The Coriolis effect is more important for ocean currents and wind because it arises from the Earth’s rotation, causing moving air and water to be deflected to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. This deflection influences the direction and patterns of currents and wind systems, leading to the formation of large-scale circulation patterns like trade winds and gyres. Without the Coriolis effect, these systems would not develop as they do, resulting in less organized and less predictable weather and ocean circulation.
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