot?
The Hadley cell named after George Hadley is 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 cells are the low-altitude overturning circulation that have air sinking at roughly zero to 30 degree latitude.
The Hadley cell named after George Hadley is 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 cells are the low-altitude overturning circulation that have air sinking at roughly zero to 30 degree latitude.
The driving force of atmospheric circulation is the uneven distribution of solar heating across the Earth which is greatest near the equator and least at the poles. The atmospheric circulation transports energy polewards thus reducing the resulting equator-to-pole temperature gradient. The mechanisms by which this is accomplished differ in tropical and extratropical latitudes.
The driving force of atmospheric circulation is the uneven distribution of solar heating across the Earth which is greatest near the equator and least at the poles. The atmospheric circulation transports energy polewards thus reducing the resulting equator-to-pole temperature gradient. The mechanisms by which this is accomplished differ in tropical and extratropical latitudes. Hadley cells exist on either side of the equator. Each cell encircles the globe latitudinally and acts to transport energy from the equator to about the 30th latitude. The circulation exhibits the following phenomena: • Warm moist air converging near the equator causes heavy precipitation. This releases latent heat driving strong rising motions. • This air rises to the tropopause about 10–15 kilometers above sea level where the air is no longer buoyant. • Unable to continue rising this sub-stratospheric air is instead forced poleward by the continual rise of air below. • As air moves poleward it both cools and gains a strong eastward component due to the Coriolis effect and the conservation of angular momentum . The resulting winds form the subtropical jet streams . • ...
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