Global strong solutions to 3-D Navier-Stokes system with strong dissipation in one direction
Marius Paicu, Ping Zhang

TL;DR
This paper proves the global existence of strong solutions for the 3-D Navier-Stokes equations with anisotropic dissipation, under conditions where vertical or horizontal viscosity is sufficiently large relative to initial data.
Contribution
It establishes global well-posedness for 3-D Navier-Stokes with anisotropic viscosity, considering different viscous coefficients in vertical and horizontal directions.
Findings
Global strong solutions exist when vertical or horizontal viscosity is large enough.
Anisotropic smallness condition on initial data ensures well-posedness.
Results extend understanding of Navier-Stokes with directional dissipation.
Abstract
We consider three dimensional incompressible Navier-Stokes equation with different viscous coefficient in the vertical and horizontal variables. In particular, when one of these viscous coefficients is large enough compared to the initial data, we prove the global well-posedness of this system. In fact, we obtain the existence of a global strong solution to when the initial data verify an anisotropic smallness condition which takes into account the different roles of the horizontal and vertical viscosity.
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Taxonomy
TopicsNavier-Stokes equation solutions · Advanced Mathematical Physics Problems · Stability and Controllability of Differential Equations
Global strong solutions to 3-D Navier-Stokes system with
strong dissipation in one direction
Marius Paicu
Université Bordeaux 1
Institut de Mathématiques de Bordeaux
F-33405 Talence Cedex, France
and
Ping Zhang
Academy of Mathematics Systems Science and Hua Loo-Keng Key Laboratory of Mathematics, The Chinese Academy of Sciences, Beijing 100190, CHINA, and School of Mathematical Sciences, University of Chinese Academy of Sciences, Beijing 100049, CHINA.
Abstract.
We consider three dimensional incompressible Navier-Stokes equation with different viscous coefficient in the vertical and horizontal variables. In particular, when one of these viscous coefficients is large enough compared to the initial data, we prove the global well-posedness of this system. In fact, we obtain the existence of a global strong solution to when the initial data verify an anisotropic smallness condition which takes into account the different roles of the horizontal and vertical viscosity.
1. Introduction
In this paper, we consider 3-D anisotropic incompressible Navier-Stokes system with different vertical and horizontal viscosity. Our goal is to study the role of a large viscous coefficient in one direction that plays in obtaining the global existence of strong solutions to Navier-Stokes system. Let us recall Navier-Stokes equations which describes the evolution of viscous fluid in
[TABLE]
where designates the horizontal Laplacian, and are respectively the horizontal and the vertical viscous coefficients, denotes the fluid velocity, and the scalar pressure function, which guarantees the divergence free condition of the velocity field.
When (1.1) is exactly the classical Navier-Stokes system. In the sequel, we shall always denote this system by Whereas when and reduces to the anisotropic Navier-Stokes system arising from geophysical fluid mechanics (see [7]). We remark that Navier-Stokes system with large vertical viscosity is a usual model to study the evolution of the fluid in a thin domain in the vertical direction (see (2.4) of [21] for instance).
We begin by recalling some important and classical results about Navier-Stokes system. Especially, we shall focus on the conditions which guarantee the global existence of strong solution to
The first important result about the classical Navier-Stokes system was obtained by Leray in the seminar paper [16] in 1933. He proved that given an arbitrary finite energy solenoidal vector field, has a global in time weak solution which verifies the energy inequality. This solution is unique and regular for positive time in but unfortunately the uniqueness and regularities of such solution in three space dimension is still one of most challenging open questions in the field of mathematical fluid mechanics. Fujita-Kato [12] gave a partial answer to the construction of global unique solution to . Indeed, the theorem of Fujita-Kato [12] allows to construct local in time unique solution to (1.1) with initial data in the homogeneous Sobolev spaces , or in the Lebsegue space (see [14]). Moreover, if the initial data is small enough compared to the the viscosity, that is, , for some sufficiently small constant then the strong solution exists globally in time.
