Add to ORKGColloque avec actes et comité de lecture. Internationale.International audienceThe interaction of tidal currents with sea-floor topography generates internal gravity waves, called internal tides. Their dissipation due to nonlinear wave breaking and concomitant three-dimensional turbulence could play an important role in mixing the abyssal ocean and hence in controlling the large-scale ocean circulation. As part of on-going work to understand the vertical distribution of wave breaking over sea-floor topography, we investigate the instability of internal tides in a simple linear model. For two-dimensional tides over one-dimensional topography, the formation of unstable regions is closely linked to singularities in the topography shape. For th...
Mixing is an essential process in the deep ocean, as it accounts for the raising of the cold abyssal...
Internal tides are a predominant source of high‐frequency variability and diapycnal mixing in the oc...
The flow in the coastal ocean, and especially on the continental shelf and slope is often characteri...
The interaction of tidal currents with sea-floor topography generates internal gravity waves, called...
Internal gravity waves are complex oscillations widely found in fluids exhibiting density stratifica...
As part of an ongoing effort to develop a parameterization of wave-induced abyssal mixing, the autho...
Mixing in the abyssal ocean is known to play an important role in controlling the large-scale ocean ...
The mixing induced by breaking internal gravity waves is an important contributor to the ocean’s ene...
A non-linear non-hydrostatic model (MIT-gcm) is used to study the generation and propagation of inte...
Oceanic internal tides are internal waves with tidal periodicities. They are ubiquitous throughout t...
We study the interplay between internal gravity waves and topography. When internal waves are imping...
It is well-known that internal wave breaking is the principle cause of ocean mixing. The latter play...
Graduation date: 2011Tide-topography coupling is important for understanding surface-tide energy los...
Mixing is an essential process in the deep ocean, as it accounts for the raising of the cold abyssal...
The small-scale roughness properties of the seafloor are increasingly being recognized as critical p...
Mixing is an essential process in the deep ocean, as it accounts for the raising of the cold abyssal...
Internal tides are a predominant source of high‐frequency variability and diapycnal mixing in the oc...
The flow in the coastal ocean, and especially on the continental shelf and slope is often characteri...
The interaction of tidal currents with sea-floor topography generates internal gravity waves, called...
Internal gravity waves are complex oscillations widely found in fluids exhibiting density stratifica...
As part of an ongoing effort to develop a parameterization of wave-induced abyssal mixing, the autho...
Mixing in the abyssal ocean is known to play an important role in controlling the large-scale ocean ...
The mixing induced by breaking internal gravity waves is an important contributor to the ocean’s ene...
A non-linear non-hydrostatic model (MIT-gcm) is used to study the generation and propagation of inte...
Oceanic internal tides are internal waves with tidal periodicities. They are ubiquitous throughout t...
We study the interplay between internal gravity waves and topography. When internal waves are imping...
It is well-known that internal wave breaking is the principle cause of ocean mixing. The latter play...
Graduation date: 2011Tide-topography coupling is important for understanding surface-tide energy los...
Mixing is an essential process in the deep ocean, as it accounts for the raising of the cold abyssal...
The small-scale roughness properties of the seafloor are increasingly being recognized as critical p...
Mixing is an essential process in the deep ocean, as it accounts for the raising of the cold abyssal...
Internal tides are a predominant source of high‐frequency variability and diapycnal mixing in the oc...
The flow in the coastal ocean, and especially on the continental shelf and slope is often characteri...