Solutions to a class of forced drift-diffusion equations with applications to the magneto-geostrophic equations
Susan Friedlander, Anthony Suen

TL;DR
This paper establishes the global existence and convergence of solutions for a class of forced drift-diffusion equations, with applications to magneto-geostrophic equations relevant to Earth's core turbulence, and analyzes their long-term behavior.
Contribution
It proves global existence, strong convergence, and attractor properties for solutions to a class of forced drift-diffusion equations, including the magneto-geostrophic model.
Findings
Global existence of classical solutions for the equations.
Strong convergence of solutions as viscosity vanishes.
Existence and upper semicontinuity of global attractors.
Abstract
We prove the global existence of classical solutions to a class of forced drift-diffusion equations with initial data and divergence free drift velocity , and we obtain strong convergence of solutions as the viscosity vanishes. We then apply our results to a family of active scalar equations which includes the three dimensional magneto-geostrophic MG equation that has been proposed by Moffatt in the context of magnetostrophic turbulence in the Earth's fluid core. We prove the existence of a compact global attractor in for the MG equations including the critical equation where . Furthermore, we obtain the upper semicontinuity of the global attractor as vanishes.
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Taxonomy
TopicsNavier-Stokes equation solutions ¡ Stochastic processes and financial applications ¡ Fluid Dynamics and Turbulent Flows
Solutions to a class of forced drift-diffusion equations with applications to the magneto-geostrophic equations
Susan Friedlander
Department of Mathematics
University of Southern California
ââ
Anthony Suen
Department of Mathematics and Information Technology
The Education University of Hong Kong
Abstract.
We prove the global existence of classical solutions to a class of forced drift-diffusion equations with initial data and divergence free drift velocity , and we obtain strong convergence of solutions as the viscosity vanishes. We then apply our results to a family of active scalar equations which includes the three dimensional magneto-geostrophic MG equation that has been proposed by Moffatt in the context of magnetostrophic turbulence in the Earthâs fluid core. We prove the existence of a compact global attractor in for the MGν equations including the critical equation where . Furthermore, we obtain the upper semicontinuity of the global attractor as vanishes.
keywords:
active scalar equations, vanishing viscosity limit, global attractor
1991 Mathematics Subject Classification:
76D03, 35Q35, 76W05
1. Introduction
Our motivation for addressing the limiting behaviour of a class of drift diffusion equations comes from a model proposed by Moffatt and Loper [33], Moffatt [35] for magnetostrophic turbulence in the Earthâs fluid core. This model is derived from the full three dimensional magnetohydrodynamic equations (MHD) in the context of a rapidly rotating, densely stratified, electrically conducting fluid. For discussions about the MHD equations in geophysical contexts see, for example, [1], [4], [17], [28], [34], [36]. Following the notation of Moffatt and Loper [33], we write the equations in terms of dimensionless variables. The orders of magnitude of the resulting non-dimensional parameters are motivated by the physical postulates of their model:
[TABLE]
The unknowns are the velocity, the magnetic field (both vector valued) and the scalar (temperature field of the fluid). is the sum of the fluid and magnetic pressures, and the Cartesian unit vectors are given by and . The physical forces governing this system are the Coriolis force, the Lorentz force and gravity acting via buoyancy, while the equation for the temperature is driven by a smooth function that represents the external forcing of the MHD system.
The non-dimensional parameters in (1.1)-(1.4) are the Rossby number, the magnetic Reynolds number, a (non-dimensional) viscosity and a (non-dimensional) thermal diffusivity. Moffatt and Loper argue that for the geophysical context they are modelling, all these parameters are small, with and being extremely small. We note that the ratio of the Coriolis to Lorentz forces in their model is of order 1, so for notational simplicity we have set this parameter, denoted by in [33], equal to 1. Hence in (1.1)-(1.4) we have a system derived from an important physical problem that is very rich in small parameters. The mathematical properties of this system under various settings of some of the parameters to zero, or in the vanishing limits have been addressed in a sequence of different articles, [19], [21], [22], [23], [24], [25], [26]. Although the physically relevant boundary for a model of the Earthâs fluid core is a spherical annulus, for mathematical tractability these studies have considered the system on the periodic domain , with all fields being mean free, a condition which is preserved by the equations. In this present paper we study the forced system (1.1)-(1.4) under these boundary conditions.