The above result was extended by Cannone, Meyer and Planchon [5] for initial data in Besov spaces with negative index. More precisely, they proved that if the initial data belongs to the Besov space, for some and its norm is sufficiently small compared to the viscosity, then has a unique global solution. The typical example of such kind of initial data reads
[TABLE]
where and . We remark that this type of initial data is not small in either or
The end-point result in this direction is given by Koch and Tataru [15]. They proved that given initial data in the derivatives of BMO space and its norm is sufficiently small compared to the viscosity, then has a unique global solution (one may check [22] for the regularities of such solutions). We remark that for , there holds
[TABLE]
and the norms to the above spaces are sclaing-invariant under the following scaling transformation
[TABLE]
We notice that for any solution of on determined by (1.2) is also a solution of on We point out that the largest space, which belongs to and the norm of which is scaling invariant under (1.2), is . Moreover, Bourgain and Pavlović [4] proved that is actually ill-posed with initial data in
We mention some examples of large initial data which generate unique global solution to . First of all, Raugel and Sell [21] obtained the global well-posedness of in a thin enough domain. This result was extended by Gallagher [13] that has a unique global periodic solution provided that the initial data can be split as , where is a bi-dimensional solenoidal vector field in and which satisfy
[TABLE]
for some being sufficiently small.
In 2006, Chemin and Gallagher [8] constructed the following example of initial data which generates a unique global solution to , and which is large in and is strongly oscillatory in one direction,
[TABLE]
where .
The other interesting class of large initial data which generate unique global solutions to is the so-called slowly varying data,
[TABLE]
which was introduced by Chemin and Gallagher in [9] (see also [10, 11]).
On the other hand, by crucially using the fact that Zhang [23] and the authors [20] improved Fujita-Kato’s result by requiring only two components of the initial velocity being sufficiently small in some critical Besov space even when and in (1.1).
Liu and the second author [17] first investigated the global well-podesness of (1.1) with and being sufficiently large. In particular, they proved the following result:
Theorem 1.1**.**
Let satisfy and Then there exists some universal positive constant such that if
[TABLE]
(1.1) has a unique global solution u\in C\bigl{(}[0,\infty[,H^{\frac{1}{2}}({\mathop{\mathbb{R}\kern 0.0pt}\nolimits}^{3})\bigr{)}\bigcap L^{2}_{\rm{loc}}\bigl{(}{\mathop{\mathbb{R}\kern 0.0pt}\nolimits}^{+};H^{\frac{3}{2}}({\mathop{\mathbb{R}\kern 0.0pt}\nolimits}^{3})\bigr{)} so that for any
[TABLE]
where
Our goal in this paper is to study the role of one big viscosity that plays in obtaining global existence of strong solutions to (1.1) even the viscous coefficients in other variables are small. One of the consequence of our result below (see Theorem 1.2) ensures that given regular initial data if the horizontal viscosity in (1.1) is small like and the vertical one is big enough like for some large enough constant then (1.1) has a unique global solution. This case is obviously not covered by Theorem 1.1. Furthermore, here we allow the initial data to have a large and slowly varying part.
The main result of this paper states as follows:
Theorem 1.2**.**
Let be a solenoidal vector field and be a horizontal solenoidal vector field in for some We also assume that and belongs to Then for any there exists a positive constant which depends on the norms of above, such that if and is so large that
[TABLE]
for some sufficiently small, the initial data
[TABLE]
generates a unique global solution to (1.1) in the space with . **
The definitions of the Besov norms will be presented in Section 3. The exact form of the constant will be given by (5.9).
Remark 1.1**.**
- (1)
We remark that the norms of in both and are scaling invariant under the scaling transformation (1.2).
- (2)
Similar result holds for (1.1) in a regular bounded domain with Dirichlet boundary condition for the velocity field. Indeed the first eigenvalue of the operator, , is bigger than . On the other hand, Avrin **[1]** proved that as long as (1.1) has a unique global solution.
