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Dynamics of Langmuir Circulation in oceanic surface layers
Anand Gnanadesikan
This work investigates whether large-scale coherent vortex structures driven by wave-current interaction (Langmuir circulation) are responsible for maintaining the oceanic mixed layer. Langmuir circulation s dominate near-surface vertical transport of momentum and density when the characteristic scale for forcing (defined as the Craik Leibovich instability parameter g (CLS)) is stronger than the characteristic scale for diffusive decay g (diff). Since the wave-current forcing is concentrated near the surface, both terms depend on the cell geometry. Cells with long wavelengths penetrate more deeply into the water column. These cells grow more slowly than the fastest growing mode for most cases, but always dominate the solution in the absence of Coriolis forces. In the presence of Coriolis forces, the horizontal wavelength and the depth of penetration are limited. When a cell geometry can be found such that g (CLS) > g (diff), the current profile produced by small-scale turbulence is unstable to Langmuir cells and the cells replace small-scale diffusion as the dominant vertical transport mechanism for momentum and density. The perturbation crosscell shear is predicted to scale as g (CLS). Such a scaling is observed during two field experiments. The observed velocity profile during these experiments is more sheared than predicted by a model which implicitly assumes instantaneous mixing by large eddies but less sheared than predicted by a model which assumes small-scale mixing by near-isotropic turbulence. The latter profile is unstable to Langmuir cells when waves are present. The inclusion of cells driven by wave-current interaction explains the failure of the mixed layer to restratify on two days with high waves and low wind. Wave-current interaction introduces a small but efficient source of energy for transporting density which goes as the surface stress times the Stokes drift.