Hadley Cell: The warm, low pressure air rises at 0 Lat. As the air cools down, it becomes more dense and sinks at 30 Lat.
Mid-Latitude Cell: The cool air from 30 Lat gets warmer as it reaches 60 Lat and rises up into the atmosphere.
Polar Cell: The rising warm air from 60 Lat moves towards 90 Lat, where it cools down and sinks back to the surface of the Earth.