- (3)
Let us note that in the periodic case if the vertical viscosity, in (1.1) is big enough, the spectrum of the Laplace on functions with null vertical mean is pushed far from zero, which ensures the exponential decay of the linear solution. So that in order to prove the global well-posedness of (1.1) in we need first to decompose the solution into a 2D part and a 3D part with vertical null mean, and then to obtain that the interactions between the 2D part and the 3D part are small. We shall not present detail here.
In the case when in (1.1), that is
[TABLE]
where we have the following global well-posedness result for (1.7):
Theorem 1.3**.**
Given solenoidal vector field there exists a small enough positive constant so that if
[TABLE]
(1.7) has a unique solution with **
We remark that the boundary condition in (1.7) is quite natural, which corresponds to the Dirichlet boundary condition for 1-D heat equation in a bounded interval. So far, we still do not know how to prove similar version of Theorem 1.3 in the whole space case.
Let us complete this section by the notations in this context.
Let be two operators, we denote the commutator between and . For , we mean that there is a uniform constant which may be different on different lines, such that . We denote by the inner product of and will be a generic element of so that . For a Banach space and an interval of we denote by the set of continuous functions on with values in and by the subset of bounded functions of For the notation stands for the set of measurable functions on with values in such that belongs to
2. Ideas of the proof and structure of the paper
In what follows, we shall always denote
[TABLE]
In order to deal with which appears in (1.6), motivated by [9, 11], we construct through
[TABLE]
By taking to the momentum equation of (2.1), we find
[TABLE]
To handle in (1.6), we construct via
[TABLE]
Then the strategy to the proof of Theorem 1.2 will be as follows: we first write
[TABLE]
It follows form (1.1), (2.1) and (2.3) that verifies
[TABLE]
We are going to prove that (2.5) has a unique global solution under the smallness condition (1.5).
In order to exploring the main idea to the proof of Theorem 1.2. Let us first assume in (1.6). Moreover, to avoid technicality, we assume Then we have the following simplified version of Theorem 1.2.
Theorem 2.1**.**
Let be a solenoidal vector field, we denote
[TABLE]
We assume that Then there exist two positive constants so that if
[TABLE]
(1.1) with initial data has a unique global solution with
[TABLE]
Here denotes the space of functions with both and belonging to **
We begin the proof of the above theorem by the following useful lemmas.
Lemma 2.1**.**
Let be a solenoidal vector field in with belonging to . Let with . Then one has
[TABLE]
Proof.
We recall that \|a\|_{H^{0,1}}=\bigl{(}\|a\|_{L^{2}}^{2}+\|\partial_{3}a\|_{L^{2}}^{2}\bigr{)}^{\frac{1}{2}}. It is easy to observe that due to \bigl{(}a\cdot\nabla b|b\bigr{)}_{L^{2}}=0, so that there holds
[TABLE]
Notice that
[TABLE]
and , we deduce from the law of product in Sobolev spaces that
[TABLE]
On the other hand, we write
[TABLE]
Integrating the above equality over and using Hölder’s inequality, we achieve
[TABLE]
As a result, it comes out
[TABLE]
Whereas observing that
[TABLE]
which together with (2.8) ensures the lemma.
The next lemma is concerned with the linear equation (2.3), which tells us the small quantities that will be used in what follows.
Lemma 2.2**.**
Let with . Let be the corresponding solution of (2.3). Then we have
[TABLE]
Proof.
Indeed by applying standard energy method to (2.3), we get
[TABLE]
which implies the lemma.
Lemma 2.3**.**
Let be given by (2.6). Then under the assumptions of Lemma 2.2 and one has
[TABLE]
Proof.
We begin by writing that
[TABLE]
Applying Lemma 2.2 and maximal principle for (2.3) gives
[TABLE]
To handle the other term in (2.9), by applying the Sobolev imbedding of we obtain
[TABLE]
which together with Lemma 2.2 implies that
[TABLE]
Whereas noticing from Sobolev imbedding Theorem that , we write
[TABLE]
Taking the norm leads to
[TABLE]
which together with Lemma 2.2 ensures that
[TABLE]
This gives rise to
[TABLE]
Along with (2.9) and (2.10), we complete the proof of the lemma.
Proof of the Theorem 2.1.
