We are concerned with the long-time solvability for 2D inviscid Boussinesq equations for a larger class of initial data which covers the case of borderline regularity. First we show the local solvability in Besov spaces uniformly with respect to a parameter κ associated with the stratification of the fluid. Afterwards, employing a blow-up criterion and Strichartz-type estimates, the long-time solvability is obtained for large κ regardless of the size of initial data.
We begin by considering the two-dimensional (2D) inviscid Boussinesq system
where , u is the fluid velocity, θ denotes the temperature (or the density in geophysical flows), p stands for the pressure, is a gravitational constant which will be associated with the stratification of the fluid (as described below), and the vector indicates the positive vertical direction.
The 2D Boussinesq equations arise as a model in lower dimensions for the 3D hydrodynamics equations by approximating the exact density of the fluid by a constant representative value [28]. In particular, these equations serve to model large scale atmospheric and oceanic flows that are responsible for cold fronts and the jet stream (see [25,27]).
Applying the “curl” to the first equation in (1.1), and recalling that the vorticity , we arrive at the equivalent vorticity formulation
Given that the atmosphere is physically observed to be mainly stable around the hydrostatic balance between the pressure gradient and gravitational effects [27], we wish to consider the initial temperature close to a physically nontrivial, stably stratified, stationary solution; namely, the hydrostatic balance , and then look for the solution of (1.2) with the temperature in the form . These modifications lead us to work with the following new system (see [31] for more details)
The parameter κ can then be interpreted as a gravitational constant with , where is the buoyancy or Brunt-Väisälä frequency, representing the strength of stable stratification. System (1.3) thus exhibits a dispersive nature due to the stable stratification terms, as will be developed below, and can be seen as a Rayleigh-Bénard convection model where hot fluid sits on top of cooler fluid.
From the mathematical point of view, the inviscid 2D Boussinesq equations (1.1) are also important because they retain essential structural features of the 3D Euler equations which derive from the vortex stretch mechanism; in fact, they are equivalent to the 3D axisymmetric Euler equations away from the symmetry axis. Additionally, this connection has prompted the analysis of this system in the presence of nonlocal dissipative mechanisms for the velocity or the temperature (or both), represented by a fractional Laplacian operator. Global regularity has been shown in various scenarios of these viscous systems, but there are still a number of open problems; see for instance [10,29,35], and references therein. In particular, the challenging problem of stabilization around the hydrostatic balance with partial viscosity or partial dissipation has been shown to be feasible by specifically exploiting the wave structure provided by the coupling of the velocity with the temperature (cf. [7,32]).
On the other hand, the regularity problem for the inviscid system (1.1) is in general more difficult, as it still appears to be unknown whether the classical application of the Beale–Kato–Majda (BKM) regularity criterion, based on the control of , is enough for the global regularity (cf. [37]). Thus, most results for this system are local in time, with various works dealing with the local well-posedness, in subcritical Besov and Sobolev spaces, by using the embedding of into , . The borderline case has added complications since is not bounded by , but this can be circumvented in the critical Besov space to show local well-posedness, where the embedding into does hold (cf. [24]).
Moreover, system (1.1) has been shown to be ill-posed in a borderline or critical regularity setting, where the notion of criticality is defined as the lower threshold where local well-posedness of strong solutions holds (cf. [9,18]). In particular, the approach in [18] hinges on showing that “the non-linearity does not serve as a stabilizing mechanism” [18], and is based on the condition that the equation be locally well-posed in the critical Besov space which imbeds in , along with the application of a nontrivial commutator estimate; so that the ill-posedness is linear and critical. Furthermore, it is shown that system (1.3) is ill-posed in the Yudovich class due to norm inflation of the vorticity. Thus, these results provide the backdrop for the ensuing proof of finite time blow-up for strong solutions of system (1.1) (cf. [17]).
However, there is a stark contrast for the inviscid system (1.3) in the presence of dispersive effects. The absence of dissipation presents the possibility of instabilities, but in [19] Elgindi and Widmayer are able to derive a sharp dispersive estimate and prove the long-time existence and non-linear stability of (1.3) about the stationary configuration, see also [34] for related results. The approach consists in showing that, in the case of , the dispersive estimate reveals the explicit time decay rate of the linearized system, while not affecting the energy estimates. The nonlinear stability then follows by improving the dependence of the local time of existence on the size of the initial data. As this structure is preserved at each level of the iterative scheme one can then obtain uniform estimates for the approximation, as we show below. Deriving the corresponding Strichartz estimates one can then control for the size of the initial data by making κ sufficiently large.
