We prove rigorous scaling laws for measures of the vertical heat transport enhancement in two models of convection driven by uniform internal heating at infinite Prandtl number. In the first model, a layer of incompressible fluid is bounded by horizontal plates held at the same constant temperature and convection reduces the fraction of the total dimensionless heat input per unit volume and time escaping the layer through the bottom boundary. We prove that this fraction decreases no faster than O(R−2), where R is a “flux” Rayleigh number quantifying the strength of the internal heating relative to diffusion. The second model, instead, has a perfectly insulating bottom boundary, so all heat must escape through the top one. In this case, we prove that the Nusselt number, defined as the ratio of the total-to-conductive vertical heat flux, grows no faster than O(R4). These power-law bounds improve on exponential results available for fluids with finite Prandtl number. The proof combines the background method with a minimum principle for the fluid’s temperature and with Hardy–Rellich inequalities to exploit the link between the vertical velocity and temperature available at infinite Prandtl number.

Convective flows driven by internal sources of heat have attracted renewed interest in recent years.1–6 Such flows are commonly encountered in geophysics, where atmospheric convection7 and mantle convection8,9 are typical examples. They also exhibit unique features not seen in boundary-driven Rayleigh–Bénard convection: for instance, it has recently been observed experimentally that internally heated (IH) convection can transport heat more efficiently than Rayleigh–Bénard convection.10,11 Nevertheless, the former remains much less studied.

Even for simple configurations, such as a uniformly heated fluid layer between parallel horizontal plates, it is a largely open challenge to rigorously predict the mean (i.e., space- and time-averaged) vertical heat flux or other related quantities that measure how much convection can enhance or hinder the transport of heat through the fluid. In particular, one would like to determine how such quantities depend on the heating strength and on the fluid’s Prandtl number Pr, defined as the ratio between the fluid’s kinematic viscosity ν and its thermal diffusivity κ.

One source of difficulty when trying to answer these questions is that the mean thermal dissipation, the mean viscous dissipation, and the mean vertical convective heat flux cannot all be related to each other via a priori relationships. This is in contrast with Rayleigh–Bénard convection, where such relationships enable one to rigorously bound the convective heat transfer through variational analysis of the mean thermal dissipation.12 Applying the same strategy to IH flows yields bounds on the mean temperature of the fluid13–16 but not the convective heat flux.

This variational strategy was recently extended by taking into account a minimum principle for the temperature, leading to bounds on the mean convective heat flux that vary exponentially with the heating rate.2,5 This exponential dependence does not match numerical simulations,15,17,18 so one wonders if it is optimal. Here, we show that it is not for fluids with infinite Prandtl number. In particular, we derive bounds that vary as algebraic powers of the heating rate.

Before stating our results precisely, we must introduce the mathematical model of IH convection we study. We consider a horizontally periodic layer of incompressible fluid with constant density ρ and specific heat capacity cp, whose motion is governed by the Boussinesq equations at infinite Prandtl number.14 The fluid is confined between two horizontal plates at a distance d from each other and is heated at a constant rate Q per unit volume. We immediately make the problem non-dimensional by taking d as the characteristic length scale, d2/κ as the time scale, and d2Q/κρcp as the temperature scale. With these choices, the fluid occupies the horizontally periodic domain Ω=T[0,Lx]×T[0,Ly]×[0,1] and satisfies

(1a)
(1b)
(1c)

where u = (u, v, w) is the fluid’s velocity in cartesian components, p is the pressure, and T is the temperature. The unit forcing in (1c) represents the non-dimensional internal heating rate. The flow is controlled by a “flux” Rayleigh number that measures the destabilizing effect of heating compared to the stabilizing effects of diffusion,

(2)

Here, g is the acceleration of gravity, α is the thermal expansion coefficient of the fluid, and all other quantities have been defined above. We will use overbars to denote infinite-time averages, angled brackets to indicate volume averages, and angled brackets with a subscript h for averages over only the horizontal directions,

(3a)
(3b)
(3c)

Having introduced the basic set of equations governing IH convection at infinite Pr, we now turn to identifying space- and time-averaged quantities that measure the enhancement in vertical heat transport due to convection. Contrary to the case of Rayleigh–Bénard convection, which quantity is used depends on the boundary conditions for the top (z = 1) and bottom (z = 0) of the fluid layer. In this work, we consider the two different cases sketched in Fig. 1, which we described in detail below alongside our main results. Following the nomenclature introduced in previous work,15 we refer to the two cases as the IH1 and IH3 configurations.

FIG. 1.

IH convection with (a) isothermal boundaries (4) and (b) insulating lower boundary (8). In both panels, IH represents the uniform unit internal heat generation. Red dashed lines (---) indicate the conductive temperature profiles. Red solid lines (—) are cartoons illustrating turbulent mean temperature profiles.

FIG. 1.

IH convection with (a) isothermal boundaries (4) and (b) insulating lower boundary (8). In both panels, IH represents the uniform unit internal heat generation. Red dashed lines (---) indicate the conductive temperature profiles. Red solid lines (—) are cartoons illustrating turbulent mean temperature profiles.

Close modal

In the IH1 configuration of Fig. 1(a), the velocity satisfies no-slip conditions and the temperature of both boundaries is held at a constant value, which can be taken as zero without loss of generality. Hence, we enforce

(4)

In this case, the enhancement in vertical heat transport can be quantified through the reduction in the fraction of heat, which leaves the domain through the bottom boundary in a statistically stationary regime. Indeed, let

(5a)
(5b)

be the nondimensional mean heat fluxes through the top and bottom boundaries. Averaging z (1c) over space and time shows that FT and FB are related to the mean vertical convective heat flux, wT̄, via

(6a)
(6b)

When the fluid does not move, so wT̄=0, all heat added to the fluid is transported to the boundaries by conduction in a perfectly symmetric way, giving FT=FB=12. Convection breaks this symmetry, causing more heat to escape through the top boundary. In fact, one can prove that 0wT̄12 uniformly in R and Pr.17 While the zero lower bound is saturated by the (possibly unstable) no-flow state, saturating the upper bound of 12 would require a flow that transports heat upward so efficiently that all heat escapes the domain through the top boundary. Our first main result, however, implies that such a flow does not exist.

Theorem 1
(isothermal boundaries, Pr = ∞).Letu = (u, v, w) andTsolve(1)subject to the no-slip isothermal boundary conditions(4). There exist constantsc, R0 > 0 such that
(7)

Using (6), one immediately obtains Rayleigh-dependent bounds on FT and FB.

