Wellposedness and convergence of solutions to a class of forced non-diffusive equations with applications
Susan Friedlander, Anthony Suen

TL;DR
This paper studies the well-posedness and convergence of solutions for a class of non-diffusive active scalar equations with applications to geophysical and porous media flows, analyzing the effects of viscosity parameters.
Contribution
It establishes Gevrey-class local well-posedness and solution convergence as viscosity vanishes for a family of singular non-diffusive equations, with applications to physical models.
Findings
Proved local well-posedness in Gevrey class for the equations.
Demonstrated convergence of solutions as viscosity parameter approaches zero.
Applied theoretical results to models of Earth's core turbulence and porous media flow.
Abstract
This paper considers a family of non-diffusive active scalar equations where a viscosity type parameter enters the equations via the constitutive law that relates the drift velocity with the scalar field. The resulting operator is smooth when the viscosity is present but singular when the viscosity is zero. We obtain Gevrey-class local well-posedness results and convergence of solutions as the viscosity vanishes. We apply our results to two examples that are derived from physical systems: firstly a model for magnetostrophic turbulence in the Earth's fluid core and secondly flow in a porous media with an "effective viscosity".
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Wellposedness and convergence of solutions to a class of forced non-diffusive equations with applications
Susan Friedlander
Department of Mathematics
University of Southern California
Anthony Suen
Department of Mathematics and Information Technology
The Education University of Hong Kong
Abstract.
This paper considers a family of non-diffusive active scalar equations where a viscosity type parameter enters the equations via the constitutive law that relates the drift velocity with the scalar field. The resulting operator is smooth when the viscosity is present but singular when the viscosity is zero. We obtain Gevrey-class local well-posedness results and convergence of solutions as the viscosity vanishes. We apply our results to two examples that are derived from physical systems: firstly a model for magnetostrophic turbulence in the Earth’s fluid core and secondly flow in a porous media with an “effective viscosity”.
keywords:
active scalar equations, vanishing viscosity limit, Gevrey-class solutions
1991 Mathematics Subject Classification:
76D03, 35Q35, 76W05
1. Introduction
Active scalar equations arise in many areas of fluid dynamics, with the most classical being the two dimensional Euler equation for an incompressible, inviscid flow in vorticity form. Another much studied active scalar equation is the surface quasi-geostrophic equation (SQG) introduced by Constantin, Majda and Tabak [5] as a two dimensional analogue of the three dimensional Euler equation (c.f [9], [8], [10], [17], [25]). The physics of an active scalar equation is encoded in the constitutive law that relates the transport velocity vector with the scalar field . This law produces a differential operator that when applied to the scalar field determines the velocity. The singular or smoothing properties of the operator are closely connected with the mathematical properties of the active scalar equation. In this present paper we study the following class of non-diffusive active scalar equations in with :
[TABLE]
where . Here is the initial condition and is a given smooth function that represents the forcing of the system.
Our motivation for addressing such a class of active scalar equations comes from two rather different physical systems that under particular parameter regimes give rise to systems of the form (1.3). The first example comes from MHD and a model proposed by Moffatt and Loper [22], Moffatt [24] for magenetostrophic turbulence in the Earth’s fluid core. Under the postulates in [22], the governing equation reduces to a 3 dimensional active scalar equation for a temperature field
[TABLE]
where the constitutive law is obtained from the linear system
[TABLE]
This system encodes the vestiges of the physics in the problem, namely the Coriolis force, the Lorentz force and gravity. Vector manipulations of (1.5)-(1.7) give the expression
[TABLE]
Here denote Cartesian unit vectors. The explicit expression for the components of the Fourier multiplier symbol as functions of the Fourier variable are obtained from the constitutive law (1) to give
[TABLE]
where
[TABLE]
The nonlinear equation (1.4) with related to via (1) is called the magnetogeostrophic (MG) equation and its mathematical properties have been studied in a series of papers including [11], [12], [13], [14], [15], [16]. In the magnetostrophic turbulence model the parameters , the nondimensional viscosity, and , the nondimensional thermal diffusivity, are extremely small. The behavior of the MG equation is dramatically different when the parameters and are present (i.e. positive) or absent (i.e. zero). The limit as either or both parameters vanish in highly singular. Since both parameters multiply a Laplacian term, their presence is smoothing. However enters (1.4) in a parabolic heat equation role whereas enters via the constitutive law (1). The mathematical properties of the MG equation have been determined in various settings of the parameters via an analysis of the Fourier multiplier symbol given by (1.9)-(1.12).
