The Germano identity is an exact relation between stresses at two filtering levels and a stress computable from the resolved field. Let a bar denote a grid filter and a hat a test filter. With the subgrid-scale stress conventionthe identity statesIt follows by substituting and cancelling the common term. Massimo Germano and collaborators used this relation to construct a dynamic subgrid-scale model.[ref]
A dynamic subgrid-scale eddy viscosity model by Massimo Germano and others (1990). §2, equations 8–10, resolved stress and algebraic two-filter identity
A scalar block-average example makes every term visible. Start with four velocity values grouped as and . Averaging within each group gives and , hence . A test average over the two groups then givesThus reads . The resolved group averages contain enough information for , although they alone do not determine the original within-group variances.
The identity has no fitted coefficient. To estimate a missing subgrid-scale stress, a closure assumes some model form at both filtering levels and tries to make their difference agree with the known . Extracting a varying coefficient from a filter, choosing a filter width and stabilizing a fit are modeling decisions; they do not enter the cancellation proof.
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