The dynamic eddy-viscosity relationship is a suitable choice for modeling t
he subgrid-scales (SGS) in a large-eddy simulation (LES) of complex turbule
nt flows in irregular domains. This algebraic relationship is easy to imple
ment and its dynamic coefficient will give negligible turbulent viscosity c
ontributions in the flow regions that are irrotational or laminar. Its fine
-scale turbulence predictions can be qualitatively reasonable if the local
grid resolution maintains the SGS field predominantly within the equilibriu
m range of turbulent energy spectra. This performance is given herein by tw
o curvilinear coordinate forms of the dynamic Smagorinsky, model that are f
ormally derived and a-priori tested using the resolved physics of the cylin
der wake. The consei-vative form evaluates the coefficient in the computati
onal (transformed) space whereas its non-dynamic conservative counterpart o
perates in the, physical domain. Although both forms equally captured the r
eal normal SGS stress reasonably well, the real shear stress and dissipatio
n rates were severely, under-predicted. Mixing the eddy-viscosity choice wi
th a scale-similarity model can ease this latter deficiency.