64 research outputs found
Enstrophy dissipation in freely evolving two-dimensional turbulence
Freely decaying two-dimensional Navier--Stokes turbulence is studied. The
conservation of vorticity by advective nonlinearities renders a class of
Casimirs that decays under viscous effects. A rigorous constraint on the
palinstrophy production by nonlinear transfer is derived, and an upper bound
for the enstrophy dissipation is obtained. This bound depends only on the
decaying Casimirs, thus allowing the enstrophy dissipation to be bounded from
above in terms of initial data of the flows. An upper bound for the enstrophy
dissipation wavenumber is derived and the new result is compared with the
classical dissipation wavenumber.Comment: No figures, Letter to appear in Phys. Fluid
Local transfer and spectra of a diffusive field advected by large-scale incompressible flows
This study revisits the problem of advective transfer and spectra of a
diffusive scalar field in large-scale incompressible flows in the presence of a
(large-scale) source. By ``large-scale'' it is meant that the spectral support
of the flows is confined to the wave-number region , where is
relatively small compared with the diffusion wave number . Such flows
mediate couplings between neighbouring wave numbers within of each other
only. It is found that the spectral rate of transport (flux) of scalar variance
across a high wave number is bounded from above by ,
where denotes the maximum fluid velocity and is the spectrum
of the scalar variance, defined as its average over the shell .
For a given flux, say , across , this bound requires
This is consistent with recent
numerical studies and with Batchelor's theory that predicts a spectrum
(with a slightly different proportionality constant) for the viscous-convective
range, which could be identified with . Thus, Batchelor's
formula for the variance spectrum is recovered by the present method in the
form of a critical lower bound. The present result applies to a broad range of
large-scale advection problems in space dimensions , including some
filter models of turbulence, for which the turbulent velocity field is advected
by a smoothed version of itself. For this case, and
are the kinetic energy spectrum and flux, respectively.Comment: 6 journal pages, 1 "cartoon" figure, to appear in PR
Impeded inverse energy transfer in the Charney--Hasegawa--Mima model of quasi-geostrophic flows
The behaviour of turbulent flows within the single-layer quasi-geostrophic
(Charney--Hasegawa--Mima) model is shown to be strongly dependent on the Rossby
deformation wavenumber (or free-surface elasticity). Herein, we
derive a bound on the inverse energy transfer, specifically on the growth rate
\d\ell/\dt of the characteristic length scale representing the energy
centroid. It is found that \d\ell/\dt\le2\norm q_\infty/(\ell_s\lambda^2),
where \norm q_\infty is the supremum of the potential vorticity and
represents the potential enstrophy centroid of the reservoir, both invariant.
This result implies that in the potential energy dominated regime
(), the inverse energy transfer is strongly
impeded, in the sense that under the usual time scale no significant transfer
of energy to larger scales occurs. The physical implication is that the
elasticity of the free surface impedes turbulent energy transfer in wavenumber
space, effectively rendering large-scale vortices long-lived and inactive.
Results from numerical simulations of forced-dissipative turbulence confirm
this prediction.Comment: 8 pages, 2 figures, accepted for publication in JF
Large-scale energy spectra in surface quasi-geostrophic turbulence
The large-scale energy spectrum in two-dimensional turbulence governed by the
surface quasi-geostrophic (SQG) equation
is studied. The nonlinear transfer of this system conserves the two quadratic
quantities and
(kinetic energy), where denotes
a spatial average. The energy density is bounded and its spectrum
is shallower than in the inverse-transfer range. For
bounded turbulence, in the low-wavenumber region can be bounded by
where is a constant independent of but dependent on the domain
size. Results from numerical simulations confirming the theoretical predictions
are presented.Comment: 11 pages, 4 figures, to appear in JF
Effective degrees of nonlinearity in a family of generalized models of two-dimensional turbulence
We study the small-scale behavior of generalized two-dimensional turbulence
governed by a family of model equations, in which the active scalar
is advected by the incompressible flow
. The dynamics of this family are characterized by the
material conservation of , whose variance is
preferentially transferred to high wave numbers. As this transfer proceeds to
ever-smaller scales, the gradient $\nabla\theta$ grows without bound. This
growth is due to the stretching term $(\nabla\theta\cdot\nabla)\u$ whose
``effective degree of nonlinearity'' differs from one member of the family to
another. This degree depends on the relation between the advecting flow $\u$
