Six subgrid models for the turbulent stress tensor are tested by condu
cting large-eddy simulations (LES) of the weakly compressible temporal
mixing layer: the Smagorinsky, similarity, gradient, dynamic eddy-vis
cosity, dynamic mixed and dynamic Clark models. The last three models
are variations of the first three models using the dynamic approach. T
wo sets of simulations are performed in order to assess the quality of
the six models. The LES results corresponding to the first set are co
mpared with filtered results obtained from a direct numerical simulati
on (DNS). It appears that the dynamic models lead to more accurate res
ults than the non-dynamic models tested. An adequate mechanism to diss
ipate energy from resolved to subgrid scales is essential. The dynamic
models have this property, but the Smagorinsky model is too dissipati
ve during transition, whereas the similarity and gradient models are n
ot sufficiently dissipative for the smallest resolved scales. In this
set of simulations, at moderate Reynolds number, the dynamic mixed and
Clark models are found to be slightly more accurate than the dynamic
eddy-viscosity model. The second set of LES concerns the mixing layer
at a considerably higher Reynolds number and in a larger computational
domain. An accurate DNS for this mixing layer can currently not be pe
rformed, thus in this case the LES are tested by investigating whether
they resemble a self-similar turbulent flow. It is found that the dyn
amic models generate better results than the non-dynamic models. The c
losest approximation to a self-similar state was obtained using the dy
namic eddy-viscosity model.