Let be determined by (2.3). We write
[TABLE]
Inserting the above substitution into (1.1) yields
[TABLE]
It follows from classical theory on Navier-Stokes system that (2.11) has a unique solution with for some maximal existing time In the following, we are going to prove that under the smallness condition (2.7). For simplicity, we just present the a priori estimate.
By taking scalar product of the equation of (2.11) with we obtain
[TABLE]
Applying Lemma 2.1 gives
[TABLE]
and
[TABLE]
Then by applying Young’s inequality, we achieve
[TABLE]
Similarly, notice that we get
[TABLE]
For the last term in (2.11), we first get, by using integrating by parts, that
[TABLE]
which implies
[TABLE]
Let us denote
[TABLE]
We are going to prove that Otherwise by substituting the above estimates into (2.12), for we arrive at
[TABLE]
Applying Gronwall’s inequality to (2.14) yields
[TABLE]
from which, Lemmas 2.2 and 2.3, for we infer
[TABLE]
Then under the smallness condition (2.7), we have
[TABLE]
which contradicts with (2.13). This in turn shows that Furthermore inserting the estimate (2.15) into (2.14) shows that This completes the proof of Theorem 2.1.
The organization of this paper is as follows:
In the third section, we shall recall some basic facts on Littlewood-Paley theory;
In the fourth section, we present the priori estimates for smooth enough solutions of (2.1) and (2.3);
In the fifth section, we prove Theorem 1.2;
In the sixth section, we present the proof of Theorem 1.3;
Finally in the Appendix, we present the proofs of several technical lemmas which have been used in the proof of Theorem 1.2.
3. Basics on Littlewood-Paley theory
Before we present the function spaces we are going to work with in this context, let us briefly recall some basic facts on Littlewood-Paley theory (see e.g. [2]). Let and be smooth functions supported in and respectively such that
[TABLE]
For we set
[TABLE]
where and denote the Fourier transform of the distribution The dyadic operators satisfy the property of almost orthogonality:
[TABLE]
Similar properties hold for and
Let us recall the anisotropic Bernstein type lemma from [11, 19] .
Lemma 3.1**.**
Let (resp. ) a ball of (resp. ), and (resp. ) a ring of (resp. ); let and Then there hold
[TABLE]
Due to the anisotropic spectral properties of the linear equation (2.3), we need the following anisotropic type Besov norm:
Definition 3.1**.**
Let and we define the norm
[TABLE]
In particular, when we denote by with
[TABLE]
We recall the classical homogeneous anisotropic Sobolev norm as follows
[TABLE]
In order to obtain a better description of the regularizing effect for the transport-diffusion equation, we will use Chemin-Lerner type spaces.
Definition 3.2**.**
Let and . We define the norms of and by
[TABLE]
and
[TABLE]
respectively. **
In particular, when we have
[TABLE]
In order to study fluid evolving between two parallel plans, namely to prove Theorem 1.3, we also need the following norms:
Definition 3.3**.**
Let and for we define
[TABLE]
To overcome the difficulty that one can not use Gronwall’s type argument for the Chemin-Lerner type norms, we need the time-weighted Chemin-Lerner norm introduced by the authors in [20]:
Definition 3.4**.**
Let , . We define
[TABLE]
Finally we recall the isentropic para-differential decomposition from [3]: let and be in ,
[TABLE]
In what follows, we shall use the anisotropic version of Bony’s decomposition for both horizontal and vertical variables.
As an application of the above basic facts on Littlewood-Paley theory, we present the following product law in the anisotropic Besov spaces.
Lemma 3.2**.**
Let with Let with let with Then one has
[TABLE]
Proof.
We first get, by applying Bony’s decomposition to in vertical variable, that
[TABLE]
Due to applying Lemma 3.1 gives
[TABLE]
from which, and the support properties to the Fourier transform of the terms in we infer
[TABLE]
Here and in all that follows, we always denote to be a generic element of so that The same estimate holds for
On the other hand, we deduce from Lemma 3.1 that
[TABLE]
where in the last step, we used the fact that so that
[TABLE]
This completes the proof of the lemma.
