Abstract
Numerical simulations of forced dissipative 2D turbulence are hindered
by the presence of the intrinsic dual cascade, enstrophy down- and
energy up-scales. When the upscale cascade expands to the lowest modes,
the ensuing energy condensation causes steepening of energy and
enstrophy spectra and generation of strong coherent vortices. To
circumvent these effects, the lowest modes energy is usually suppressed
via introducing an energy sink in the form of linear drag or infrared
hyperviscosity which do, however, distort intermodal energy and
enstrophy exchange leading to violation of Kolmogorov--Kraichnan
statistical laws. Here, we introduce a new concept of the large scale
drag: it is conceptually similar to the two-parametric viscosity by
Kraichnan and is designed to withdraw the large scale energy without
distorting the inverse cascade. This new large scale drag has been used
in both DNS and LES in a periodic box setting where a robust steady
state was preserved for many eddy turnover times. The flow field
remained structureless and in good agreement with the Kolmogorov
statistics; coherent structures did not form at any time. We conclude
that homogeneous, isotropic, forced, dissipative 2D turbulence in the
energy subrange is not prone to coherent structure formation as long as
its inverse cascade remains undisturbed.
Original language | English GB |
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State | Published - 1 Nov 1997 |