The system as investigated by Moffatt and Loper neglects the terms multiplied by and in comparison with the remaining terms. Essentially this means that the evolution equations (1.1) and (1.2) for the coupled velocity and magnetic vectors take a simplified âquasi-staticâ form. A linear relationship is then established between the vector fields and the scalar temperature . The sole remaining nonlinearity in the system occurs in the evolution equation for given by (1.3). This equation is then an advection-diffusion equation where the constitutive law that relates the divergence free velocity vector and the scalar is obtained from the reduced 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]
We study the forced active scalar equation
[TABLE]
via an examination of the Fourier multiplier symbol of the operator obtained from (1). This active scalar equation is called the magnetogeostrophic (MG) equation. We also refer to (1.11) as the MGν equation when , and to the case when as the MG0 equation. In Section 5, we write the explicit expression for the Fourier multiplier symbol of obtained from (1). We observed that the limit is a highly singular limit: in particular, when the operator is smoothing of degree 2, however when the operator is singular of degree . The goals of the current article are to examine the convergence of solutions to (1.11) in the limit as the viscosity goes to zero and to study the long time behaviour of the forced system.
Friedlander and Vicol [24] analyzed the unforced system (1)-(1.11) with the viscosity parameter set to zero, i.e. the unforced MG0 equation. In this situation the drift diffusion equation (1.11) is critical in the sense of the derivative balance between the advection and the diffusion term. They used De Giorgi techniques to obtain global well-posedness results for the unforced critical MG0 equation in a similar manner to the proof of global well-possedness given by Caffarelli and Vaseur [3] for the critical SQG equation. In Section 3 of this present paper we verify that the technical details of the De Giorgi techniques are, in fact, valid for drift diffusion equations with a smooth force. This procedure leads to the proof of Theorem 1.1, namely the existence of smooth classical solutions to the forced MGν, equations. The existence of uniform bounds on these smooth solutions proved in Section 4 implies convergence of solutions as vanishes which is stated in Theorem 1.2.
The second main result of this current paper concerns the existence of a global attractor for the critical MG0 equation. The issue of the existence of a global attractor for active scalar equations is important in the general context of the long time averages of solutions to forced fluid equations (c.f., [11]). In particular there are recent results concerning the existence of a global attractor for the dynamics of the forced critical SQG equation [8], [10], [12], [13]. In [8], Cheskidov and Dai prove that the forced critical SQG equation possesses a global attractor in provided the force is in , . They use âclassicalâ viscosity solutions and the abstract framework of evolutionary systems introduced by Cheskidov and Foias [6], [9]. We prove an analogous result for the forced three dimensional critical MG0 equation using the concept of a âvanishing viscosityâsolution that arises naturally from the results of Theorem 1.2 concerning the convergence in the âvanishing viscosityâ limit of solutions for the MGν and MG0 equations. Our treatment of the MGν, , equations is novel in the sense that traditionally the existence of a global attractor is obtained from asymptotic compactness. For the MG equations the asymptotic compactness is not known a priori and the existence of the global attractor follows from
- (a)
the energy equality, which implies that the energy cannot grow rapidly (see Proposition 6.4),
- (b)
the absence of anomalous dissipation for complete bounded trajectories.
We note that the suggestion that this strategy might work for various equations was first proposed in [8].
The analysis in [24] of the unforced MG equations was given in the context of a class of drift diffusion equations where the divergence free drift velocity lies in , which class includes the MG0 equation. We follow their approach using De Giorgi techniques to obtain global well-posedness results for a class of forced drift diffusion equations. More specifically, we study the following active scalar equation in with :
[TABLE]
where . Here is a diffusive constant, is the initial condition and is a given smooth function that represents the forcing of the system. is a sequence of operators which satisfy:
- (1.11)
for any smooth functions . 2. (1.12)
are bounded for all . 3. (1.13)
There exists a constant independent of , such that for all ,
[TABLE]
[TABLE]
where T^{0}_{ij}=T_{ij}^{\nu}\Big{|}_{\nu=0}. 4. (1.14)
For each ,
[TABLE]
for all .
The main results that we prove for the forced problem are stated in the following theorems:
Theorem 1.1* (Existence of smooth solutions).*
Let , and be given, and assume that satisfy conditions (1.11)-(1.14). There exists a classical solution of (1.14), evolving from for all .
Theorem 1.2* (Convergence of solutions as ).*
Let , and be given, and assume that satisfy conditions (1.11)-(1.14). If are smooth classical solutions of the system (1.14) for and respectively with initial data , then given , for all , we have
[TABLE]
whenever .
