The proper scale decomposition in flows with significant density variations
is not as straightforward as in incompressible flows, with many possible ways
to define a `length-scale.' A choice can be made according to the so-called
\emph{inviscid criterion} \cite{Aluie13}. It is a kinematic requirement that a
scale decomposition yield negligible viscous effects at large enough
`length-scales.' It has been proved \cite{Aluie13} recently that a Favre
decomposition satisfies the inviscid criterion, which is necessary to unravel
inertial-range dynamics and the cascade. Here, we present numerical
demonstrations of those results. We also show that two other commonly used
decompositions can violate the inviscid criterion and, therefore, are not
suitable to study inertial-range dynamics in variable-density and compressible
turbulence. Our results have practical modeling implication in showing that
viscous terms in Large Eddy Simulations do not need to be modeled and can be
neglected.Comment: 31 pages, 37 figures, accepted in Physical Review Fluid