Abstract
We consider the 2D dissipative quasi-geostrophic equation with the time periodic external force and prove the existence of a unique time periodic solution in the case of the supercritical dissipation. In this case, the smoothing effect of the semigroup generated by the dissipation term is too weak to control the nonlinearity in the Duhamel term of the corresponding integral equation. In this paper, we give a new approach which does not depend on the contraction mapping principle for the integral equation.
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1 Introduction
We consider the 2D dissipative quasi-geostrophic equation with the time periodic external force:
where \(\theta =\theta (t,x)\) and \(u=(u_1(t,x),u_2(t,x))\) represent the unknown potential temperature of the fluid and the unknown velocity field of the fluid, respectively. The given external force \(F=F(t,x)\) is T-time periodic, that is F satisfies \(F(t+T)=F(t)\) \((t\in {\mathbb {R}})\) for some \(T>0\). The two operators \((-\Delta )^{\frac{\alpha }{2}}\) \((0<\alpha \leqslant 2)\) and \({\mathcal {R}}_k\) \((k=1,2)\) denote the nonlocal differential operators so-called the fractional Laplacian and the Riesz transforms on \({\mathbb {R}}^2\), respectively, and they are defined by
In this paper, we prove the existence of a unique T-time periodic solution of (1.1) with the supercritical dissipation if the given T-time periodic external force is sufficiently small.
Before we state the main result precisely, we recall some known results for the initial value problem of the 2D dissipative quasi-geostrophic equation with the case \(F=0\):
Based on the scaling transform and the \(L^{\infty }({\mathbb {R}}^2)\)-conservation, the dissipative quasi-geostrophic equation is divided into the subcritical case \(1<\alpha \leqslant 2\), critical case \(\alpha =1\) and supercritical case \(0<\alpha <1\). In the subcritical case, Constantin-Wu [6] proved the existence of a weak solution and decay estimates with respect to \(L^2\) norm for the initial data \(\theta _0\in L^2({\mathbb {R}}^2)\). Wu [14] proved the global well-posedness for small data in the scaling subcritical setting \(\theta _0\in L^p({\mathbb {R}}^2)\) (\(p>2/(\alpha -1)\)) via the contraction mapping principle for the corresponding integral equation. In the critical case, the order of the spatial derivative in the dissipation term coincides with that in the nonlinear term. Zhang [16] used this property and proved the existence of the global in time mild solution in the scaling critical Besov space \({\dot{B}}_{p,1}^{\frac{2}{p}}({\mathbb {R}}^2)\) (\(1\leqslant p \leqslant \infty \)). Global well-posedness in the Triebel–Lizorkin spaces \(F_{p,q}^s({\mathbb {R}}^2)\) (\(s>2/p\), \(1<p,q<\infty \)) is proved by Chen-Zhang [5]. In the supercritical case, the order of the spatial derivative in the dissipation term is less than that in the nonlinear term. Therefore, the smoothing effect of the fractional heat kernel \(e^{-t(-\Delta )^{\frac{\alpha }{2}}}\) is too weak to control the spatial derivative in the nonlinear term. This implies that it seems to be impossible to construct a solution of (1.2). It is able to overcome this and the local well-posedness for large data and the global well-posedness for small data in the scaling critical Sobolev \(H^{2-\alpha }({\mathbb {R}}^2)\) by Miura [12] and Besov spaces \({B}_{p,q}^{1+\frac{2}{p}-\alpha }({\mathbb {R}}^2)\) (\(2\leqslant p<\infty \), \(1\leqslant q<\infty \)) by Chae-Lee [3] and Chen-Miao-Zhang [4]. Their method is based on the energy estimates for the iteration of the transport-diffusion-type equation, and they control the nonlinear term by the divergence free condition \(\nabla \cdot u=0\) and the commutator estimates.
On the other hand, despite the large number of previous studies on the well-posedness of the initial value problem (1.2), the study on the existence of time periodic solutions to the 2D quasi-geostrophic equation is hardly known.
In this manuscript, we consider the supercritical case and prove the existence of a unique time periodic solution to (1.1) in the scaling critical Besov space if the given time periodic external force is sufficiently small. More precisely, our main result of this paper reads as follows:
Theorem 1.1
Let \(T>0\) and \(2/3<\alpha <1\). Let exponents p, q and r satisfy
Then, there exist positive constants \(\delta =\delta (\alpha ,p,q,r,T)\) and \(K=K(\alpha ,p,q,r,T)\) such that if the given T-time periodic external force \(F\in BC({\mathbb {R}}; {\dot{B}}_{r,\infty }^0({\mathbb {R}}^2))\) satisfies
then there exist a unique T-time periodic solution \(\theta \) to (1.1) satisfying
Remark 1.2
-
(1)
If \(\theta \) and F satisfy (1.1), then
$$\begin{aligned} \theta _{\lambda }(t,x)=\lambda ^{\alpha -1}\theta (\lambda ^{\alpha }t,\lambda x),\quad F_{\lambda }(t,x)=\lambda ^{2\alpha -1}F(\lambda ^{\alpha }t,\lambda x) \end{aligned}$$also satisfy (1.1) for all \(\lambda >0\). Since it holds
$$\begin{aligned} \begin{aligned} \sup _{t\in {\mathbb {R}}}\Vert \theta _{\lambda }(t)\Vert _{{\dot{B}}_{p,q}^{1+\frac{2}{p}-\alpha }}&=\sup _{t\in {\mathbb {R}}}\Vert \theta (t)\Vert _{{\dot{B}}_{p,q}^{1+\frac{2}{p}-\alpha }},\\ \sup _{t\in {\mathbb {R}}}\Vert F_{\lambda }(t)\Vert _{{\dot{B}}_{2/(2\alpha -1),\infty }^0}&=\sup _{t\in {\mathbb {R}}}\Vert F(t)\Vert _{{\dot{B}}_{2/(2\alpha -1),\infty }^0} \end{aligned} \end{aligned}$$for all dyadic numbers \(\lambda >0\), the function spaces \(BC({\mathbb {R}};B_{p,q}^{1+\frac{2}{p}-\alpha }({\mathbb {R}}^2))\) and \(BC({\mathbb {R}};{\dot{B}}_{r,\infty }^0({\mathbb {R}}^2))\) in Theorem 1.1 are scaling critical and subcritical setting, respectively.
