Turbulent flows are characterized by the non-linear cascades of energy and other inviscid
invariants across a huge range of scales, from where they are injected to where they are …

The ocean circulation is a cause and consequence of fluid scale interactions ranging from
millimeters to more than 10,000 km. Although the wind field produces a large energy input to …

▪ Abstract We review the mechanisms of steepening and breaking for internal gravity waves
in a continuous density stratification. After discussing the instability of a plane wave of …

A weak wave turbulence theory is established for incompressible fluids under rapid rotation
using a helicity decomposition, and the kinetic equations for energy E and helicity H are …

We present numerical simulations of stably stratified, vortically forced turbulence at a wide
range of Froude numbers. Large-scale vortical forcing was chosen to represent geophysical …

We investigate the steepening of the magnetic fluctuation power law spectra observed in the
inner Solar wind for frequencies higher than 0.5 Hz. This high frequency part of the spectrum …

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

Many major oceanographic internal wave observational programs of the last 4 decades are
reanalyzed in order to characterize variability of the deep ocean internal wavefield. The …

When a Bose-Einstein condensate (BEC) is driven out of equilibrium, density waves interact
nonlinearly and trigger turbulent cascades. In a turbulent BEC, energy is transferred toward …

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 …