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Filtering in the context of large eddy simulation (LES) is a mathematical operation intended to remove a range of small scales from the solution to the Navier-Stokes equations. Because the principal difficulty in simulating turbulent flows comes from the wide range of length and time scales, this operation makes turbulent flow simulation cheaper by reducing the range of scales that must be resolved. The LES filter operation is low-pass, meaning it filters out the scales associated with high frequencies.
Filtering in the context of large eddy simulation (LES) is a mathematical operation intended to remove a range of small scales from the solution to the Navier-Stokes equations. Because the principal difficulty in simulating turbulent flows comes from the wide range of length and time scales, this operation makes turbulent flow simulation cheaper by reducing the range of scales that must be resolved. The LES filter operation is low-pass, meaning it filters out the scales associated with high frequencies.
Contents
Homogeneous filters
Definition in physical space
The low-pass filtering operation used in LES can be applied to a spatial and temporal field, for example
ϕ
(
x
,
t
)
{\displaystyle \phi ({\boldsymbol {x}},t)}
. The LES filter operation may be spatial, temporal, or both. The filtered field, denoted with a bar, is defined as:
ϕ
(
x
,
t
)
¯
=
∫
−
∞
∞
∫
−
∞
∞
ϕ
(
r
,
t
′
)
G
Definition in spectral space
The filtering operation removes scales associated with high frequencies, and the operation can accordingly be interpreted in Fourier space. For a scalar field
Homogeneous LES filters must satisfy the following set of properties when applied to the Navier-Stokes equations.
1. Conservation of constants
The value of a filtered constant must be equal to the constant,
a
¯
=
a
,
{\displaystyle {\overline {a}}=a,}
which implies,
∫
−
∞
∞
∫
−
∞
∞
G
(
ξ
,
t
′
)
d
3
ξ
d
t
′
=
1.
Inhomogeneous filters
Implementations of filtering operations for all but the simplest flows are inhomogeneous filter operations. This means that the flow either has non-periodic boundaries, causing problems with certain types of filters, or has a non-constant filter width
Δ
{\displaystyle \Delta }
, or both. This prevents the filter from commuting with derivatives, and the commutation operation leads to several additional error terms:
[
∂
∂
x
,
G
⋆
]
ϕ
=
∂
∂
x
(
G
⋆
ϕ
)
−
G
⋆
∂
ϕ
∂
x
=
∂
Classic large eddy simulation filters
There are three filters ordinarily used for spatial filtering in large eddy simulation. The definition of
The spectral interpretation of the filtering operation is essential to the filtering operation in large eddy simulation, as the spectra of turbulent flows is central to LES subgrid-scale models, which reconstruct the effect of the sub-filter scales (the highest frequencies). One of the challenges in subgrid modeling is to effectively mimic the cascade of kinetic energy from low to high frequencies. This makes the spectral properties of the implemented LES filter very important to subgrid modeling efforts.