The Polar Cell is a component of the Earth's atmospheric circulation, primarily found in the polar regions. It is characterized by cold air sinking at the poles, which creates high-pressure areas. This cold air then moves towards the equator at the surface, where it warms up and rises, contributing to the overall circulation of the atmosphere. In the Polar Cell, the movement of air is influenced by the Earth's rotation, leading to the formation of the Polar Front. This front separates the cold polar air from the warmer air of the mid-latitudes, playing a crucial role in weather patterns and climate in regions like the Arctic and Antarctic.