The tropical atmospheric circulation associated with rising winds along the intertropical convergence zone (ITCZ) and descending air in the subtropics are called Hadley cells. or Hadley circulation
The Hadley circulation, also known as the Hadley cell, is a worldwide tropical atmospheric circulation pattern that occurs due to uneven solar heating at different latitudes surrounding the equator. The Hadley circulation causes air around the equator to rise to about 10-15 kilometers, flow poleward (toward the North Pole above the equator, the South Pole below the equator), descend in the subtropics, and then flow back to the equator along the Earth's surface.
Climate scientists are interested in Hadley cell because it controls precipitation in the subtropics and creates a region known as the intertropical convergence zone, which produces a band of major, highly precipitous storms.
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Scientists need to gather information that is based on direct observation rather than opinion or feelings.
Answer:
Greenhouse effect
Explanation:
Greenhouse effect is the trapping of the sun's warmth in a planet's lower atmosphere, due to the greater transparency of the atmosphere to visible radiation from the sun than to infrared radiation emitted from the planet's surface.