Corollary 1.1.

Under the same assumptions as Theorem 1,FT1cR2andFBcR2for allR > R0.

The Proof of Theorem 1, presented in Sec. II D, actually provides the explicit constants c = 216 and R0 = 1892. Our bounds therefore apply to the entire regime where convection is observed, since the conductive state is globally attractive only for R ≤ 269 26.6.15 The stated values of c and R0, however, are suboptimal in the sense that one could increase the value of c at the expense of increasing R0. In particular, one could optimize various constants in our proofs to increase c and R0 until R0 = 26 926.6, so our bounds apply only to the convective regime.

For the IH3 configuration in Fig. 1(b), the velocity satisfies no-slip conditions, the top boundary is held at a constant zero temperature, and the bottom boundary is a perfect thermal insulator. This gives

(8)

Since no heat can escape through the bottom boundary, the enhancement of heat transport due to convection can no longer be quantified by looking at the boundary fluxes FT and FB. Indeed, one has FT=1 and FB=0 at all values of R because no heat can leave the fluid layer through the bottom boundary. Instead, one can define a more classical Nusselt number Nu as the ratio of the space- and time-averaged total heat flux to the conductive heat flux. Since the latter is equal to the mean temperature difference δT̄h=T|z=0̄hT|z=1̄h between the boundaries, one obtains

(9)

This can be rewritten in terms of wT̄ alone as

(10)

using the identity T|z=0̄hT|z=1̄h=12wT̄, which is obtained upon averaging (1 − z)⋅(1c) over space and infinite time.

The uniform bounds 0wT̄12 from Ref. 19 hold also for the IH3 case and guarantee that Nu ≥ 1. However, they do not rule out the possibility that Nu becomes infinite at a finite value of R. The second main result of this work confirms that this somewhat non-physical situation is indeed impossible because wT̄ is always smaller than 12 by an O(R−4) quantity.

Theorem 2
(insulating bottom and isothermal top, Pr = ∞).Letu = (u, v, w) andTsolve(1)subject to the boundary conditions(8). There exist constantsc, R0 > 0 such that
(11)

We immediately conclude from (10) that Nu is finite at every finite value of R and cannot increase faster than O(R4).

Corollary 2.1.

Under the same assumptions as Theorem 2,NucR4for allR > R0.

The Proof of Theorem 2, given in Sec. III D, provides the explicit but suboptimal constants c ≈ 0.0107 and R0 = 2961. Since a state of no flow is stable only when R ≤ 1429.86,19 our bounds therefore apply to every value of R at which convection can occur. As in the IH1 configuration discussed previously, the values of c and R0 could be optimized if desired.

Let us conclude this Introduction with some general remarks about the proofs of Theorems 1 and 2. The first key ingredient in these proofs is a variational problem giving an upper bound on wT̄. This variational problem is derived by enforcing a minimum principle for the fluid’s temperature within the classical “background method,”12,20,21 which for simplicity we formulate using the language of a more general framework for bounding infinite-time averages22–25 (the link between the two approaches has recently seen detailed discussed23,26). Using this minimum principle is essential to obtain bounds on wT̄ that asymptote to 12 from below. This has already been shown for the IH1 configuration at finite Pr: for this case, without the minimum principle, one obtains only wT̄R1/5,2 while with it one can prove that wT̄12O(R1/5exp(R3/5)) uniformly in Pr.5 A similar (but not identical) exponentially varying bound of wT̄12O(R1/5exp(R3/5)) uniformly in Pr was also obtained for the IH3 configuration.5 

The second key ingredient in our proofs are estimates of Hardy–Rellich type, obtained by observing that the reduced momentum equation (1b) determines the vertical velocity field as a function of the temperature field. Specifically, taking the vertical component of the double curl of (1b) gives

(12)

where Δhx2+y2 is the horizontal Laplacian. Using the no-slip boundary conditions with the incompressibility condition (1a), the vertical velocity w satisfies

(13)

Equation (12) was exploited in Rayleigh–Bénard convection to improve the scaling of upper bounds on Nu.27 This was achieved by using (12) to derive inequalities of the Hardy–Rellich type (see Lemma 4) that help the construction of a background field with a logarithmically varying stable stratification in the bulk.27,28 Here, we use the same inequalities to construct (different) background fields suited to IH convection, which will enable us to bound wT̄ in the infinite Pr limit.

The rest of this paper is structured as follows: Sec. II details the Proof of Theorem 1, while Theorem 2 is proven in Sec. III. Some technical steps of the proof are relegated to the  Appendixes A and  B to streamline the argument. Further discussion and perspective for possible future work are offered in Sec. IV.

We first consider the IH1 configuration, where the top and bottom plates are held at zero temperature. In Sec. II A, we show that wT̄ can be bounded from above by constructing suitably constrained functions of the vertical coordinate z. Section II B describes parametric Ansätze for such functions, while Sec. II C establishes auxiliary results that simplify the verification of the constraints and the evaluation of the bound. We then prove Theorem 1 in Sec. II D by prescribing R-dependent values of the free parameters in our Ansätze.

To simplify the notation, we introduce two sets of temperature fields that encode the thermal boundary conditions and the pointwise nonnegativity constraint implied by the minimum principle,

(14a)
(14b)

where n = 1 or 3, depending on the boundary conditions of IH1 and IH3 respectively. In Sec. II, T belongs to H1.

To bound wT̄, we employ the auxiliary function method.22,26 The method relies on the observation that the time derivative of any bounded functional V{T(t)} along solutions of the Boussinesq equations (1) averages to zero over infinite time, so

(15)

If V is chosen such that the quantity being averaged on the right-hand side is bounded above pointwise in time, then this pointwise bound is also an upper bound on wT̄.

Following analysis at finite Prandtl number,2 we restrict our attention to quadratic functionals taking the form

(16)

which are parameterized by a positive constant βR+ and a piecewise-differentiable function τ:[0,1]R with the square-integrable derivative. We require τ to satisfy

(17)

so the coefficient multiplying T in (16) vanishes at z = 0 and z = 1. This choice enables us to integrate by parts without picking up boundary terms when calculating ddtV{T(t)}. To ensure that the resulting expression wT+ddtV{T} can be bounded from above pointwise in time, we also require that the pair (β, τ) satisfies a condition called the spectralconstraint.

