Algebraic Bounds on the Rayleigh-B\'enard attractor
Yu Cao, Michael S. Jolly, Edriss S. Titi, Jared P. Whitehead

TL;DR
This paper establishes algebraic bounds on the Rayleigh-Bénard attractor's size using mathematical estimates, improving over previous bounds, and verifies these bounds with numerical simulations.
Contribution
It introduces algebraic bounds on the Rayleigh-Bénard attractor using enstrophy estimates, enhancing the precision of previous estimates.
Findings
Bounds are algebraic in viscosity and thermal diffusivity.
Numerical simulations confirm the sharpness of the bounds.
The approach simplifies analysis by using symmetry and boundary condition equivalences.
Abstract
The Rayleigh-B\'enard system with stress-free boundary conditions is shown to have a global attractor in each affine space where velocity has fixed spatial average. The physical problem is shown to be equivalent to one with periodic boundary conditions and certain symmetries. This enables a Gronwall estimate on enstrophy. That estimate is then used to bound the norm of the temperature gradient on the global attractor, which, in turn, is used to find a bounding region for the attractor in the enstrophy, palinstrophy-plane. All final bounds are algebraic in the viscosity and thermal diffusivity, a significant improvement over previously established estimates. The sharpness of the bounds are tested with numerical simulations.
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Algebraic Bounds on the Rayleigh-Bénard attractor
Yu Cao1
,
Michael S. Jolly1,†
1Department of Mathematics
Indiana University
Bloomington, IN 47405
corresponding author
,
Edriss S. Titi2
2Department of Mathematics, Texas A&M University, 3368 TAMU, College Station, TX 77843-3368, USA. Department of Computer Science and Applied Mathematics, Weizmann Institute of Science, Rehovot 76100, Israel. Department of Applied Mathematics and Theoretical Physics, University of Cambridge, Cambridge CB3 0WA, UK.
and
Jared P. Whitehead3
3Department of Mathematics
Brigham Young University
Provo, UT 84602
[email protected] and [email protected]
Abstract.
The Rayleigh-Bénard system with stress-free boundary conditions is shown to have a global attractor in each affine space where velocity has fixed spatial average. The physical problem is shown to be equivalent to one with periodic boundary conditions and certain symmetries. This enables a Gronwall estimate on enstrophy. That estimate is then used to bound the norm of the temperature gradient on the global attractor, which, in turn, is used to find a bounding region for the attractor in the enstrophy–palinstrophy plane. All final bounds are algebraic in the viscosity and thermal diffusivity, a significant improvement over previously established estimates. The sharpness of the bounds are tested with numerical simulations.
Key words and phrases:
Rayleigh-Bénard convection, global attractor, synchronization
2010 Mathematics Subject Classification:
35Q35, 76E06, 76F35 34D06
1. Introduction
The long-time behavior of the Rayleigh-Bénard problem was analyzed in [10, 17] for several types of boundary conditions. In that work the authors derived explicit estimates for enstrophy and the (-norm of the) temperature gradient on the global attractor for the case of no-slip boundary conditions in space dimension two. They also outlined the functional setting for the case of stress-free velocity boundary conditions (see (2.2a), (2.2b)), and mentioned that corresponding estimates can be carried out in a similar fashion. In this paper we revisit the 2D, stress-free boundary conditions case, and as in the case of rigorous bounds on the time averaged heat transport [18], we find estimates on the global attractor which are dramatically reduced from those in the no-slip boundary conditions case. We also derive estimates for the palinstrophy and -norm of the temperature.
One marked difference between no-slip and stress-free boundary conditions is that in the latter case, the system is not dissipative for general initial velocity data. This is due to the existence of steady states with arbitrarily large -norms, namely velocity of the form , (where is a constant) with zero temperature such as the shear-dominated flow investigated in [12]. Since, however, the spatial average is conserved for these flows, the system is dissipative within each invariant affine space of fixed horizontal velocity average. This wrinkle does not influence the estimates on the temperature or higher Sobolev norm estimates on the velocity.
