Temperature patches for the subcritical Boussinesq–Navier–Stokes System with no diffusion
Abstract
In this paper, we prove that temperature patch solutions to the subcritical Boussinesq–Navier–Stokes System with no diffusion preserve the Hölder regularity of their boundary for all time, which generalises the previously known result by F. Gancedo and E. García-Juárez [Annals of PDE, 3(2):14, 2017] to the full range of subcritical viscosity.
Keywords Boussinesq–Navier–Stokes System, temperature patch, subcritical dissipation, global existence.
MSC Classification 35R05 (Primary) 35Q35, 35F25, 35A01, 35A02 (Secondary)
1 Introduction
This paper studies temperature patch solutions of the following initial-value problem for the subcritical Boussinesq–Navier–Stokes equations, :
(1.6) |
Here, is a fractional Laplacian on defined initially for Schwartz functions as a Fourier multiplier . Also, , is the velocity of the fluid, is the pressure of the fluid, is the temperature of the fluid, and are the initial data of the system.
This active scalar transport system for arises as a natural generalisation of the Boussinesq–Navier–Stokes system, where the dissipation is the full Laplacian (corresponding to ). Details of the physics described by the Boussinesq–Navier–Stokes system can be found in [44]. Actually, (1.6) is a special case of a two parameter family of equations where there is also a diffusion term in the temperature equation; see for instance the papers [54], [43], [50], [53], and citations within. Only local results for the zero viscosity and zero diffusion case are known, such as those in [6].
In addition, some authors consider the opposite situation, where and (called the Euler–Boussinesq system) such as [30], [29], and [52], but to the best of the authors’ knowledge, there are no other papers currently available studying temperature patches for (1.6) with .
We consider solutions in the following sense:
Definition 1.1.
We say that with is a solution to (1.6) if for every divergence-free , and for every
(1.7) | |||
(1.8) |
By a ‘temperature patch solution’, we mean a solution of (1.6) where is an indicator function for each time . These are similar to the sharp front solutions of the SQG equation and their variants which have been and are extensively studied [47], [46], [20], [19], [18], [21], [13], [5], [7], [38], [39], [34], [35], [32], [33], and the more classical theory of vortex patches for the 2D Euler equation as laid out in [41], and also [10], [11], and [37]. The Boussinesq system also supports initial data of ‘Yudovich’ type. We mention a recent paper [42] working on local-in-time Yudovich solutions to the full inviscid equation. The case of critical diffusion was studied in [55]. Similar problems can be and have been studied for other systems with a transport equation with no diffusion [12], [26] [23], and multiple patch solutions for SQG have also been studied [36], [25]. Finally we mention some recent work [24] on piecewise Hölder solutions to the 3D analogue of the system (1.6) with .
Global unique classical solutions to (1.6) with were shown to exist in spaces in [4] and [31]; global (weak) solutions in were studied in [2], and global (weak) solutions in were proven to exist in [27] with uniqueness proven in [14]. In the case of temperature patches, Abidi and Hmidi [1] proved the persistence of regularity of the boundary, and Danchin and Zhang [15] improved this result to regularity. In Gancedo and García–Juárez [22], a second proof of Danchin and Zhang’s result was given, and they improved the result to persistence, in particular implying that the curvature of the patch remains bounded.
In [28], the critical equation has been studied in a low regularity scenario. However, the well-posedness result there requires initial data which falls short of allowing data, of which temperature patches are a special case. Our work shows that this seems to be a special feature of the critical case, as data is allowed for all This is a curious property, as the the transport evolution of gives that weak solutions cannot increase norms of . At the same time, there was some foreshadowing, as the method of Gancedo and García-Juárez which relies on the explicit formula for the heat kernel can only be replicated for the critical case , and has roughly the same regularity as (as opposed to being better behaved than : see [22] for details.)
Our main technical result is the following existence and uniqueness result:
Theorem 1.2.
Using Theorem 1.2, for any , we can control the boundary regularity of temperature patch solutions to (1.6):
Theorem 1.3.
Suppose that , for some , , and be an indicator function of a simply connected set with for some . Then the global solution to (1.6) remains an indicator, where for all .
The main method of proof is the use of the special structure of the equation by the study of , where is a smoothing operator. It turns out that it is easier to study this combination of terms than the vorticity by itself. This is the method used in [28], but since the proof is more streamlined.
Theorem 1.2 raises the following interesting questions: (a) Is it possible to control the curvature for , as it is possible in ? (b) can the critical equation support unique temperature patch solutions, and what regularity of their boundary is preserved?
