Classical Solutions for the 3D Quasi-Geostrophic System on a Bounded Domain
Matthew Novack, Alexis Vasseur

TL;DR
This paper proves the local-in-time existence of classical solutions for a 3D quasi-geostrophic flow model on bounded cylindrical domains, revisiting and extending previous work on inviscid geophysical fluid dynamics.
Contribution
It establishes the existence of classical solutions for the 3D quasi-geostrophic system on bounded domains, providing a rigorous mathematical foundation for this model.
Findings
Proved local-in-time existence of classical solutions.
Revisited and extended previous models for 3D quasi-geostrophic flow.
Provided mathematical rigor for inviscid geophysical fluid dynamics on bounded domains.
Abstract
We revisit a model for three-dimensional, inviscid quasi-geostrophic flow on bounded, cylindrical domains introduced by the authors in \cite{nv18}. We prove the local-in-time existence of classical solutions.
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Classical Solutions for the 3D Quasi-Geostrophic System on a Bounded Domain
Matthew D. Novack
and
Alexis F. Vasseur
Department of Mathematics,
The University of Texas at Austin, Austin, TX 78712, USA
Department of Mathematics,
The University of Texas at Austin, Austin, TX 78712, USA
Abstract.
We revisit a model for three-dimensional, inviscid quasi-geostrophic flow on bounded, cylindrical domains introduced by the authors in [20]. We prove the local-in-time existence of classical solutions.
Key words and phrases:
Quasi-geostrophic equation, classical solution, bounded domains
2010 Mathematics Subject Classification:
76B03,35Q35
Acknowledgment: The second author was partially funded by the NSF during this work
1. Introduction
The quasi-geostrophic system is a set of equations used to describe oceanic and atmospheric motion over large time-scales. Much of the existing literature treats the case of a physical boundary at the (top and) bottom of the domain while specifying that the horizontal variables belong to either . In these cases, the equations take the form
[TABLE]
The normal derivative of on is denoted by , while , and . The operator is defined by
[TABLE]
where is a smooth function depending only on and is related to the density of the fluid. To ensure ellipticity of one requires that
[TABLE]
for some .
In a recent work [20], the fully three-dimensional system was considered on a domain with non-trivial lateral boundary conditions for the first time. Using only the assumption that the fluid velocity does not penetrate the boundary (i.e. ), the following model was derived:
[TABLE]
The quantity
[TABLE]
is therefore a datum that must be prescribed along with an initial vorticity and Neumann condition . We emphasize however that we do not prescribe the lateral boundary values . They instead arise as the boundary conditions naturally dual to (1) when solving an elliptic problem in an appropriate Hilbert space (see Definition 2.1). In [20], we proved the existence of a global weak solution to this system.
In this paper we prove the existence of a classical solution to this system for smooth enough initial data on a short time interval.
Theorem 1.1**.**
Given , , , such that
- (1)
* is , there exists such that , and for * 2. (2)
* and vanishes in a neighborhood of * 3. (3)
* and is compactly supported in * 4. (4)
* and for *
there exists a time which for large data satisfies
[TABLE]
such that QG posed on the cylindrical domain has a classical solution on the time interval .
The compatibility conditions appear necessary for the construction of smooth solutions. Essentially, we can only treat data , which are zero in a neighborhood of the corners and datum which retain smoothness after even reflection over the boundaries at . While we can prove higher order elliptic regularity under weaker conditions on the data , , , and (see Definition 2.3), it is not clear that these conditions are preserved by the evolution of the system (see (Claim 1:) on page 11). However, an important consideration is that our conditions are still sufficiently general to treat a broad class of initial data for the special case of 2D SQG (see the next subsection for a discussion of the relation of our model to proposed models for 2D SQG on bounded domains).