The a priori estimates are carried out in Section 4. The key to finding sharper bounds in the stress-free case is to extend the physical domain, as done in [8], to one that is fully periodic and twice the height of the original. This makes the trilinear term vanish from the enstrophy balance, giving an easy bound that is in terms of the kinematic viscosity . Though the trilinear term persists when estimating the temperature gradient, we are able to avoid the exponential bound that resulted from using a uniform Gronwall lemma in [10], by using the algebraic bound on the enstrophy. We find that on the global attractor the (-norm of the) temperature gradient satisfies a bound that is , for , where Ra is the Rayleigh number and Pr is the Prandtl number.
We then follow the approach in [5] for the Navier-Stokes equations (NSE) to obtain an estimate for the palinstrophy, with the temperature playing the role of the body force in the NSE. This leads to curves which bound the attractor in the enstrophy–palinstrophy plane, with an overall bound on palinstrophy that is for . Using this palinstrophy bound, we then follow a similar procedure to find a bounding region for temperature in the – plane.
In Section 5 we recall from [8] how all of these bounds impact the practicality of data assimilation by nudging with just the horizontal component of velocity of the stress-free Rayleigh-Bénard system. The sharpness of our rigorous bounds are tested with numerical simulations over a range of Rayleigh numbers in Section 6. Simulations are also presented there to demonstrate that the nudging algorithm works for data with much lower resolution than the analysis requires. This is actually what suggested we might improve on the exponential bounds in [10, 17]. All the bounds here on the attractor are algebraic in the physical parameters.
2. Preliminaries
The Rayleigh-Bénard (RB) problem on the domain can be written in dimensionless form as (see, e.g., [10])
[TABLE]
where and is the thermal diffusivity. In this paper, we consider the following set of boundary conditions that are stress-free on the velocity:
[TABLE]
where the indices 1 and 2 refer the horizontal and vertical components, respectively.
Following [8], in the rest of this paper, we consider the equivalent formulation of problem (2.1) subject to the fully periodic boundary conditions on the extended domain with the following special spatial symmetries:
[TABLE]
for . As a result of this symmetry, we observe that smooth enough functions satisfy
[TABLE]
2.1. Function spaces
We will use the same notation indiscriminately for both scalar and vector Lebesgue and Sobolev spaces, which should not be a source of confusion. We denote
[TABLE]
and
[TABLE]
Note that is not a norm, but will form part of one in (2.4). We define function spaces corresponding to the relevant physical boundary conditions as in [8], where
is the set of trigonometric polynomials in , with period in the -variable, that are even, with period in the -variable,
and
is the set of trigonometric polynomials in , with period in the -variable, that are odd, with period in the -variable.
The space of smooth vector-valued functions which incorporates the divergence-free condition shall be denoted by
[TABLE]
We denote the closures of and in by and , respectively, which are endowed with the usual inner products
[TABLE]
and the associated norms
[TABLE]
We define for
[TABLE]
Finally, we denote the closures of and in by and respectively, endowed with the inner products
[TABLE]
and associated norms
[TABLE]
where is the volume of .
2.2. The linear operators
Let and . Let () be the unbounded linear operators defined by
[TABLE]
Due to periodic boundary conditions, we have . The operator is a nonnegative operator and possesses a sequence of eigenvalues with
[TABLE]
associated with an orthonormal basis of . The operator is a positive self-adjoint operator and possesses a sequence of eigenvalues with
[TABLE]
associated with an orthonormal basis of . Observe that we have the Poincaré inequality for temperature:
[TABLE]
where .
2.3. The bilinear maps
Denote the dual space of by (). Define the bilinear map (and the trilinear map ) by the continuous extension of
[TABLE]
Define the scalar analogue (and the trilinear map ) by the continuous extension of
[TABLE]
The bilinear maps (and the trilinear maps ), , have the orthogonality property:
[TABLE]
Furthermore, due to periodicity on , i.e., since , we have
[TABLE]
as well as
[TABLE]
(see, e.g., [17] for (2.6), [9] for (2.7)).
2.4. Functional setting
Following [10], we have the functional form of the RB problem (2.1):
[TABLE]
where denotes the Leray projector.
3. Statement of result
Theorem 3.1*.*
The Rayleigh-Bénard problem (2.1) with stress-free boundary conditions (2) has a global attractor within the invariant affine space
[TABLE]
The elements in satisfy
[TABLE]
[TABLE]
[TABLE]
[TABLE]
[TABLE]
where the functions , are defined below in (4.28), (4.35), respectively, Pr is the Prandtl number , is the Rayleigh number, and means for a nondimensional universal constant that is independent of the physical parameters.
