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Stage 2: Sinking Air
About 30 degrees N and S of the equator, warm air cools and sinks, creating a high-pressure area.
Return to Equator
The sinking air moves back towards the equator.
Stage 3: Remaining Air
The rest of the cooler air moves towards the poles.
Coriolis Effect (Northern Hemisphere)
Winds are deflected to the right of their direction.
Coriolis Effect (Southern Hemisphere)
Winds are deflected to the left of their direction.
Trade Winds
Steady breezes that consistently blow towards the equator.
The Horse Latitudes
Areas of still, dry weather at 30 degrees north and south of the equator.