Global Atmospheric Circulation

Without solar energy the air around the earth would remain still

At the equator, sunlight hits the surface directly

At the poles, sunlight hits the surface at an angle

Causes less heating

Light is spread over a greater area

More sunlight is reflected from the oceans and ice

1kW per square meter

0.5 kW per square meter

Sunlight warms the earth's surface

Radiates infrared radiation into the atmosphere

Some of this radiation is absorbed by greenhouse gasses, causing the atmosphere to warm

Water vapour

Carbon Dioxide

Methane

Other green house gasses

Warm air is lighter and rises

Cold air is heavier and sinks

Different parts of the earth's surface are travelling at different speeds

Forms a high pressure cell

Forms a low pressure cell

Due to the earth's rotation, wind does not move in a straight line

Due to inertia, winds blowing from the poles are deflected

The hot air rising from the equator is pushed towards the poles

They end up spinning around the polar regions

0º (on the equator), the surface travels at 1600 km/h

30º from the equator, the surface travels at 1400 km/h

60º from the equator, the surface travels at 800 km/h

90º from the equator (at the poles), the surface is stationary and does not move

Cells

Hadley Cell
(0º to 30º)

Polar Cell
(60º to 90º)

Air flows towards the faster traveling equator but drops behind because it is slower than the surface it is moving towards

Subtropical Jet
(30º, high pressure belt)

When the air from the equator is pushed towards a region where the earth is slower, the air will overtake the surface and will end up heading east

Air is diverted north and south

Polar Front
(60º, low pressure belt)

Westerly winds meet the cold polar easterly winds at a collision zone

Warm, moist, westerly air rises above the cold polar air

This produces a belt of storms

Inter Tropical Convergence Zone
(0º, low pressure belt)

Where the north east and south east trade winds meet

Ferrel Cell
(30º to 60º)

Air moving from high to low pressure systems is deflected by the Coriolis effect