We note that the Fourier multiplier symbols given by (1.9)-(1.12) with are not bounded in all regions of Fourier space [15]. More specifically in “curved” regions where the symbols are unbounded as with for some positive constant . Thus when the relation between and is given by a singular operator of order 1. The implications of this fact for the inviscid MG equation are summarized in the survey article by Friedlander, Rusin and Vicol [11]. In particular, when the inviscid but thermally dissipative MG equation is globally well-possed. In contrast when and , the singular inviscid MG0 equation is ill-possed in the sense of Hadamard in any Sobolev space. In a recent paper [14] Friedlander and Suen examine the limit of vanishing viscosity in the case when . They prove global existence of classical solutions to the forced MGν equations and obtain strong convergence of solutions as the viscosity vanishes. In this present paper we turn to the case where and examine the MGν system, without the benefit of thermal diffusion, both when and in the case where the operator MG0 is singular of order 1. We obtain Gevrey-class local well-posedness and convergence of solutions as . The precise statements of the theorems are given in Section 2 in the context of a general class of non-diffusive active scalar equations that includes the MG equations with .
The second example of a physical system which can be modeled by an active scalar equation where a small smoothing parameter enters into the constitutive law comes from flow in a porous medium. The incompressible porous media Brinkman equation with an “effective viscosity” is derived via a modified Darcy’s Law as suggested by Brinkman [4]. The 2D equation relating the velocity , the density and the pressure is given in non-dimensional form by
[TABLE]
which produces the constitutive law
[TABLE]
where is the vector of Riesz transforms. The 2D components of the Fourier multiplier symbol corresponding to (1) are
[TABLE]
Again there is a dramatic difference in the operator between the two cases and . In the first case the operator is smoothing of order 2 and in the second case the operator is singular of order zero. The IPMB active scalar example is a 2 dimensional nonlinear equation for given by
[TABLE]
coupled with the constitutive law (1).
The well known IPM equations, i.e. (1)-(1.17) without the effective viscosity , have been studied in a number of papers, c.f [6], [7]. As we observed when the operator in (1) is a singular integral operator of order zero. This is also the case for the SQG equations. However the SQG operator is odd where as the IPM operator is even, a property that it shares with the MG operator. Implications for well/ill posedness due to the odd/even structure of the operator in an active scalar equation are explored in [10], [12], [19]. In this present paper we study the system (1)-(1.17) in the limit of vanishing viscosity. We obtain results analogous to those for the MGν system in the limit of vanishing viscosity. The principal difference is that the MG0 operator is singular of order 1 where as the IPM operator is singular of order zero. In the “smoother” IPM case our convergence results are valid in Sobolev spaces rather than the Gevrey-class convergence results for the MG equation.
2. Main Results for a General Class of Active Scalar Equations
We now return to the abstract formulation of our problem in the setting of the following system of active scalar equations parameterized by a “viscosity” parameter .
[TABLE]
where with . We assume that for all . is a sequence of operators111For simplicity, we sometime write T^{0}_{ij}=T_{ij}^{\nu}\Big{|}_{\nu=0} and . which satisfy:
- A1
for any smooth functions for all . 2. A2
are bounded for all . 3. A3
For each , there exists a constant such that for all ,
[TABLE] 4. A4
For each ,
[TABLE]
for all .
Moreover, we further assume that satisfy either one of the following assumption:
- A51
There exists a constant independent of , such that for all ,
[TABLE]
[TABLE] 2. A52
There exists a constant independent of , such that for all ,
[TABLE]
[TABLE]
Here are some remarks regarding the assumptions on :
- •
The assumption A1 implies that is divergence-free for all .