The remainder of the paper is organised as follows. In Section 2, we list the notation that we use for function spaces and inequalities. In Section 3, we explain how introducing the term leads to better estimates. In Section 4, we give some easy a priori estimates from the equation obtained by classical means. In Section 5, we use the equation for to derive better a priori estimates for the vorticity (and hence the velocity). In Section 6, we use the Osgood Lemma to prove uniqueness of solutions. In Section 7, we use the quantitative bound from the Osgood Lemma to show existence of solutions, and also present the proof for conservation of Hölder regularity of temperature patch boundaries.
2 Preliminaries
We follow the notation of [28] as follows.
-
•
We write to denote any function of the form
-
•
We write to mean that for some constant that does not depend on or any other variable under consideration. We write to emphasise that the implicit constant depends on the quantities .
-
•
When is a Banach space, we will write for
to denote the Bochner space ; a function with values in is in if
(2.1) In a norm, we also abusively adopt the notation that a subscripted variable , like below, means that the norm is to be taken with respect to . This should not cause confusion with the above convention for time integrals. See for instance [17] or [48] for details on Bochner spaces.
2.1 Littlewood–Paley Decomposition and Function spaces
We fix our notation for Littlewood–Paley decompositions here; see [3], [8], [45], [51], or [49] for more details about Littlewood–Paley, Besov spaces, and Tilde spaces.
There exist two radial non-negative functions and such that
-
(i)
,
-
(ii)
if .
For every we define Fourier multipliers by
Lemma 2.1 (Bernstein Inequalities).
There exists constant such that for and for
(2.2) | ||||
(2.3) |
2.1.1 Besov and Tilde Spaces
The Besov space for is the space of distributions such that
In a norm, a subscripted variable like above means that the norm is to be taken with respect to . Since we will only consider functions on , we will only write (and similarly instead of ). Also write . The Besov spaces trivially satisfy
(2.4) | ||||
(2.5) |
and there is also the analogue of Sobolev embedding in 2D:
(2.6) |
In addition, we have the embeddings for any ,
We say that a function belongs to the ‘Tilde space’ if
In comparison with
From the generalised Minkowski inequality if and embeddings between Besov spaces, we have the following relations:
(2.7) | ||||
(2.8) |
where is arbitrarily small. In particular .
3 Study of and some commutators
3.1 Introduction of the term
We use the technique of [28], [52], [43], and other papers of introducing an auxillary quantity determined from the equation, that has better regularity properties than the original functions under consideration. The equation is obtained by applying the operator to the first equation of (1.6). By writing , i.e. , the equation takes the form
By adding to both sides of the equation, we obtain an equation for which has a commutator:
(3.1) |
This structure will be key in deriving the a priori estimates for . An important lemma for the study of the critical dissipation case is Lemma 3.3 in Hmidi–Keraani–Rousset’s paper [28]. The generalisation of Lemma 3.3 (ii) is the following result of Wu–Xue [52]:
Proposition 3.1 (Proposition 4.2 of [52]).
Let be a smooth divergence-free vector field of with vorticity and be a smooth scalar function. Then we have that for every
Besides, if we also have
We will similarly generalise Lemma 3.3 (i) of [28] by using Bony’s decomposition, as follows.
Theorem 3.2.
For any and any smooth with ,
We prove this result using the following lemma and the equivalent of Hmidi–Keraani–Rousset’s Proposition 3.1 (Wu–Xue’s Proposition 4.1). This lemma is also quoted in [29]. We give its short proof here, which is a variant of Lemma 2.97 of [3].
Lemma 3.3 (Lemma 3.2 of [28]).
Let , and let , and be three functions such that , , and . Then
(3.2) |
Proof.
By a direct computation and the fundamental theorem of calculus, setting ,
(3.3) | ||||
(3.4) | ||||
(3.5) |
Therefore, Hölder’s inequality and translation invariance of the Lebesgue measure gives
(3.6) | ||||
(3.7) | ||||
(3.8) |
for any . In particular, setting , we obtain the claimed result. ∎
Proposition 3.4 (Proposition 4.1 of [52]).
Let , , and . Then:
-
1.
For every and defined by , is a bounded map .
-
2.
Let . Then for each and ,
(3.9) Moreover, is a convolution operator with kernel satisfying
-
3.
Let be an annulus centered at the origin. Then there exists with spectrum supported away from such that for every with spectrum in ,
(3.10)
Proof of Theorem 3.2.
We use Bony’s decomposition,
(3.11) | ||||
(3.12) | ||||
(3.13) | ||||
(3.14) |
where (and ). The terms and are low-high and high-low interactions; the term are the interactions at similar frequencies (low-low and high-high).
