The Eckman spiral occurs as a result of:

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The Eckman spiral is a phenomenon observed in bodies of water where there is wind-induced circulation. As the wind blows across the surface of the water, it creates a net drag force that induces a current in the water. This current, known as the Eckman current, is deflected to the right of the wind direction in the Northern Hemisphere and to the left in the Southern Hemisphere due to the Coriolis effect. This deflection causes the current to spiral downwards as it moves away from the surface, resulting in the Eckman spiral. Salinity, transparency, pressure, and dissolved gases do not play a significant role in the formation of the Eckman spiral.

The Eckman Spiral Occurs as a Result Of