Definition 1
(spectral constraint). The pair (β, τ) is said to satisfy the spectral constraint if
(18)
where w = −RΔ−2ΔhT solves (12) with the boundary conditions (13).

If the spectral constraint is satisfied, then it is possible to bound wT̄ from above in terms of τ, β, and another suitably constrained function λ:[0,1]R.

Proposition 1
(bounding framework, IH1).Suppose that the pair (β, τ) satisfies the spectral constraint and the boundary conditions in(17). Furthermore, letλL2(0, 1) be a nondecreasing function such thatλ=1. Then,

Proof.
A standard calculation using integration by parts, the incompressibility condition (1a), and the boundary conditions on u and T yields
(19)
The infinite-time average on the right-hand side is bounded above by the largest value of the argument over the global attractor of the infinite-Prandtl-number Boussinesq equations (1). The minimum principle for the temperature field implies that the global attractor is contained in the set H+ defined in (14b). Consequently, we can estimate
(20)
This upper bound is finite if and only if unless the pair (β, τ) satisfies the spectral constraint (cf. Definition 1), in which case the supremum over T can be evaluated using a technical convex duality argument detailed in  Appendix A. The result of the argument is that the bound in (20) is equivalent to
(21)

This inequality clearly implies the upper bound on wT̄ stated in the proposition, which is therefore proven.□

Remark 1.

The function λ that arises when deriving (21) from (20) can be viewed as a Lagrange multiplier enforcing the pointwise non-negativity of temperature fields in the set H+. Further details regarding this interpretation (with slightly different notation) are given in previous work (Ref. 2, Sec. 4 4).

Remark 2.

The best upper bound on wT̄ provable with our approach is found upon minimizing the expression U(τ, λ, β) over all choices of τ, λ, and β that satisfy the conditions of Proposition 1. This is hard to do analytically but can be done computationally using a variety of numerical schemes.26 We leave such computations to future work and focus on proving Theorem 1 by constructing suboptimal τ, λ, and β analytically.

To prove the upper bound on wT̄, we seek β > 0, τ(z), and λ(z) that satisfy the conditions of Proposition 1 and make the quantity U(β, τ, λ) as small as possible. To simplify this task, we restrict τ to take the form

(22)

and λ to be given by

(23)

These piecewise-defined functions, sketched in Fig. 2, are fully specified by the bottom boundary layer width δ(0,12), the top boundary layer width ε(0,12), and the parameter A > 0 that determines the amplitude of τ in the bulk of the layer.

FIG. 2.

Sketches of the functions τ(z) in (22) and λ(z) in (23) used to prove Theorem 1.

FIG. 2.

Sketches of the functions τ(z) in (22) and λ(z) in (23) used to prove Theorem 1.

Close modal

We also fix

(24)

This choice is motivated by the desire to minimize the right-hand side of the inequality

(25)

which is used later in Lemma 2 by estimating from above the value of the bound U(β, τ, λ) for our choices of τ and λ.

For any choice of the parameters δ, ɛ, and A, the function τ satisfies the boundary conditions in (17), while λ is nondecreasing and satisfies the normalization condition λ=1. To establish Theorem 1 using Proposition 1, we only need to specify parameter values such that U(β,τ,λ)12O(R2) while ensuring that the pair (β, τ) satisfies the spectral constraint. For the purposes of simplifying the algebra in what follows, we shall fix

(26)

from the outset. As explained in Remark 5, this choice arises when insisting that the upper estimate on U(β, τ, λ) derived in Lemma 2 be strictly less than 12 for some values of δ and ɛ, at least when all other constraints on these parameters are ignored.

We now derive a series of auxiliary results that make it simpler to specify the boundary layer widths δ and ɛ. The first result gives estimates on the value of β in (24).

Lemma 1
(estimates on β). Letτ(z),λ(z), andβbe given by(22),(23), and(24), respectively, withAspecified by(26). Suppose that the boundary layer widthsδandɛsatisfy
(27a)
(27b)
(27c)
Then,
(28)

Remark 3.

Condition (27c) is key to prove the auxiliary results of this section. The other two restrictions, instead, are introduced to more easily keep track of constants in our estimates, which is necessary to obtain an explicit prefactor for the O(R−2) term. We have not attempted to optimize this prefactor.

Remark 4.

Condition (27c) implies that δɛ. We will use this fact often in the proofs of this section.

Proof of Lemma 1.
It suffices to estimate |τλ|212 from above and below. For a lower bound, substitute our choices for τ and λ to estimate
Expanding the square, dropping the non-negative term 2z(1z), and recalling that ε13 and δ16<13 by assumption, we can further estimate
(29)
Taking the square root of both sides and substituting for the value of A from (26) gives |τλ|21/2(315/20)δ, which combined with (24) proves the lower bound on β stated in (28).
For the upper bound on β, recall that condition (27c) implies δɛ, so 1 − ɛ ≤ 1 − δ ≤ 1. Then,
Using the inequality (a + b)2 ≤ 2a2 + 2b2, we can further estimate
Finally, we observe that 12δ1δ1 for all δ ≥ 0 and apply (27c) to arrive at
(30)
Substituting our choice of A from (26) and taking a square root gives |τλ|21/2(33/4)δ, which combined with (24) yields the upper bound on β in (28).□

Our second auxiliary result estimates the upper bound U(β, τ, λ) on wT̄ from Proposition 1 in terms of the bottom boundary layer width δ alone.

Lemma 2
(estimates on U(β, τ, λ)). Letτ(z),λ(z), andβbe given by(22),(23), and(24), respectively, withAspecified by(26). Suppose the boundary layer widthsδandɛsatisfy the conditions of Lemma 1. Then,
(31)

Proof.
Using inequality (25), our choice of β from (24), and the upper bound on ⟨|τ′ − λ|2⟩ from (30) yields
Moreover, since we have chosen τ to be a non-negative function, we can estimate τ=01τ(z)dz0δτ(z)dz=12δ to obtain
(32)
Substituting our choice of A from (26) into this inequality gives (31).□

Remark 5.

The right-hand side of (32) can be strictly smaller than 12 only if Aδ3/2. It is this observation that dictates the choice of A in (26). For any fixed value of R, one should choose Aδ3/2 with a (possibly R-dependent) prefactor that optimizes the balance between the positive and negative terms, subject to constraints on A, δ, and all other parameters that ensure the spectral constraint. To simplify our proof, however, we choose to fix this prefactor a priori irrespective of R.