Estimation of
Estimation of
Similarly to , we write
(3.22) |
Lemma 3.3 this time gives
(3.23) | ||||
(3.24) |
We want to use again; this time we will use the discrete Young’s inequality. Multiplying by , we note that
(3.25) | ||||
(3.26) |
where denotes the discrete convolution on ,
Applying the discrete Young’s inequality (note that ) with parameters ,
(3.27) | ||||
(3.28) |
Estimation of
We further split into high-high and low-low interactions,
(3.29) | ||||
(3.30) | ||||
(3.31) |
with no low frequency terms is dealt with as before, giving
(3.32) |
so that
(3.33) | ||||
(3.34) | ||||
(3.35) |
Under the assumption that , we have by the discrete Young’s inequality again,
(3.36) |
For , the lowest frequency terms don’t have a corresponding annulus for us to apply Lemma 3.3, so the Riesz transform has to be dealt with in a different way. We proceed without using the commutator structure, instead relying on Bernstein inequalities and boundedness of for defined by (as in Proposition 3.4):
(3.37) | ||||
(3.38) | ||||
(3.39) | ||||
(3.40) |
(Note that all constants from Bernstein inequalities are left implicit because is a finite sum.) This completes the estimation of and the Theorem is proved. ∎
4 Basic A Priori Estimates
Here we collect some estimates for smooth solutions of (1.6). Since solves a transport equation with no diffusion, and by testing the equation with itself, we obtain
(4.1) | ||||
(4.2) |
These imply
(4.3) | ||||
(4.4) |
and therefore:
Proposition 4.1.
Suppose are smooth solutions of (1.6) with initial data and . Then
(4.5) | ||||
(4.6) |
Proposition 4.2.
Suppose are smooth solutions of (1.6) with initial data and . Then for ,
(4.7) |
Proof.
As mentioned, we set . It solves the equation
(4.8) |
Taking the inner product with and using that in the form of the identity ,
(4.9) | ||||
(4.10) |
By Theorem 3.2, Proposition 4.1, and Proposition 3.4,
(4.11) | ||||
(4.12) | ||||
(4.13) | ||||
(4.14) | ||||
(4.15) |
Therefore,
(4.16) |
Young’s inequality for products gives
(4.17) |
An application of Grownwall’s inequality finishes the proof. ∎
5 A Priori Estimates for the Vorticity
Proposition 5.1.
Let be a smooth solution of (1.6), and let , with , , and . Then for ,
(5.1) |
Proof.
We will again use the equation for ,
From the estimates in Corollary 3.6 of Cordoba–Cordoba (they prove the estimate for the homogeneous equation ; what we need follows by Duhamel’s principle),
By Proposition 3.1,
Therefore, using and the boundedness of ,
and Gronwall’s inequality completes the proof. ∎
The following result is the analogue of Theorem 6.3 in [28].
Theorem 5.2.
Let solve (1.6) with initial data , , and with . Then for and ,
(5.2) |
Proof.
For we set Then, we localise in frequencies the equation (5.1) for to get
Multiplying the above equation by and integrating in the space variable we find
From [9] or [40], we have the following generalised Bernstein inequality,
valid for some independent of , and hence we find
This yields (writing and )
By taking the norm and by using convolution inequalities, we find (since , and )
(5.3) | |||
(5.4) | |||
(5.5) |
To estimate the second integral of the RHS of (5.5), we use Proposition 3.1. This gives uniformly in ,
(5.6) | ||||
(5.7) | ||||
(5.8) |
For the first integral of the RHS of (5.5) we use the following lemma:
Lemma 5.3 (Lemma 6.4 of [28]).
Let be a smooth divergence-free vector field and be a smooth scalar function. Then, for all and ,
Using Lemma 5.3, the bound (Proposition 4.2), and the bound on (Proposition 5.1), we can interpolate (recall ) to bound , giving
(5.9) |
Now we show how to estimate the sum in of (5.5). For high frequencies, since i.e. , we have
(5.10) |
so that by (5.5), for an to be chosen,
(5.11) | |||
(5.12) |
(The and is from the first and second integral terms, respectively.) For low frequencies of , we just use
(5.13) |
replacing on the right by the worse term , we see that
(5.14) | ||||
(5.15) |
Taking , we obtain as claimed. ∎
Proposition 5.4.
Proof.
The result is stronger for closer to 2, so without loss of generality, make smaller so that (this is for the application of Theorem 5.2). By triangle inequality and ,
(5.17) |
The first term is controlled by some by the embedding and the previous result, Proposition 5.3. Recalling that , we can use Bernstein inequalities to see that
(5.18) | ||||
(5.19) | ||||
(5.20) | ||||
(5.21) |
where we have used that . Since ,
(5.22) |
Hence, , and therefore Then we obtain (using Bernstein’s inequality for the low frequency term)
(5.23) | ||||
(5.24) | ||||
(5.25) |
∎
6 Uniqueness of solutions
In order to prove the uniqueness, we will rely on the following Osgood lemma, which can be found as Theorem 5.2.1 in [8], or in [16]:
Lemma 6.1 (Osgood Lemma).
Let a continuous non-decreasing function, and a measurable function satisfying
If we assume that then
If we assume and then .