Theorem 1.3* (Existence of a global attractor for the MG equation).*
Let , and be given. The system (1.11) with possesses a compact global attractor in , namely
[TABLE]
For any bounded set , and for any , there exists such that for any , every âvanishing viscosityâ solution with satisfies
[TABLE]
for some complete trajectory on the global attractor .
Furthermore, for , there exists a compact global attractor for (1.11) such that and is upper semicontinuous at , which means that
[TABLE]
Our paper is organised as follows. In Section 2, we give some preliminaries and notations which will be used in later sections. In Section 3, we state and prove Theorem 1.1, namely the existence of a smooth solution to (1.14). In Section 4, we obtain a uniform -bound on smooth solutions to (1.14) and prove Theorem 1.2. In Section 5 we show that the MGν equation with satisfies the general conditions formulated for the active scalar equation in (1.10)-(1.14). Hence Theorem 1.2 can be applied to prove convergence as of solutions of the subcritical MGν equation to solutions of the critical MG0 equation. In Section 6, we introduce the concept of a âvanishing viscosityâ weak solution of the MG0 equation and we prove that the forced critical MG0 equation possesses a compact global attractor in satisfying (1.16).
2. Preliminaries and notations
In this section, we give some preliminaries and notations which are useful in later sections (also refer to [16] for more detailed discussion).
Throughout this paper, we shall denote by for , and similarly for , etc. Also, for any and .
Let be a smooth function valued in such that is supported in the shell . Denote
[TABLE]
where is the dual lattice associated to . For , we define the periodic dyadic blocks as follows:
[TABLE]
For and , the Besov norm for is defined as (summation over repeated indices is understood):
[TABLE]
We also recall the Chemin-Lerner space-time Besov space , with norm given by
[TABLE]
where , and is a time interval.
We will make use of the following well-known embedding theorems in later sections (refer to [2] for more details).
Gagliardo-Nirenberg-Sobolev inequality: Assume that . There exists a constant depending only on and , such that
[TABLE]
for all .
Gagliardo-Nirenberg interpolation inequality: Fix and . Suppose that satisfy
[TABLE]
where is the dimension, then
[TABLE]
where is a constant which depends only on .
Gagliardo-Nirenberg interpolation inequality for Sobolev space: Let and with . There exists a positive dimensional constant such that
[TABLE]
with and .
Besov Embedding Theorem: Let . If and , then
[TABLE]
3. Existence of smooth solutions
In this section, we prove the existence of smooth solutions to the forced non-linear problem (1.14). It can be stated as follows.
Theorem 3.1*.*
Let , and be given, and assume that satisfy conditions (1.11)-(1.14). There exists a classical solution of (1.14), evolving from for all .
The Linear Problem
Theorem 3.1 can be proved by the similar method as given in [24] with modification for the presence of a forcing term in (1.14). Following the proof given in [24], we first consider the linear problem:
[TABLE]
where the velocity vector is given, and . Additionally, let satisfies
[TABLE]
in the sense of distributions. We express as
[TABLE]
and we denoted . The matrix is given, and satisfies
[TABLE]
for all .
We first prove the following proposition for the existence of smooth solutions to (3.1)-(3.4).
Proposition 3.2*.*
Given and , and assume that satisfies (3.4). Let
[TABLE]
be a global weak solution of the initial value problem associated to (3.1)-(3.4). If additionally we have for all and some , then there exists such that .
Remark 3.3*.*
Note that for divergence-free , the existence of a weak solution to (3.1)-(3.4) evolving from is well-known (for example, see [37] where the more general case is discussed, also [3] and references therein). Here is a weak solution to (3.1)-(3.4) in the sense that satisfies (3.1)-(3.4) in a distributional sense, that is, for any ,
[TABLE]
where is the standard -inner product on .
Proof of Proposition 3.2.
In view of Theorem 2.1 in [24], we prove Proposition 3.2 in the following steps. Throughout the proof, we assume for simplicity.
Step 1: A weak solution to (3.1)-(3.4) is bounded for positive time. In other words, there exists a positive constant such that for all ,
[TABLE]
Proof.
It follows by the similar method in proving Lemma 2.3 as in [8]. First, for , we have the energy inequalities
[TABLE]
[TABLE]
And for , we have the following level set energy inequality for the truncated function :
[TABLE]
for all .