- •
The assumption A3 is needed for obtaining global-in-time wellposedness for (2.3) for the case , which implies that are operators of smoothing order 2 for .
- •
The assumption A52 is stronger than assumption A51. In particular, assumption A52 implies that are operators of zero order.
- •
The assumption A4 is needed for obtaining convergence of solutions as , and is consistent with the one given in [14].
- •
All the assumptions A1–A4 and A51 are consistent with the case for the magnetogeostrophic (MG) equations, while assumptions A1–A4 and A52 are consistent with the case for incompressible porous media Brinkmann (IPMB) equations.
The main results that we prove in this present work are stated in the following theorems:
Theorem 2.1* (Wellposedness in Sobolev space in the case ).*
Let for and be a -smooth source term. Then for each , under the assumptions A1–A3 and A5i for or 2, we have:
- •
if , there exists unique global weak solution to (2.3) such that
[TABLE]
In particular, weakly in as . Here stands for bounded continuous functions.
- •
if , there exists a unique global-in-time solution to (2.3) such that for all . Furthermore, for , we have the following single exponential growth in time on :
[TABLE]
where is a constant which depend only on and the spatial dimension .
Theorem 2.2* (Gevrey-class global wellposedness in the case ).*
Fix . Let and be of Gevrey-class with radius of convergence . Then for each , under the assumptions A1–A3 and A5i for or 2, there exists a unique Gevrey-class solution to (2.3) on with radius of convergence at least for all , where is a decreasing function satisfying
[TABLE]
Here is a constant which depends on but independent of .
Theorem 2.3* (Gevrey-class local wellposedness in the case ).*
Fix , and . Let and be of Gevrey-class with radius of convergence and satisfy
[TABLE]
For , under the assumptions A1–A2 and A51, there exists and a unique Gevrey-class solution to (2.3) defined on with radius of convergence at least . In particular, there exists a constant such that for all ,
[TABLE]
Moreover, if the assumption A3 holds as well, then we have
[TABLE]
where are Gevrey-class solutions to (2.3) for as described in Theorem 2.2.
Theorem 2.4* (Local wellposedness in Sobolev space in the case and Property A52 holds).*
For , we fix . Assume that have zero-mean on . Then for , under the assumption A1–A2 and A52, there exists a and a unique smooth solution to (2.3) such that
[TABLE]
Theorem 2.5* (Convergence of solutions as ).*
Depending on the assumptions A and A, we have the following cases:
- •
Assume that the hypotheses and notations of Theorem 2.3 are in force. Under the assumptions A3–A4, if and are Gevrey-class solutions to (2.3) for and respectively with initial datum on with radius of convergence at least as described in Theorem 2.3, then there exists and such that, for , we have
[TABLE]
- •
Assume that the hypotheses and notations of Theorem 2.4 are in force. Under the assumptions A3–A4, for and and , we have
[TABLE]
3. Preliminaries
We introduce the following notations. We say is a weak solution to (2.3) if they solve the system in the weak sense, that means for all , we have
[TABLE]
is the usual inhomogeneous Sobolev space with norm . For simplicity, we write , , etc. unless otherwise specified. We also write .
We define to be the Log-Lipschitz norm given by
[TABLE]
As in [16], [23], for , the Gevrey-class is given by
[TABLE]
for any , where
[TABLE]
where denotes the radius of convergence and .
We also recall the following facts from the literature (see for example Azzam-Bedrossian [1], Bahouri-Chemin-Danchin [2] and Ziemer [27]): there exists a constant such that
[TABLE]
and for , there are constants such that
[TABLE]
If and , then we have
[TABLE]
4. The non-diffusive active scalar equations
In this section, we study the non-diffusive equations (2.3) for . Depending on the values of , we subdivide it into two cases, namely and .
4.1. The case where
In this subsection we study the non-diffusive equations (2.3) for . First, given and initial datum with , we prove that (2.3) has a unique global-in-time solution .
We begin with the following lemma which gives a priori bounds on .
Lemma 4.1*.*
Let and for and , and let be a -smooth source term. Then we have
[TABLE]
and we also have a priori bounds on
[TABLE]
Here is a constant which depends on and the spatial dimension .