Regions that bound the global attractor in the enstrophy–palinstrophy and – planes are depicted in Figures 1, 2, below.
4. A priori estimates
Global existence and uniqueness follows by the standard Galerkin procedure based on the trigonometric basis functions in the definitions of and . We thus proceed with a priori estimates.
4.1. bound on temperature
We have the following maximum principle from Lemma 2.1 in [10]
[TABLE]
where is the volume of ,
[TABLE]
and
[TABLE]
While the proof in [10] was done for no-slip boundary conditions, the only place the velocity enters is the orthogonality property . The proof carries over verbatim to the stress-free case by (2.5). Consequently, we have (4.1) for each strong solution of (2.8).
4.2. bounds on velocity
We denote the space average of the horizontal velocity over the extended domain by
[TABLE]
From (2.1) and the periodic boundary conditions on , we find that the spatial average of the horizontal velocity is conserved, i.e., . It follows that satisfies
[TABLE]
Since has zero average, it satisfies the Poincaré inequality
[TABLE]
Note that since has zero mean, it satisfies a Poincaré inequality
[TABLE]
even though does not. Taking the scalar product with , and applying (2.5), the Cauchy-Schwarz and Young inequalities as well as (4.2), we get
[TABLE]
Applying (4.2) once again, together with (4.1) and Young’s inequality, we have
[TABLE]
so that
[TABLE]
and thus,
[TABLE]
4.3. An enstrophy bound
We note that has zero average over by the periodicity of . As a consequence, we have the Poincaré inequality
[TABLE]
Taking the scalar product of (2.8a) with , we have by the orthogonality property (2.6)
[TABLE]
hence, by (4.1) and (4.6) we have
[TABLE]
and thanks to the Gronwall inequality we obtain
[TABLE]
Similar to the no-slip case analyzed in [10, 17], if , , and we have from (4.1), (4.5) and (4.8) that there exists such that
[TABLE]
4.4. Bound on the temperature gradient
We start by taking the scalar product of (2.8b) with , integrating by parts and applying the Cauchy-Schwarz and Young inequalities
[TABLE]
We apply integration by parts to rewrite the trilinear term as
[TABLE]
We then use the chain rule to rewrite the first sum, again apply integration by parts, and then incompressibility to find
[TABLE]
Applying the Hölder, Ladyzhenskaya and Young inequalities to each of the remaining four terms, we obtain
[TABLE]
Now combine (4.12), (4.14) and the Poincaré inequality (4.3) so that
[TABLE]
We note that by the Cauchy-Schwarz inequality and (4.1),
[TABLE]
so that
[TABLE]
Let , , for as in (4.9)–(4.11). From (4.9), (4.11), (4.15) and Young’s inequality, we have for all
[TABLE]
where
[TABLE]
We claim that
[TABLE]
To prove this we take , as above, and consider two possibilities.
Case I: If , for all , then clearly
[TABLE]
Case II: Suppose there exists such that . We would then have that
[TABLE]
We conclude that is strictly decreasing at a rate faster than for all such that . In particular, there exists , with such that . Moreover, for all we have . As a result, we again obtain (4.17).
In either case we may now take to conclude (4.16). Introducing the Rayleigh and Prandtl numbers in (4.16) and using the concavity of the square root function, we arrive at the bounding expression
[TABLE]
Thus, the ball , defined by
[TABLE]
is absorbing. This gives for each the existence of a global attractor , within the invariant subspace of solutions where the spatial average of velocity is fixed at . The global attractor is contained in .
4.5. Palinstrophy bound
To estimate palinstrophy on we follow [5] almost verbatim except that the effect of time independent forcing of the Navier-Stokes equations is played by the bound . The other difference is that our velocity is not normalized as in [5]. For completeness, and in order to arrive at an overall bound in terms of , we distill the essential argument here.
