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Stokes drift

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Stokes drift [¦stōks ‚drift]
(fluid mechanics)
The drift of particles in a gravity wave, which arises from the fact that particle velocities are periodic with a mean which is not zero.


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On the sides of Georges Bank, the Stokes drift is in the opposite direction to the Eulerian mean current and only about one-third as big, so that the mean Lagrangian, or particle, motion is in the same direction as the Eulerian mean flow, clockwise around the Bank, but at about two-thirds the rate.
 
 
 
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