-
(2)
The assumption \(2/3<\alpha \) in Theorem 1.1 ensures the existence of p and r satisfying (1.3).
Our approach can be applied to the time periodic problem on the half time line \((0,\infty )\):
Here, we note that F is a given T-time periodic external force and the initial data \(\theta _0\) is unknown. In this setting, we prove the existence of a unique suitable initial data \(\theta _0\) such that (1.5) possesses a unique T-time periodic solution \(\theta \). More precisely, the following theorem is obtained:
Theorem 1.3
Let \(T>0\) and \(2/3<\alpha <1\). Let exponents p, q and r satisfy
Then, there exist positive constants \(\delta =\delta (\alpha ,p,q,r,T)\) and \(K=K(\alpha ,p,q,r,T)\) such that if the given T-time periodic external force \(F\in BC((0,\infty ); {\dot{B}}_{r,\infty }^0({\mathbb {R}}^2))\) satisfies
then there exist a unique initial data \(\theta _0 \in B_{p,q}^{1+\frac{2}{p}-\alpha }({\mathbb {R}}^2)\) and a unique T-time periodic solution \(\theta \) to (1.5) satisfying
In the study of the Navier–Stokes equation, the existence of time periodic solutions is often proved by applying the contraction mapping principle to the corresponding integral equation. (It was in [10] that first used this idea.) However, in the case of our problem, the supercritical dissipation prevents us from using this scheme. Indeed, when we apply the idea of [10] to (1.1), we meet the difficulty that the smoothing effect of the fractional heat kernel \(e^{-t(-\Delta )^{\frac{\alpha }{2}}}\) is too weak to control the first-order spatial derivative of the nonlinear term and it is pretty difficult to find a Banach space X satisfying
As another approach, let us consider the successive approximation defined by the transport diffusion-type equation
Then, we can obtain the a priori estimates for the approximation solutions by the energy method, with some commutator estimates, which is the similar method to the analysis of the initial value problem. However, it seems to be difficult to construct a time periodic linear solution \(\theta ^{(n+1)}\) of (1.8) when \(\theta ^{(n)}\) is determined. Therefore, we are not able to proceed in parallel with the energy method of the initial value problem for the supercritical case.
We now introduce an idea to overcome these difficulties and get a time periodic solution. Once Theorem 1.3 is proved, then we can get the time periodic solution on \({\mathbb {R}}\) by extending the time periodic solution on \([0,\infty )\) to the other half time line \((-\infty ,0)\) periodically. Thus, in the following, we only consider the time periodic problem (1.5) and Theorem 1.3.
Outline of our idea is to construct a specific initial data \(\theta _0\) and the corresponding local in time solution \(\theta \) on [0, T] satisfying \(\theta (T)=\theta (0)=\theta _0\). Then, we get a T-time periodic solution by extending \(\theta \) periodically in time. In order to construct such a solution on [0, T], we define a new approximation sequences.
Let us explain the new approximation system more precisely. If a solution \(\theta \) to (1.5) satisfies \(\theta (T)=\theta (0)=\theta _0\), then we have
Therefore, from this observation, we approximate (1.5) together with (1.9) successively and define the iteration scheme \(\{\theta _0^{(n)}\}_{n=0}^{\infty }\) and \(\{\theta ^{(n)}\}_{n=0}^{\infty }\) as follows:
((1.10) is the formal definition. See Sect. 3 for the accurate definition of the approximation sequences.)
Finally, we remark the estimates for the approximation sequences. It is well known that the uniform boundedness is a key property of the convergence of sequences. The uniform boundedness of \(\{\theta ^{(n)}\}_{n=0}^{\infty }\) can be obtained by the classical energy estimates (see, for instance, [1]). However, the new idea is required for the uniform boundedness of \(\{\theta _0^{(n)}\}_{n=0}^{\infty }\) since \(\{\theta _0^{(n)}\}_{n=0}^{\infty }\) is defined by solving the following time-independent equation:
To obtain estimates for \(\{\theta _0^{(n)}\}_{n=0}^{\infty }\), we establish Lemmas 2.6 and 2.7 in Sect. 2 which are inspired by the idea of [8, Theorem 2.4].
This paper is organized as follows. In Sect. 2, we summarize some notations and introduce lemmas which are used in the proof of the main results. In Sect. 3, we prove Theorem 1.1.