and the active scalar $\theta$ and is wide ranging, from approximately linear
to highly superlinear. Linear dynamics are realized when $\nabla\u$ is a
quantity of no smaller scales than $\theta$, so that it is insensitive to the
direct transfer of the variance of $\theta$, which is nearly passively
advected. This case corresponds to $\alpha\ge2$, for which the growth of
$\nabla\theta$ is approximately exponential in time and non-accelerated. For
$\alpha<2$, superlinear dynamics are realized as the direct transfer of
entails a growth in \nabla\u, thereby enhancing the production
of . This superlinearity reaches the familiar quadratic
nonlinearity of three-dimensional turbulence at and surpasses that
for . The usual vorticity equation () is the border line,
where \nabla\u and are of the same scale, separating the linear and
nonlinear regimes of the small-scale dynamics. We discuss these regimes in
detail, with an emphasis on the locality of the direct transfer.Comment: 6 journal pages, to appear in Physical Review
Constraints on scalar diffusion anomaly in three-dimensional flows having bounded velocity gradients
This study is concerned with the decay behaviour of a passive scalar
in three-dimensional flows having bounded velocity gradients. Given an
initially smooth scalar distribution, the decay rate of the
scalar variance is found to be bounded in terms of controlled
physical parameters. Furthermore, in the zero diffusivity limit, ,
this rate vanishes as if there exists an
independent of such that for
. This condition is satisfied if in the limit ,
the variance spectrum remains steeper than for large wave
numbers . When no such positive exists, the scalar field may be
said to become virtually singular. A plausible scenario consistent with
Batchelor's theory is that becomes increasingly shallower for
smaller , approaching the Batchelor scaling in the limit
. For this classical case, the decay rate also vanishes, albeit
more slowly -- like , where is the Prandtl or Schmidt
number. Hence, diffusion anomaly is ruled out for a broad range of scalar
distribution, including power-law spectra no shallower than . The
implication is that in order to have a -independent and non-vanishing
decay rate, the variance at small scales must necessarily be greater than that
allowed by the Batchelor spectrum. These results are discussed in the light of
existing literature on the asymptotic exponential decay , where is independent of .Comment: 6-7 journal pages, no figures. accepted for publication by Phys.
Fluid
Velocity-pressure correlation in Navier-Stokes flows and the problem of global regularity
Funding: Yu is supported by an NSERC Discovery grant.Incompressible fluid flows are characterised by high correlations between low pressure and high velocity and vorticity. The velocity-pressure correlation is an immediate consequence of fluid acceleration towards low pressure regions. On the other hand, fluid converging to a low pressure centre is driven sideways by a resistance due to incompressibility, giving rise to the formation of a strong vortex, hence the vorticity-pressure correlation. Meanwhile, the formation of such a vortex effectively shields the low pressure centre from incoming energetic fluid. As a result, a local pressure minimum can usually be found at the centre of a vortex where the vorticity is greatest but the velocity is relatively low,hence the misalignment of local pressure minima and velocity maxima. For Navier--Stokes flows, this misalignment has profound implications on extreme momentum growth and maintenance of regularity. This study examines the role of the velocity-pressure correlation on the problem of Navier--Stokes global regularity. On the basis of estimates for flows locally satisfying the critical scaling of the Navier--Stokes system, a qualitative theory of this correlation is considered. The theory appears to be readily quantified, advanced and tested by theoretical, mathematical and numerical methods. Regularity criteria depending on the degree of the velocity-pressure correlation are presented and discussed in light of the above theory. The result suggests that as long as global pressure minimum (or minima) and velocity maximum (or maxima) are mutually exclusive, then regularity is likely to persist. This is the first result that makes use of an explicit measure of the velocity-pressure correlation as a key factor in the maintenance of regularity or development of singularity.PreprintPublisher PDFPeer reviewe
Note on Prodi-Serrin-Ladyzhenskaya type regularity criteria for the Navier-Stokes equations
X.Y. is partially supported by the Discovery Grant No. RES0020476 from NSERC.In this article we prove new regularity criteria of the Prodi-Serrin-Ladyzhenskaya type for the Cauchy problem of the three-dimensional incompressible Navier-Stokes equations. Our results improve the classical Lr(0,T;Ls) regularity criteria for both velocity and pressure by factors of certain nagative powers of the scaling invariant norms ||u||L3 and ||u||H1/2.PostprintPeer reviewe
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