Sun warms air at the equator, causing it to rise
Creates a low pressure belt
Rising air cools and moves away from the equator
At 30° N/S, cool air sinks, creating high pressure
Cool air moves back to the equator (trade winds) or towards poles (westerlies)
Winds curve due to Earth's rotation (Coriolis effect)
At 60° N/S, warmer winds meet colder air, causing warm air to rise
Cool air sinks at the poles, creating high pressure
High pressure air is drawn back towards the equator