Throughout this paper, we denote by C the constant, which may differ in each line. In particular, \(C=C(a_1,...,a_n)\) means that C depends only on \(a_1,...,a_n\). We define a commutator for two operators A and B as \([A,B]=AB-BA\).
2 Preliminaries
Let \({\mathscr {S}}({\mathbb {R}}^2)\) be the set of all Schwartz functions on \({\mathbb {R}}^2\), and let \({\mathscr {S}}'({\mathbb {R}}^2)\) be the set of all tempered distributions on \({\mathbb {R}}^2\). For \(f\in {\mathscr {S}}({\mathbb {R}}^2)\), we define the Fourier transform and the inverse Fourier transform of f by
respectively. \(\{\varphi _j\}_{j\in {\mathbb {Z}}}\) is called the homogeneous Littlewood–Paley decomposition if \(\varphi _0\in {\mathscr {S}}({\mathbb {R}}^2)\) satisfy \(\mathrm{supp}\ \widehat{\varphi _0} \subset \{2^{-1}\leqslant |\xi |\leqslant 2\}\), \(0\leqslant \widehat{\varphi _0}\leqslant 1\) and
where \(\widehat{\varphi _j}(\xi )=\widehat{\varphi _0}(2^{-j}\xi )\). Let us write
for \(j\in {\mathbb {Z}}\) and \(f\in {\mathscr {S}}'({\mathbb {R}}^2)\). Using the homogeneous Littlewood–Paley decomposition, we define the Besov spaces. For \(1\leqslant p,q\leqslant \infty \) and \(s\in {\mathbb {R}}\), the homogeneous Besov space \({\dot{B}}^s_{p,q}({\mathbb {R}}^2)\) is defined by
where \({\mathscr {S}}_0'({\mathbb {R}}^2)\) is the dual space of
Note that \({\dot{B}}_{p,q}^s({\mathbb {R}}^2)\) is a Banach space with respect to the norm \(\Vert \cdot \Vert _{{\dot{B}}_{p,q}^s}\). It is well known that if \(1\leqslant p,q\leqslant \infty \) and \(s<2/p\), then we can identify \({\dot{B}}_{p,q}^s({\mathbb {R}}^2)\) as:
(See for the detail in [11] and [13].) For \(s>0\) and \(1\leqslant p,q\leqslant \infty \), the inhomogeneous Besov space \(B_{p,q}^s({\mathbb {R}}^2)\) is defined by
In this paper, we also use the space-time Besov spaces defined by
for \(1\leqslant p,q,r\leqslant \infty ,s\in {\mathbb {R}}\) and \(0<T\leqslant \infty \).
Next, we introduce the semigroup generated by the fractional Laplacian \((-\Delta )^{\frac{\alpha }{2}}\). It is given explicitly by using the Fourier transform:
Then, this semigroup possesses the following properties:
Lemma 2.1
Let \(\alpha >0\) and \(1\leqslant p,q \leqslant \infty \). Then, the followings hold:
-
(1)
There exists a positive constant \(C=C(\alpha )\) such that
$$\begin{aligned} \left\| e^{-t(-\Delta )^{\frac{\alpha }{2}}} \Delta _j f \right\| _{L^p} \leqslant C e^{-C^{-1}2^{\alpha j}t} \Vert \Delta _jf\Vert _{L^p} \end{aligned}$$holds for all \(t>0\), \(j\in {\mathbb {Z}}\) and \(f\in {\mathscr {S}}'_0({\mathbb {R}}^2)\) with \(\Delta _j f\in L^p({\mathbb {R}}^2)\).
-
(2)
Let \(s_1,s_2\in {\mathbb {R}}\) satisfy \(s_1\leqslant s_2\). Then, there exists a positive constant \(C=C(\alpha ,s_1,s_2)\) such that
$$\begin{aligned} 2^{s_2 j}\left\| e^{-t(-\Delta )^{\frac{\alpha }{2}}}\Delta _j f\right\| _{L^p} \leqslant C t^{-\frac{s_2-s_1}{\alpha }}2^{s_1 j}\Vert \Delta _j f\Vert _{L^p} \end{aligned}$$holds for all \(t>0\), \(j\in {\mathbb {Z}}\) and \(f\in {\mathscr {S}}'_0({\mathbb {R}}^2)\) with \(\Delta _j f\in L^p({\mathbb {R}}^2)\). In particular, it holds
$$\begin{aligned} \left\| e^{-t(-\Delta )^{\frac{\alpha }{2}}}f\right\| _{{\dot{B}}_{p,q}^{s_2}} \leqslant C t^{-\frac{s_2-s_1}{\alpha }}\Vert f\Vert _{{\dot{B}}_{p,q}^{s_1}} \end{aligned}$$for all \(t>0\) and \(f\in {\dot{B}}_{p,q}^{s_1}({\mathbb {R}}^2)\).