This dispersive estimate is also used for the analogous result in the case of the dispersive inviscid surface quasigeostrophic (SQG) equation, where dispersive effects are associated with strong rotation; indeed, both proofs have the same structure. We refer the reader to [1,3,16,23], and references therein, where the authors showed that high speeds of rotation tend to smooth out 3D Navier–Stokes and Euler flows.
In this direction, the long-time solvability of the system in the limit of strong stratification is important to reveal the structure of solutions and their main dynamics. For instance, in the case of the 3D Boussinesq system, Widmayer [36] shows that as the dispersive parameter grows to infinity, the limiting system is a stratified system of 2D Euler equations with stratified density.
This problem was analyzed for the SQG equations and the Boussinesq system (1.3) by Wan and Chen [35] to show the long-time solvability of strong solutions for large enough . The term solvability here refers to the pair of existence-uniqueness of solutions in an appropriate sense. The approach in [35] is based on generalizing the dispersive estimate of [19] and deriving the corresponding Strichartz estimates, to then show long-time solvability via a blow-up criterion of BKM-type in Sobolev spaces , with . Using an alternative argument, Takada [31] then improved this result with a weaker smoothness condition on the initial data, as only belonging to (), also showing the asymptotics of solutions as . Nevertheless, the results of [31] and [35] do not reach the case that appears as a borderline value for the long-time solvability of (1.3) in Sobolev spaces , and Besov spaces , with .
Thus, bearing in mind the lack of control on the vorticity in the context of local well-posedness in the borderline Besov space, we are motivated to show how the solvability can be extended in this context to arbitrary times through the strong linear dispersive stabilization. For this we exploit the paraproduct estimates which derive from the embedding of into , following the theme in Vishik’s result of long-time uniqueness for the 2D Euler equations in the borderline regularity case [33]. In particular, since we need to show local estimates which are uniform in κ, in contrast to [24], we must develop specific commutator estimates.
Then, in view of the identifications and for and (see [8, Theorem 6.4.4]), we are able to recover the results in [35] and also cover the case , with similar power laws for the time decay rate. Our main results read as follows:
Let s and q be real numbers such thatwithorwith.
(Local uniform solvability) Letand. There exists(depending ofand) such that (
1.3
) has a unique solutionwithand, for all.
(Long-time solvability) Let,, and. There existssuch that ifthen (
1.3
) has a unique solutionsuch thatand.
An analogous theorem for the SQG system was proved in our previous work [2], and although the general argument is structured in a similar vein, there are significant technical differences with the proof provided here for Theorem 1.1, which derive from the how the stabilization due to the coupling of velocity and temperature works at different levels.
In order to prove Theorem 1.1, and show how the regularization of the temperature feeds into further stabilization, we construct approximate solutions via a Picard iteration scheme, and show a priori estimates uniform with respect to the dispersive parameter κ, so as to obtain a solution as the limit of in the Besov spaces with the borderline regularity for (1.3) (see Section 4 and the proof of Theorem 1.1).
To do this in the framework of borderline regularity, we employ an intersection of spaces for the vorticity ω. In fact, is important to control the influence of κ on the existence time T, and then obtain a uniform time w.r.t κ, via a cancellation effect involving the -inner product (see, e.g., (4.2)), while the homogeneous Besov space provides the necessary control on the regularity, particularly for the borderline case. More precisely, we need to show that is bounded in and Cauchy in , both uniformly w.r.t. κ. It is worth noting that this difficulty does not appear in the context of inviscid SQG and Euler equations (with or without dispersive effects) when analyzing local solvability and borderline regularity in Besov spaces (see [1,2,26,33]).
We also note that to prove the uniform solvability in this context, it is central to use commutator estimates in the framework of homogeneous Besov spaces, which we present in a form which we could not find elsewhere in the literature (see Section 3). Subsequently, for large values of and , we obtain the long-time solvability by showing a blow-up criterion and handling globally the integral , using Strichartz estimates as presented in [23,35].