Our final auxiliary result gives sufficient conditions on δ and ɛ that ensure the spectral constraint (cf. Definition 1) is satisfied.

Lemma 3
(sufficient conditions for the spectral constraint).Letτ(z),λ(z), andβbe given by(22),(23), and(24), respectively, withAspecified by(26). Suppose the boundary layer widthsδandɛsatisfy the conditions of Lemma 1. Suppose further that
(33a)
and
(33b)

Then, the pair (β, τ) satisfies the spectralconstraint.

The proof of this result relies on Hardy–Rellich inequalities established in Ref. 14, which extract a positive term from the a priori indefinite term ⟨τwT⟩.

Lemma 4
(Hardy–Rellich inequalities14).LetT,w:ΩRbe horizontally periodic functions such that Δ2w = −RΔhTsubject to velocity boundary conditions(13). Then,
(34a)
and
(34b)

Proof of Lemma 3.
Let 1(a,b) denote the indicator function of the interval (a, b). Define the functions
(35a)
(35b)
Given our choice of τ from (22), we can rewrite the spectral constraint as
where
(36a)
(36b)

Here, w is determined as a function of T by solving (12) subject to the boundary conditions in (13). We shall prove that F and G are individually non-negative.

First, let us consider F. The Hardy–Rellich inequality (34a) gives
(37)
Next, we estimate ⟨f(z)wT⟩. Since T vanishes at z = 0 by virtue of the thermal boundary conditions in (4), we can use the fundamental theorem of calculus and the Cauchy–Schwarz inequality to estimate |T(,z)|z(01|T|2dz)1/2. Squaring both sides and taking the horizontal average of which give T2hz|T|2. Then, the use of the Cauchy–Schwarz inequality, substitution for T2h, and Young’s inequality gives
Upon using the lower bound on β from (28) to estimate the last term from above, we obtain
(38)
This can be substituted into (37) along with our choice of A from (26) to find
(39)
To conclude, we show that the term in parentheses is non-negative when δ satisfies δ16 and (33a). To do this, we observe that the function f(z) in (35a) is non-negative function and that it is nonzero only if zδ. We can therefore bound it from above on the interval (0, δ) using the estimates 11z11δ65 and, consequently, obtain
Using the assumption that δ16 to estimate the expression in parentheses by its value at δ=16, followed by an application of assumption (33a) to estimate the remaining δ1/2 term in terms of R, we arrive at the desired inequality
Analogous arguments show that G{T} is non-negative. Using the Hardy–Rellich inequality (34b)
(40)
To estimate the last term, we use (in order) the inequality T2h(1z)|T|2, the Cauchy–Schwarz inequality, and Young’s inequality,
Using the lower bound on β from (28) gives
(41)
which can be substituted into (40) along with the value of A from (26) to obtain
(42)
To conclude the argument, we show that the term in parentheses is non-negative. To demonstrate this, we first estimate g(z) on the interval (1 − ɛ, 1) from above using the assumption that ε13, so 23z1 and 1z(1z)32(1z). Thus,
Then, we use the assumptions δ16 and δɛ (cf. Remark 4) to observe that ln(1εδ)ln(1δ2)ln2(1δ2) and 3434ln2(1δ2). Combining these estimates with the upper bound on g derived above gives
as desired. This concludes the Proof of Lemma 3.□

It is now straightforward to prove the upper bound on wT̄ by specifying boundary layer widths δ and ɛ that satisfy the conditions of Lemmas 1, 2, and 3.

Since the estimate for the resulting upper bound obtained in Lemma 2 is minimized when δ is as large as possible, we choose the largest value consistent with (33a),

(43)

With this choice of δ, conditions (27c) and (33b) require ɛ to satisfy

(44)

which is possible for R > R0 ≃ 1891.35 (cf. Fig. 3). For R > R0, any choice of ɛ in this range is feasible. The optimal value could be determined at the expense of more complicated algebra either by optimizing the full bound U(β, τ, λ) or by deriving better ɛ-dependent estimates for it. However, we expect that any ɛ-dependent terms will contribute only higher-order corrections to our bound on wT̄.

FIG. 3.

Variation with R of the allowed values for the bottom boundary layer width ɛ (shaded region), determined by condition (27c) in Lemma 1 and condition (33b) in Lemma 3 when the bottom boundary layer width δ (blue solid lines) is chosen as in (43). Also shown are the uniform upper bounds δ16 (blue dashed lines) and ε13 (red dashed lines) imposed on these variables. A black vertical line marks the Rayleigh number R0 ≃ 1891.35 above which all constraints on δ and ɛ are satisfied.

FIG. 3.

Variation with R of the allowed values for the bottom boundary layer width ɛ (shaded region), determined by condition (27c) in Lemma 1 and condition (33b) in Lemma 3 when the bottom boundary layer width δ (blue solid lines) is chosen as in (43). Also shown are the uniform upper bounds δ16 (blue dashed lines) and ε13 (red dashed lines) imposed on these variables. A black vertical line marks the Rayleigh number R0 ≃ 1891.35 above which all constraints on δ and ɛ are satisfied.

Close modal

To conclude the Proof of Theorem 1, there remains to verify that our choice of δ is no larger than 16 and that any ɛ satisfying (44) is no larger than 13. It is easily checked that both conditions hold when RR0 (see Fig. 3 for an illustration). For all such values of R, therefore, Lemma 2 and our choice of δ yield the upper bound wT̄U(β,τ,λ)12cR2 with c = 216.

We now move on to studying IH convection in the IH3 configuration, where the top boundary is maintained at constant (zero) temperature and the bottom boundary is insulating. First, in Sec. III A, we derive a bounding framework for wT̄ following steps similar to those used for the IH1 case (cf. Sec. II A). In Sec. III B, we present Ansätze for τ and λ, with which we obtain crucial estimates in Sec. III C, which give the bound in Sec. III D. Throughout this section, T belongs to H3. Observe that this changes the set of temperature fields over which the spectral constraint in Definition 1 is imposed. The notation H+ still denotes the subset of temperature fields in H3 that are non-negative pointwise almost everywhere.