-
(3)
Let \(s\in {\mathbb {R}}\). Then, for each \(f\in {\dot{B}}_{p,q}^s({\mathbb {R}}^2)\), it holds
$$\begin{aligned} \lim _{t\rightarrow \infty } \left\| e^{-t(-\Delta )^{\frac{\alpha }{2}}}f\right\| _{{\dot{B}}_{p,q}^s}=0. \end{aligned}$$
Proof
(1) is proved in [9] and [16]. (2) is immediately obtained by (1) and
Let us prove (3). The density property yields that for any \(\varepsilon >0\), there exists a \(f_{\varepsilon }\in {\mathscr {S}}_0({\mathbb {R}}^2)\) such that \(\Vert f_{\epsilon }-f\Vert _{{\dot{B}}_{p,q}^s}<\varepsilon \). Then, we see that
which implies
Since \(\varepsilon >0\) is arbitrary, the proof is completed. \(\square \)
Next, we derive some bilinear estimates. We first recall the definition and basic properties of the Bony paraproduct formula. For \(f,g\in {\mathscr {S}}_0({\mathbb {R}}^2)\), we decompose the product fg as:
where
Here, \(S_lf\) is defined by
Then, considering the supports of the functions of the Fourier side, we have
Using them, we have for \(T>0\), \(1\leqslant p,q \leqslant \infty \) and \(s_1,s_2\in {\mathbb {R}}\) with \(s_1<0\) (if \(q=1\), then \(s_1\leqslant 0\)) that
and it also holds for \(1\leqslant p,q \leqslant \infty \) and \(s_1,s_2\in {\mathbb {R}}\) with \(s_1+s_2>0\)
See [2] for the idea of the proof of these estimates. From easy applications of (2.1) and (2.2), we obtain the following lemma:
Lemma 2.2
Let \(2\leqslant p\leqslant \infty \) and \(1\leqslant q \leqslant \infty \). Let \(s_1,s_2\in {\mathbb {R}}\) satisfy \(s_1+s_2>0\) and \(s_1,s_2<2/p\). Then, there exists a positive constant \(C=C(p,q,s_1,s_2)\) such that
holds for all \(T>0\), \(f\in {\widetilde{L}}^{\infty }(0,T;{\dot{B}}_{p,q}^{s_1}({\mathbb {R}}^2))\) and \(g\in {\widetilde{L}}^{\infty }(0,T;{\dot{B}}_{p,q}^{s_2}({\mathbb {R}}^2))\).
By the standard argument of the proof of commutator estimates (see, for instance, [2, 12]), we get the following lemma:
Lemma 2.3
Let \(2\leqslant p\leqslant \infty \) and \(1\leqslant q \leqslant \infty \). Let \(s_1,s_2\in {\mathbb {R}}\) satisfy \(s_1+s_2>0\), \(0<s_1<1+2/p\) and \(s_2<2/p\). Then, there exists a positive constant \(C=C(p,q,s_1,s_2)\) such that
holds for all \(T>0\), \(f\in {\widetilde{L}}^{\infty }(0,T;{\dot{B}}_{p,q}^{s_1}({\mathbb {R}}^2))\) and \(g\in {\widetilde{L}}^{\infty }(0,T;{\dot{B}}_{p,q}^{s_2}({\mathbb {R}}^2))\).
The next lemma helps us to control the product term which will appear in equations of the perturbation such as (3.5), (3.22) and (3.32).
Lemma 2.4
Let \(\lambda >0\), \(\alpha >0\), \(\beta \leqslant \alpha \), \(2\leqslant p\leqslant \infty \) and \(1\leqslant q \leqslant \infty \). Let \(s_1,s_2\in {\mathbb {R}}\) satisfy \(s_1+s_2>0\), \(2/p<s_1<2/p+\alpha \) and \(s_2<2/p\). Then, there exists a positive constant \(C=C(\lambda ,\alpha ,\beta ,p,q,s_1,s_2)\) such that
holds for all \(T>0\), \(f\in L^{\infty }(0,T;L^p({\mathbb {R}}^2))\cap {\widetilde{L}}^{\infty }(0,T;{\dot{B}}_{p,q}^{s_1}({\mathbb {R}}^2))\) and \(g\in {\dot{B}}_{p,q}^{s_2}({\mathbb {R}}^2)\).
In particular, if \(\beta <\alpha \), then the following estimate holds:
Remark 2.5
Let \(1/2<\alpha <1\) and \(2\leqslant p < 4/(2\alpha -1)\). Then, it immediately follows from (2.3) with \(s_1=s_\mathrm{c}:=1+2/p-\alpha \) and the continuous embedding \({\widetilde{L}}^{\infty }(0,T;{\dot{B}}_{p,1}^0({\mathbb {R}}^2))\hookrightarrow L^{\infty }(0,T;L^p({\mathbb {R}}^2))\) that
where \(X_T^{p,q}:={\widetilde{L}}^{\infty }(0,T;{\dot{B}}_{p,1}^0({\mathbb {R}}^2)) \cap {\widetilde{L}}^{\infty }(0,T;{\dot{B}}_{p,q}^{s_\mathrm{c}}({\mathbb {R}}^2))\). If \(\beta <\alpha \), then (2.4) yields that
Proof of Lemma 2.4
First, we prove (2.3). It follows from an inequality of (2.1) type and (2) of Lemma 2.1 that
By virtue of \(s_1-2/p<\alpha \) and \(\beta \leqslant \alpha \), it is easy to see that
Hence, taking \(l^q({\mathbb {Z}})\)-norm of (2.7) and using
we obtain that
Since it holds
taking \(l^q({\mathbb {Z}})\)-norm of (2.10), we see by (2.2) and (2) of Lemma 2.1 that
Here, we have used
Similarly, it follows from (2.1) and (2) of Lemma 2.1 that
Combining (2.9), (2.11) and (2.13), we complete the proof of (2.5). Next, we show (2.4). By similar inequality to (2.1) and (2) of Lemma 2.1, we see that
We also obtain from (2.2) and (2) of Lemma 2.1 that
Here, we have used the following inequalities in (2.14) and (2.15):
Similarly, we have
Hence, we complete the proof by combining (2.14), (2.15) and (2.17).