Remark 3.1**.**
We remark that the law of product (3.6) works also for Chemin-Lerner norms.
4. The a priori estimates of and
The goal of this section is to present the a priori estimates of and
Proposition 4.1**.**
Let and be the corresponding solution of (2.3). Then we have
[TABLE]
Proof.
We get, by first applying the operator to the system (2.3) and then taking inner product of the resulting equation with that
[TABLE]
Integrating the above equality over and then taking square root of the resulting equality, we write
[TABLE]
By multiplying to the above inequality and taking norm with respect to and then taking norm with respect to we achieve
[TABLE]
Whereas it follows from Fourier-Plancherel equality and Lemma 3.1 that
[TABLE]
from which and (4.2), we infer
[TABLE]
This leads to the first inequality of (4.1).
On the other hand, we get, by first applying the operator to the system (2.3) and then taking inner product of the resulting equation with that
[TABLE]
Integrating the above equality over and taking square root of the resulting equality, and then taking norm with respect to we obtain the second inequality of (4.1). This completes the proof of the proposition.
Lemma 4.1**.**
Let and be in Then (2.1) has a unique global solution so that
[TABLE]
If moreover, for some then we have
[TABLE]
Proof.
Theorem 1.2 of [11] ensures the global existence of solutions to (2.1). Moreover, (2.4) of [11] gives (4.3). To prove the estimate (4.4), we introduce
[TABLE]
Then in view of (2.1), we write
[TABLE]
It follows from Theorem 1.2 of [11] that
[TABLE]
Yet by virtue of (4.5), we have
[TABLE]
from which and (4.7), we deduce (4.4).
Proposition 4.2**.**
Under the assumptions of Lemma 4.1, for any we have
[TABLE]
where is given by (4.4).**
Proof.
Let us denote
[TABLE]
Then by virtue of (2.1), we write
[TABLE]
By applying to the above equation and then taking inner product of the resulting equation with we obtain
[TABLE]
By applying Bony’s decomposition (3.5) to for the vertical variable, one has
[TABLE]
Due to the support properties to the Fourier of the terms in we deduce
[TABLE]
By applying Hölder’s inequality and using Definition 3.4, we get
[TABLE]
Along the same line, we have
[TABLE]
which implies
[TABLE]
As a result, it comes out
[TABLE]
By integrating (4.10) over and then inserting (4.11) into the resulting inequality, we find
[TABLE]
Multiplying the above inequality by and taking square root of the resulting inequality, and then summing up the resulting inequality over we achieve
[TABLE]
Taking in the above inequality leads to
[TABLE]
from which, and (4.9), we infer
[TABLE]
Note that
[TABLE]
we deduce that
[TABLE]
This together with (4.3) and (4.4) ensures (4.8).
Proposition 4.3**.**
Let be a smooth enough solution of (2.1). Then for any and we have
[TABLE]
and
[TABLE]
where is given by (4.4). **
Proof.
In fact, (4.12) and (4.13) follows directly from Lemma 4.2 of [11] and Lemma 4.1. To prove (4.14), we get, by first applying to (2.1) and then taking inner product of the resulting equation with that
[TABLE]
Applying Lemma 1.1 of [6] yields
[TABLE]
Due to the law of product in Sobolev spaces implies that
[TABLE]
Along the same line, one has
[TABLE]
Inserting the above estimates into (4.15) and integrating the resulting equality with respect to gives rise to
[TABLE]
Notice that
[TABLE]
we get, by applying Young’s inequality, that
[TABLE]
Applying Gronwall’s inequality and using (4.13) leads to (4.14).
Corollary 4.1**.**
Under the assumptions of Theorem 1.2, for any we have
[TABLE]
Proof.
Indeed it follows from interpolation inequality in Besov spaces that
[TABLE]
which together with Proposition 4.3 ensures (4.16).
5. The proof of Theorem 1.2
The goal of this section is to present the proof of Theorem 1.2.
Proof of Theorem 1.2.
