The Smagorinsky subgrid model is revised to properly account for grid
anisotropy, using energy equilibrium considerations in isotropic turbu
lence. For moderate resolution anisotropies, Deardorff's estimate invo
lving an equivalent grid scale DELTA(eq) = (DELTA1DELTA2DELTA3)1/3 is
given a rigorous basis. For more general grid anisotropies, the Smagor
insky eddy viscosity is recast as nu(T) = [c(s)DELTA(eq)f(a1, a2)]2 ab
solute value of S, where f (a1,a2) is a function of the grid aspect ra
tios a1 and a2, and absolute value of S is the resolved strain rate ma
gnitude. The asymptotic behavior of nu(T) at several limits of the asp
ect ratios are examined. Approximation formulas are developed so that
f (a1,a2) can easily be evaluated in practice, for arbitrary values of
a1 and a2. It is argued that these results should be used in conjunct
ion with the dynamic model of Germano et al. whenever the anisotropy o
f the test-filter differs significantly from that of the basic grid.