To derive some estimates for initial data related to a time periodic solution in the proof of the main results, we introduce the following two lemmas whose ideas are inspired by [8].
Lemma 2.6
Let \(\alpha >0\), \(1\leqslant p \leqslant \infty \), \(1\leqslant q< \infty \) and \(s\in {\mathbb {R}}\). Then, for any \(f\in {\dot{B}}_{p,q}^s({\mathbb {R}}^2)\cap {\dot{B}}_{p,q}^{s-\alpha }({\mathbb {R}}^2)\), the series
converges in \({\dot{B}}_{p,q}^s({\mathbb {R}}^2)\) and u satisfies
Moreover, there exists a positive constant \(C=C(\alpha )\) such that
Proof
Let \(m,n\in {\mathbb {N}}\) satisfy \(m<n\). Then, it follows from (1) of Lemma 2.1 that
where C is the same constant as in (1) of Lemma 2.1. Since it holds
we have
Hence, it follows from (2.21) and the dominated convergence theorem that
Thus, the series (2.18) converges in \({\dot{B}}_{p,q}^s({\mathbb {R}}^2)\), and we find that u satisfies (2.20) by
where we have used (2.22). Finally, we show (2.19). Let
Note that \(u_N\) converges to u in \({\dot{B}}_{p,q}^s({\mathbb {R}}^2)\) as \(N\rightarrow \infty \). By a simple calculation, we see that
Here, it follows from (2) of Lemma 2.1 that
as \(N\rightarrow \infty \) and it holds by (3) of Lemma 2.1 that
as \(N\rightarrow \infty \). Hence, letting \(N\rightarrow \infty \) in (2.23) by (2.24) and (2.25), we find that u satisfies (2.19). This completes the proof. \(\square \)
Lemma 2.7
Let \(T>0\), \(\alpha >0\), \(1\leqslant p\leqslant \infty \), \(1\leqslant q <\infty \) and \(s<2/p\). Then, for any T-time periodic function F satisfying
there exists a unique element \(u_0\in {\dot{B}}_{p,q}^s({\mathbb {R}}^2)\) such that the function
is T-time periodic. Moreover, \(u_0\) satisfies
where C is the same constant as in Lemma 2.6.
Proof
By Lemma 2.6, the series
converges in \({\dot{B}}_{p,q}^s({\mathbb {R}}^2)\) and \(u_0\) satisfies (2.26) and
By the periodicity of F, we have
Therefore, it follows from (2.27) and (2.28) that
for all \(t>0\). Hence, u(t) is T-time periodic. Next, we prove the uniqueness. Let \(v_0\) be an arbitrary element of \({\dot{B}}_{p,q}^s({\mathbb {R}}^2)\) such that \(v(t):=e^{-t(-\Delta )^{\frac{\alpha }{2}}}v_0+f(t)\) is a T-time periodic function. Then, since \(u_0-v_0=u(NT)-v(NT)=e^{-NT(-\Delta )^{\frac{\alpha }{2}}}(u_0-v_0)\) holds for all \(N\in {\mathbb {N}}\) by the periodicity, we obtain by (3) of Lemma 2.1 that
as \(N\rightarrow \infty \). Therefore, we have \(u_0=v_0\) in \({\dot{B}}_{p,q}^s({\mathbb {R}}^2)\) and this completes the proof. \(\square \)
Finally, we recall a positivity lemma for the \(L^p\)-energy of the fractional dissipation:
Lemma 2.8
([4, 15]) Let \(0<\alpha \leqslant 2\) and \(2\leqslant p <\infty \). Then, there exists a positive constant \(\lambda =\lambda (\alpha ,p)\) such that
for all \(j\in {\mathbb {Z}}\) and \(f\in {\mathscr {S}}'_0({\mathbb {R}}^2)\) with \(\Delta _jf \in L^p({\mathbb {R}}^2)\).
3 Proof of main results
In this section, we prove Theorems 1.1 and 1.3. Once Theorem 1.3 is proved, then we can get the time periodic solution on \({\mathbb {R}}\) by extending the solution on \([0,\infty )\) to the other half time line \((-\infty ,0)\) periodically. Therefore, we only prove Theorem 1.3.
