The characteristics of turbulence caused by three-dimensional breaking
of internal
gravity waves beneath a critical level are investigated by means of high-resolution
numerical simulations. The flow evolves in three stages. In the first one
the flow is
two-dimensional: internal gravity waves propagate vertically upwards and
create a
convectively unstable region beneath the critical level. Convective instability
leads to
turbulent breakdown in the second stage. The developing three-dimensional
mixed region
is organized into shear-driven overturning rolls in the plane of wave propagation
and into counter-rotating streamwise vortices in the spanwise plane. The
production
of turbulent kinetic energy by shear is maximum. In the last stage, shear
production
and mechanical dissipation of turbulent kinetic energy balance.
The evolution of the flow depends on topographic parameters (wavelength
and amplitude),
on shear and stratification as well as on viscosity. Here, only the implications
of the viscosity for the instability structure and evolution in terms of
the Reynolds
number are considered. Smaller viscosity leads to earlier onset of convective
instability and overturning waves. However, viscosity retards the onset
of smaller-scale
three-dimensional instabilities and leads to a reduced momentum transfer
to the mean
flow below the critical level. Hence, the formation of secondary overturning
rolls is
sustained by lower viscosity.
The budgets of total kinetic and potential energies are calculated.
Although the
domain-averaged turbulent kinetic energy is less than 1% of the total kinetic
energy,
it is strong enough to form a patchy and intermittent turbulent mixed layer
below
the critical level.