Local and global strong solutions for SQG in bounded domains
Peter Constantin, Huy Quang Nguyen

TL;DR
This paper establishes local and global existence results for the SQG equation in bounded domains, depending on the presence and strength of dissipation and the size of initial data.
Contribution
It proves local well-posedness in bounded domains and demonstrates global existence of strong solutions under various dissipation and data size conditions.
Findings
Local well-posedness for inviscid SQG in bounded domains
Global existence with fractional dissipation for small data
Global existence with arbitrary data in subcritical cases
Abstract
We prove local well-posedness for the inviscid surface quasigeostrophic (SQG) equation in bounded domains of . When fractional Dirichlet Laplacian dissipation is added, global existence of strong solutions is obtained for small data for critical and supercritical cases. Global existence of strong solutions with arbitrary data is obtained in the subcritical cases.
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Local and global strong solutions for SQG in bounded domains
Peter Constantin
Department of Mathematics, Princeton University, Princeton, NJ 08544
and
Huy Quang Nguyen
Program in Applied and Computational Mathematics, Princeton University, Princeton, NJ 08544
(Date: today)
Abstract.
We prove local well-posedness for the inviscid surface quasigeostrophic (SQG) equation in bounded domains of . When fractional Dirichlet Laplacian dissipation is added, global existence of strong solutions is obtained for small data for critical and supercritical cases. Global existence of strong solutions with arbitrary data is obtained in the subcritical cases.
Key words and phrases:
SQG, local well-posedness, global strong solutions, bounded domains
- MSC Classification: 35Q35, 35Q86.*
To Edriss Titi, with friendship, respect and admiration
1. Introduction
Let be an open bounded set with smooth boundary. The surface quasigeostrophic (SQG) equation in is the equation
[TABLE]
where
[TABLE]
The Laplacian above has homogeneous Dirichlet boundary conditions, and the equation is an active scalar equation: the scalar determines for by
[TABLE]
The nonnegative number distinguishes between the dissipative SQG equation (1.1), when , and the inviscid SQG equation when .
The domain of the Laplacian with homogeneous Dirichlet boundary conditions is
[TABLE]
and the fractional Laplacian , is defined using eigenfunction expansions. The domain of definition of the fractional Laplacian, is endowed with a natural norm and is a Hilbert space (see section 2 below for details). In particular, the norm of is equivalent to the norm.
The main results of this paper concerning the dissipative SQG equation are the local well-posedness for the whole range of for arbitrary data in and the existence of unque global solutions for small data in .
Theorem 1.1**.**
Let and . Let be an initial datum.
1. There exists a constant depending only on , such that, on the time interval , with
[TABLE]
(1.1) has a unique solution in
[TABLE]
2. There exists a positive constant depending only on such that the following holds: if
[TABLE]
then there exists a unique global-in-time solution
[TABLE]
of (1.1). Moreover, the norm of is bounded by its initial value:
[TABLE]
The subcritical SQG equation (1.1) with is globally well-posed, as in the case without boundaries:
Theorem 1.2**.**
Let , , and . Let be an initial datum. There exists a unique solution
[TABLE]
of (1.1).
The result of this paper concerning the inviscid SQG equation is the local well-posedness in a class of classical solutions.
Theorem 1.3**.**
Let . For every , there exist and unique solution
[TABLE]
to (1.1) with .
The surface quasigeostrophic equation of geophysical significance ([13]) serves as a two-dimensional model for the three-dimensional Euler equations due to many mathematical and physical analogies between them ([8]). There is a vast literature devoted to local and global well-posedness issues for SQG in and . It is known that global weak solutions exist for arbitrary data ([20]). The subcritical dissipative case is well-understood ([20, 11, 12]) and global solutions with small initial data in the critical space for the critical SQG were obtained in [5]. Global regularity for the critical dissipative case is subtle and was first obtained independently in [4, 15]. There are several later proofs of this result [16, 10]. The global regularity for the supercritical dissipative and inviscid SQG are outstanding open problems.
