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Without the Coriolis effect, there would likely be only three major atmospheric convection cells in each hemisphere: the Hadley cell, the Ferrel cell, and the Polar cell. The Coriolis effect causes the deflection of winds and influences the formation of these cells, leading to a more complex circulation pattern. Without it, air would rise at the equator and sink at the poles, resulting in a simpler, direct flow of air from the equator to the poles. This would significantly alter global wind patterns and climate systems.

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