Next, we apply De Giorgi iteration method based on (3.9). First we fix and define
[TABLE]
where , , and to be chosen later. Then we have
[TABLE]
where is the characteristic function and
[TABLE]
For the first term on the right side of (3.10), using Gagliardo-Nirenberg inequality (2.2), it can be estimated as follows.
[TABLE]
where , and is a dimensional constant independent of . Similarly, the second term on the right side of (3.10) is bounded by
[TABLE]
Hence we conclude from (3.10) that
[TABLE]
We choose in (3.11) large enough so that
[TABLE]
then the nonlinear iteration inequality (3.11) implies that converges to 0 as .
Hence for almost every . Applying the same procedure to gives a lower bound for . To show that (3.6) holds, we need to estimate the term . Using (3.8), we have
[TABLE]
We combine (3.13) with (3.12) to obtain, for ,
[TABLE]
On the other hand, we fix in (3.14) and shift it by in time for . Since the equation (3.1) is autonomous, we obtain, for ,
[TABLE]
Using the energy inequality (3.7),
[TABLE]
Combining the above with (3.15) and using the fact that for , we obtain, for ,
[TABLE]
Combining (3.14) and (3.16), we conclude that (3.6) holds for . â
Step 2: Next, we show that satisfies the first energy inequality, namely for any and , we have
[TABLE]
where , is a positive constant, and we have denoted for and an arbitrary . Notice that by (3.6), the right side of (3) is finite.
Proof.
We follow the method for proving Lemma 2.6 in [24] and the only difference here comes from the extra forcing term . Fix and let be such that . Define to be a smooth cutoff function such that
in ;
in and in cl;
, ââ, ââ in ,
for some positive constant . Define and let be arbitrary. Multiply (3.1) by and then integrate on to obtain
[TABLE]
From the estimates as shown in [24], it follows from (3) that
[TABLE]
Using the Gagliardo-Nirenberg-Sobolev inequality (2.1) for , the second term on the right side of (3) can be bounded by
[TABLE]
and hence using HĂślderâs inequality, the term can be absorbed by the left side of (3) and hence (3) follows. â
Step 3: We give an estimate on the supremum of on a half cylinder in terms of the supremum on the full cylinder. Assume that , where is arbitrary, then we have
[TABLE]
for some positive constant .
Proof.
To facilitate the proof, we first introduce the following notations:
,
,
Let and . By the definitions of and , we have
[TABLE]
Following the proof of Lemma 2.10 in [24], using (3.21) and the first energy inequality (3) as proved in Step 2, we have
[TABLE]
By combining (3.21) and (3), we obtain
[TABLE]
We now apply the De Giorgi iteration method based on (3). Let , , and , for all , where and are as given and is to be chosen later. By letting , , , and in (3), we have
[TABLE]
We let and choose large enough so that
[TABLE]
then by induction, we obtain from (3.24) that for all . The rest follows from the argument given in [24] and we omit the details here. â
Step 4: We have the following second energy inequality in controlling the possible growth of level sets of the solution: fix an arbitrary , let , , and . Then we have
[TABLE]
where is a sufficiently large positive constant. Notice that by (3.6), the right side of (3.25) is finite.
Proof.
Similar to the first energy inequality, we follow the method for proving Lemma 2.11 in [24] and the only difference here comes from the forcing term . Given , we define to be a smooth cutoff function such that
;
on and on ;
\displaystyle|\nabla\eta(x)|\leq\min\Big{\{}\frac{C}{R-r},\frac{CR}{(R-r)^{2}}\|(\theta-h)_{+}\|_{L^{\infty}((t_{1},t_{2})\times B_{R})}\Big{\}} for all ,
for some positive constant . Multiply (3.1) by and integrate on , it follows from the estimates given in [24] that
[TABLE]
where is a positive constant. Using the Gagliardo-Nirenberg-Sobolev inequality (2.1) for , we bound the far right side of the above as follows.
[TABLE]
By using (3) on (3), we can choose sufficiently large enough so that (3.25) holds. â
Step 5: Using the second energy inequality (3.25), we can bound whenever . Fix , let be the least integer such that , and let where is the constant from (3.25). For , if
[TABLE]
then for all we have
[TABLE]
where we define , âââ, âââ, âââ and
.
Proof.
