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- W2808173652 abstract "Many years of simultaneous hourly buoy wind and directional wave spectra data in the Gulf of Mexico and the Pacific were used to estimate Stokes drift and u* ew where u* = (magnitude of the local windstress/water density)1/2 and ew is a unit vector in the direction of the local wind. Stokes drift and u* ew were strongly vectorally correlated, the two vectors on average being within a few degrees of one another. This result remained valid even when there was evidence of remotely forced swell. Extension of the observed wave spectra above 0.35 Hz to the u*-dependent wave breaking frequency shows that typically the e-folding scale of the Stokes drift with depth is less than 1.8 m, much smaller than the Ekman layer e-folding scale. Therefore, there is negligible induced Eulerian cancellation of the Stokes drift, and the surface particle movement is governed by the Eulerian velocity + |uStokes|ew. Taking into account wave spreading, |uStokes| typically ranges from about 3 to 13 cm/s. Thus, the Stokes drift, which can be estimated directly from the wind stress, is an order one contributor to the surface transport of particles." @default.
- W2808173652 created "2018-06-21" @default.
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- W2808173652 date "2018-07-01" @default.
- W2808173652 modified "2023-10-16" @default.
- W2808173652 title "The Relationship of Near‐Surface Flow, Stokes Drift and the Wind Stress" @default.
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- W2808173652 doi "https://doi.org/10.1029/2018jc014102" @default.
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