Let T, \(\alpha \), p, q and r satisfy the assumptions of Theorem 1.3 and let \(\sigma \) satisfy \(\alpha -2/p<\sigma <2/p\). We use the following notation for simplicity in this section:
We consider the successive approximation sequences \(\{\theta _0^{(n)}\}_{n=0}^{\infty }\subset {\dot{B}}_{p,1}^0({\mathbb {R}}^2)\cap {\dot{B}}_{p,q}^{s_\mathrm{c}}({\mathbb {R}}^2)\) of the initial data and \(\{\theta ^{(n)}\}_{n=0}^{\infty }\subset X_T^{p,q}\) of solutions to (1.5) defined inductively as follows:
First, let \(\theta _0^{(0)}(x)=0\) and \(\theta ^{(0)}(t,x)=0\). Next, if \(\theta _0^{(n)}\) and \(\theta ^{(n)}\) are determined, then we define \(\theta _0^{(n+1)}\) and \(\theta ^{(n+1)}\) by the following linear equation:
where \(\theta _0^{(n+1)}\) is given by
For \(n\in {\mathbb {N}}\cup \{0\}\), we put \(\psi ^{(n)}(t):=\theta ^{(n)}(t)-e^{-t(-\Delta )^{\frac{\alpha }{2}}}\theta ^{(n)}(0)\) and
The well-definedness of the sequences is assured if the series in (3.2) converges in \({\dot{B}}_{p,1}^0({\mathbb {R}}^2)\cap {\dot{B}}_{p,q}^{s_\mathrm{c}}({\mathbb {R}}^2)\). In the following lemma, we check the convergence and derive some properties of the sequences.
Lemma 3.1
Let n be an positive integer. Assume that \(\theta _0^{(n)}\in {\dot{B}}_{p,1}^0({\mathbb {R}}^2)\cap {\dot{B}}_{p,q}^{s_\mathrm{c}}({\mathbb {R}}^2)\) and \(\theta ^{(n)}\in X_T^{p,q}\). Then, for every \(F\in BC((0,\infty );{\dot{B}}_{r,\infty }^0({\mathbb {R}}^2))\), the series in (3.2) converges in \({\dot{B}}_{p,1}^0({\mathbb {R}}^2)\cap {\dot{B}}_{p,q}^{s_\mathrm{c}}({\mathbb {R}}^2)\) and it holds
in \({\dot{B}}_{p,1}^0({\mathbb {R}}^2)\cap {\dot{B}}_{p,q}^{s_\mathrm{c}}({\mathbb {R}}^2)\). Moreover, there exist positive constants \(\delta _1=\delta _1(\alpha ,p,q,r,T)\) and \(C_1=C_1(\alpha ,p,q,r,T)\) such that if F satisfies
then it holds
Proof
To prove the convergence of the series in (3.2) in \({\dot{B}}_{p,1}^0({\mathbb {R}}^2)\cap {\dot{B}}_{p,q}^{s_\mathrm{c}}({\mathbb {R}}^2)\), Lemma 2.6 yields that it suffices to check
Since \(\psi ^{(n)}\) satisfies
applying \(\Delta _j\) to (3.5), we see that
Multiplying (3.6) by \(p|\Delta _j \psi ^{(n)}|^{p-2}\Delta _j\psi ^{(n)}\) and integrating over \({\mathbb {R}}^2\), we have by the Hölder inequality that
By Lemma 2.8, we obtain that
for some \(\lambda =\lambda (\alpha ,p)>0\). On the other hand, it follows from the divergence free condition \(\nabla \cdot u^{(n-1)}=0\) that
Substituting (3.8) and (3.9) in (3.7), we have
which implies that
Let \(s\in \{s_\mathrm{c},s_\mathrm{c}-\alpha \}\). Multiplying (3.10) by \(2^{sj}\), we have
Taking \(l^{q}({\mathbb {Z}})\)-norm of (3.11), we see by (2.12) that
Hence, it follows from Lemma 2.3 and (2.5) that
Using
and the boundedness of the Riesz transform on the homogeneous space-time Besov spaces, we obtain
Hence, it follows from (3.12) and Lemma 2.6 that
Let \(s':=s-s_\mathrm{c}\in \{-\alpha ,0\}\). Multiplying (3.10) by \(2^{s'j}\) and
taking \(l^1({\mathbb {Z}})\)-norm, we see that
It follows from Lemma 2.3 and (2.6) that
Therefore, by the same argument as above, we have
and we see that the series in (3.2) converges in \({\dot{B}}_{p,1}^0({\mathbb {R}}^2)\) and
Combining (3.12) and (3.14), we find that Lemma 2.6 implies the series in (3.2) converges in \({\dot{B}}_{p,1}^0({\mathbb {R}}^2)\cap {\dot{B}}_{p,q}^{s_\mathrm{c}}({\mathbb {R}}^2)\) and (3.3) also holds.
Next, we prove (3.4). Since \(\Delta _j \theta ^{(n+1)}\) satisfies
the same argument as in the derivation of (3.10) yields that
which implies that
Taking \(L^{\infty }_t(0,T)\)-norm of (3.16) and then taking \(l^{q}({\mathbb {Z}})\)-norm, we see by Lemma2.3 that
On the other hand, by (3.15), we see that
Taking \(L^{\infty }_t(0,T)\)-norm and then \(l^1({\mathbb {Z}})\)-norm of (3.18), we have
Using Lemma 2.3 and the second inequality of (2.16), we obtain that
Hence, combining estimates (3.12), (3.14), (3.17) and (3.19), we obtain
for some \(C_1=C_1(\alpha ,p,q,r,T)\).
On the other hand, since \(\theta ^{(1)}\) satisfies
the simpler argument than above yields that
Hence, if F satisfies
then by (3.20), (3.21) and the inductive argument, we obtain
for all \(m\in {\mathbb {N}}\cup \{0\}\). This completes the proof. \(\square \)
Next lemma ensures the convergence of the approximation sequences.