By using (3.25), the proof of (3.28) follows by the same argument given by the proof of Lemma 2.12 in [24] and we omit the details here. â
Step 6: Applying Step 1 to Step 5, the proof of Proposition 3.2 now follows by showing that there exists independent of , such that
[TABLE]
where , and . Here are defined as in Step 5, and we recall that and are arbitrary. We refer the reader to ([24], pp. 293â294) for details in proving (3.29). The estimate (3.29) implies the HĂślder regularity of the solution (the HĂślder exponent may be calculated explicitly from ) which finishes the proof of Proposition 3.2. â
The Nonlinear Problem
We now focus back on the non-linear problem (1.14) and give the proof of Theorem 3.1.
Proof of Theorem 3.1.
To begin with, we notice that given and , there exists a global-in-time Leray-Hopf weak solution of (1.14) evolving from (a proof for it can be found in [24]). Using the same method as in proving (3.6), we have and it follows from the Calder n-Zygmund theory of singular integrals that , for any and , where . Therefore, we may treat (1.14) as a linear evolution equation (see also [3], [15], [24]), where the divergence-free velocity field is given, and , for any . This is precisely the setting of Proposition 3.2 for the linear evolution equation and it can be applied to the nonlinear problem (1.14) to give HĂślder regularity of the solution. Finally, since HĂślder regularity is sub-critical for the natural scaling of (1.14), one may bootstrap to prove that the solution is in a higher regularity class. We refer to [24] for further details and conclude the proof of Theorem 3.1. â
4. Uniform bounds on smooth solutions and proof of Theorem 1.2
4.1. Uniform bounds on smooth solutions
We have the following uniform -bound on smooth solutions to (1.14) which will be used in proving Theorem 1.2.
Theorem 4.1*.*
Assume that the hypotheses and notations of Theorem 3.1 are in force. Then given and , there exists a positive constant independent of such that
[TABLE]
where is the constant as stated in condition (1.13).
Proof of Theorem 4.1.
Fix for some . By Theorem 3.1, there exists such that for each ,
[TABLE]
Depending on the value of , we consider the following 2 cases:
Case 1: . The proof is based on the one given in [26] and we just need to take extra care of the forcing term . It is given in the following steps:
Step (i): Assume further that
[TABLE]
for some , then we have
[TABLE]
for all , and for all , where .
Proof.
Let be as defined in Section 2. We apply to (1.14), multiply by , integrate over , and use Proposition 29.1 in [31] (also refer to [5]) to obtain, for ,
[TABLE]
where is a positive constant independent of . Using HĂślder inequality, the second term on the right side of (4.5) is bounded by . Hence applying the similar estimates given in the proof of Lemma 2 in [26] pp. 259â261, we obtain
[TABLE]
where is a positive constant independent of and is defined in condition (1.13). Applying GrĂśnwallâs inequality on (4.1),
[TABLE]
where
[TABLE]
We take the norm of (4.1) and apply the similar estimates given in [26] pp. 260â261 to obtain
[TABLE]
Multiply the above on both sides by and take an -norm,
[TABLE]
Since , the two norms on the right side of the above estimate are finite for any . On the other hand, the last term on the right side of (4.1) can be bounded by . Hence we have which finishes the proof of (4.4). â
Step (ii): Assume that satisfies (4.2), we then have
[TABLE]
Proof.
We follow the proof of Lemma 3 in [26] pp. 262â263. First, we note that , so we may apply Step (i) with and obtain that for any . Since , we may bootstrap and apply Step (i) once more to obtain that for all . For any fixed , we have and hence as . By iterating Step (i) finitely many times, we obtain
[TABLE]
Fix large enough (which will be explicitly chosen later), and let . From the estimate (4.1), for any ,
[TABLE]
Choose
[TABLE]
then for all . By taking the norm of (4.1) and using Besov embedding theorem (2.4), we have
[TABLE]
We pick so that , then we obtain from (4.13) that
[TABLE]
Lastly, from condition (4.2), we have , hence (4.10) follows from the the borderline Sobolev embedding theorem that . â
Using the results obtained from Step (i) and Step (ii) as described above, we are ready to prove the bound (4.2) for . First, by using (4.10), we have
[TABLE]
where is a positive constant independent of . Next, by the condition (1.2), is divergence free and we have the a priori estimate derived from (1.14) that
[TABLE]
By absorbing the term on the left side of (4.15) and using the bound (4.14), we obtain, for all ,
[TABLE]
Since and functions are finite a.e., is finite for a.e. , with bounds in terms of but independent of . Hence (4.16) implies with
[TABLE]
By further taking derivatives of the equation (1.14) and repeating the above argument, (4.1) also holds for all and we finish the proof of (4.1) for .
