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- W2772036299 abstract "Abstract This study shows that the presence of Stokes drift u s in the turbulent upper ocean induces a near-surface Eulerian current that opposes the Stokes drift. This current is distinct from previously studied anti-Stokes currents because it does not rely on the presence of planetary rotation or mean lateral gradients. Instead, the anti-Stokes flow arises from an interaction between the Stokes drift and turbulence. The new anti-Stokes flow is antiparallel to u s near the ocean surface, is parallel to u s at depth, and integrates to zero over the depth of the boundary layer. The presence of Stokes drift in large-eddy simulations (LES) is shown to induce artificial energy production caused by a combination of the new anti-Stokes flow and LES numerics. As a result, care must be taken when designing and interpreting simulations of realistic wave forcing, particularly as rotation becomes weak and/or u s becomes perpendicular to the surface wind stress. The mechanism of the artificial energy production is demonstrated for a generalized LES subgrid scheme." @default.
- W2772036299 created "2017-12-22" @default.
- W2772036299 creator A5030045471 @default.
- W2772036299 date "2018-01-01" @default.
- W2772036299 modified "2023-09-27" @default.
- W2772036299 title "Turbulence-Induced Anti-Stokes Flow and the Resulting Limitations of Large-Eddy Simulation" @default.
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- W2772036299 doi "https://doi.org/10.1175/jpo-d-17-0208.1" @default.
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