1.1. Previous Results
Quasi-geostrophic flow is an asymptotic limit of 3D Navier-Stokes or Euler equations as the Rossby number . Study of the inviscid three dimensional QG system was initiated in the absence of boundary conditions by Bourgeois and Beale [2]. With the aid of viscosity at the boundary, Desjardins and Grenier built global-in-time weak solutions [12]. Both of the afore-mentioned papers also include proofs that on the interval of time for which a smooth solution to the limiting system persists, the solutions to Navier-Stokes/Euler converge to the solution to QG. In [22], Puel and the second author introduced a reformulation of the inviscid 3D QG system in terms of which allowed for the construction of weak solutions via compactness. Using again the reformulation, the first author then extended this existence result to a wider class of initial data and determined the conditions under which the energy is conserved [18]. In a recent work, the first author also addressed the case of energy-dissipative weak solutions via a convex integration argument [19]. Global regularity to the 3D model with dissipation was shown by the authors in [21].
A special case of the three-dimensional model called the surface quasi-geostrophic equation arises by specifying that , , and . Then the stream function remains harmonic for all times , in which case the dynamics can be described completely by the evolution of . Since is harmonic, one has that and where is the vector of two dimensional Riesz transforms, and thus the equation can be written as
[TABLE]
Study of 2D SQG began with the work of Constantin, Majda, and Tabak [5]. Weak solutions were constructed by Resnick [23], with an extension of the theory by Marchand [16]. The equivalences of the various notions of weak solutions to 2D SQG and 3D QG were shown by the first author in [18]. In the presence of a viscous term , global regularity of 2D SQG has been shown by Kiselev, Nazarov, and Volberg [14], Caffarelli and the second author [4], Constantin and Vicol [6], and Kiselev and Nazarov [13].
One way of approaching two-dimensional quasi-geostrophic dynamics on a smooth, bounded set is to specify a notion of Riesz transform in order to define the velocity . A natural choice is to define the half-Laplacian spectrally using the Dirichlet eigenfunctions, an approach initiated by Constantin and Ignatova in [8] and [7]. Further work by Constantin and Nguyen [11], [10], Nguyen [17], and Constantin, Nguyen, and Ignatova [9] has explored further questions concerning this model. However, it is not hard to see that solutions to inviscid SQG constructed using the spectral Riesz transform and extended harmonically to cannot coincide with the solutions to 3D QG we produce in this paper. The difference lies in the lateral boundary conditions. The use of the Dirichlet Laplacian imposes that the extended stream function
[TABLE]
However, the lateral boundary values of our stream function are not uniformly zero. Furthermore, in the introduction of [20], we show that solutions constructed via the spectral Riesz transform do not satisfy (1) either. Therefore, one of the main motivations of this work was to validate the physical relevance of the three-dimensional model and associated lateral boundary conditions derived in [20].
The outline for this paper is as follows. In the next section, we first provide an intuition for the elliptic problem in the simple case that is a ball. We then recall previous results and prove the higher regularity estimates needed to construct classical solutions. In the third section, we construct classical solutions using a fixed-point argument. The appendix contains a short justification for the use of a commutator estimate in our setting which is classical for or .
2. A Non-Standard Elliptic Problem
2.1. A Simple Case
As described previously, building solutions to QG on a cylinder requires a choice of datum which encodes the ”average Neumann condition” as
[TABLE]
With this choice, reconstrucing at a given time can be done by solving an elliptic problem using , , and as data. This elliptic problem takes the form
[TABLE]
As alluded to before, we cannot choose ; rather, it arises as the condition naturally dual to the average Neumann datum . Let us suppose now that is the unit ball so that we have access to rotational symmetries. Define to be the rotational average of
[TABLE]
and set . Assuming for the time being that we can solve the elliptic problem , what is the equation satisfied by ? Due to the fact that commutes with rotations in , we see that
[TABLE]
In addition, we will also have that , where is the rotational average of . Finally, as is invariant under rotations and depends only on , we find that solves the Neumann problem
[TABLE]
By linearity, then solves
[TABLE]
That is, encodes the rotationally symmetric portion of and solves a Neumann problem, while encodes the deviations from rotational symmetry and solves an elliptic problem with Neumann data on the top and bottom and Dirichlet data on the lateral boundaries. We remark that even in this simplified setting, it is evident that the data must satisfy some compatibility conditions at the corners in order for to be smooth.
