Near the center, the pressure gradient force (the pressure at the center of the cyclone compared to the pressure outside the cyclone) and the Coriolis force must be in approximate balance, or the cyclone would collapse on itself due to the pressure difference. The wind flow around a large cyclone is counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere due to the Coriolis effect. (A high cyclone, on the other hand, rotates clockwise in the Northern Hemisphere and counterclockwise in the Southern Hemisphere.)

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