For simplicity, we just present the priori estimates for smooth enough solutions of (2.5). Let be a smooth enough solution of (2.1). Let and we denote
[TABLE]
And similar notations for and Then it follows from (2.5) that
[TABLE]
where with being given by (2.5).
Applying the operator to (5.2) and taking inner product of the resulting equation with yields
[TABLE]
The estimate of the above terms relies on the following lemmas:
Lemma 5.1**.**
There holds
[TABLE]
Lemma 5.2**.**
There holds
[TABLE]
Lemma 5.3**.**
There holds
[TABLE]
Lemma 5.4**.**
Let be given by (2.2). Then for any we have
[TABLE]
We shall postpone the proof of the above lemmas in the Appendix.
Let us admit the above Lemmas for the time being and continue to handle the terms in the second line of (5.3). We first get, by using integration by parts, that
[TABLE]
Then applying the law of product, Lemma 3.2, gives
[TABLE]
and
[TABLE]
Along the same line, by using integrating by parts, one has
[TABLE]
It follows from the law of product in anisotropic Besov space, Lemma 3.2, that
[TABLE]
which implies
[TABLE]
Whereas we get, by using integrating by parts, that
[TABLE]
Applying Lemma 5.1 leads to
[TABLE]
Applying Lemma 5.2 gives
[TABLE]
Applying Lemma 5.3 yields
[TABLE]
Finally for any we get, by applying Lemma 5.4, that
[TABLE]
Let us denote
[TABLE]
Then it follows from Proposition 4.1 that
[TABLE]
By integrating (5.3) over and inserting the above estimates into the resulting inequality, and then we take the square root of resulting inequality to achieve
[TABLE]
Multiplying to the above inequality and summing up the resulting inequality for leads to
[TABLE]
Let us assume that Then by applying Young’s inequality, we obtain
[TABLE]
and
[TABLE]
and
[TABLE]
and
[TABLE]
Inserting the above estimates into (5.5) leads to
[TABLE]
In view of (5.6), we deduce from standard theory of Navier-Stokes system that (2.5) has a unique solution with for some maximal existing time . We are going to prove that under the smallness condition (1.5). Otherwise, we denote
[TABLE]
and we take
[TABLE]
Then for we deduce from (5.4), (5.6) and (5.7) that
[TABLE]
which together with (5.1) implies that
[TABLE]
from which and Proposition 4.2 and Corollary 4.1, we deduce that for
[TABLE]
where is given by (4.4).
Then under the smallness condition (1.5), we obtain
[TABLE]
This contradicts with (5.7), which in torn shows that This completes the proof of Theorem 1.2.
6. The case of fluid evolving between two parallel plans
The goal of this section is to investigate the global well-posedness of the anisotropic Navier-Stokes system with only vertical viscosity, (1.7). To do it, let us first present the following lemmas:
Lemma 6.1**.**
Let and satisfy and (see Definition 3.3). Then one has
[TABLE]
Proof.
We first get, by applying Lemma 3.1, that
[TABLE]
Recalling that Poincar’e inequality holds in the strip with Dirichlet boundary condition
[TABLE]
So that we obtain
[TABLE]
This completes the proof of the lemma.
Lemma 6.2**.**
Let be a smooth solenoidal vector field on Then one has
[TABLE]
Proof.
To estimate the trilinear term \bigl{(}\Delta_{k}^{\rm h}(u\cdot\nabla u)|\Delta_{k}^{\rm h}u\bigr{)}_{L^{2}(\Omega)}, we have to distinguish the terms containing the horizontal derivatives with the term containing the vertical derivative. We write
[TABLE]
We start with the estimate of . Applying Bony’s decomposition (3.5) to in the horizontal variables gives
[TABLE]
Through a commutative argument, we find
[TABLE]
It follows from standard commutator’s estimate (see [2]) and Lemma 3.1 that
[TABLE]
so that we deduce from Lemma 6.1 that
[TABLE]
The same estimate holds for
To handle we first get, by using integrating by parts and that
[TABLE]
from which, we infer
[TABLE]
Applying (6.1) gives
[TABLE]
As a result, it comes out
[TABLE]
Whereas observing that
[TABLE]
which together with (6.1) and Lemma 6.1 ensures that
[TABLE]
Along with (6.3), we conclude that
[TABLE]
To handle we get, by applying Bony’s decomposition (3.5) to in the horizontal variables, that
[TABLE]
We first observe from Lemma 6.1 that
[TABLE]
Similarly, we get, by applying (6.1), that
[TABLE]
This leads to
[TABLE]
Together with (6.2) and (6.4), we complete the proof of Lemma 6.2.