Lemma 3.2
There exists a positive constant \(\delta _2=\delta _2(\alpha ,p,q,r,\sigma ,T)\leqslant \delta _1\) such that if \(F\in BC((0,\infty );{\dot{B}}_{r,\infty }^0({\mathbb {R}}^2))\) satisfies
then it holds
Proof
Due to
and Lemma 2.6, we consider the estimates of \(\psi ^{(n+1)}(T)-\psi ^{(n)}(T)\) in \({\dot{B}}_{p,q}^{\sigma -\alpha }({\mathbb {R}}^2)\cap {\dot{B}}_{p,q}^{\sigma }({\mathbb {R}}^2)\). Since \(\psi ^{(n+1)}-\psi ^{(n)}\) satisfies
we see that
Thus, the similar energy calculation as in the proof of Lemma 3.1 yields that
Let \(s\in \{\sigma ,\sigma -\alpha \}\). Multiplying this by \(2^{sj}\) and
taking \(l^q({\mathbb {Z}})\)-norm of this, we obtain that
Therefore, it follows from Lemmas 2.2, 2.3 and (2.5) that
This gives
Since \(\theta ^{(n+2)}-\theta ^{(n+1)}\) satisfy
we see that
By the similar energy calculation as in the proof of Lemma 3.1, we have
Multiplying (3.25) by \(2^{\sigma j}\), we see that
By taking \(L^{\infty }_t(0,T)\) and then \(l^q({\mathbb {Z}})\)-norm, it follows from (2.16) and Lemmas 2.2 and 2.3 that
Since it holds
we have by (3.26) that
Therefore, combining (3.24) and (3.27), we obtain
for some \(C_2=C_2(\alpha ,p,q,r,\sigma ,T)>0\). Here, we assume that
Let \(N\in {\mathbb {N}}\) satisfy \(N\geqslant 2\). Then, summing (3.28) over \(n=1,...,N-1\) and using Lemma 3.1, we have
for some constant \(C_T>0\) depending on T. This implies
Hence, we have
which completes the proof. \(\square \)
Lemma 3.3
There exists a positive constant \(C_3=C_3(\alpha ,p,q,r,T,\sigma )\) such that
for all T-time periodic solutions \(\theta \in BC([0,\infty );B_{p,q}^{s_\mathrm{c}}({\mathbb {R}}^2))\cap X_{T}^{p,q}\) and \({\widetilde{\theta }}\in BC([0,\infty );B_{p,q}^{s_\mathrm{c}}({\mathbb {R}}^2))\cap {\widetilde{L}}^{\infty }(0,\infty ;{\dot{B}}_{p,q}^{s_\mathrm{c}}({\mathbb {R}}^2))\) to (1.5) with the same T-time periodic external force F.
Proof
Since \(\theta -{\widetilde{\theta }}\) satisfies
where \(u={\mathcal {R}}^{\perp }\theta \), \({\widetilde{u}}={\mathcal {R}}^{\perp }{\widetilde{\theta }}\), we see that
Therefore, it follows from the similar energy calculation as in the derivation of (3.27) that
Next, we derive the estimate for \(\theta (0)-{\widetilde{\theta }}(0)\). Since \(\theta -{\widetilde{\theta }}\) is T-time periodic and the Duhamel principle gives
we have by Lemma 2.7 that
where \(\psi (t):=\theta (t)-e^{-t(-\Delta )^{\frac{\alpha }{2}}}\theta (0)\) and \({\widetilde{\psi }}(t):={\widetilde{\theta }}(t)-e^{-t(-\Delta )^{\frac{\alpha }{2}}}{\widetilde{\theta }}(0)\). Since it holds
applying \(\Delta _j\) to (3.32), we have
Hence, by the similar energy calculation as in the derivation of (3.23), we obtain
Here, we have used
Combining (3.30), (3.31) and (3.33), we get (3.29). This completes the proof. \(\square \)
Now we are in a position to prove Theorem 1.3.