Lastly, we remark that the stability problem for the more general setting where the viscosity and thermal diffusivity are non-zero, which is also physically important [21,27], has received considerable attention. In particular, for the case of system (1.1) with positive viscosity but zero thermal diffusivity, the global well-posedness and inviscid limit have been shown through refined energy methods, see [12,14,20,22], whereas the stabilization around the hydrostatic balance has been recently studied in the case of bounded or strip domains with Dirichlet or periodic boundary conditions, see [10,15,32]. For the latter problem, the viscous term introduces a wave structure in the linearized system for which explicit decay rates can be shown, but so that the convergence to the full nonlinear equations is considerably more involved. Given that the energy estimates for this system has a parallel structure to the inviscid system, it is possible that the iterative scheme could be useful for controlling the decay rate and obtaining the asymptotic limit of large dispersive forcing.
The plan of the manuscript is as follows. In Section 2 we present some preliminaries about Besov spaces and Strichartz estimates, among others. Section 3 is devoted to the commutator estimates. In Section 4, we analyze the approximation scheme and obtain the local-in-time solvability of (1.3) uniformly with respect to the parameter κ. The proof of Theorem 1.1 (ii) is carried out in Section 5.
Preliminaries
The purpose of this section is to provide some basic definitions and properties about Besov spaces as well as some estimates useful for our ends, such as product, embeddings, Strichartz estimates, among others. We refer the reader to the book [8] for more details on Besov spaces and their properties.
First, we denote the Schwartz space on by and its dual by (tempered distributions). For , stands for the Fourier transform of f. Select a radial function satisfying , and
where . For each , we consider defined in Fourier variables as
We observe that
For and , the Littlewood–Paley operator is the convolution which works as a filter on the support of . We also consider the family of operators defined as and for every integer .
Let denote the set of polynomials and consider and . The homogeneous Besov space is the set of all such that
The nonhomogeneous version of , namely the Besov space , is the space of all such that the norm , where
The pairs and are Banach spaces. Also, for and , it follows that
For , we have the equivalence of norms
In the case , we recall the inclusion , for all .
(Bernstein’s Lemma).
Letandbe such that. Then, we have the estimateswhereis a positive constant.
Using the above lemma, one can prove the equivalence
Moreover, considering and , with if , we have that (see, e.g., [8, Sections 6.5 and 6.8])
Then,
where and with in the case .
The uniform estimates we develop rely on inequalities (2.1) and (2.2) in their respective regularity ranges and . For the case and the corresponding s, these inequalities hold in homogeneous Besov spaces. However, as our results are aimed for more general and s, and deal with the full inviscid case, we restrict to the case of nonhomogeneous spaces, where they are guaranteed to be valid, and leave open the question of working with homogeneous Besov spaces for the component ρ.
Some Leibniz-type rules in Besov spaces are the subject of the lemma below (see [11]).
Let,,andbe such that. Then, we have the estimateswhereis a universal constant.
We will employ the Strichartz estimates of [35], linked to the dispersive term obtained from (1.3), which will allow us to obtain long-time solvability for (1.3). In particular, we will use the following results found in [2,23] and [35].
Let,andbe such thatThen, there holdsfor all, whereandis a compactly supported smooth function in.
The present section is devoted to commutator estimates in and that will be useful to obtain convergence of our approximate solutions. We state and prove some of them, as we have not been able to locate them in the literature with the needed hypotheses and conclusions for our purposes.
Recall the commutator operator
Using the Hölder inequality in a slightly different way than used in [11,30,38], it is possible to obtain the following estimates for the commutator:
Letandbe such that.
Let,and. Assume further that,and. Then, we have the estimatewhereis a universal constant.
Let,and. Assume further thatand. Then, we have the estimatewhereis a universal constant.
With the help of Lemma 6.3 in [38] (see also [4]), the properties of the operator , considering the same hypotheses of Lemma 3.1 and using the same arguments in the proof of the same result, we obtain the following commutator estimate
Recall that the Bony formula for the paraproduct of f and g is given by
where
In the sequel we state and prove the following commutator-type estimates:
Letandbe such that.
