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What is the convection pattern between 30°S and 30°N latitude?
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Cooler air rises and moves away from the equator, then warms and falls and moves back to the equator.
Cooler air rises and moves away from the equator, then warms and falls and moves back to the equator.
Hotter air rises and moves away from the equator, then cools and falls and moves back to the equator.
Hotter air rises and moves away from the equator, then cools and falls and moves back to the equator.
Hotter air rises and moves toward the equator, then cools and falls and moves away from the equator.
Hotter air rises and moves toward the equator, then cools and falls and moves away from the equator.
Cooler air rises and moves toward the equator, then warms and falls and moves away from the equator.
Cooler air rises and moves away from the equator, then warms and falls and moves back to the equator.
Hotter air rises and moves away from the equator, then cools and falls and moves back to the equator.
Hotter air rises and moves away from the equator, then cools and falls and moves back to the equator.
Hotter air rises and moves toward the equator, then cools and falls and moves away from the equator.
Hotter air rises and moves toward the equator, then cools and falls and moves away from the equator.
Cooler air rises and moves toward the equator, then warms and falls and moves away from the equator.
Answered by
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The convection pattern between 30°S and 30°N latitude is known as the Hadley Cell. It is a large-scale atmospheric circulation pattern in which warm, moist air rises near the equator, moves towards the poles at high altitudes, cools and sinks at around 30°N and 30°S, and then returns towards the equator at lower altitudes. This creates a band of low pressure near the equator and a band of high pressure at around 30°N and 30°S. The Hadley Cell plays an important role in the global climate system and influences weather patterns in many regions of the world.