Proof.
The assertion (4.1) follows from standard energy estimates. And for (4.2), we let ’s be the dyadic blocks for . Applying on (2.3),
[TABLE]
where . Since
[TABLE]
with , which implies (4.2). ∎
Proof of Theorem 2.1.
We divide it into several cases.
Case 1*.*
. First, we observe that, by the assumption A3, is a smoothing operator of degree 2 for . Hence with the help of the Fourier multiplier theorem (see Stein [26]), given , there exists some constant such that
[TABLE]
Together with (4.1), for , if and , then we have
[TABLE]
where . Next, using embedding theorems (3.1)-(3.3) and (4.4) for , we have
[TABLE]
and
[TABLE]
which shows that both and are bounded in terms of and . A bound on the Log-Lipschitzian norm of is essential to assure the existence and uniqueness of the flow map, and hence the existence and uniqueness of the solution.
More precisely, to prove the existence of flow map, we consider the standard mollifier , and we set for and . By a standard argument, given , we can obtain a sequence of global smooth solution to (2.3) with . Define to be the flow map given by
[TABLE]
One can show (for example in [3]) that
[TABLE]
where is independent of and , and the norm is given by
[TABLE]
with
[TABLE]
Using (1) (with replaced by ) and (4.8), we obtain
[TABLE]
for all , where are some continuous functions which depends on and . Furthermore, for , using (1) (with replaced by ),
[TABLE]
Applying the estimates (4.9) and (1), we see that the family is bounded and equicontinuous on every compact set in . By Arzela-Ascoli theorem, it implies the existence of a limiting trajectory as . Performing the same analysis for , where is the inverse of , we see that is a Lebesgue measure preserving homeomorphism with
[TABLE]
Define and . The rest of the proof then follows from the one given in [13], which shows that is a weak solution to (2.3).
To show that is unique, let and , and suppose that and solve (2.3) on with . Following the similar argument given in [2], there exists a constant such that for all and , we have
[TABLE]
where . We define
[TABLE]
then by the bounds (4.4) and (1), is well-defined. We let
[TABLE]
Using Theorem 3.28 in [2], for all and ,
[TABLE]
Summing over and taking supremum over , we conclude that on . By repeating the argument a finite number of times, we obtain the uniqueness on the whole interval .
Case 2*.*
. We only need a priori bounds on . In view of (4.2) with , it remains to obtain a bound on . We claim
[TABLE]
We subdivide into two subcases.
Case 2(a): . Define . Then and using the embedding that , we have
[TABLE]
Therefore using (3.4), (4.1) and (4.3) with , we conclude that
[TABLE]
Case 2(b): . Using (4.3), we take , which gives
[TABLE]
On the other hand, we apply (4.1), and the embeddings and to get
[TABLE]
We substitute the above estimates on into (4.2) with and obtain the desired a priori required bounds on , namely
[TABLE]
Finally, the single exponential growth in time on follows readily from (2) and Poincaŕe inequality. We finish the proof of Theorem 2.1.
∎
Remark 4.2*.*
For , if we take , then by the Sobolev embedding theorem (3.5) and the bound (2), we have
[TABLE]
where . Hence Theorem 2.1 implies that there exists a unique global-in-time solution to (2.3) whenever and for and .
Next we study the Gevrey-class solutions to (2.3) for when the initial datum and forcing term are in the same Gevrey-class. Recall that for , there exists a constant such that for all ,
[TABLE]
which gives 2-orders of smoothing
[TABLE]
To prove the global-in-time existence as claimed in Theorem 2.2, we give the estimates of as follows. We take -inner product of (2.3)1 with and obtain
[TABLE]
The following lemma gives the estimates on the term .
Lemma 4.1**.**
For and , we have
[TABLE]
where depends on .
Proof.
The proof is reminiscent of the one given in [23]. Since we have
[TABLE]
which gives
[TABLE]
We make use of the inequality for and the triangle inequality to obtain
[TABLE]
Hence we have
[TABLE]
where we have used the fact that . Using the property (4.13), we have
[TABLE]
Hence there is such that
[TABLE]
which finishes the proof of (4.15). ∎
To complete the proof of Theorem 2.2, we apply (4.15) on (4.1) to obtain
[TABLE]
Choose such that
[TABLE]
then we have
[TABLE]
which gives
[TABLE]
Hence satisfies
[TABLE]
and the proof of Theorem 2.2 is complete.