Let now present the proof of Theorem 1.3.
Proof of Theorem 1.3.
For simplicity, we only present the a priori estimates for smooth enough solutions of (1.7). By taking inner product of the momentum equation of (1.7) with we get
[TABLE]
Integrating the above inequality over leads to
[TABLE]
which implies
[TABLE]
On the other hand, by applying the operator to the momentum equation of (1.7) and performing inner product of the resulting equation with we obtain
[TABLE]
Integrating the above inequality over and then applying Lemma 6.2 yields
[TABLE]
By taking square root of the above inequality and multiplying the resulting inequality by and then summing up the resulting inequality for we achieve
[TABLE]
Summing up (6.5) with (6.6) gives rise to
[TABLE]
Thanks to (6.7), we deduce by a standard argument that (1.7) has a unique solution with for some maximal existing time We are going to prove that under the assumption of (1.8).
Let us denote
[TABLE]
Then for we deduce from (6.7) that
[TABLE]
In particular, under the assumption of (1.8), for we have
[TABLE]
as long as in (1.8) is small enough. This contradicts with the definition of determined by (6.8), which in turn shows that We complete the proof of Theorem 1.3.
Appendix A The proof of Lemmas 5.1 to 5.4
The goal of this section is to present the proof of Lemmas 5.1 to 5.4.
Proof of Lemma 5.1.
Applying Bony’s decomposition (3.5) to in the vertical variable yields
[TABLE]
Considering the support properties to the Fourier transform of the terms in we find
[TABLE]
On the other hand, it follows from Lemma 3.1 that
[TABLE]
from which and Definition 3.4, we infer
[TABLE]
for being given by (5.1). As a result, it comes out
[TABLE]
Exactly along the same line, we have
[TABLE]
which implies
[TABLE]
Along with (A.1), we complete the proof of Lemma 5.1.
Proof of Lemma 5.2.
Applying Bony’s decomposition (3.5) to in the vertical variable gives
[TABLE]
We first observe that
[TABLE]
where we used Definition 3.4 in the last step.
Similarly, we have
[TABLE]
then by applying Hölder’s inequality and using Definition 3.4, we obtain
[TABLE]
This completes the proof of Lemma 5.2.
Proof of Lemma 5.3.
By applying Bony’s decomposition (3.5) to in the vertical variable to we write
[TABLE]
Note that
[TABLE]
Applying Hölder’s inequality gives
[TABLE]
On the other hand, we observe that
[TABLE]
Then along the same line to proof of (A.2), we arrive at
[TABLE]
This together with (A.2) completes the proof of Lemma 5.3.
Proof of Lemma 5.4.
In view of (2.2), we get, by applying Bony’s decomposition (3.5) to in the vertical variable that
[TABLE]
We first observe from Lemma 3.1 that for any
[TABLE]
where denotes Fourier multiplier with symbol Then noticing the definition of given by (5.1), we get, by applying Hölder’s inequality and Definition 3.4, that
[TABLE]
Along the same line, we have
[TABLE]
which together with the fact that implies that
[TABLE]
Then by virtue of (A.3), we complete the proof of Lemma 5.4.
Acknowledgments. M. Paicu was partially supported by the Agence Nationale de la Recherche, Project IFSMACS, Grant ANR-15-CE40-0010. P. Zhang is partially supported by NSF of China under Grants 11371347 and 11688101, Morningside Center of Mathematics of The Chinese Academy of Sciences and innovation grant from National Center for Mathematics and Interdisciplinary Sciences.
The reference list from the paper itself. Each links out to its DOI / PubMed record.
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