2.2. Previous Results and Definitions
Following [20], we define the Hilbert space to which the solution will belong for each time .
Definition 2.1**.**
Define by
[TABLE]
Using the notation , equip with the inner product
[TABLE]
Define the Hilbert space as the closure of under the norm induced by this inner product.
The construction of weak solutions requires a compatibility condition on the initial data due to the fact that test functions which are equal to a nontrivial constant throughout do not belong to .
Definition 2.2** (Basic Compatibility).**
Any triple of functions with , , is compatible if
[TABLE]
For compatible data, we proved the following existence result.
Lemma 3.1** ([20]).**
For compatible data , there exists a unique solution to the elliptic problem
[TABLE]
satisfying the bound
[TABLE]
Let and be the sequence of eigenfunctions and corresponding eigenvalues for the operator on with homogenous Dirichlet boundary conditions; that is,
[TABLE]
For , define
[TABLE]
It is well known (consult section 2 of [11] for example) that the domain of the homogenous Dirichlet Laplacian is , and for such functions the and norms are equivalent.
We now define the higher-order compatibility conditions needed to prove higher regularity estimates. Data which satisfy Definition 2.2 and Definition 2.3 will be called fully compatible.
Definition 2.3** (Fully Compatible Data).**
A triple of functions is fully compatible if it is compatible (Definition 2.2) and satisfies in addition that
- (1)
* and vanishes on * 2. (2)
** 3. (3)
* and for and the solution to*
[TABLE]
the equality
[TABLE]
holds.
We now recall Lemma 3.4 from [20].
Lemma 3.4**.**
([20]) Consider the equation
[TABLE]
for , . Then there exists a solution which satisfies
[TABLE]
In [20], we proved the following elliptic regularity theorem (refer to Lemmas 3.4, 3.5, 3.6 from [20] for the details).
Theorem 3.2**.**
([20]) Let , and let , , and . Let be the solution to . Then
[TABLE]
2.3. Higher Regularity
In order for the lateral boundary conditions to make sense, we assume the boundary of has no discrete subcomponents. Higher (than ) regularity is likely available through a more careful analysis of higher order compatibility conditions. However, the following result is satisfactory for building smooth solutions to QG and already somewhat delicate, and so we do not pursue any higher regularity here.
Theorem 2.1** (Higher Regularity).**
Let be a bounded, open set in with a smooth (, non-self-intersecting, no discrete subcomponents) boundary . Consider the elliptic problem
[TABLE]
for a fully compatible triple of data . Then and satisfies the bound
[TABLE]
Proof.
Throughout the proof, we use the notation to describe constants that depend only on , , and may change from line to line. The proof is broken into two steps, which proceed as follows. In Step 1, we isolate the effect of and while imposing homogenous Dirichlet conditions on . The regularity for Step 1 proceeds via a combination of a change of variables in and bootstrapping. By using classical elliptic regularity for and 3.4 for , we obtain regularity. We note that we require the compatibility condition on in this first step. Then in Step 2, we analyze the effect of by reflecting over the boundaries at and utilizing 3.2 and the compatibility condition between and and .
- Step 1:
Let be the solution to
[TABLE]
We can construct variationally in the subspace of consisting of functions which vanish on . Then satisfies the bound
[TABLE]
Now consider
[TABLE]
for solving
[TABLE]
By the strict positivity and smoothness of , is well-defined, smooth, and a bijection for . Then we can calculate
[TABLE]
Notice that although only belongs to for now, is well-defined pointwise on and vanishes by the assumption on and the fact that on . Letting , we have shown that solves
[TABLE]
for and .
