Ekman transport
Ekman transport is a natural phenomenon in oceanography that describes the vertical movement of water in the ocean due to the effect of wind on the surface of the water. Named after the Swedish scientist Vagn Walfrid Ekman, who first formulated the theory in 1902, Ekman transport is a crucial component in understanding the dynamics of the ocean's surface layer and its interaction with the atmosphere.
Theory[edit | edit source]
The theory of Ekman transport is based on the balance between the Coriolis effect and the frictional force acting on the water surface due to wind. When wind blows across the surface of the ocean, it exerts a force on the water. This force is balanced by the Coriolis effect, which is the apparent deflection of moving objects caused by the rotation of the Earth. The result is a net movement of water at an angle to the direction of the wind; this movement is known as Ekman transport.
In the Northern Hemisphere, Ekman transport causes water to move to the right of the wind direction, while in the Southern Hemisphere, it moves to the left. This is due to the difference in the direction of the Coriolis effect in the two hemispheres.
Impact[edit | edit source]
Ekman transport has significant impacts on the ocean circulation, climate, and marine life. It plays a key role in the formation of ocean gyres, large systems of rotating ocean currents. It also contributes to the upwelling and downwelling of water, processes that bring nutrients from the deep ocean to the surface and vice versa, supporting marine life.
Furthermore, Ekman transport influences the distribution of heat in the ocean, affecting the climate. For example, it helps drive the Gulf Stream, a warm ocean current that has a significant impact on the climate of Western Europe.
See also[edit | edit source]
References[edit | edit source]
- Ekman, V. W. (1905). On the Influence of the Earth's Rotation on Ocean Currents. Arkiv för matematik, astronomi och fysik, 2(11), 1-52.
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