5,050 research outputs found
Predictability of the energy cascade in 2D turbulence
The predictability problem in the inverse energy cascade of two-dimensional
turbulence is addressed by means of direct numerical simulations. The growth
rate as a function of the error level is determined by means of a finite size
extension of the Lyapunov exponent. For error within the inertial range, the
linear growth of the error energy, predicted by dimensional argument, is
verified with great accuracy. Our numerical findings are in close agreement
with the result of TFM closure approximation.Comment: 3 pages, 3 figure
Chaos and predictability of homogeneous-isotropic turbulence
We study the chaoticity and the predictability of a turbulent flow on the
basis of high-resolution direct numerical simulations at different Reynolds
numbers. We find that the Lyapunov exponent of turbulence, which measures the
exponential separation of two initially close solution of the Navier-Stokes
equations, grows with the Reynolds number of the flow, with an anomalous
scaling exponent, larger than the one obtained on dimensional grounds. For
large perturbations, the error is transferred to larger, slower scales where it
grows algebraically generating an "inverse cascade" of perturbations in the
inertial range. In this regime our simulations confirm the classical
predictions based on closure models of turbulence. We show how to link
chaoticity and predictability of a turbulent flow in terms of a finite size
extension of the Lyapunov exponent.Comment: 5 pages, 5 figure
Condensate in quasi two-dimensional turbulence
We investigate the process of formation of large-scale structures in a
turbulent flow confined in a thin layer. By means of direct numerical
simulations of the Navier-Stokes equations, forced at an intermediate scale, we
obtain a split of the energy cascade in which one fraction of the input goes to
small scales generating the three-dimensional direct cascade. The remaining
energy flows to large scales producing the inverse cascade which eventually
causes the formation of a quasi two-dimensional condensed state at the largest
horizontal scale. Our results shows that the connection between the two actors
of the split energy cascade in thin layers is tighter than what was established
before: the small scale three-dimensional turbulence acts as an effective
viscosity and dissipates the large-scale energy thus providing a
viscosity-independent mechanism for arresting the growth of the condensate.
This scenario is supported by quantitative predictions of the saturation energy
in the condensate
Split energy cascade in turbulent thin fluid layers
We discuss the phenomenology of the split energy cascade in a
three-dimensional thin fluid layer by mean of high resolution numerical
simulations of the Navier-Stokes equations. We observe the presence of both an
inverse energy cascade at large scales, as predicted for two-dimensional turbu-
lence, and of a direct energy cascade at small scales, as in three-dimensional
turbulence. The inverse energy cascade is associated with a direct cascade of
enstrophy in the intermediate range of scales. Notably, we find that the
inverse cascade of energy in this system is not a pure 2D phenomenon, as the
coupling with the 3D velocity field is necessary to guarantee the constancy of
fluxes
Turbulent channel without boundaries: The periodic Kolmogorov flow
The Kolmogorov flow provides an ideal instance of a virtual channel flow: It
has no boundaries, but nevertheless it possesses well defined mean flow in each
half-wavelength. We exploit this remarkable feature for the purpose of
investigating the interplay between the mean flow and the turbulent drag of the
bulk flow. By means of a set of direct numerical simulations at increasing
Reynolds number we show the dependence of the bulk turbulent drag on the
amplitude of the mean flow. Further, we present a detailed analysis of the
scale-by-scale energy balance, which describes how kinetic energy is
redistributed among different regions of the flow while being transported
toward small dissipative scales. Our results allow us to obtain an accurate
prediction for the spatial energy transport at large scales.Comment: 7 pages, 8 figure
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