The study of SQG in bounded domains with smooth boundaries was initiated in [6, 7] where global weak solutions were obtained and global Lipschitz a priori interior estimates were obtained for critical SQG. global weak solutions for the inviscid SQG were obtained in [9], and generalized in [19] for SQG-type equations with more singular constitutive laws, with . As in the cases without boundary, uniqueness of weak solutions is not known. The presence of boundaries makes the well-posedness issues become more delicate. The main source of difficulties is the lack of translation invariance of the fractional Laplacian in bounded domains. This manifests itself in particular in the commutator estimates for the fractional Laplacian. In order to appreciate these difficulties, let us consider the local well-posedness in Sobolev spaces for the inviscid SQG. For the flow to be well-defined it is good for the velocity to be Lipschitz continuous, and so natural Sobolev spaces for local well-posedness (in two dimensions) are with (because is obtained from through Riesz transforms). The main tools for proving local well-posedness in the whole space ([8, 12], see also [22]) are the well-known Kato-Ponce commutator estimate ([14])
[TABLE]
with , where , with denoting the Fourier transform. Additionally, it is useful that withe Riesz transforms are continuous in Sobolev spaces
[TABLE]
The bound (1.5) follows directly from the Plancheral theorem. In bounded domains the estimate (1.4) fails because the fractional Laplacian does not commute with differentiation, and the existing sharp estimate [6] is too expensive. In order to do regularity calculations the commutator between and needs to be considered. This has a singular behavior at the boundary [7], [9] (which is sharp in half-space):
[TABLE]
with , , and . In order to overcome this and to obtain local well-posedness in the inviscid case the idea is to take even indices , , because then commutes with on the domain of . This in turn however requires that the nonlinearity to belong to , provided . Unfortunately, this is not true in general. It is true for because vanishes on the boundary. This is due to the following structure: is tangent to the boundary because , and is normal to the boundary, because . Taking derivatives of unfortunately breaks down this structure. Forced to work with , we face another obstacle: is not Lipschitz continuous. Therefore in Theorem 1.3 we prove local well-posedness in with , hence ensuring that is Lipschitz. The added difficulty now is that continuity of the Riezs transform from to is not available. The proof then consists of three bootstraps: Galerkin approximations to obtain the regularity, a transport estimate to obtain the regularity for any , and finally another transport estimate to gain the full regularity.
The paper is organized as follows. In section 2 we present the functional setup for the fractional Laplacian in domains using eigenfunction expansions. Theorems 1.1, 1.2, 1.3 are proved in sections 3, 4, 5, respectively. Appendices 1 and 2 are devoted to bounds and local well-psoedness for the linear advection-diffusion equations with fractional dissipation.
2. Preliminaries
Let be an open bounded set of , , with smooth boundary. The Laplacian is defined on . Let be an orthonormal basis of comprised of normalized eigenfunctions of , i.e.
[TABLE]
with .
The fractional Laplacian is defined using eigenfunction expansions,
[TABLE]
for and
[TABLE]
The norm of in is defined by
[TABLE]
It is also well known that and are isometric, where is equipped with the norm
[TABLE]
In the language of interpolation theory,
[TABLE]
Moreover, it is readily seen by virtue of the Hölder inequality that
[TABLE]
provided , , and .
As mentioned above,
[TABLE]
hence
[TABLE]
Consequently, we can identify with usual Sobolev spaces (see Chapter 1 [18]):
[TABLE]
We have the following relation between and .
Proposition 2.1**.**
The continuous embedding
[TABLE]
holds for all .
Proof.
By interpolation, it suffices to prove (2.4) for . The case is obvious while the case follows from (2.3). Assume by induction (2.4) for with . Let then and thus by the induction hypothesis. On the other hand, vanishes on the boundary in the trace sense because . Elliptic regularity then implies that and
[TABLE]
which is (2.4) for . ∎
Below is the list of some notations used throughout this paper:
- •
: the scalar product.