Let,withand, andwith. Then, there exists a universal constantsuch that
Let,withand, and. Then, there exists a universal constantsuch that
The proof of part (i), it follows from the calculations obtained by Chae in [11]. We show the part (ii). We follow closely the argument in [33] (see also [5,13]). By Bony’s paraproduct formula (3.1), we can write
For I, in view of (3.2), it follows that
We observe that and , if . Then,
Using integration by parts, we arrive at
which yields
For estimate , by an argument similar to the one above, we first note that
Then, using and integration by parts, it holds that
Therefore,
which leads us to
For , we have that
Applying the -norm, we arrive at
For the parcel , we can decompose
Since , it follows that
Then
On the other hand, note that
Also, we can write
Hence,
and
Summing up the estimates (3.3), (3.4), (3.5), (3.6) and (3.7), we obtain
Multiplying by and computing the -norm, we can estimate
Now, observing that
we have that
and similarly .
For , note that
Therefore,
This completes the proof of (ii). □
An approximate linear iteration problem and local-in-time solvability
In order to prove the local existence to (1.3), we consider the approximate linear iteration problem
From (4.1), we provide uniform estimates for the sequence and then obtain a solution for (1.3).
Uniform estimates. Applying in (4.1), taking the product with in and the product with in in the first and second equations, respectively, and using the divergence-free condition , we obtain that
Adding the two above inequalities and using the properties
we arrive at
Integrating over , it follows that
Thus, by Grönwall’s inequality (see Proposition 1.2 in [6, page 24]), we have
Multiplying by , applying the -norm and Lemma 2.1, it follows that
From Remark 3.2 and Lemma 3.1, we have
Then,
On the other hand, taking the product with in and the product with in in the first and second equations of (4.1), respectively, and using the divergence-free condition , we obtain that
Here, we have used the equality , Lemma 2.1, Remark 2.2, the embedding and the property (4.2). Now, we integrate over and we use a Grönwall-type inequality to get
Combining (4.3) and (4.4), we obtain
Doing , we have
Since and , Grönwall’s inequality yields
where and the constants are independent of n. We wish to show that there exist and satisfying
In fact, for , note that
where . Similarly, for we have
for all , where . Denoting and making the same calculations for , we arrive at
Thus, continuing in the same way, we obtain (4.5) by induction.
Continuity of the sequence. Our intent now is to show that the sequences and belong to and , respectively. For that, considering the equality for all divergence free vector fields f, Remark 2.2, Lemma 2.3, the embedding , the following estimates
estimate (4.5), and the two first equations of (4.1), we have that and . Thus,
For and n fixed, we denote and . We claim that in and in , respectively, as . Using the Littlewood–Paley operators, we can also write
for each . Since and are absolutely continuous functions from to and , we obtain that
It follows that
As and , by Lemmas 2.3 and 3.3, the R.H.S. of the three above estimates go to zero as , and then the desired claim follows. Moreover, we get
Thus, and . Then
Convergence and local solution. Now, we show that and converge in and , for some , respectively. For that, we consider the following system
where and .
We take the -product with and the -product with in (4.8) to obtain
Next, adding the above two equalities, using the property , the equality for all divergence free vector fields f, Cauchy–Schwarz and Hölder inequalities, Lemma 2.1, Remark 2.2, the embedding and the estimate (4.5) to arrive at
Integrating over and using a Grönwall-type inequality, we have that
On the other hand, we applies to the first and second equations in (4.8), and afterwards take the -product with and the -product with in order to get
Adding the two previous equalities, employing the property
and using Cauchy–Schwarz and Hölder inequalities, we obtain that
Integrating over and using a Grönwall-type inequality, it follows that
Taking into account Lemma 2.1, multiplying by and taking the -norm, we have that
First, thanks to the embedding and the inequality
we can estimate and . For and , let us first note that by the equality for all divergence free vector fields f, Hölder inequality, Remark 2.2, the equality , the embedding and estimate (4.5), we have that
Then,
In view of Remark 3.2, Lemma 3.1 and using the same arguments to estimate and , we see that
Thus,
Combining (4.9) and (4.10), and using (4.11), (4.12) and (4.13), it holds that
By Grönwall inequality, it follows that
Denoting , and , we observe that
Following the iterative process, we arrive at
Let be such that for all . Then, it is fulfilled that and for all and . Moreover, there exists such that for all . Therefore, for some constant , we have
Let be such that , then there exists satisfying
This implies that and are Cauchy in the spaces and , respectively. Therefore, there are and such that if , then
Furthermore, since the sequences and belong to and , respectively, we have that and .
