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1. Introduction Surface gravity waves induce a rectified motion of fluid particles and thus a wave-averaged difference between the mean Eulerian velocity, uE, and the mean Lagrangian velocity uL [1,2] uL=uE+uS.1.1 uS is the Stokes velocity, also known as Stokes drift. The Stokes velocity is fundamental to understanding wave-averaged effects, such as the CL vortex force and the Stokes–Coriolis force, in the wave-averaged momentum and vorticity equations [3–7].
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