Remark 4.3*.*
We notice that for the “diffusive” case, i.e. for the following system when :
[TABLE]
one can obtain global-in-time existence of solution Gevrey class with lower bound on that does not vanish as . To see it, we apply the previous analysis on (4.18) to obtain
[TABLE]
Choosing such that
[TABLE]
then we have
[TABLE]
Hence we obtain
[TABLE]
and
[TABLE]
Observe that the lower bound tends to zero as .
4.2. The case where
In this subsection we study the non-diffusive equations (2.3) for . Recall that we consider the following active scalar equation
[TABLE]
where is an operator which satisfies assumptions A1–A2 and either A or A. Based on the assumptions A and A, we consider the following two cases separately:
4.2.1. When A is in force.
Different from the case for , as it was proved in [16], the equation (4.22) is ill-posed in the sense of Hadamard, which means that the solution map associated to the Cauchy problem for (4.22) is not Lipschitz continuous with respect to perturbations in the initial datum around a specific steady profile , in the topology of a certain Sobolev space . Nevertheless, as pointed out in [16], it is possible to obtain the local existence and uniqueness of solutions to (4.22) in spaces of real-analytic functions, owing to the fact that the derivative loss in the nonlinearity is of order at most one (both in and in ).
In the present work, we extend the results of [16] to the case of Gevrey-class solutions. We first state and prove the following proposition which gives the Gevrey-class local wellposedness for (4.22).
Proposition 4.4*.*
Fix and . Let and be of Gevrey-class with radius of convergence and
[TABLE]
where . There exists and a unique Gevrey-class solution on to the initial value problem associated to (4.22).
Proof.
The idea of the proof follows by a similar argument given in [16]. For , we define
[TABLE]
We take -inner product of (4.22) with and obtain
[TABLE]
Write , then it can rewritten as
[TABLE]
Using the assumption A2 that and the fact for and , we have
[TABLE]
where the last inequality follows since . Hence we obtain from (4.24) that
[TABLE]
Let be deceasing and satisfy
[TABLE]
with initial condition , then we have , and from (4.25) that
[TABLE]
as long as . Hence it implies the existence of a Gevrey-class solution on , where the maximal time of existence of the Gevrey-class solution is given by . ∎
Proof of Theorem 2.3.
By choosing and , where , are as defined in Proposition 4.4, if and be of Gevrey-class , both with radius of convergence at least and satisfy (4.23), then there exists a unique Gevrey-class solution to (2.3) for defined on with radius of convergence at least . The time and radius on convergence should only depend on as described in assumption A3, hence they can be chosen independent of and the proof of Proposition 4.4 also applies to (2.3) for . The bounds (2.9)-(2.10) follow immediately from (4.26). ∎
Remark 4.5*.*
By uniqueness, for , the Gevrey-class solution as obtained in Theorem 2.2 coincides with the one as obtained in Theorem 2.3 on .
4.2.2. When A is in force.
Contrary to the previous case, when assumption A is in force, the operator becomes a zero order operator with being bounded. Following the idea given in [11], we show that under the assumptions A1–A2 and A, the equation (4.22) is locally wellposed in Sobolev space for , thereby proving Theorem 2.4.
Before we give the proof of Theorem 2.4, we recall the following proposition from [11]:
Proposition 4.6*.*
Suppose that and . If , then
[TABLE]
where , , and .
Proof of Theorem 2.4.
For simplicity, we denote and by and respectively. We subdivide the proof into 3 steps.
Step 1*.*
We consider the sequence of approximations given by the solutions of
[TABLE]
and
[TABLE]
System (1) can be solved easily and for all , we also have the bound
[TABLE]
where . For the system (1), we consider the linear approximated system
[TABLE]
and the details follow from Theorem A1 in [11]. This shows that there exists a unique solution of (1).