Upper bounds on wT̄ for the IH3 configuration can be derived using a quadratic auxiliary function V{T} similar to that used for the IH1 case. Precisely, we still take V to be defined as in (16), where the positive constant β and the piecewise-differentiable square-integrable function τ(z) are tunable parameters. However, this time we impose only the boundary condition

(45)

These changes result in the following family of parameterized upper bounds on wT̄:

Proposition 2
(bounding framework, IH3).Suppose that the pair (β, τ) satisfies the spectral constraint (cf. Definition 1) and the boundary condition in(45). Furthermore, letλL2(0, 1) be a nondecreasing function such thatλ(0) = −1. Then,

Proof.
Proceeding as in the Proof of Proposition 1 shows that
(46)
The supremum on the right-hand side can be evaluated using the convex duality argument summarized in  Appendix B, leading to the equivalent inequality
(47)

This clearly implies the upper bound stated in the proposition.□

The procedure for the proof of an upper bound on wT̄ is the same as that employed for isothermal boundaries. We construct β > 0, τ(z), and λ(z) that satisfy the conditions of Proposition 2, while trying to minimize the corresponding bound U(β, τ, λ). Due to the Neumann boundary condition on T at z = 0, we can no longer employ the Poincaré estimates used in Sec. II C to control the sign-indefinite term in the spectral constraint at the bottom boundary. Instead, we modify τ(z) in (δ, 1 − ɛ) to increase slower than logarithmically in z and use results established in previous work on Rayleigh–Bénard convection.28 The function τ(z) is hence chosen to have the form

(48)

where

(49)

On the other hand, the Lagrange multiplier λ(z) is still chosen to be

(50)

These piecewise functions, sketched in Fig. 4, are fully specified by the bottom and top boundary layer widths δ,ε(0,12), the constant A > 0, and the exponent α ∈ (0, 1) driving the behavior of τ(z) in the bulk.

FIG. 4.

Sketch of the functions τ(z) (48) and λ(z) in (50) used to prove Theorem 2.

FIG. 4.

Sketch of the functions τ(z) (48) and λ(z) in (50) used to prove Theorem 2.

Close modal

For β, we take

(51)

This choice is motivated by minimizing the right-hand side of the estimate,

(52)

which is used in Lemma 6 to estimate the value of the bound U(β, τ, λ) from above when τ and λ are define by (48) and (50), respectively.

For any choice of the parameters δ, ɛ, A, and α, the function τ satisfies the boundary conditions in (45), while λ is nondecreasing and satisfies the condition λ(0) = −1. Thus, to establish Theorem 2 using Proposition 2, we need only specific parameter values such that U(β,τ,λ)12O(R4) while ensuring that (β, τ) satisfy the spectral constraint. For the purposes of simplifying the algebra in what follows, we shall fix

(53)

from the outset. This choice arises when insisting that the upper estimate on U(β, τ, λ) derived in Lemma 6 should be strictly less than 12 for suitable choices of δ and ɛ, at least when all other constraints on these parameters are ignored.

We now derive auxiliary results that simplify the choice of the exponent α and of the boundary widths δ and ɛ. The first gives estimates on the value of β in (51).

Lemma 5
(estimates on β). Letτ(z),λ(z), andβbe given by(48),(50), and(51)withAspecified in(53). Suppose thatα(12,1)and the boundary layer widthsδandɛsatisfy
(54a)
(54b)
(54c)
Then,
(55)

Remark 6.

Condition (54a) and the bounds on α imposed in the Lemma imply that 0δ16. These uniform bounds will be used repeatedly in the following proofs:

Proof of Lemma 5.
It suffices to estimate |τλ|212 from above and below. For a lower bound, we can substitute our choices of τ and λ and then estimate
Dropping the positive term 1/(1 − z) from the integrand and integrating the rest gives
For every α(12,1), the second term inside the parentheses can be estimated upon observing that constraints (54a) and (54b) imply
(56)
Thus, we obtain
(57)
Taking the square root of (57) and using (53) gives |τλ|21269δ2, which combined with (51) proves the lower bound on β stated in (55).
To prove the upper bound on β, we start by using the inequality (a + b)2 ≤ 2a2 + 2b2, evaluating exactly the integral of τ′ − λ, and dropping the negative terms to get
(58)
Using assumption (54c), the second and final term in (58) can be estimated from above to arrive at
(59)
Next, we observe that for all ε(0,13), δ(0,16), and α(12,1), we can estimate
so B−2 ≤ 1/2. Using this estimate in (59), taking a square root, and substituting in the value of A given in (53) leads to the inequality |τλ|21/2(43/9)δ2. Combining this with (51) yields the upper bound on β stated in (55) and concludes the Proof of Lemma 5.□

The second auxiliary result of this section estimates the upper bound U(β, τ, λ) on wT̄ given by Proposition 2 using only the bottom boundary layer width δ.

Lemma 6
(estimates on U(β, τ, λ)).Letτ(z),λ(z), andβbe specified by(48),(50), and(51), respectively, withAgiven by(53). Supposeαand the boundary layer widthsδ,ɛsatisfy the conditions of Lemma 5. Then,
(60)

Proof.
Inequality (52) and the upper bound on β from (55) give
(61)
The result follows upon observing that τ is non-negative, so τ=01τ(z)dz0δτ(z)dz=12δ2.□

Remark 7.

The right-hand side of (61) can be strictly smaller than 12 when δ2 is small only if Aδα+3/2. This observation dictates the choice of A in (53). For any fixed value of R, one should choose Aδα+3/2 with a (possibly R-dependent) prefactor that optimizes the balance between the positive and negative terms, subject to constraints on A, δ, and all other parameters that ensure the spectral constraint. To simplify our proof, however, we choose to fix this prefactor a priori irrespective of R.

Our final auxiliary result gives the sufficient conditions on δ and ɛ that ensure that the spectral constraint (cf. Definition 1) is satisfied.

Lemma 7
(sufficient conditions for spectral constraint).Letτ(z),λ(z), andβbe specified by(48),(50), and(51), respectively, withAgiven by(53). Suppose thatαand the boundary layer widths satisfy the conditions of Lemma 5. Furthermore, let
(62)
and suppose that
(63a)
(63b)
(63c)

Then, the pair (β, τ) satisfies the spectralconstraint.