Case 2: . We adopt the method given in [26] pp. 257â258. Similar to Case 1, the goal is to prove that (4.10) holds for . Once (4.10) is proved, same argument given in the previous case can then be applied which gives the bound (4.1). First, note that if satisfies (4.2), then , where and is fixed and to be chosen later. Then, for fixed, we have
[TABLE]
Using the Bony paraproduct decomposition and the method given in [26], the first term on the right side of (4.17) can be bounded by , where is a constant which may depend on as in condition (1.13) but independent of . On the other hand, the term can be bounded by . By applying the bounds on (4.17), using GrĂśwall inequality and the Besov embedding theorem (2.4), we obtain
[TABLE]
for all . Choose , then . Since , we conclude that (4.10) holds for and we finish the proof of (4.1) for . â
4.2. Proof of Theorem 1.2
The proof can be divided into two cases:
Case 1: . Let , then satisfies the following equation:
[TABLE]
Multiply (4.18) by and integrate,
[TABLE]
We estimate the right side of (4.19) as follows. For each ,
[TABLE]
where is the constant as stated in condition (1.13). We focus on the term as in (4.20), and for simplicity we sometime drop the variable . Using Plancherel Theorem, for each ,
[TABLE]
Using the condition (1.13), the term can be estimated by
[TABLE]
For the term , by Theorem 3.1, is smooth and . So the condition (1.4) can be applied and we have
[TABLE]
We apply (4.22) on (4.21) to obtain
[TABLE]
and hence using (4.24) on (4.20),
[TABLE]
Applying (4.25) on (4.19), using GrĂśnwallâs inequality, taking and using (4.23), for all , we conclude that
[TABLE]
Case 2: . We apply the Gagliardo-Nirenberg interpolation inequality for homogeneous Sobolev space (2.3) to obtain, for and ,
[TABLE]
where depends on , and is a positive constant which depends on but is independent of . Using the bounds (4.1) as in Theorem 4.1, the term is bounded uniformly in for all . Hence by taking and applying the convergence (4.26), we have
[TABLE]
which finishes the proof of Theorem 1.2.
5. The MG Equations
5.1. The explicit symbol of the MG operator
We now return to the magnetogeostrophic active scalar equation discussed in the introduction. Specifically, we are interested in the following active scalar 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 obtained from the constitutive law (1) to give
[TABLE]
where
[TABLE]
Here and are some diffusive constants, is the initial condition, and is a given smooth function that represents the forcing of the system. Furthermore, we restrict the system (5.3) to the function spaces where all functions (including the forcing and initial data ) have zero mean with respect to (refer to section 4 of [24] for further discussion of this restriction).
Details of the singular behaviour of the Fourier multiplier symbols for the operator in certain regions of Fourier space are given in [24]. More general issues concerning the ill-posedness and well-posedness of the unforced MG0 equation can be found in [21], [24], [25]. In particular, it is to be noted that the MG0 with is the so-called critical MG equation in the sense of the delicate balance between the nonlinear term and the dissipative term. Various critical active scalar equations such as surface quasi-geostrophic equation (SQG) have received considerable attention in the past decade because of the challenging nature of this delicate balance, [3], [13], [14], [15], [18], [20], [29], [30]. On the other hand, as we discussed in [23], the MGν equation with , where the symbol decays like , is a case where the dissipative term dominates the nonlinear term. In [23] it is shown that in the case of the MGν equation with and , even for singular initial data, the global solution is instantaneously -smoothed and satisfied classically for all . With this dichotomy in mind, we seek to determine the long time behaviour of the forced critical MG0 equation through the âvanishing viscosityâ limit of the MGν equation.
5.2. The MG equations in the class of drift-diffusion equations
We will now show that the MGν, , equations satisfy the conditions of the general class of drift diffusion equations given by (1.11)-(1.14). We write
[TABLE]
where we have denoted
[TABLE]
In order to show that conditions (1.11)-(1.14) are satisfied, we need the following lemmas for :
Lemma 5.1*.*
Let be as defined in (5.8)-(5.9) in terms of and . There are constants independent of such that, for all ,
[TABLE]
[TABLE]
Proof.
The bound (5.11) follows from the discussion in ([24], Section 4) and we omit the proof.
To show the bound (5.10), we only give the details for since the cases for and are almost identical.