- •
: the dual pairing between and its dual .
- •
: the trace of on .
- •
: the trace of on where is the outward unit normal to .
3. Proof of Theorem 1.1
3.1. Technical lemmas
We start with an estimate for the Riesz transforms in Sobolev spaces.
Lemma 3.1**.**
If with then
[TABLE]
Proof.
Indeed, we have with . It follows from (2.4) that
[TABLE]
∎
The next lemma provides the key estimate needed for the proof of Theorem 1.1.
Lemma 3.2**.**
Let and . Denote and . There exists a positive constant such that
[TABLE]
where
[TABLE]
Proof.
A direct computation gives
[TABLE]
where
[TABLE]
if
[TABLE]
Using the facts that commutes with the Riesz transforms, because it commutes with both and , the Riesz transforms are bounded in for all , a fact that holds for domains (see Theorem C in [21]), together with (2.3) we deduce
[TABLE]
where the embedding was used in the second inequality.
Let satisfy . By the embeddings (2.4), and interpolation we have
[TABLE]
Let us note that , so vanishes on the boundary in the trace sense. Elliptic estimates in together with the embeddings and (2.4) imply
[TABLE]
Thus,
[TABLE]
Now regarding the term we first use the embedding and the estimate (3.1) to have
[TABLE]
and then by the interpolation inequality (2.2)
[TABLE]
Finally, putting together (3.5)-(3.8) we arrive at (3.2) by using the Hölder inequality with exponents and . ∎
We recall the following product rule (see Chapter 2, [1]) in , ,
[TABLE]
provided
[TABLE]
By extension, interpolation, and duality, (3.9) still holds in smooth bounded domains of .
Lemma 3.3**.**
Let , , , and . Then .
Proof.
First, let us note that and . In particular, is well defined in by virtue of the product rule (3.9) for . Since , is tangent to the boundary, and since , is normal to the boundary. Therefore, vanishes on the boundary. Because the mapping is continuous in view of (3.9), . For the same reason, we have and hence . ∎
3.2. Uniqueness
Let
[TABLE]
, be two solutions of the inviscid SQG equation with the same initial data . Then the difference solves
[TABLE]
Here, . Multiplying this equation by , then integrating over gives
[TABLE]
After integrating by parts, the last term is nonpositive, the first term vanishes because is divergence free. The middle term is bounded by
[TABLE]
where we used the embeddings . Because \theta_{2}\in L^{2}\big{(}[0,T];D(\Lambda^{2+\alpha})), the Grönwall lemma concludes that on , and thus .
3.3. Local existence
Let and let be an initial datum. We prove local existence of solutions using the Galerkin approximations. Denote by the projection in onto the linear span of eigenfunctions , i.e.
[TABLE]
It is readily seen that commutes with on for any .