Let be an open, bounded set in with smooth boundary such that , and . Let be an Sobolev extension of to restricted to . Then consider the elliptic problem
[TABLE]
Classical elliptic regularity theory yields that . Note as well that since vanishes on , for any on . Therefore, we can set to be the solution to
[TABLE]
where . Then by 3.4, . Bootstrapping this estimate, we find that , and therefore by the same extension and restriction argument as before. Then , and so from 3.4. Bootstrapping again gives that . By the trace, . But since vanishes at , , and applying 3.4 again gives that . Bootstrapping yet again yields , and by the trace, . We now claim that . For this to be true, we must show that . For this we write
[TABLE]
by the earlier remark that vanishes at . Therefore, we can apply 3.4 to deduce that . Then bootstrapping a final time with gives that . Thus we find that , and we obtain that . 2. Step 2:
Now we analyze the effect of . Define
[TABLE]
and set . Then solves
[TABLE]
To show higher regularity estimates on , we will reflect over the boundaries at . Let be a smooth, compactly supported function of such that for . Let be the reflection of over the boundary , and let be the reflection of over . By the assumptions of Definition 2.3, for ,
[TABLE]
Therefore retains integrability up to derivatives of order . Here is the only point that we require the higher-order compatibility conditions on .
Let us extend the operator by even reflection of to . By the assumption that at , we have that has well-defined derivatives up to order 4 on . One finds immediately that for all . We now calculate by writing
[TABLE]
We have that is well-defined since vanishes at 0 and vanishes at 0, and
[TABLE]
Note that by 3.2, and so this estimate makes sense. Continuing the analysis, then satisfies the equation
[TABLE]
Applying 3.2, we obtain that and satisfies the bound
[TABLE]
Repeating the argument, but this time with a reflection of over , shows that
[TABLE]
We must show that as well. Letting denote the tangent vector to , we have that , and therefore we can differentiate in the direction near . Then we have that
[TABLE]
Therefore we can differentiate in the direction near the lateral boundaries as well. Thus for any near , we have found a basis of directions such that , , and all belong to , and therefore .
We now outline how to obtain higher regularity ( for ) inductively. The estimate (Step 2:) yielded regularity contingent on the finiteness of the norm of . Differentiating this equality again in and arguing as before gives a finite norm of . We remark that as in the equality (Step 2:), the vanishing of , , and eliminates singularities or Dirac deltas at which arise when calculating . Applying the same reasoning another time, we reach . For the final half-derivative, runs out of differentiability at order 4, and so we reach .
∎
3. Construction of a Smooth Solution
We begin this section with a technical lemma which will be used to show that under the assumptions on and in the statement of Theorem 1.1, and vanish in a neighborhood of for all .
Lemma 3.1**.**
Let be a divergence-free vector field belonging to such that for . Let be the solution to the
[TABLE]
for and . Let . Then for all .
Proof.
First, by the regularity assumption on and the vanishing of the normal component of on , is well-defined as the solution to the ODE. Note that if , remains in forwards and backwards in time from since is tangent to . Conversely, it then holds that any point in the interior of at time remains so under the flow of . Consider the function which gives the distance from to for . By the continuity in of , for a fixed , is a continuous function on . However, we know that since maps the interior of to itself. Since the domain of is compact, the image of under is compact in and therefore has a minimum value which must be strictly larger than [math]. Therefore, for the distance from to is strictly bounded away from zero, and thus remains compactly supported in for all .
∎
Throughout the remainder of this section, the notation indicates a constant which depends on but may change from line to line (similarly for , , , etc.). Constants whose values remain fixed from line to line will be noted. We aim to build a smooth solution on a short time interval to the system
[TABLE]
Consider the set of functions
[TABLE]
for to be chosen later. For , we define a solution operator , which maps to the solution of the linearized version of the system with velocity field . Specifically, let and solve
[TABLE]
and for , define as the solution to the elliptic problem
[TABLE]
- Claim 1:
is a well-defined mapping.
Proof.
We first note that by the incompressiblity of the flow, the quantities
[TABLE]
are preserved in time. Therefore the compatibility condition from Definition 2.2 is satisfied for all time so that is well-defined as the solution to the elliptic problem. We now show that for all time .