Returning to (4.7), we integrate by parts, and then apply the Cauchy-Schwarz inequality to get
[TABLE]
We denote
[TABLE]
Then whenever
[TABLE]
we have
[TABLE]
Setting in (2.7) and applying Agmon’s inequality, we have
[TABLE]
We next take the scalar product of (2.8a) with , and integrate by parts to obtain
[TABLE]
Note that by the Cauchy-Schwarz inequality
[TABLE]
in the region
[TABLE]
It follows that
[TABLE]
and hence, as in [5],
[TABLE]
To close the system (eliminate ) we find that the maximum of is achieved at
[TABLE]
We note that
[TABLE]
so that by (4.22)
[TABLE]
and
[TABLE]
We see that
[TABLE]
By considering the steepest descent possible below
[TABLE]
and the most shallow ascent possible above this parabola, we find three bounding curves , , after solving, in order, three final value problems. The first combines the (positive) bound in (4.25) with the upper bound in (4.20)
[TABLE]
The second picks up where the first leaves off and combines the (positive) bound in (4.26) with the upper bound in (4.20)
[TABLE]
while the third combines the (negative) bound in (4.26) with the lower bound in (4.20)
[TABLE]
where , are determined by the intersections of and (defined below) with the parabolas
[TABLE]
respectively. This results in a convex function in
[TABLE]
and concave functions in
[TABLE]
A qualitative sketch of these three curves is shown in Figure 1. It is shown in [5] that the curve does not intersect the curve . Let
[TABLE]
To prove (3.4), suppose there is an element in such that . The solution through any element in exists for all negative time. If for all , since increases with negative time, as long as , we have . By the upper bound in (4.20), would then exceed in finite negative time. Thus, we must have at some . But forward in time, the region is invariant, contradicting the assumption that the initial condition satisfied .
We now find an overall bound on palinstrophy in . A straightforward calculation shows that substituting
[TABLE]
reduces to
[TABLE]
Similarly, using
[TABLE]
leads to
[TABLE]
so that
[TABLE]
4.6. A bound on
From (4.12) and (4.14) we have
[TABLE]
Thus, if
[TABLE]
it follows that
[TABLE]
We next take the scalar product of the temperature equation with and using the fact that , write
[TABLE]
We need to move two derivatives in the trilinear term in order to ultimately obtain a bound for it in which the highest order norm is . We integrate by parts to write
[TABLE]
We then integrate the first summation by parts
[TABLE]
and split the resulting first summation as
[TABLE]
Proceeding as in (4.13), we find that . Integrating by parts again, we have
[TABLE]
Since the first sum is zero by incompressibility, we have by symmetry that , and thus . Integrating by parts one more time, we have
[TABLE]
After gathering what remains, we use Agmon’s and Ladyzhenskaya’s inequalities to estimate the trilinear term as
[TABLE]
where , and for convenience in what follows, we take .
Using this in (4.31), we find
[TABLE]
Thus, invoking our palinstrophy bound , we have
[TABLE]
We find that
[TABLE]
and that
[TABLE]
In terms of , our enstrophy bound on the attractor, (4.30) holds for
[TABLE]
Once again, by the Cauchy-Schwarz inequality, we have
[TABLE]
Thus for
[TABLE]
we combine
[TABLE]
and solve
[TABLE]
to find a straight-line solution
[TABLE]
We then find the intersection of this line with to be at , where
[TABLE]
For we combine
[TABLE]
and solve
[TABLE]
to find
[TABLE]
where
[TABLE]
As we argued in Section 4.5, if an element in the global attractor were to project in the – plane above
[TABLE]
then by (4.33) the solution through it would, in finite negative time, have to enter the region below the curves in (4.35). Yet, this region is invariant. We conclude from (4.34) and (4.29) that we have an overall bound on the global attractor of
[TABLE]
A qualitative sketch of the region bounding the global attractor in this plane is shown in Figure 2.
5. Implications for data assimilation
Suppose reality is represented by a particular solution to an evolution equation
[TABLE]
where the initial data is not known. Instead continuous data of the form is known over an interval, , for a certain type of interpolating operator with spatial resolution . The nudging approach to data assimilation amounts to solving the auxiliary system
[TABLE]
using any initial condition, e.g., . It was shown in [3, 2] that if is sufficiently large, and correspondingly, sufficiently small, then , in some norm, at an exponential rate, as . In fact, computations indicate that this approach works with data that is much more coarse than suggested by rigorous estimates (see [1, 7, 11, 6]). Flexibility in the choice of interpolant is one of the main advantages of injecting the observed data through a feedback nudging term, rather than into terms involving spatial derivatives [2, 14]. Numerical errors are shown to be bounded uniformly in time for semi-discrete [15] and fully discrete schemes [13] for (5.1).
