Turbulent mixing from breaking oceanic internal waves drives a vertical transport of water,
heat and other climatically important tracers in the ocean, thereby playing an important role …

Oceanic lee waves are generated in the deep stratified ocean by the flow of ocean currents
over sea floor topography, and when they break, they can lead to mixing in the stably …

A (an) cyclonic (anticyclonic) eddy is usually associated with a cold (warm) core caused by
the eddy-induced divergence (convergence) motion. However, there are also some cyclonic …

Turbulent mixing, which is critically important for the equilibrium of ocean circulation, is
controlled by finescale turbulent shear (S 2) of oceanic flows through shear instability …

It is an open question whether turbulent mixing across density surfaces is sufficiently large to
play a dominant role in closing the deep branch of the ocean meridional overturning …

Arbic, BK, and G. Flierl, 2004: Baroclinically unstable geostrophic turbulence in the limit of
strong and weak bottom Ekman friction: Application to mid-ocean eddies. J. Phys …

We characterize the internal wave field at a standing meander of the Antarctic Circumpolar
Current (ACC) where strong winds, bathymetry, and a strong eddy field combine to form a …

Suppression of Internal Wave Breaking in the Antarctic Circumpolar Current near
Topography in: Journal of Physical Oceanography Volume 44 Issue 5 (2014) Jump to …

The lower limb of the global overturning circulation represents the transformation of waters
previously made dense by cryogenic processes around Antarctica that have found their way …

Lee waves generated by stratified flow over rough bottom topography in the ocean extract
momentum and energy from the geostrophic flow, causing drag and enhancing turbulence …