Answer :
J) Hadley cells. In the subtropics, air rises near the equator, flows poleward at a height of 10 to 15 kilometers above the earth's surface, descends, and then moves back toward the equator near the surface. This tropical atmospheric circulation is known as the Hadley cell, after George Hadley. The trade winds, tropical rain belts, hurricanes, subtropical deserts, and jet streams are all products of this circulation.
The low-latitude overturning circulations known as Hadley Cells are characterized by air rising near the equator and air sinking at about 30° latitude. They regulate low-latitude weather patterns and are in charge of the trade winds in the Tropics. Warm air rises close to the equator, cools as it travels poleward at high altitude, sinks as cold air, and warms as it travels equatorward. also: a planet with a comparable atmospheric circulation pattern (such as Mars). Due to uneven solar heating at various latitudes surrounding the equator, the Hadley circulation, also known as the Hadley cell, causes air in the region of the equator to rise to a height of about 10-15 kilometers and flow poleward (toward the North Pole above the equator, the South Pole below). There are Hadley cells on both sides of the equator. Energy is transported by each cell as it circles the earth latitudinally, from the equator to around the 30th latitude. The circulation displays the following characteristics: Heavy precipitation is brought on by a convergence of warm, humid air near the equator.
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Match the following.
a) thermocline
b) Ferrel cells
c) thermal inversion
d) stratosphere
e) thermosphere
f) mesosphere
g) troposphere
h) high-pressure system
i) low-pressure system
j) Hadley cells
Convective cells near the equator.