The th Galerkin approximation of (1.1) is the following ODE system in the finite dimensional space :
[TABLE]
with and automatically satisfying . Note that in general . The existence of solutions of (3.11) at fixed follows from the fact that this is an ODE:
[TABLE]
with
[TABLE]
Since is self-adjoint in , is divergence-free and vanishes at the boundary , integrations by parts give
[TABLE]
and
[TABLE]
It follows that
[TABLE]
and in particular, the norm of is bounded:
[TABLE]
This can be seen directly on the ODE because is antisymmetric in . Therefore, the smooth solution of (3.11) exists globally. Observe that for the sake of global existence of (3.11), the dissipative effect is not needed, i.e. can be [math]. Obviously, for all and . According to Lemma 3.3, which combined with the fact that implies . Now applying to (3.11) and noticing that commutes with on result in
[TABLE]
Next, we take the scalar product with , use the commutator estimate (3.2), and the fact that is self-adjoint in to arrive at the differential inequality
[TABLE]
where and are defined as in (3.3) for . Then an application of the Young inequality allows us to hide on the right-hand side of (3.13) and obtain
[TABLE]
Ignoring and integrating (3.14) leads to
[TABLE]
with
[TABLE]
In other words, is uniformly in bounded in . Using the equation we find that is uniformly in bounded in . The Aubin-Lions lemma ([17]) then allows us to conclude the existence of a solution of (1.1) on . Moreover, by integrating (3.14) we find that satisfies
[TABLE]
3.4. Global existence
Let and let be an initial datum. We reuse the notations of section 3.3. Recall from (3.13) that
[TABLE]
It is readily seen by the interpolation inequality (2.2) that
[TABLE]
Consequently
[TABLE]
and thus
[TABLE]
Integrating this leads to
[TABLE]
By a coninuity argument, if
[TABLE]
then for and thus, in view of (3.17), for . In other words, the norm of is uniformly in bounded over all finite time interval . Using the equation, we deduce a uniform bound for in . Passing to the limit then can be done by virtue of the Aubin-Lions lemma ([17]) on each finite time interval . By uniqueness, we obtain a unique global solution.
4. Proof of Theorem 1.2
We first prove the following key estimate for the nonlinearity.
Lemma 4.1**.**
Let , , . Fix and put
[TABLE]
Then with and we have for all
[TABLE]
Proof.
According to Lemma 3.3, . Let satisfy and put
[TABLE]
Note that and is the conjugate exponent of , i.e. . By (2.3), if and if . Writing we estimate using the Hölder inequality
[TABLE]
if , and similarly,
[TABLE]
if .
In we have
[TABLE]
in view of the embedding . Then by extension and interpolation the following inequality holds in
[TABLE]
which implies
[TABLE]
The same estimate holds with replaced with . We thus obtain in both cases
[TABLE]
By interpolation, we have
[TABLE]
Applying Young inequalities yields for all
[TABLE]
and similarly,
[TABLE]
Using the embedding and putting together the above considerations leads to the estimate (4.1). ∎
Remark 4.2**.**
When , the estimate (4.1) holds for any (see Chapter 3 [20]). Here, for domains with boundaries, the restriction was imposed because requires more vanishing conditions for on in order to have . In addition, product rules for with are not available. In the above proof, the fact that helped bounding by , in view of (2.3), and then we could use the product rules in usual Sobolev spaces.
The restriction at first limits the regularity of the solution, i.e. . In order to gain the full regularity we note that with because . Then, using the result of Appendix 2, we know that in general the linear transport equation
[TABLE]
has a solution . Moreover, uniqueness holds in the class of . The known regularity of is thus enough to conclude that , and thus has the full regularity. The rest of this section is devoted to implement this strategy.
Let be an initial datum and be fixed. We construct a solution for (1.1) using the retarded mollifications. To this end we pick a , , with , and let
[TABLE]
where we set for all . In particular, depends on the values of only for .
Step 1. We pick a sequence and consider the approximate equations for
[TABLE]
with initial data and velocity . For a fixed , equation (4.2) is linear on each subinterval , , , because is determined by the values of on the two previous subintervals and . By our setting, on . On , and the linear equation (4.2) with initial data has a unique solution
[TABLE]
Direct estimates show that
[TABLE]
This implies in view of (3.1) that
[TABLE]
with . This regularity of on suffices to conclude by applying Theorem 4 in [6] that there exists a unique solution on and thus, by induction, on for all , and
[TABLE]
The proof of Theorem 4 in [6] makes use of a general commutator estimate for in derived in the same paper. In Appendix 2, we give a direct proof without the commutator estimate.
We showed so far that for any fixed integer , equation (4.2) with initial data has a solution
[TABLE]
Step 2. We appeal to Lemma 4.1 to pass to the limit in the larger space . First, it follows from (3.1), (4.3), and the definition of that
[TABLE]
Secondly, according to Proposition 6.1, the bounds
[TABLE]
hold for all .