Since solves
[TABLE]
we apply to the equation for , multiply by , and integrate by parts to obtain
[TABLE]
Summing over and using Sobolev embedding to control , we obtain that
[TABLE]
Applying Grönwall’s inequality gives that for ,
[TABLE]
An entirely analogous argument for yields
[TABLE]
Before applying Theorem 2.1, we must verify the compatibility conditions from Definition 2.3. Applying Lemma 3.1, we deduce that if the support of for fixed , then the support of . By the assumption on in Theorem 1.1, for close enough to [math] or , the support of . Therefore, , and thus remains at positive distance from for all time. Then , and we have now shown the first condition from Definition 2.3.
To show the second condition, we must show that we can replace the norms in the differential equality for with . Since is compactly supported in by the assumptions of Theorem 1.1, applying Lemma 3.1 shows that is compactly supported in for all time. Therefore,
[TABLE]
Next, we have that due to the continuous inclusion of the domain of into the classical Sobolev space for (consult [11] for example), replacing with on the right hand side can be done immediately without any assumptions on , and we have shown the second condition from Definition 2.3.
To verify the third compatiblity condition, after appealing to the assumptions on in Theorem 1.1, it suffices to show that
[TABLE]
for and the solution to
[TABLE]
For , we use the compact support of to notice that in a neighborhood (in and ) of . For , first note that by the assumption on in Theorem 1.1,
[TABLE]
Therefore, we can write that
[TABLE]
by the fact that and vanish near . Thus we have verified the third compatibility condition from Definition 2.3. We remark that this step of the argument is the one of the main reasons that we impose the conditions on , , , and in the statement of Theorem 1.1.
Now we can apply Theorem 2.1 to give that is a self-map of , and
[TABLE]
showing that maps into itself (for any ). ∎ 2. Claim 2:
There exists a choice of and a set such that .
Proof.
Define
[TABLE]
where is the constant from (Claim 1:), and by
[TABLE]
We have that is independent of , and
[TABLE]
For and , (Claim 1:) shows that
[TABLE]
Since this bound varies continuously in and is strictly less than at , we can find such that for all and ,
[TABLE]
To check the size of for large data, we must control the exponential term , which given the choice of remains comparable to 1 for
[TABLE]
∎ 3. Claim 3:
There exists such that has a fixed point in .
Proof.
Define , and define the sequence of functions
[TABLE]
inductively. Since is a self-map of , is well-defined for all . We claim that for a suitable choice of , is a Cauchy sequence in the space
[TABLE]
Let integers and be fixed. Then satisfies the equation
[TABLE]
Multiplying by , integrating by parts, and using Gronwäll’s inequality again shows that for ,
[TABLE]
A completely analogous argument holds for . Solving the elliptic problem and summing then shows that
[TABLE]
if is chosen to absorb the constant . Iteratively applying this bound then shows that is a Cauchy sequence as desired. In addition, the choice of gives the desired lower bound on for large data.
Since converges strongly to in and is uniformly bounded in , interpolation gives that converges strongly in for . Then define to be the solution to the elliptic problem
[TABLE]
Passing to the limit in the QG equations, we have therefore shown that is a fixed point of .
∎
4. Appendix
Proposition 4.1** (Commutator Estimate).**
For , there exist constants such that for a multi-index with ,
[TABLE]
Proof.
Substituting for , the statement is precisely the Klainerman-Majda commutator estimate from [15]. The ingredients of the proof in that case are Hölder’s inequality and the Gagliardo-Nirenberg interpolation inequality. As Hölder’s inequality is valid for , we can follow the classical proof provided that the Gagliardo-Nirenberg inequality holds for . Since is a bounded domain Lipschitz domain, Stein’s linear Sobolev extension operator [24] gives that for and ,
[TABLE]
is bounded with constants depending only on , , , and . Utilizing the extension, it is simple to show that Gagliardo-Nirenberg holds for , completing the proof. ∎
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