Step 2*.*
Next we show that is bounded. We fix a time (to be chosen later) such that
[TABLE]
Assume that
[TABLE]
for . By A, we have
[TABLE]
for all . Apply on (1) and take inner product with , we obain
[TABLE]
The term can be rewritten as
[TABLE]
Upon integration by parts, the term vanishes since . Using (4.27) for , , , , , , , and applying the assumption A, we have
[TABLE]
Hence we obtain from (4.31) and (2) that
[TABLE]
Applying the bound (4.30) on , we have
[TABLE]
and hence by integrating (4.34) over and choosing small enough, (4.30) also holds for .
Step 3*.*
Finally, we show that is a Cauchy sequence. Denote the difference of and by
[TABLE]
It follows from (1) that satisfies
[TABLE]
where . Apply on (4.35) and take inner product with ,
[TABLE]
The term can be estimated as follows.
[TABLE]
where we used (4.27) for , , , , , , and the assumption A.
On the other hand, using Proposition 2.1 in [11], the term can be estimated by
[TABLE]
Hence we deduce from (4.36) that
[TABLE]
[TABLE]
Integrating (4.38) over and choosing small enough, we obtain
[TABLE]
Thus is Cauchy in with converges strongly to in . Since we assume that , this also implies that the strong convergence occurs in a Hölder space relative to as , hence the limiting function is a solution of (4.22). Uniqueness of follows by the same argument given in [11] and we omit the details. It finishes the proof of Theorem 2.4.
∎
5. Convergence of solutions as
In this section, we address the convergence of solutions to (2.3) as under the assumption A4 and give the proof of Theorem 2.5. Depending on the assumptions A and A, we can address the convergence of solutions in two cases respectively:
- •
As we discussed before, it was proved in [16] that under the assumption A, the equation (2.3) for is ill-posed in the sense of Hadamard over . Hence we focus on the case for Gevrey-class solutions to (2.3). By Theorem 2.3, given Gevrey-class initial datum and forcing , there exists and a unique Gevrey-class solution to (2.3) defined on with radius of convergence at least for all . A natural question is the following: will the Gevrey-class solutions converge as ? The answer is affirmative and is presented in Theorem 2.5, which shows that the Gevrey-class solutions converges to in some Gevrey-class norm as .
- •
On the other hand, when assumption A is in force, by Theorem 2.4, the equation (2.3) for is locally wellposed in Sobolev space for . For sufficiently smooth initial data and forcing term , we aim at showing that as for and . Such result is parallel to the one proved in [14], in which the authors proved that if are smooth classical solutions of the diffusive system (4.18) for and respectively with initial datum and forcing term , then as for and .
Remark 5.1*.*
In the diffusive system (4.18) studied in [14] there is no smoothing assumption imposed on when . The main reason for the difference is that the diffusive term present in (4.18) is sufficient to smooth out the solution for all .
Proof of Theorem 2.5.
We divide the proof into two cases:
Case 1*.*
When A51 is in force. Fix and . Throughout this proof, is a generic constant which depends on , and is independent of . Let be the Gevrey-class solutions to (2.3) on as obtained in Theorem 2.3. We define and write
[TABLE]
Then satisfies the following equation on
[TABLE]
where for all . From (5.1), we have the a priori estimate
[TABLE]
Using Plancherel’s theorem, the nonlinear term can be written as
[TABLE]
The term can be estimated as follows.
[TABLE]
where the last inequality holds since and . Similarly, can be estimated by
[TABLE]
Using the bounds (1) and (5.4) on (1), we obtain
[TABLE]
Choose such that
[TABLE]
then using the bounds (2.9) and (2.10), there exists such that for , we have
[TABLE]
Integrating the above with respect to , for , we obtain
[TABLE]
Since with , it implies , and hence by the assumption A4,
[TABLE]
Therefore the result (2.11) follows.
Case 2*.*
When A52 is in force. Fix , let be the to (2.3) on as obtained in Theorem 2.4. We define , then satisfies (5.1) on .