Let us fix and
[TABLE]
Applying in (4.2), then taking the scalar product with we obtain
[TABLE]
Using (4.1) (note that ) to estimate the right-hand side and then integrating the differential inequality we obtain for
[TABLE]
We choose , being sufficiently large, use (4.4), (4.5), (2.4) and the Grönwall lemma to arrive at
[TABLE]
with . The use of equation (4.2) and the bound (4.4) implies that is uniformly in bounded in . The Aubin-Lions lemma ([17]) then allows us to conclude the existence of a solution
[TABLE]
of (1.1). Moreover, obeys the bound (4.6).
We note that with and hence with . According to Theorem 7.1 1., there exists a solution
[TABLE]
of the linear equation
[TABLE]
The regularity of is sufficient to conclude using Theorem 7.1 2. that and thus has the full regularity as in (4.7). Uniqueness follows from section 3.2.
5. Proof of Theorem 1.3
Let with . The proof proceeds by Picard’s iterations in each of which a viscosity approximation is added: , , is defined as the solution of the problem
[TABLE]
We prove by induction that there exist
[TABLE]
both are independent of and , such that
[TABLE]
and
[TABLE]
When , both (5.2) and (5.3) hold for any . Assume they hold for , , we prove it for . The regularity (5.2) of will be obtained by three bootstraps: , then with , and finally .
Step 1. regularity. We note that . On the other hand, by Sobolev’s embedding for some , and , Proposition 3.1 [3] then yields , and thus . Thus,
[TABLE]
Note however that we do not have in general but only , by interior elliptic estimates. Then according to Theorem 7.1, the transport problem (5.1) has a unique solution
[TABLE]
for any and
[TABLE]
Step 2. regularity. Fix . We observe that satisfies
[TABLE]
It follows from (5.4), (5.5), and the embeddings for any , that
[TABLE]
here .
In addition, because and , elliptic estimates combined with (5.5) imply
[TABLE]
Now we multiply (5.6) by , using the inequality (6.5), the fact that , and (5.9) to get
[TABLE]
Consequently, for any ,
[TABLE]
for some increasing function , where (5.7), (5.4) were used. In what follows, may change from line to line but is independent of and .
As in (5.9), elliptic estimates yield
[TABLE]
Step 3. regularity. By the Sobolev embedding , we have
[TABLE]
which, combined with (5.4), implies
[TABLE]
Then, multiplying (5.6) by and argue as above leads to the bound
[TABLE]
By elliptic estimates, we obtain that
[TABLE]
Step 4. Concluding. Now by the induction hypothesis,
[TABLE]
with , . Therefore, if we choose
[TABLE]
then
[TABLE]
and thus
[TABLE]
This completes the proof of (5.2) and (5.3). Then, using the first equation in (5.1), (5.4), (5.5), it follows easily that
[TABLE]
for some independent of and .
Using the uniform bounds (5.3), (5.11), we can first pass to the limit by virtue of the Aubin-Lions lemma, then send to obtain a solution
[TABLE]
to the inviscid SQG equation. Finally, uniqueness follows easily by an energy estimate for the difference of two solutions as done in section 3.2, noticing that with .
6. Appendix 1: bounds
Let be an open set with smooth boundary.
Proposition 6.1**.**
Let and . Let be a divergence-free vector field and consider the linear advection-diffusion equation
[TABLE]
(i) If and
[TABLE]
is a solution of (6.1) then we have for any
[TABLE]
(ii) If and
[TABLE]
is a solution of (6.1) then (6.3) holds for any .
Proof.
We first note that in both cases, equation (6.1) is satisfied in for any . Therefore, for any .
