The primary force involved in the development of surface currents is the wind. As winds blow across the ocean's surface, they exert frictional drag on the water, causing it to move. Additionally, the Coriolis effect, resulting from the Earth's rotation, influences the direction of these currents, causing them to flow in a circular pattern. Other factors, such as oceanic topography and temperature gradients, can also play a role in shaping surface currents.
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