Unlike the analogous result obtained in Sec. II C, Lemma 7 cannot be proven using only the Hardy–Rellich inequalities stated in Lemma 4. The lack of a fixed boundary temperature at z = 0 makes it impossible to gain sufficient control on the contribution of the bottom boundary layer to the quadratic form in (18). This difficulty can be overcome using the following result, obtained as a particular case of a more general analysis by Whitehead and Wittenberg28 [Eqs. (59) and (77)], which upon setting (in their notation) ν1=α2ν2 and ν2=121+2(1α2).

Lemma 8
(adapted from Ref. 28).Fixα(12,1)andμ, R > 0. Supposeφ(z):[0,1]Rbe a non-negative function, satisfying
(64)
Then, for everywandTsolving (12) subject to the boundary conditions (13),
(65)

We are now ready to prove Lemma 7.

Proof of Lemma 7.
Let 1(a,b) denote the indicator function of the interval (a, b) and define the functions
(66a)
(66b)
Given our choice of τ, we can rewrite the spectral constraint as
where
(67a)
(67b)

Observe that F{T} and G{T} are functionals of the temperature field only because w is determined as a function of T by solving (12) subject to the boundary conditions in (13). We shall prove that F{T} and G{T} are individually non-negative for all temperatures T from the space H3, which is sufficient for the spectral constraint to hold.

To prove that F{T}0, we apply Lemma 8 with φ(z) = f(z)/β and μ = A/β, where f is given by (66a) and A given by (53). We therefore need to check that
(68)
To verify this inequality, we first bound from above the weighted integral on the left-hand side. By assumption, we have 0zδ16 and α(12,1), from which we obtain 11z1zα. Using this estimate and the definition of A from (53), we can therefore estimate
Using again that 0δ16 and α(12,1), the bracketed expression can be bounded from above to obtain
(69)
Next, we bound from below the right-hand-side of (68). Using the lower bound on β from Lemma 5, the definition (53) of A, and the fact that α(12,1), we have
(70)
Combining (69) and (70), we conclude that (68) holds if
which is true because δ satisfies (63a) by assumption. This proves that F{T}0, as desired.
We now prove that G{T} is also non-negative. This can be done following the same steps used in Sec. II C. The Hardy–Rellich inequality (34b) gives
(71)
To estimate the last term, as before, we use the inequality T2h(1z)|T|2, the Cauchy–Schwarz inequality, and Young’s inequality,
Using the lower bound on β from (55) gives
which can be substituted into (71) along with the value of A from (53) to obtain
(72)
To conclude the argument, we need to show that the term in the parentheses is non-negative. To demonstrate this, we first estimate from above the function g(z) given in (66b) on the interval (1 − ɛ, 1). Our assumption that δɛ implies that 1 − ɛ ≤ 1 − δ ≤ 1 and ln(1ε)ln(1δ). Thus, for all δ16 and α(12,1), the first term in g(z) can be bounded as
(73)
To estimate the other terms in g(z), we observe that the assumptions ε13 and α(12,1) imply that 1zα12(1α)(1z) and 11z12(1α)(1z). Consequently, we arrive at
(74)
Finally, using (74) and evaluating the integral in the parentheses of (72) with the fact that ln(1δ)ln2(1δ) and 1313ln(1δ) give
(75)
This concludes the Proof of Lemma 7.□

To prove Theorem 2, we only need to specify R-dependent values for α and for the boundary layer widths δ and ɛ that satisfy the conditions of Lemmas 5, 6, and 7.

Motivated by the desire to minimize the upper bound on U(β, τ, λ) stated in Lemma 6, we choose

(76)

where α*=(1+13)/6 is the unique maximizer of h(α) on the interval (12,1) [see Fig. 5(b)]. With these choices, conditions (54c) and (63b) require ɛ to satisfy

(77)

where c0, c1, and c2 are non-negative constants independent of R. Using the upper bound on B from (73), it suffices to find ɛ such that

(78)

Figure 5 shows that suitable values of ɛ exist when RR0 ≈ 2960.89. One can also check that for all such values of R and any ɛ in the range given by (78), one has δ16, ε13, and δɛ. We have therefore verified all conditions of Lemmas 5, 6, and 7.

FIG. 5.

(a) Variation with R of the allowed values for the bottom boundary layer width δ (76) (blue solid line) and the feasible region of ɛ (78) (shaded region). Also shown are uniform upper bounds of δ16 (blue dashed line) and ε13 (red dashed line) imposed on the variables. A black vertical line marks the Rayleigh number, R0 ≈ 2960.89, above which all constraints are satisfied. (b) Plot of the function h(α) (62) (blue solid line). Shown also is the optimal α*=(1+13)/6 (blue dashed line).

FIG. 5.

(a) Variation with R of the allowed values for the bottom boundary layer width δ (76) (blue solid line) and the feasible region of ɛ (78) (shaded region). Also shown are uniform upper bounds of δ16 (blue dashed line) and ε13 (red dashed line) imposed on the variables. A black vertical line marks the Rayleigh number, R0 ≈ 2960.89, above which all constraints are satisfied. (b) Plot of the function h(α) (62) (blue solid line). Shown also is the optimal α*=(1+13)/6 (blue dashed line).

Close modal

To conclude the Proof of Theorem 2, we simply substitute our choice of δ from (76) into Lemma 6 to find the upper bound wT̄U(β,τ,λ)12cR4, where c=h2(α*)180.0107.

Remark 8.

The top boundary layer width ɛ is not uniquely determined in our construction. Its optimal value could be obtained by considering more refined estimates on U(β, τ, λ) than Lemma 6, but we expect such estimates to provide only higher-order corrections to the eventual bound on wT̄.

We have proven bounds on the enhancement of heat transport by convection for two configurations of infinite-Prandtl-number convection driven by internal heating between no-slip boundaries. In the first case, where both boundaries are held at a constant temperature, we find wT̄12O(R2) for all sufficiently large R (cf. Theorem 1). This result implies that the outward heat fluxes through the top and bottom are bounded by FT1O(R2) and FBO(R2), respectively. In the second configuration, where the top boundary remains isothermal but the bottom one is insulating (no-flux condition), we find wT̄12O(R4) (cf. Theorem 2). In this case, we conclude from (10) that the Nusselt number is bounded above by NuO(R4). Explicit suboptimal values for the prefactors in the Rayleigh-dependent terms were also obtained (cf. Secs. II D and III D).

