1.3.2

The Global Atmospheric Circulation Model

Test yourself

The Global Atmospheric Circulation Model

The global atmospheric circulation model describes how air circulates between low and high-pressure belts as a result of differing conditions at different latitudes. This involves the transfer of heat via circulation cells.

Illustrative background for What happens at the equator?Illustrative background for What happens at the equator? ?? "content

What happens at the equator?

  • The Earth's surface is warmed by the Sun at the equator. The Earth transmits this heat to the nearby air. This air gets hotter and rises. The rising, hot air forms a low-pressure belt. As the hot air rises, the air will begin to cool, with water vapour condensing, creating rain and clouds.
  • The rising air cools and moves away from the equator towards 30o north and 30o south.
Illustrative background for What happens at 30<sup>o</sup> north and south?Illustrative background for What happens at 30<sup>o</sup> north and south? ?? "content

What happens at 30o north and south?

  • At 30o north and south, the air is further from the equator and the cool air falls. This results in a high-pressure belt with minimal rainfall and no clouds.
  • When the cool air reaches the Earth's surface, surface winds blow the cool air either towards the equator, or away from the equator towards the Poles.
Illustrative background for What happens at 60<sup>o</sup> north and south?Illustrative background for What happens at 60<sup>o</sup> north and south? ?? "content

What happens at 60o north and south?

  • At 60o north and south, cold air blown from the poles meets warm air surface winds. Because the warmer air is less dense, it rises and forms a low-pressure belt.
  • The air splits, with some returning back towards the equator and the rest heading to the poles.
Illustrative background for At the polesIllustrative background for At the poles ?? "content

At the poles

  • At the North Pole and the South Pole, cool air will sink, forming a high-pressure belt.
  • This high-pressure belt will move back towards the Earth's equator as a surface wind.
Illustrative background for contentIllustrative background for undefined ?? "content

Jump to other topics

1The Challenge of Natural Hazards

1.1Natural Hazards

1.2Tectonic Hazards

1.3Weather Hazards

1.4Climate Change

2The Living World

3Physical Landscapes in the UK

3.1The UK Physical Landscape

3.2Coastal Landscapes in the UK

3.3River Landscapes in the UK

3.4Glacial Landscapes in the UK

4Urban Issues & Challenges

5The Changing Economic World

6The Challenge of Resource Management

6.1Resource Management

6.2Food

6.3Water

6.4Energy

Go student ad image

Unlock your full potential with GoStudent tutoring

  • Affordable 1:1 tutoring from the comfort of your home

  • Tutors are matched to your specific learning needs

  • 30+ school subjects covered

Book a free trial lesson