Now consider this approach for the stress-free Rayleigh-Bénard system (2.8) using data from only the horizontal component of velocity. This means solving the auxiliary system
[TABLE]
It was proved in [8] that if and
[TABLE]
then
[TABLE]
at an exponential rate. Also shown there was that if
[TABLE]
then the stronger convergence
[TABLE]
holds at an exponential rate. The bounds in this paper on , and are all algebraic, suggesting that data assimilation by nudging with just the horizontal velocity could be effective for the stress-free Rayleigh-Bénard system. We present computational evidence to this effect in the next section.
6. Computational Results
The computations presented below were done using Dedalus, an open-source package for solving partial differential equations using pseudo-spectral methods (see [4]). The time stepping is done by a four-stage third order Runge-Kutta method.
We solve (2.1) with in the physical domain . The physical parameters of viscosity and thermal diffusivity are related to the Rayleigh and Prandtl numbers through
[TABLE]
We take so that in our dimensionless variables and use Fourier modes in the -direction and Chebyshev modes in the -direction. The numbers of modes used are , , and for runs at respectively.
6.1. Sharpness
Each plot in Figure 3 shows the projection of a solution after a transient phase in a plane spanned by the norms bounded by our analysis. The solutions are plotted over the time period for and over for (time units in the RB system (2.1)). The initial condition in each case is so the average of the horizontal velocity is zero.
It is not surprising that our rigorous overall bounds as well as the curves in Figures 1, 2 are orders of magnitude greater than the norms of these solutions. Plotting the bounds and curves together with the solutions is not revealing. Instead, to see a trend in sharpness, we plot in Figure 4 the ratios
[TABLE]
Using the numerical values for the ratio, we gauge the (highest) power in (3.2) to be inflated (at least over this range of the Rayleigh number), by an addition of , where
[TABLE]
A similar calculation for the ratio gives . We note that the curves are bending favorably for the ratios for and .
6.2. Data assimilation
Nudging is carried out at using the interpolant operator at every nodal value in each direction, i.e.,
[TABLE]
where is a positive integer, and
[TABLE]
where are the Chebyshev grid points in the -direction of the physical space. For , this means and . The nudging parameter is fixed at .
Figure 6 shows that at the solution to the data assimilation system converges to the reference solution at an exponential rate. At the error appears to saturate around during rapid oscillations (see Figure 6). We found that at the nudged solution does not converge to the reference at all (not shown). This demonstrates a critical value of .
Data assimilation by nudging works much more effectively than the rigorous analysis can guarantee. The value of and corresponding resolution of the data suggested by the conditions (5.2) and (5.3) are based on compounded, conservative estimates derived using general inequalities which are not saturated by 2D convective flows. In addition, as demonstrated in (6.1), our algebraic rigorous estimates for , , and in this case of stress-free boundary conditions, though much better than the exponential bounds previously found for the no-slip case in [10], are still somewhat artificially inflated. Numerical nudging tests in [7] for the Rayleigh-Bénard system with no-slip boundary conditions suggest that better bounds on the attractor might hold in that case as well. The key here in the stress-free case was extending the physical domain to be fully periodic, hence there is effectively, no boundary. Since, in the no-slip case one is unable to remove the physical boundary, one should have to resolve the boundary layer scales in order to determine the behavior of the solutions. This is even more pronounced in the estimates of the dimension of the global attractor of the 2D Navier-Stokes equations with no-slip boundary conditions in comparison to the case with periodic boundary conditions. Thus, improving the bounds in the no-slip case would require entirely different techniques.
7. Acknowledgments
The authors acknowledge the Indiana University Pervasive Technology Institute (see [16]) for providing HPC (Big Red II, Carbonate), storage resources that have contributed to the research results reported within this paper.
The work of Y. Cao was supported in part by National Science Foundation grant DMS-1418911, that of M.S. Jolly by NSF grant DMS-1818754. The work of E.S. Titi was supported in part by the Einstein Visiting Fellow Program, and by the John Simon Guggenheim Memorial Foundation. J.P. Whitehead acknowledges support from the Simons Foundation through award number 586788, and the hospitality of the Department of Mathematics at Indiana University where part of this work was instigated.
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