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Kelvin-Helmholtz (KH) instability, characterized by the distinctive
finite-amplitude billows it generates, is an important mechanism in the development
of turbulence in the stratified interior of ...
Effects of Horizontal Advection on Upper Ocean Mixing：A Case of Frontogenesis
Horizontal Advection Upper Ocean Mixing Frontogenesis
2009/2/10
The wind stress on the ocean surface induces horizontal advection and vertical mixing, two mechanisms which are capable of changing the surface water density. Advection and mixing can enhance or parti...
Implications for Ocean Mixing of Internal Wave Scattering off Irregular Topography
Ocean Mixing Internal Wave nonlinear interactions geometric effects
2009/1/5
Earlier work has suggested that internal wave reflection off sloping bottoms may cause significant diapycnal mixing in the deep ocean, and may also represent an important sink of internal wave energy....
The Influence of Ocean Mixing on the Absolute Velocity Vector
Ocean Mixing Absolute Velocity Vector
2008/12/11
The Influence of Ocean Mixing on the Absolute Velocity Vector.
Observations of Overturning in the Thermocline: The Context of Ocean Mixing
Thermocline Context Ocean Mixing
2008/6/30
The time sequence of events that lead to internal wave breaking and ocean turbulence is investigated. Data are obtained from depths 100–400 m with a repeat profiling CTD and a coded-pulse Doppler sona...
Effects of Equatorial Undercurrent Shear on Upper-Ocean Mixing and Internal Waves
Effects Equatorial Undercurrent Shear Upper-Ocean Mixing Internal Waves
2008/6/4
The effect of equatorial undercurrent (EUC) shear on equatorial upper-ocean mixing is studied using a large eddy simulation (LES) model. This study consists of five numerical experiments of convection...