To prove (5.10), 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 (5.10) holds for some independent of . â
Lemma 5.2*.*
For each ,
[TABLE]
Proof.
Again we only give the details for . We fix , then for each with , we have
[TABLE]
Hence
[TABLE]
â
Lemma 5.3*.*
Let be a function such that . Then we have
[TABLE]
Proof.
Fix with and let be given. Then , so there exists such that . Hence
[TABLE]
Using Lemma 5.2 and taking on (5.14),
[TABLE]
Since is arbitrary, (5.13) follows. â
In view of Lemma 5.1â5.3, the sequence of operators given by (5.8)-(5.9) satisfy the conditions (1.11) and (1.13)-(1.14). Moreover, following the discussion given in [24] pp. 298â299, also satisfy (1.12). By Theorem 3.1 and Theorem 4.1, there exists classical solutions of (5.3)-(5.7), evolving from which satisfy the uniform bounds (4.1). The abstract Theorem 1.1 and Theorem 1.2 may therefore be applied to the MG equations in order to obtain the convergence of smooth solutions, and hence we have proven:
Theorem 5.4*.*
Let , and be given. There exists a classical solution of (5.3)-(5.7), evolving from for all .
Theorem 5.5*.*
Let , and be given. Then if are smooth classical solutions of (5.3)-(5.7) for and respectively with initial data , then given , for all , we have
[TABLE]
whenever .
6. The Existence of a Global Attractor
With the results of Theorems 5.4 and 5.5 in place, we define a weak solution to the MG0 equation which we call a âvanishing viscosityâsolution. We use this concept to prove the existence of a compact global attractor in for the MGν equations (5.3)-(5.7) including the critical equation where . We further obtain the upper semicontinuity of the global attractor as vanishes. First, we define a class of solutions to (1.14) as follows.
Definition 6.1*.*
A weak solution to (5.3)-(5.7) with is a function with zero spatial mean that satisfies (5.3) in a distributional sense. That is, for any ,
[TABLE]
where u=u\Big{|}_{\nu=0}. A weak solution to (5.3) on with is called a âvanishing viscosityâsolution if there exist sequences and such that are smooth solutions to (5.3) as given by Theorem 3.1 and in as .
Remark 6.2*.*
By Theorem 5.4 and Theorem 5.5, for any initial data , there exists a âvanishing viscosityâ solution of (1.14) on with .
We prove that the equation (5.3) driven by a force possesses a compact global attractor in which is upper semicontinuous at . More precisely, we have
Theorem 6.3*.*
Assume . Then the system (5.3)-(5.7) with possesses a compact global attractor in , namely
[TABLE]
For any bounded set , and for any , there exists such that for any , every âvanishing viscosityâ solution with satisfies
[TABLE]
for some complete trajectory on the global attractor . Furthermore, for , there exists a compact global attractor for (5.3) such that and is upper semicontinuous at , which means that
[TABLE]
Before we give the proof of Theorem 6.3, we state the following proposition. It gives an energy equality which is important in obtaining an absorbing ball for (5.3) (see Remark 6.6 below).
Proposition 6.4* (The energy equality).*
Let be a âvanishing viscosityâ solution of (5.3) on with . Then satisfies the following energy equality:
[TABLE]
for all .
Proof.
It suffices to show that the flux term equals zero; for which a proof can be found in [8] and we omit the details. The proof uses techniques of Littlewood-Paley decomposition. It is analogous to the proof given in [7] that the energy flux is zero for weak solutions of the three dimensional Euler equation that are smoother than Onsager critical. â
Remark 6.5*.*
Based on the equality (6.2), we can see that every âvanishing viscosityâ solution to (5.3) is strongly continuous in .
Remark 6.6*.*
Moreover, in view of (6.2), there exists an absorbing ball for (5.3) given by
[TABLE]
where is any number larger than . Then for any bounded set , there exists a time such that
[TABLE]
for every âvanishing viscosityâ solution with the initial data .
To facilitate the proof of Theorem 6.3, we introduce the following notions:
We denote the strong and weak distances on respectively by
[TABLE]
where and are the Fourier coefficients of and .
We let
[TABLE]
and for each , let denote the set of all -valued functions on (here is the absorbing ball given by (6.3) in Remark 6.6).
We define as the map , where is the solution to (5.3)-(5.7) given by Theorem 5.4.
We first prove the following lemma which gives the continuity of in for a given . More precisely, we have:
Lemma 6.7*.*
For , is continuous in , uniformly for in compact subsets of .