All of these results were derived using the background method, which we formulated as a search over quadratic auxiliary functionals of the form (16) and augmented using a minimum principle for the fluid’s temperature. Similar to previous works on infinite-Prandtl-number Rayleigh–Bénard convection, the background temperature fields used vary linearly in thin boundary layers and increase either logarithmically (IH1 configuration) or as a power law (IH3 configuration) in the bulk of the fluid layer. This bulk behavior enables us to use Hardy–Rellich inequalities14 (Lemma 4) and a previously established integral estimate28 (Lemma 8) that were originally developed in the context of Rayleigh–Bénard convection. In contrast to the latter, however, our background fields lack symmetry in the vertical direction, which reflects the lack of vertical symmetry of IH convection problems.

In our choice of background fields, allowing the bottom boundary layer width δ to be smaller than the top boundary layer width ɛ is essential to prove Theorems 1 and 2. For the IH1 configuration, forcing δ = ɛ worsens the R-dependent correction to 12 in Theorem 1 to O(R−2 ln−2(R)). For the IH3 configuration, instead, no upper bound on wT̄ that asymptotes to 12 from below as R increases can be obtained with our method of proof if δ = ɛ. This boundary layer asymmetry contrasts the construction of background fields for IH convection at finite Pr,5 where taking δɛ appears to bring no qualitative improvement to the exponentially varying upper bounds on wT̄. We also stress that the a priori uniform limits on the allowed values of δ and ɛ imposed throughout Secs. II and III have been chosen with the only goal of simplifying the algebra in our proofs. Varying these limits affects the prefactors of the R-dependent terms in Theorems 1 and 2, as well as the range of R values for which they hold. Both could be optimized further if desired.

One crucial difference between our constructions for the IH1 and IH3 configurations is the leading-order behavior of the background temperature fields—or, more precisely, of the function τ(z)—as the bottom boundary layer edge is approached from the bulk region. For the IH1 configuration, it suffices for τ to have the same logarithmic behavior as the background temperature fields used to study Rayleigh–Bénard convection.27 For the IH3 configuration, however, this choice does not work due to the loss of control on the temperature of the bottom boundary, and we are instead forced to take τ(z) ∼ z1−α with α ∈ (0, 1). This modification was already used in the context of Rayleigh–Bénard convection between imperfectly conducting boundaries,28 where the optimal exponent α depended logarithmically on the Rayleigh number. Within our proof, instead, the optimal α is a constant. Whether this difference is due to our choice of estimates or the inherent differences between Rayleigh-Bénard and IH convection remains an open question.

More generally, we do not know whether the upper bounds on wT̄ stated in Theorems 1 and 2 are qualitatively sharp. To check if the O(R−2) and O(R−4) corrections to the asymptotic value of 12 are optimal within our bounding framework, one could employ a variation of the computational approach taken in previous studies by the authors2,26 and optimize the tunable parameters τ, β, and λ in full. A more interesting but also more challenging problem is to identify which convective flows maximize wT̄ and the corresponding optimal scaling of this quantity with R. Considerable insight in this direction can be gained through direct numerical simulations, which to the best of our knowledge have only been performed at finite Pr numbers for the IH1 and IH3 models studied here.19,29 These works report values for wT̄ or related quantities, but it is not clear that their functional dependence on R should remain the same at infinite Prandtl number. Other promising approaches could be the calculation of steady but unstable solution of the Boussinesq equations (1), which may transport heat more efficiently than turbulence as recently observed in the context of Rayleigh–Bénard convection30,31 and the explicit design of flows that optimize heat transport.6,32–35 Finally, it would be interesting to investigate if more sophisticated PDE analysis techniques used for Rayleigh–Bénard convection36 can be extended to IH convection to interpolate between the algebraic bounds on wT̄ proved in this paper for infinite-Pr fluids with the finite-Pr exponential bounds.5 

A.A. acknowledges funding by the EPSRC Centre for Doctoral Training in Fluid Dynamics across Scales (Award No. EP/L016230/1). G.F. was supported by an Imperial College Research Fellowship and would like to thank the Isaac Newton Institute for Mathematical Sciences, Cambridge, for support and hospitality during the program “Mathematical aspects of turbulence: where do we stand?” (EPSRC Grant No. EP/L016230/1) where work on this paper was undertaken.

The authors have no conflicts to disclose.

Ali Arslan: Formal analysis (lead); Investigation (lead); Writing – original draft (equal); Writing – review & editing (equal). Giovanni Fantuzzi: Supervision (equal); Writing – original draft (equal); Writing – review & editing (equal). John Craske: Supervision (equal); Writing – original draft (equal); Writing – review & editing (equal). Andrew Wynn: Supervision (equal); Writing – original draft (equal); Writing – review & editing (equal).

The data that support the findings of this study are available from the corresponding author upon reasonable request.

The equivalence between (20) and (21) follow from a relatively standard convex duality argument. It will be enough to show that

(A1)

where

To establish this identity, we start by rewriting the maximization on the left-hand side as a minimization problem for the Legendre transform of Φ. Recall that the Legendre transform of a functional Λ:HR is the functional

which acts on the dual space H* of bounded linear functionals Tμ{T} on H. We shall write H+*H* for the subset of non-negative bounded linear functionals on H, meaning that μH+* if and only if μH* and μ{T} ≥ 0 for all TH+.

Lemma 9.

If the pair (β, τ) satisfies the spectral constraint,supTH+Φ{T}=infμH+*Φ*{μ}.

Proof.
Define a functional Ψ from H into R{+} via
Its Legendre transform is
We claim that
The first, second, and fourth equalities are immediate consequences of the definitions of inf, sup, Ψ, and Ψ*. The third one, instead, follows from the Fenchel–Rockafellar minmax theorem when H is viewed as a Hilbert space with the inner product T1T2 and norm T2. To apply this theorem as stated in Ref. 37 (Theorem 1.12), we need to verify that the functionals Φ and Ψ are convex and that Φ is continuous (with respect to the norm on H) at some T0dom(Φ)dom(Ψ)=H+.
The convexity of Ψ is obvious, while that of Φ follows from the assumption that the pair (β, τ) satisfies the spectral constraint (cf. Definition 1). To see this, write Φ{T}=Q{T,T}(τβz)zT, where Q is the bilinear form
and observe that the spectral constraint ensures Q{T,T}0 for all T in the linear space H. Thus, for any λ ∈ [0, 1], we can set λ̄=1λ and estimate
proving that Φ is convex. The continuity of Φ at any T0H+ follows because Φ is continuous on the whole space H. Indeed, the terms T2 and ⟨(τ′ − βz)zT⟩ in the expression for Φ{T} are clearly continuous on H. To see that the remaining term is also continuous, it is enough to establish that TkT in H implies φk ≔ Δ−2ΔhTk → Δ−2ΔhTφ in H. This can be shown by combining the Poincaré inequalities φ2Δφ2 and T2T2 with the estimate
which implies Δφ2T2. This concludes the Proof of Lemma 9.□

Next, we prove that since Φ{T} is invariant under horizontal translations of the temperature field T, the minimization of its Legendre transform Φ* can be restricted to functionals μH+* that are translation invariant. Specifically, for any real numbers r, s, define the translation map Sr,s:HH and its adjoint Sr,s*:H*H* via

The functional μH* is translation invariant if Sr,s*μ=μ for all r and s.

