What is the convection pattern between 30'S and 30°N latitude? (1 point)

O Cooler air rises and moves toward the equator, then warms and falls and moves away from the equator.
O Hotter air rises and moves away from the equator, then cools and falls and moves back to the equator.
O Hotter air rises and moves toward the equator, then cools and falls and moves away from the equator.
O Cooler air rises and moves away from the equator, then warms and falls and moves back to the equator.
It’s a unit test “climate unit test” and I’m on question 4

The equator is hot. 30 N and S are cooler.

hot air rises, moves N and S, cools
cool air is denser, drops and gets sucked back to the equator for rewarming.

No.1

The correct answer is:

Hotter air rises and moves toward the equator, then cools and falls and moves away from the equator.

To determine the convection pattern between 30°S and 30°N latitude, you can reference the general atmospheric circulation pattern known as the Hadley Cell. The Hadley Cell is a large-scale atmospheric circulation pattern that plays a central role in Earth's climate system.

In the Hadley Cell, warmer air near the equator rises, creating a low-pressure area. As the air rises, it cools and water vapor condenses, resulting in the formation of clouds and precipitation. This process releases heat into the atmosphere, further warming the air. The rising air moves poleward and eventually cools and sinks in the subtropical regions around 30°N and 30°S latitude.

So, in the specific latitudinal range of 30°S to 30°N, the correct answer would be:

- Hotter air rises and moves towards the equator, then cools and falls and moves away from the equator.

This process of warm air ascending near the equator, cooling, and descending in the subtropics creates a continuous loop of air circulation, known as the Hadley Cell, which helps to drive global weather patterns.

O Hotter air rises and moves toward the equator, then cools and falls and moves away from the equator.