Abstract
It has been recognized that the subgrid-scale (SGS) parameterization
represents
a critical component of a successful large-eddy simulation (LES). Commonly
used
linear SGS models produce erroneous mean velocity profiles in LES of high-Reynolds-number boundary layer flows. Although recently proposed approaches
to solving this
problem have resulted in significant improvements, questions about the
true nature
of the SGS problem in shear-driven high-Reynolds-number flows remain open.We argue that the SGS models must capture inertial transfer effects including
backscatter of energy as well as its redistribution among the normal SGS
stress
components. These effects are the consequence of nonlinear interactions
and
anisotropy.
In our modelling procedure we adopt a phenomenological approach whereby
the
SGS stresses are related to the resolved velocity gradients. We show that
since the
SGS stress tensor is not frame indifferent a more general nonlinear model
can be
applied to the SGS parameterization. We develop a nonlinear SGS model capable
of
reproducing the effects of SGS anisotropy characteristic for shear-driven
boundary
layers. The results obtained using the nonlinear model for the LES of a
neutral
shear-driven atmospheric boundary layer show a significant improvement
in
prediction of the non-dimensional shear and low-order statistics compared
to
the linear
Smagorinsky-type models. These results also demonstrate a profound effect
of the
SGS model on the flow structures.
Publisher
Cambridge University Press (CUP)
Subject
Mechanical Engineering,Mechanics of Materials,Condensed Matter Physics
Cited by
226 articles.
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