Remark 6.2.
In the case , an explicit bound is also given in [8]. We will use the similar function , for which in the case , we have the estimate
(6.1) |
This estimate follows elementarily from for . In particular, note that as .
We now recall some results (with mild modifications) from Section 4 of Hmidi–Keraani–Rousset’s paper [28].
6.1 Estimates for transport-diffusion models
First, we have a result for transported scalars, which we will apply to the temperature of our system.
Proposition 6.3.
Let be a smooth divergence-free vector field. Then every scalar solution of the equation
satisfies for every ,
(6.2) |
Secondly, we have the following proposition for the linearised velocity equation. The proof is similar to the proof in Hmidi–Keraani–Rousset, so we omit the details. We will only apply this proposition with .
Proposition 6.4.
Let be a smooth divergence-free vector field, , and . Let be a smooth solution of the linear system
Then we have for each , with ,
We also need the following estimates adapted from the Appendix of [28]; essentially the same proofs can prove these lemmas, so we will omit them.
Lemma 6.5.
For every , if is a smooth divergence-free vector field, and is a smooth function, then
Lemma 6.6.
If , then .
Now we prove the uniqueness of solutions.
Theorem 6.7.
Proof.
Let and be two solutions to (1.6) in the space . Set and . Then, they solve
(6.4) | ||||
(6.5) |
with zero initial data. For the velocity , we write where solve the equations
(6.6) | ||||
(6.7) |
Proposition 6.4, first with and then with , gives
(6.8) | ||||
(6.9) |
since . Together, we obtain
(6.10) | ||||
(6.11) |
By Lemma 6.5 with , we have
(6.12) |
By using the logarithmic interpolation inequality of Lemma 6.6, we obtain
(6.13) |
We have used which can be proven for instance by using Bernoulli’s inequality for in the form . Writing , the above inequality can be rewritten as
(6.14) |
For the temperature, Proposition 6.3 with gives
(6.15) |
By Lemma 6.5 with ,
(6.16) |
By combining (6.11) with (6.12), (6.14), (6.15), (6.16), we obtain
(6.17) | |||
(6.18) | |||
(6.19) | |||
(6.20) | |||
(6.21) | |||
(6.22) |
Setting
(6.23) | ||||
(6.24) | ||||
(6.25) |
We obtain the following integral inequality for :
(6.26) |
Since , by Lemma 6.1, for every , which proves the uniqueness of solutions. ∎
7 Existence of solutions
We now use the above results to prove our main technical result.
Proof of Theorem 1.2.
The uniqueness is guaranteed by Theorem 6.7 so we focus on the existence. Following [6] (or Chapter 3 of [41]), if the initial data are smooth, we can obtain smooth solutions in to (1.6). By the a priori estimate of Proposition 5.4 and the Beale–Kato–Majda type blow-up criterion [6], the solution is globally defined.
Now let with , for some , and . Consider the sequence of initial data defined by Littlewood–Paley projections,
(7.1) | ||||
(7.2) |
These functions are smooth, so they define smooth solutions . Moreover, we have a priori estimates uniform in that imply for any and ,
(7.3) | ||||
(7.4) |
The spaces and are essentially equivalent by standard embeddings of Besov spaces due to the small loss in , so we can replace one with the other at any point.
Up to subsequences, we have that and converge weakly to functions and . By taking as initial data, the proof of Theorem 6.7 and Remark 6.2 gives that as soon as
we obtain
(7.5) | |||
(7.6) |
for an explicit function given by (6.1) with as . Thus is Cauchy and hence strongly convergent to in . Interpolation yields strong convergence of to in . This implies to strongly in . Also, since in , the product in . Thus, all terms in Definition 1.1 make sense, and is a solution to (1.6). ∎
Finally, for completeness, we give a standard argument that shows the boundary regularity for the temperature patches is preserved.
Proof of Theorem 1.3.
Let denote the flow of the vector field , i.e. the solution of
(7.7) | ||||
(7.8) |
Taking the gradient in gives
(7.9) |
so that
and similarly,
This shows that the flow remains in . To apply this to the boundary of the patch, suppose that at time , is parameterised by the curve . Then at time , the flow transports it to the curve
Then , and the Hölder seminorm of is controlled:
This proves that the Hölder regularity is preserved for all time. ∎
Acknowledgements
Both authors were partially supported by the NSF of China (Grant No. 11771045, 11871087).
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C. Khor
Laboratory of Mathematics and Complex Systems (Ministry of Education), School of Mathematical Sciences, Beijing Normal University, Beijing 100875, People’s Republic of China. [email protected]X. Xu
Laboratory of Mathematics and Complex Systems (Ministry of Education), School of Mathematical Sciences, Beijing Normal University, Beijing 100875, People’s Republic of China. [email protected]