In a previous paper, Germane, et al. (1991) proposed a method for comp
uting coefficients of subgrid-scale eddy viscosity models as a functio
n of space and time. This procedure has the distinct advantage of bein
g self-calibrating and requires no a priori specification of model coe
fficients or the use of wall damping functions. However, the original
formulation contained some mathematical inconsistencies that limited t
he utility of the model. In particular, the applicability of the model
was restricted to flows that are statistically homogeneous in at leas
t one direction. These inconsistencies and limitations are discussed a
nd a new formulation that rectifies them is proposed. The new formulat
ion leads to an integral equation whose solution yields the model coef
ficient as a function of position and time. The method can be applied
to general inhomogeneous flows and does not suffer from the mathematic
al inconsistencies inherent in the previous formulation. The model has
been tested in isotropic turbulence and in the flow over a backward-f
acing step.