Characteristics of Langmuir Turbulence in the Ocean Mixed Layer

• Published in: Journal of physical oceanography Vol. 39; no. 8; pp. 1871 - 1887
• Main Authors: GRANT, Alan L. M, BELCHER, Stephen E
• Format: Journal Article
• Language: English
• Published: Boston, MA American Meteorological Society 01.08.2009
• Subjects: Boundary layers; Earth, ocean, space; Exact sciences and technology; External geophysics; Friction; Kinetic energy; Marine; Meteorology; Oceanic turbulence; Oceans; Physics of the oceans; Studies; Turbulence; Velocity; Friction velocity; Mixed layer; Large eddy simulation; Entrainment (atmosphere, ocean); Skin friction; Shear turbulence; Turbulence energy; longshore currents; Shear layer; Variance; Drift wave
• ISSN: 0022-3670; 1520-0485
• DOI: 10.1175/2009jpo4119.1

Abstract This study uses large-eddy simulation (LES) to investigate the characteristics of Langmuir turbulence through the turbulent kinetic energy (TKE) budget. Based on an analysis of the TKE budget a velocity scale for Langmuir turbulence is proposed. The velocity scale depends on both the friction velocity and the surface Stokes drift associated with the wave field. The scaling leads to unique profiles of nondimensional dissipation rate and velocity component variances when the Stokes drift of the wave field is sufficiently large compared to the surface friction velocity. The existence of such a scaling shows that Langmuir turbulence can be considered as a turbulence regime in its own right, rather than a modification of shear-driven turbulence. Comparisons are made between the LES results and observations, but the lack of information concerning the wave field means these are mainly restricted to comparing profile shapes. The shapes of the LES profiles are consistent with observed profiles. The dissipation length scale for Langmuir turbulence is found to be similar to the dissipation length scale in the shear-driven boundary layer. Beyond this it is not possible to test the proposed scaling directly using available data. Entrainment at the base of the mixed layer is shown to be significantly enhanced over that due to normal shear turbulence.