Atmospheric convection cells are large-scale patterns in Earth's atmosphere where warm air rises near the equator and cold air sinks near the poles. These cells play a crucial role in redistributing heat and moisture around the planet.
Related terms
Hadley cell: A type of atmospheric convection cell that exists between 0° and 30° latitude, responsible for tropical weather patterns.
Ferrel cell: A type of atmospheric convection cell that exists between 30° and 60° latitude, influencing mid-latitude weather patterns.
Polar cell: A type of atmospheric convection cell that exists near the poles, playing a role in polar climate conditions.