A dynamic subgrid-scale model estimates its closure coefficient from the resolved flow as the calculation proceeds. In a common construction, a second, coarser test filter probes interactions among resolved scales, providing information for a subgrid-scale model below the original resolution.[ref]
A dynamic subgrid-scale eddy viscosity model by Massimo Germano and others (1990). Abstract and §2, dynamic coefficient from two filtering levels
Write a bar for the original spatial averaging filter and a hat for the test filter. DefineDirect subtraction gives the Germano identityThe rightmost expression uses only resolved quantities. The identity is exact for these definitions; extrapolating a closure between the filter levels is the modeling step.[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
For instance, suppose a chosen closure writes the deviatoric stresses as and , and assumes can be taken outside the test filtering. Then , where . One way to choose is to minimize . Differentiation giveswhen the denominator is nonzero. This is a least squares fit of a scalar to tensor data. In a one-component illustrative fit, and give .
The coefficient need not remain positive. Depending on the closure, a negative value can permit turbulent backscatter, but a small denominator can also make an estimate unreliable. Averaging, bounds and treatment of weak strain are additional choices. Dynamically fitting a coefficient does not remove these assumptions or make unresolved motion observable.
A test filter is an additional spatial averaging filter applied to already resolved data in a dynamic subgrid-scale model. If is the field after the grid filter, a test kernel givesIt probes interactions within the available resolved motion at a coarser analysis level. It does not measure the original subgrid motion directly.[ref]
A dynamic subgrid-scale eddy viscosity model by Massimo Germano and others (1990). §2, grid and test filter construction and two-level stress definitions
For example, suppose two resolved values of one velocity component are and . A test average gives and , so the resolved differenceis nonzero. This quantity is computable from the resolved samples; a dynamic subgrid-scale model uses such information to constrain a closure.
The combined filter is , so its width cannot always be identified with the width of alone. A centred box averaging filter of width has second moment . Combining it with one of width gives second moment , because centred convolution kernels add their second moments. A single box of width has the same second moment, but not the same kernel shape.
Choosing a width convention is therefore part of the model. The Germano identity holds for the filters actually defined; an assumed relation between modeled stresses at those levels is an additional approximation. Near boundaries, the test operation also needs a specified treatment of data outside the available region.
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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