We first show that, for ,
[TABLE]
Following the proof of Theorem 2.4, shrinking the time if necessary, there exists independent of such that, for all ,
[TABLE]
We multiply (5.1) by and integrate, for ,
[TABLE]
We estimate the right side of (5.7) as follows. Using Sobolev embedding theorem and the bound (5.6),
[TABLE]
We focus on the term as in (2). Using Plancherel Theorem and assumption A, for each ,
[TABLE]
where . Applying the above estimate on (2), we obtain
[TABLE]
For , since , by assumption A4, we have . Hence taking and using Grönwall’s inequality, we conclude that (5.5) holds for .
Finally, we apply the Gagliardo-Nirenberg interpolation inequality and the bound (5.6) to obtain, for ,
[TABLE]
where depends on and is a positive constant which depends on but is independent of . By taking and applying the -convergence (5.5) just proved, we conclude that (2.12) holds for as well.
∎
6. Applications to physical models
We now apply our results claimed in Section 2 to some physical models, namely the magnetogeostrophic (MG) equations and the incompressible porous media (IPMB) equations discussed in Section 1.
6.1. Magnetogeostrophic equations
We first consider the following magnetogeostrophic (MG) equation in the domain with periodic boundary conditions:
[TABLE]
via a Fourier multiplier operator which relates and . More precisely,
[TABLE]
for . The explicit expression for the components of as functions of the Fourier variable are given by (1.9)-(1.12) in Section 1. We write for convenience. To apply the results from Section 2, it suffices to show that the sequence of operators satisfy the assumptions A1–A4 and A given in Section 1. We first prove the following lemma for the MG equations.
Lemma 6.1*.*
For each ,
[TABLE]
Proof.
We only give the details for , since the cases for and are similar. We fix , then for each with , we have
[TABLE]
Hence
[TABLE]
∎
Proposition 6.2*.*
Let , where is given by (1.9)-(1.11). Then satisfy the assumptions A1–A4 and A given in Section 1.
Proof.
The details for the proof can be found in [14] Lemma 5.1–5.2 and from the discussion in ([15], Section 4). For example, to show satisfy the assumption A3, we only give the details for since the cases for and are almost identical. We fix and consider the following cases:
Case 1*.*
. Then for each ,
[TABLE]
Since , so for , in particular . Hence we obtain
[TABLE]
Case 2*.*
. Then for each ,
[TABLE]
Combining two cases, we have
[TABLE]
and hence assumption A3 holds for some independent of , which means that
[TABLE]
On the other hand, to show satisfy the assumption A4, Fix with and we claim that
[TABLE]
Let be given. Then , so there exists such that . Hence for , we have
[TABLE]
where the last inequality follows by the bound (6.5). Using (6.4) in Lemma 6.1 and taking on (6.7),
[TABLE]
Since is arbitrary, (6.6) follows and therefore satisfy the assumption A4.
∎
In view of Proposition 6.2, the abstract Theorem 2.1-2.3 and Theorem 2.5 may therefore be applied to the MG equations (6.3) in order to obtain the wellposedness and convergence of Gevrey-class solutions. More precisely, we have
Theorem 6.3* (Wellposedness in Sobolev space for the MG equations).*
Let for and be a -smooth source term. Then for each , we have:
- •
if , there exists unique global weak solution to (6.3) such that
[TABLE]
In particular, weakly in as .
- •
if , there exists a unique global-in-time solution to (6.3) such that for all . Furthermore, for , we have the following single exponential growth in time on :
[TABLE]
where is a constant which depends only on some dimensional constants.
Theorem 6.4* (Gevrey-class global wellposedness for the MG equations).*
Fix . Let and be of Gevrey-class with radius of convergence . Then for each , there exists a unique Gevrey-class solution to (6.3) on with radius of convergence at least for all , where is a decreasing function satisfying
[TABLE]
Here is a constant which depends on but independent of .
Theorem 6.5* (Gevrey-class local wellposedness for the MG equations).*
Fix , and . Let and be of Gevrey-class with radius of convergence and
[TABLE]
There exists and a unique Gevrey-class solution to (6.3) for defined on with radius of convergence at least . Moreover, there exists a constant independent of such that for all ,
[TABLE]
Here are Gevrey-class solutions to (6.3) for as described in Theorem 6.4.