Proof of Theorem 1.3
Let \(\alpha ,p,q,r\) and T satisfy the assumptions of Theorem 1.3 and let \(\sigma :=\alpha /2\). Then, \(\sigma \) satisfies \(\alpha -2/p<\sigma <2/p\). We put
and let \(F\in BC((0,\infty );{\dot{B}}_{r,\infty }^0({\mathbb {R}}^2))\) satisfy
It follows from (3.4) that
From Lemma 3.2, there exist limits \(\theta _0\in {\dot{B}}_{p,q}^{\sigma }({\mathbb {R}}^2)\) and \(\theta \in L^{\infty }(0,T;{\dot{B}}_{p,q}^{\sigma }({\mathbb {R}}^2))\) such that
By Lemma 3.1 and (3.34), we see that \(\theta _0\in {\dot{B}}_{p,q}^{s_\mathrm{c}}({\mathbb {R}}^2)\), \(\theta \in X_T^{p,q}\) and
It is easy to check that \(\theta \) is a solution to (1.5) on [0, T]. Next, we show the continuity in time of the solution \(\theta \) by the idea in [7]. Let \((s,\rho )\in \{(s_\mathrm{c},q),(0,1)\}\). Since it holds \(\partial _t\Delta _j\theta =\Delta _jF-(-\Delta )^{\frac{\alpha }{2}}\Delta _j\theta -\Delta _j(u\cdot \nabla \theta )\), we have
which implies \(\partial _t\Delta _j\theta \in L^{\infty }(0,T;{\dot{B}}_{p,\rho }^s({\mathbb {R}}^2))\). Therefore, we have
It follows from \(q<\infty \) and (3.35) that
Hence, we see that \(\theta \in C([0,T];{\dot{B}}_{p,1}^0({\mathbb {R}}^2)\cap {\dot{B}}_{p,q}^{s_\mathrm{c}}({\mathbb {R}}^2)) \subset C([0,T];B_{p,q}^{s_\mathrm{c}}({\mathbb {R}}^2))\). Since
as \(n\rightarrow \infty \), we obtain by letting \(n\rightarrow \infty \) in (3.3) that
which implies
Let us extend \(\theta \) to the function on the interval \([0,\infty )\) periodically as
Then, \(\theta \in BC([0,\infty );B_{p,q}^{s_\mathrm{c}}({\mathbb {R}}^2))\) and \(\theta \) is a T-time periodic solution to (1.5) satisfying (1.4). Finally, we prove the uniqueness. Let \({\widetilde{\theta }}\) be arbitrary solution satisfying (1.7). Note that since \(0<\sigma <s_c\), we see that \(\theta ,{\widetilde{\theta }} \in L^{\infty }(0,T;L^p({\mathbb {R}}^2)) \cap {\widetilde{L}}^{\infty }(0,T;{\dot{B}}_{p,q}^{s_\mathrm{c}}({\mathbb {R}}^2)) \subset {\widetilde{L}}^{\infty }(0,T;{\dot{B}}_{p,q}^{\sigma }({\mathbb {R}}^2))\) holds by the similar calculation as (2.8). Then, it follows from (3.29) and (3.35) that
Thus, we see that \({\widetilde{\theta }}=\theta \) on [0, T]. The periodicity of \(\theta \) and \({\widetilde{\theta }}\) implies \(\theta ={\widetilde{\theta }}\) on \([0,\infty )\). This completes the proof.
References
Bae, Hantaek, Global well-posedness of dissipative quasi-geostrophic equations in critical spaces, Proc. Amer. Math. Soc., 136, 2008
Bahouri, Hajer, Chemin, Jean-Yves, Danchin, Raphaël, Fourier analysis and nonlinear partial differential equations, 343, Springer, Heidelberg, 2011,
Chae, Dongho, Lee, Jihoon, Global well-posedness in the super-critical dissipative quasi-geostrophic equations, Comm. Math. Phys., 233, 2003, 297–311,
Chen, Qionglei, Miao, Changxing, Zhang, Zhifei, A new Bernstein’s inequality and the 2D dissipative quasi-geostrophic equation, Comm. Math. Phys., 271, 2007
Chen, Qionglei, Zhang, Zhifei, Global well-posedness of the 2D critical dissipative quasi-geostrophic equation in the Triebel-Lizorkin spaces, Nonlinear Anal., 67, 2007, 1715–1725,
Constantin, Peter, Wu, Jiahong, Behavior of solutions of 2D quasi-geostrophic equations, SIAM J. Math. Anal., 30, 1999, 937–948,
Danchin, R., Global existence in critical spaces for compressible Navier-Stokes equations, Invent. Math., 141, 2000, 579–614,
Geissert, Matthias, Hieber, Matthias, Nguyen, Thieu Huy, A general approach to time periodic incompressible viscous fluid flow problems, Arch. Ration. Mech. Anal., 220, 2016, 1095–1118,
Hmidi, Taoufik, Keraani, Sahbi, Global solutions of the super-critical 2D quasi-geostrophic equation in Besov spaces, Adv. Math., 214, 2007, 618–638,
Kozono, Hideo, Nakao, Mitsuhiro, Periodic solutions of the Navier-Stokes equations in unbounded domains, Tohoku Math. J. (2), 48, 1996, 33–50,
Kozono, Hideo, Yamazaki, Masao, Semilinear heat equations and the Navier-Stokes equation with distributions in new function spaces as initial data, Comm. Partial Differential Equations, 19, 1994, 959–1014,
Miura, Hideyuki, Dissipative quasi-geostrophic equation for large initial data in the critical Sobolev space, Comm. Math. Phys., 267, 2006
Sawano, Yoshihiro, Theory of Besov spaces, Developments in Mathematics, 56, Springer, Singapore, 2018,
Wu, Jiahong, Dissipative quasi-geostrophic equations with \(L^p\) data, Electron. J. Differential Equations, 2001, No. 56, 13,
Wu, Jiahong, Lower bounds for an integral involving fractional Laplacians and the generalized Navier-Stokes equations in Besov spaces, Comm. Math. Phys., 263, 2006, 803–831,
Zhang, Zhi-fei, Global well–posedness for the 2D critical dissipative quasi-geostrophic equation, Sci. China Ser. A, 50, 2007, 485–494,
Acknowledgements
The author would like to express his sincere gratitude to Professor Jun-ichi Segata, Faculty of Mathematics, Kyushu University, for many fruitful advices and continuous encouragement. This work was partly supported by Grant-in-Aid for JSPS Research Fellow Grant Number JP20J20941.
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Fujii, M. Time periodic solutions to the 2D quasi-geostrophic equation with the supercritical dissipation. J. Evol. Equ. 22, 24 (2022). https://doi.org/10.1007/s00028-022-00787-6
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DOI: https://doi.org/10.1007/s00028-022-00787-6