Internal gravity waves play a primary role in geophysical fluids: They contribute significantly
to mixing in the ocean, and they redistribute energy and momentum in the middle …

We report the quantitative experimental observation of the weak inertial-wave turbulence
regime of rotating turbulence. We produce a statistically steady homogeneous turbulent flow …

We present laboratory experiments on turbulence in a linearly stratified fluid driven by an
ensemble of internal gravity waves which approaches statistical homogeneity and …

Density-stratified and/or rotating fluids are very common in geophysical and astrophysical
flows and enable the propagation of respectively internal gravity waves and inertial waves …

Recent developments of the weak turbulence theory applied to internal waves exhibit a
power-law solution of the kinetic energy equation close to the oceanic Garrett-Munk …

The theoretical framework that should be used for describing rotating turbulence,, is the
subject of an active debate. It was shown experimentally, and numerically, that the formalism …

Internal waves are believed to be of primary importance as they affect ocean mixing and
energy transport. Several processes can lead to the breaking of internal waves and they …

We perform one of the first studies into the non-linear evolution of tidally excited inertial
waves in a uniformly rotating fluid body, exploring a simplified model of the fluid envelope of …

We present experimental evidence for a double cascade of kinetic energy in a statistically
stationary rotating turbulence experiment. Turbulence is generated by a set of vertical flaps …

Internal waves are ubiquitous in the ocean and play an essential role in the transport of
energy and mixing. Their peculiar reflection enables the concentration of energy on a limit …