Theorem 6.6* (Convergence of solutions as for the MG equations).*
Fix , and . Let and be of Gevrey-class with radius of convergence and satisfy the assumptions given in Theorem 6.5. If and are Gevrey-class solutions to (6.3) for and respectively with initial datum on with radius of convergence at least as described in Theorem 6.5, then there exists and such that, for , we have
[TABLE]
6.2. Incompressible porous media equation
Next we study the incompressible porous media Brinkmann (IPMB) equation. Specifically, we address the following active scalar equation in with periodic boundary conditions:
[TABLE]
where the symbol of is given by (1.16) with
[TABLE]
We also write for convenience. To apply the results from Section 2, it suffices to show that the sequence of operators satisfy the assumptions A1–A4 and A given in Section 1.
Proposition 6.7*.*
Let , where is given by (6.11)-(6.12). Then satisfy the assumptions A1–A4 and A52 given in Section 1.
Proof.
It suffices to check that satisfy assumptions A3 and A4. To show that satisfy A3, for each ,
[TABLE]
since . Similarly, . And to see that satisfies A, similar to the case of MG equation, it suffice to show that for each ,
[TABLE]
Fix and for each with , we have
[TABLE]
hence
[TABLE]
By the same argument, we also have and (6.13) follows. ∎
Thanks to Proposition 6.7, the abstract Theorem 2.1-2.5 can be applied to the IPMB equations (6.10). More precisely, we have
Theorem 6.8* (Wellposedness in Sobolev space for the IPMB equations).*
Let for . Then for each , we have:
- •
if , there exists unique global weak solution to (6.3) such that
[TABLE]
In particular, weakly in as .
- •
if , there exists a unique global-in-time solution to (6.3) such that for all . Furthermore, for , we have the following single exponential growth in time on :
[TABLE]
where is a constant which depends only on some dimensional constants.
Theorem 6.9* (Gevrey-class global wellposedness for the IPMB equations).*
Fix . Let be of Gevrey-class with radius of convergence . Then for each , there exists a unique Gevrey-class solution to (6.10) on with radius of convergence at least for all , where is a decreasing function satisfying
[TABLE]
Here is a constant which depends on but independent of .
Theorem 6.10* (Local wellposedness in Sobolev space for the IPMB equations).*
Fix and assume that has zero-mean on . Then there exists a and a unique smooth solution to (6.10) with such that
[TABLE]
Theorem 6.11* (Convergence of solutions as for the IPMB equations).*
Assume that the hypotheses and notations of Theorem 6.10 are in force. For , we have
[TABLE]
Remark 6.12*.*
The results given in Theorem 6.10 are consistent with those discussed in [6]-[7]. Furthermore , the abstract Theorem 2.4 can also be applied to the non-diffusive SQG equation to show local wellposedness in Sobolev spaces [25].
Remark 6.13*.*
In [10], the authors studied the singular incompressible porous media (SIPM) equations set in with periodic boundary conditions, which are given by
[TABLE]
The operator in (6.15) is a pseudodifferential operator of order , in which the Fourier multiplier symbol can be computed explicitly as . It is proved in [10] that when the SIPM equations are ill-posed in Sobolev spaces, however local well-posedness holds for certain patch type weak solutions.
It is straightforward to see that for the case , the system (6.14)-(6.15) satisfies the properties A1–A2 and A51 (by taking ), so the abstract Theorem 2.3 also holds in analogy with those for the MG equations. More specifically, we obtain the following local-in-time Gevrey class existence theorem for the SIPM equations:
Theorem 6.14* (Gevrey-class local wellposedness for the SIPM equations).*
Fix , , and . Let be of Gevrey-class with radius of convergence and satisfies
[TABLE]
There exists and a unique Gevrey-class solution to (6.14)-(6.15) defined on with radius of convergence at least . In particular, there exists a constant such that for all ,
[TABLE]
Acknowledgment
S. Friedlander is supported by NSF DMS-1613135 and A. Suen is supported by Hong Kong Early Career Scheme (ECS) grant project number 28300016.
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