Six recent Langmuir turbulence parameterization schemes and five traditional schemes are
implemented in a common single‐column modeling framework and consistently compared …

Langmuir turbulence consists of Langmuir circulation (LC) generated at the surface of rivers,
lakes, bays, and oceans by the interaction between the wind-driven shear and surface …

Langmuir circulations (LCs) generated by the interaction between wind-driven currents and
surface waves can engulf the whole water column in neutrally stratified shallow water and …

Langmuir turbulence is a boundary layer oceanographic phenomenon of the upper layer
that is relevant to mixing and vertical transport capacity. It is a manifestation of imposed …

Turbulence in the ocean surface layer is forced by a mixture of buoyancy, wind, and wave
processes that evolves over time scales from the diurnal scale of buoyancy forcing, through …

In this study, we expand previous large eddy simulation (LES) modeling investigations of
Langmuir turbulence (LT) to real ocean conditions using field observations collected under …

Langmuir circulation cells extending through entire water columns exert a profound
influence on sediment transport on shallow shelves, hence their designation as" Langmuir …

Velocity, hydrographic, and microstructure observations collected under moderate to high
winds, large surface waves, and significant ocean-surface heat losses were utilized to …

Various forms of regime diagrams have become an accepted means of identifying the
dominant type of forcing of turbulence in the ocean surface layer. However, all of the …

The ocean boundary layer (OBL) is forced by atmosphere-ocean and sea ice-ocean
momentum fluxes, wave dynamics, and buoyancy; in coastal zones, OBL dynamics are …