Proof.
We let be a compact subset of and fix . Let , then for each , we have
[TABLE]
where for . We follow the argument given in the proof of Theorem 1.2 to obtain
[TABLE]
Using the bound (4.1) for , the second term on the right side of (6.5) is bounded by
, for some constant independent of but depends on the compact set and . On the other hand, the term can be bounded as follows.
[TABLE]
where are defined in (5.9). Using the bound (4.1) for again and applying the similar argument given in the proof of Lemma 5.1 and Lemma 5.2, there exists constant such that
[TABLE]
Hence we conclude from (6.4) that
[TABLE]
Integrating the above over and using GrĂśnwallâs inequality, it further implies
[TABLE]
hence we prove the continuity of in uniformly for in . â
Next, the following lemma shows that the weak upper semicontinuity implies the strong upper semicontinuity.
Lemma 6.8*.*
Let and be such that
[TABLE]
for some sequence . Then
[TABLE]
Proof.
Assume the conclusion of the lemma does not hold. Then passing to a subsequence and dropping a subindex, we can assume that
[TABLE]
There are solutions (with and respectively) which are complete bounded in such that and .
Due to the energy equality (6.2) and the fact that the radius of the absorbing ball does not depend on , there exists a constant independent of such that
[TABLE]
for all . This implies there exists a sequence such that
[TABLE]
Since the interval is compact, passing to a subsequence and dropping a subindex, we can assume that for some . And using (6.8), by compactness, we can pass to another subsequence and drop a subindex to obtain
[TABLE]
for some .
For , we consider solutions and with and . Note that we have in as . Following a similar proof of (6), there exists a constant independent of such that
[TABLE]
Similarly, we also have
[TABLE]
So we have shown that there is a sequence such that
[TABLE]
Hence and we have as , which contradicts (6.7). â
We are now ready to prove Theorem 6.3.
Proof of Theorem 6.3.
We define
[TABLE]
[TABLE]
then is an evolutionary system (see [6] and [8] for the definition), so by Theorem 4.5 in [8], there exists a weak global attractor to with
[TABLE]
Furthermore, by the Aubin-Lions Lemma (also refer to [11] for the case of Navier-Stokes equation), if is any sequence of âvanishing viscosityâ solutions of (1.14) such that for all , then there exists a subsequence of that converges in to some âvanishing viscosityâ solution (here refers to the metric space ). Applying the arguments given in [8], satisfies all the following properties:
- A1
is a compact set in ( is endowed with the weak topology induced by );
- A2
for any , there exists such that for every and ,
[TABLE]
for a.e. in ;
- A3
if and in for some , then strongly a.e. in .
Therefore, together with Remark 6.6, Theorem 4.5 in [8] can then be applied again to our evolutionary system , which implies that
- â˘
the strong global attractor exists, it is strongly compact and ; and
- â˘
for any bounded set , and for any , there exists such that for any , every âvanishing viscosityâ solution
[TABLE]
for some complete trajectory on the global attractor .
Finally, to prove that (6.1) holds, we recall that is the map , where is the solution to (5.3)-(5.7) given by Theorem 5.4. Then for each , is a semigroup on . And using the above argument, there exists a compact global attractor for given by
[TABLE]
Moreover, for , is the global attractor for satisfying
for all ;
for any bounded set , as .
We claim that the following conditions hold:
- L1
has a global attractor for every in the weak- sense, which means that
for all ;
for any bounded set , as .
- L2
there is a compact subset of in the weak topology induced by such that for every .
- L3
for , is continuous in , uniformly for in compact subsets of .
Notice that Lemma 6.7 implies L3, so we only have to show L1 and L2:
To show L1, we note that the absorbing ball as given by (6.3) has radius which is independent of , hence has a global attractor for every satisfying L1.
To show L2, using A1, we have that is a compact set in , where refers to the metric space endowed with the weak topology induced by . Hence we take and for every .
In view of L1 to L3, the result from [27] implies the weak upper semicontinuity, namely
[TABLE]
Hence using Lemma 6.8, (6.10) further implies the strong upper semicontinuity given by (6.1). This completes the proof of Theorem 6.3. â
Acknowledgment
We thank Vlad Vicol for his very helpful advice. We also thank the referees for their most valuable comments. A.S. is partially supported by Hong Kong Early Career Scheme (ECS) grant project number 28300016. S.F. is partially supported by NSF grant DMS-1613135.
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