(i) Case 1: and . It suffices to consider because the case follows by sending . We have
[TABLE]
In two dimensions, the condition implies . Since is divergence-free, the first term on the right-hand side vanishes in view of the Stokes formula. Regarding the dissipative term, we use the Córdoba-Córdoba inequality ([12], see also [20]) which was proved for bounded domains in ([6]):
[TABLE]
almost everywhere in for and convex satisfying . Note that in two dimensions, and , hence each term in (6.5) is well defined in . Under condition (6.2), with , , we have
[TABLE]
Consequently and (6.3) follows.
(ii) Case 2: and . If it suffices to assume with and convex to get the inequality (6.5). Indeed, we then have and thus belongs to . Therefore, (6.3) holds for any by choosing as in (i). ∎
7. Appendix 2: Linear advection-difussion
Let , , be an open set with smooth boundary. Let and . Let be a vector field on and consider the linear advection-diffusion equation of ,
[TABLE]
Define
[TABLE]
endowed with its natural norm. We prove (see also [6])
Theorem 7.1**.**
Assume that is divergence-free and parallel to the boundary, i.e. .
1. (Existence) Assume with . Equation (7.1) with initial data has a solution satisfying
[TABLE]
2. (Uniqueness) Assume . Equation (7.1) has at most one weak solution satisfying
[TABLE]
Proof.
- We proceed as in section 3.1 using the Galerkin approximations. It suffices to derive a priori bounds for solution to
[TABLE]
As in Lemma 3.3, , and hence . Applying in the first equation of (7.3) , then taking the scalar product with and taking into account the fact that is self-adjoint and commutes with on we obtain
[TABLE]
Since vanishes on the boundary and is divergence-free, an integration by parts gives
[TABLE]
We recall from (3.4) that
[TABLE]
hence
[TABLE]
We obtain thus
[TABLE]
Passing to the limit can be done by means of the Aubin-Lions lemma ([17]).
- Under the assumed regularity of and , equation (7.1) is satisfied in :
[TABLE]
In addition, , hence and for a.e. (see Chapter 2, [2])
[TABLE]
Since , . The Stokes formula then yields
[TABLE]
for and . Consequently,
[TABLE]
and thus for if . ∎
Acknowledgment. The work of PC was partially supported by NSF grant DMS-1209394
The reference list from the paper itself. Each links out to its DOI / PubMed record.
- 1[1] Hajer Bahouri, Jean-Yves Chemin, and Raphaël Danchin, Fourier analysis and nonlinear partial differential equations , volume 343 of Grundlehren der Mathematischen Wissenschaften [Fundamental Principles of Mathematical Sciences] . Springer, Heidelberg, 2011.
- 2[2] F. Boyer, P. Fabrie, Elements of analysis for the study of some incompressible flow models of viscous fluids , Springer-Verlag, Berlin, 2006.
- 3[3] X. Cabre, J. Tan, Positive solutions of nonlinear problems involving the square root of the Laplacian. Adv. Math. 224 (2010), no. 5, 2052-2093.
- 4[4] L. Caffarelli, A. Vasseur, Alexis, Drift diffusion equations with fractional diffusion and the quasi-geostrophic equation. Ann. of Math. 171 (2010), no. 3, 1903–1930.
- 5[5] P. Constantin, D. Cordoba, and J. Wu, On the critical dissipative quasi-geostrophic equation. Indiana Univ. Math. J. 50 (Special Issue): 97–107, 2001. Dedicated to Professors Ciprian Foias and Roger Temam (Bloomington, IN, 2000).
- 6[6] P. Constantin, M. Ignatova, Remarks on the fractional Laplacian with Dirichlet boundary conditions and applications. Internat. Math. Res. Notices , (2016), 1–21.
- 7[7] P. Constantin, M. Ignatova, Critical SQG in bounded domains. Annals of PDE , (2016) 2:8.
- 8[8] P. Constantin, A.J. Majda, and E. Tabak, Formation of strong fronts in the 2 2 2 -D quasigeostrophic thermal active scalar. Nonlinearity , 7(6) (1994), 1495-1533.
