What is the convection pattern between 30°S and 30°N latitude?(1 point)
Responses
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 toward the equator, then warms and falls and moves away from 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.
Cooler air rises and moves away from the equator, then warms 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.
The correct answer is: Hotter air rises and moves toward the equator, then cools and falls and moves away from the equator.
The correct answer is: Hotter air rises and moves toward the equator, then cools and falls and moves away from the equator.
To understand the convection pattern between 30°S and 30°N latitude, we need to understand the concept of convection and the global air circulation patterns. The convection process is driven by temperature differences and plays a crucial role in atmospheric circulation.
In this case, between 30°S and 30°N latitude, the region is known as the tropical zone, which is characterized by warm temperatures throughout the year. The sun's rays hit this area more directly, resulting in heating of the air near the equator.
As the air gets heated, it becomes less dense and starts to rise. This rising warm air creates an area of low pressure near the equator. This upward motion of air is known as convection. As the air rises, it moves towards the poles.
As it moves away from the equator, the air cools due to expansion and interaction with cooler air from higher latitudes. The cooler air becomes denser and starts to sink, creating an area of high pressure. From this high-pressure region, the air then flows back towards the equator, completing the circulation pattern.
This convection pattern between 30°S and 30°N latitude is known as the Hadley cell circulation, which is one of the three major global circulation cells, along with Ferrel and Polar cells. It plays a crucial role in shaping weather patterns and climate in the tropical regions.