Lemma 10.
SupposeΦ:HRsatisfiesΦ{Sr,sT}=Φ{T}for allr,sR. Then,

Proof.
It suffices to show that for every νH*, there exists a translation-invariant μH* such that Φ*{μ} = Φ*{ν}. Since every temperature field TH is horizontally periodic, such a μ can be constructed simply by averaging the functionals Sr,s*ν over horizontal translations r and s, i.e., by letting
To show that Φ*{μ} = Φ*{ν}, we establish the complementary inequalities Φ*{μ} ≤ Φ*{ν} and Φ*{μ} ≥ Φ*{ν}. For the first one, use the translation invariance of Φ and the definition of the Legendre transform to estimate
for all TH and all horizontal shifts r,sR. Averaging over horizontal shifts shows that μ{T} − Φ{T} ≤ Φ*{ν} for all TH, which implies Φ*{μ} ≤ Φ*{ν}.
To obtain the reverse inequality, observe that by definition of Φ*, for any ɛ > 0, there exists TεH such that ν{Tɛ} − Φ{Tɛ} ≥ Φ*{ν} − ɛ. Then, since Φ is translation invariant,
Upon averaging this inequality over all horizontal shifts r,sR and applying Jensen’s inequality to Φ*, which is concave because it is the supremum of linear functions, we find
Letting ɛ → 0 yields Φ*{μ} ≥ Φ*{ν}, as desired. Lemma 10 is therefore proved.□

To establish identity (A1), we now need to show that its right-hand side coincides with the infimum of Φ* over translation-invariant functionals μH+*. For this, we use a characterization of such μ established in (Appendix C, Arslan et al. 2021).2 

Lemma 11.

LetH+*be the set of positive linear functionals on the temperature spaceHdefined in(14a). IfμH+*is translation invariant, there exists a nondecreasing functionλL2(0, 1) withλ=1such thatμ{T}=λ(z)zT.

Thanks to this representation, all that remains to do is to calculate

(A2)

To solve this maximization problem, let η(z) = ⟨Th(z) be the horizontal mean of T and set ξ = Tη. Since Δhη = 0 and ⟨ξh(z) = 0 by construction, we can therefore substitute T = η + ξ in (A2) and solve the equivalent problem

(A3)

The boundary conditions on η and ξ follow from those on T. The three terms on the second line vanish identically because ⟨ξh(z) = 0 at all z ∈ [0, 1]. To verify this claim, observe that

for any function f(z) that depends only on the vertical direction. Similarly, one can show that

because the function w = −RΔ−2ΔhT = −RΔ−2Δhξ also has zero horizontal mean. Indeed, taking the horizontal average of (12) yields the ODE wh(z)=0, whose only solution satisfying the boundary conditions in (13) is ⟨wh(z) = 0. The minimization in (A3) therefore simplifies into

(A4)

Since the pair (β, τ) was assumed to satisfy the spectral constraint (cf. Definition 1), the choice ξ = 0 is optimal. The optimal η, instead, satisfies the Euler–Lagrange equation 2βη″ = (τ′ − λβz)′. Solving this equation using the boundary conditions, the constraints τ(0) = 1 and τ(1) = 0, and the normalization ⟨λ⟩ = −1 gives η=12b[τλb(z12)], which can be substituted back into (A4) to give

(A5)

Minimizing the left-hand side over translation invariant μ in H+* is the same as minimizing the right-hand side over λ satisfying the conditions in Lemma 11, which is exactly the problem on the right-hand side of (A1).

The equivalence between the upper bounds (46) and (47) for the IH3 configuration follows from the identity

(B1)

where

(B2)

This identity can be proven using a convex duality argument analogous to that in  Appendix A. Indeed, Lemmas 9 and 10 apply to the functional Φ considered in this section with no changes to their proofs. Consequently,

(B3)

To calculate the Legendre transform Φ*, however, we must replace Lemma 11 with a different characterization of translation-invariant linear functionals μH+*. This is due to the different boundary conditions imposed on the temperature space H.

Lemma 12.

LetH+*be the set of positive linear functionals on the temperature spaceHdefined in(14a). IfμH+*is translation invariant, there exists a nondecreasing functionλL2(0, 1) non-negative almost everywhere and such thatμ{T}=λ(z)zT.

Proof.
Straightforward modifications to the Proof of Lemma 3 (Arslan et al., 2021)2 reveal that any translation-invariant μH* admits the representation μ{T}=λ(z)zT for some function λL2(0, 1). If μ is also positive, then the argument in the proof of Ref. 2 (Lemma 2) shows that λ must be nondecreasing. To see that, we must have λ(z0) ≥ 0 at almost every z0 ∈ (0, 1), fix ɛ > 0 sufficiently small, and consider the temperature field TεH+ given by
Then, since μ is a positive functional by assumption,
By Lebesgue’s differentiation theorem, the right-hand side tends to 2λ(z0) for almost all z0 ∈ (0, 1) as ɛ → 0. Thus, we must have λ ≥ 0 almost everywhere on (0,1).□

To conclude the argument, we need to calculate Φ*{μ} for translation-invariant μH+*, which by Lemma 12 is given by

Since the pair (β, τ) was assumed to satisfy the spectral constraint, this maximization problem can be restricted to temperature fields that depend only on the vertical coordinate z (this can be proven by splitting T into its horizontal mean η and a perturbation ξ with zero horizontal mean, as outlined at the end of  Appendix A). The optimal value can then be shown to be

and can be substituted into (B3) to arrive at

Changing the optimization variable on the right-hand side to λ̃=λ1 yields (B1).

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