On the other hand, as and are bounded in and , respectively, we can extract subsequences and such that and in and , respectively. Thus,
with , where P and are as in (4.5).
Now, with the above convergence in hand, we sketch the convergence of the nonlinearity of the second equation and the coupling term in (4.1). The others follow similarly and are left to the reader. By Hölder’s inequality, Remark 2.2, the identity , the embedding and with , Lemma 2.1 and (4.5), it follows that
which implies
Moreover, since in , we have
and then
So, we can pass the limit in the integral formulation of approximate system (4.1) and obtain that is an integral solution for (1.3) in , namely
Considering , , using (4.15), and proceeding as in the proof of (4.6) and (4.7), it follows that , , in and in , as . Then, , , and the integral system (4.16) is indeed verified in , and consequently and , as desired.
Uniqueness. In this part, we suppose that system (1.3) possesses two solutions and with the same initial data and we show that and . For that, we set and , respectively. Then, satisfy the following system
Considering the spaces and in (4.17) and employing the argument used in (4.8) to estimate and , we obtain an inequality similar to inequality (4.14) as follows
Therefore, by Grönwall’s inequality we obtain for all . Thus, , implying that and , which shows the uniqueness of solution to (1.3).
Long-time solvability
In this section we prove the long-time solvability of (1.3) for large values of . We start with a proposition containing a blow-up criterion.
Let s and q be such thatwithorwith. Forand, considerthe corresponding solution of (
1.3
) satisfyingwhereis an existence time. If, then there existssuch thatcan be extended towith
By standard procedures used to estimate ω and ρ in Besov norms, we obtain the following estimates:
If we denote by I and J the penultimate and last term of the previous inequality, respectively, by Lemma 3.1, we have that
Denoting and employing the above inequalities in (5.1), it holds
Then, by using the inequality and the Grönwall-type inequality, it follows that there exists a constant such that
for all . Thus, by standard arguments, can be continued to for some , whenever
□
Long-time solvability. For , , let be the solution of system (1.3) satisfying
with maximal existence time . If , we are done. Assume that . Denoting , we can use Duhamel’s principle to get
where and . For , we define
In what follows, we continue to use the notation . We first consider the case with . We can estimate
For , we use Hölder’s inequality and Lemma 2.5 with to get
For , we employ the Minkowski and Hölder inequalities, Lemma 2.5 and Remark 2.2 to obtain
Thus, for each , we use (5.2), the embedding and the equality to get
Now, we deal with the case with . For each , we take such that . Note that since we have the nonhomogeneous embedding , so that we can estimate by the -norm of V. Thus, we have that
We now estimate . Using the embedding , Hölder’s inequality and Lemma 2.5, we can estimate
Also, by Lemma 2.4, we have that
Therefore,
We proceed to estimate . Hölder’s inequality, the embedding and Lemma 2.5 yield
Here we have proceeded as for the term in the case , . Also, by Lemma 2.4, the continuity of in and the embedding , we arrive at
It follows that
Thus, for each , we have
Therefore, for both cases of s and q such that with or with , we have that there exists such that
Next, for each we define , where
We first show that . We proceed by contradiction. So, assume on the contrary that . We have that there exists such that . It follows that
is uniformly continuous on , and
We now take a large enough so that
Using (5.3), (5.4) and (5.5), we obtain that
Thus, we can choose such that with . This contradicts the definition of . It follows that when κ verifies (5.5). If , then and
It follows that and, in view of the blow-up criterion, we obtain a contradiction with the maximality of . This concludes the proof.
Footnotes
Acknowledgements
L.C.F. Ferreira was supported by FAPESP (grant: 2020/05618-6) and CNPq (grant: 308799/2019-4), Brazil. L. Kosloff was supported by FAPESP (grant: 2016/15985-0), Brazil.
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