Abstract
We construct a linear approximation of the solution to the surface quasi-geostrophic equation in 2-dimensional Euclidean space, and obtain a convergence rate in the Lebesgue norm between the solution and this approximation with respect to time. We also demonstrate that the nonlinear term of the solution is bounded sharply by the same function of time.
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1 Introduction
This paper is concerned with the surface quasi-geostrophic equation.
Here, \(\theta : (0,\infty ) \times \mathbb {R}^2 \rightarrow \mathbb {R}\) is an unknown function, representing the potential temperature of a fluid parcel at a point (t, x) in spacetime; and u represents the velocity of a fluid parcel. \(R_j = \partial _j (-\Delta )^{-1/2} = \mathcal {F}^{-1}[ \, i\xi _j / |\xi | \, ]*\) is the jth Riesz transform; and \(\alpha \in [1,2]\). We refer to references [1, 3, 11, 16,17,18] for the physical meaning and derivation of the equations. We will prove existence and uniqueness results for given initial data; and, under some slightly stronger restrictions, we will consider the large-time behaviour of solutions.
Let us recall several existing results related to the regularity of solutions. In the subcritical case, \(\alpha \in (1,2],\) unique global existence and regularity can be shown, for initial data
by classical methods using the Banach fixed point theorem, similarly to [8, 13]. Global unique existence and regularity for the subcritical case are also proven on the torus in [5].
In the critical case, \(\alpha = 1\), we can guarantee local existence of a solution for uniformly continuous initial data (see [20], which studies the problem in the framework of Besov spaces larger than \(L^\infty \)). The local smooth solutions are then extended to global smooth solutions, as in the papers [2, 4, 15].
Finally, for the supercritical case, \(\alpha \in [0,1),\) the paper [7] proves global regularity for all \(\alpha \in [\alpha _0,1)\), where \(\alpha _0\) grows with respect to the size of the initial data. Global regularity for large data in the supercritical case is an open problem.
In this paper, we discuss an optimal decay estimate of the nonlinear part of the solution in the subcritical and critical cases. This is the first paper to prove such optimality for equations with divergence-free flow. We also construct a linear approximation of the solution in \(L^p\).
We begin our study of (1.1) by defining the following function
which is the fundamental solution to the fractional heat equation, the linear part of (1.1). We will use this new function to introduce the idea of mild solutions.
For this paper, we set the initial data as follows
which provides us with sufficient regularity for global existence and smoothness of solutions in the subcritical and critical cases.
Definition
(Mild solution) A function \(\theta \) is a mild solution of (1.1) if
We also define M, the “mass” of the solution \(\theta \) as
and denote the linear part of \(\theta \) by
We state an existence result for global solutions.
Proposition 1.1
Let \(\alpha \in [1,2]\) and \(\theta _ 0 \in W^{1,1} \cap W^{1,\infty }\). Then there exists a unique global mild solution \(\theta \in C( [0,\infty ) ; W^{1,p} ) \cap C((0,\infty ) ; W^{1,1} \cap W^{1,\infty })\) of (1.1), for all \(1 \le p < \infty \).
The above proposition can be easily shown in the subcritical case \(\alpha \in (1,2]\) using the Banach fixed point argument. In fact, for the subcritical case it is sufficient to set \(\theta _0 \in L^1 \cap L^p\) with \(p \in (\frac{2}{\alpha -1},\infty ]\). For existence in the critical case, we refer to [14, 15].
As a first step in creating a linear approximation of the solution, it is possible to prove that, for \(1 \le p \le \infty \),
This explains that the \(L^p\)-decay of the solution is essentially equivalent to that of the linear solution. In this paper, we will extract the optimal decay of the nonlinear part of \(\theta \). Our result reads as follows:
Theorem 1.2
Let \(\alpha \in [1,2]\), \(p \in [1,\infty ]\) and
Let \(\theta _0 \in W^{1,1} \cap W^{1,\infty }\), and let \(\theta \) be a mild solution. Also assume \(|x|^2 \theta _0 \in L^1({\mathbb {R}}^2) \). Then we have the following convergence:
where \(R := (-R_2, R_1)\). Furthermore, there exists \(\theta _0\) such that the nonlinear component is optimally bounded by \(b_{\alpha ,p}(t)\) in the \(p=2\) case. That is
for all sufficiently large t.
Our proof of (1.10) is fully self-contained, with all necessary work shown explicitly in this paper. For the bound from above in (1.10), the proof mainly consists of carefully taking Besov norms of the solution via Littlewood-Paley decomposition; and, in the case of the \(L^p\) norm for \(1\le p <2\), applying the Hardy–Littlewood–Sobolev and Grönwall inequalities. For the bound from below, we force the initial data to take a shape resemblant of a Gaussian function with a narrow support, and exploit this assumption to achieve the necessary inequalities.
The first term inside the norm of (1.9) is the solution \(\theta \). The second, third, and fourth terms are a (Taylor-expanded) approximation of the linear term of \(\theta \). The final term is a linear approximation of the nonlinear term in \(\theta \).
Remark 1.3
If the initial data \(\theta _0\) is radially symmetric, the approximation of the nonlinear term becomes 0 (see e.g. [9, page 46]). That is,
Notation. For a function f we denote the Fourier transform of f as follows:
The inverse Fourier transform is then written as
For the purpose of calculating inequalities, we will frequently omit the factor of \(1/2\pi \), as it will have no influence on the proofs. Let \({\mathcal {S}}' = {\mathcal {S}}'({\mathbb {R}}^2)\) be the space of tempered distributions. Let \({\mathcal {P}} = {\mathcal {P}} ({\mathbb {R}}^2)\) be the set of all polynomials.
2 Preliminaries
We recall the definition and some basic properties of Besov spaces, and write the \(L^p\)-norm decay of the solution, \(\theta \).
2.1 Besov spaces
We use the Littlewood-Paley decomposition of unity to define homogeneous Besov spaces.
Definition
Let \(\{ \phi _k \}_{k\in \mathbb {Z}}\) be a set of non-negative measurable functions such that
-
1.
\(\sum _{k\in \mathbb {Z}} \hat{\phi }_k (\xi ) = 1, \text { for all } \xi \in {\mathbb {R}}^2 \backslash \{0\}\),
-
2.
\(\hat{\phi }_k(\xi ) = \hat{\phi }_0(2^{-k}\xi )\),
-
3.
\(\text { supp }\hat{\phi }_k (\xi ) \subseteq \{ \xi \in {\mathbb {R}}^2 \ | \ 2^{k-1} \le |\xi | \le 2^{k+1} \}\).
The Besov norm is then defined as follows. For \(f \in \mathcal {S'}/\mathcal {P}\), \(1 \le p,q \le \infty \), and \(s \in {\mathbb {R}}\),
Finally, the set \(\dot{B}^{s}_{p,q}\) is defined as the set of distributions, \(f \in \mathcal {S'}/\mathcal {P}\), whose Besov norm is finite.
We introduce the following propositions, and refer to [19] for their proofs.
Proposition 2.1
Let \(1 \le p,q \le \infty \), and \(s \in {\mathbb {R}}\). Then for \(f \in \dot{B}^{s+1}_{p,q}\),
Proposition 2.2
Let \(1 \le p \le \infty \). Then for \(f \in \dot{B}^{2(1-\frac{1}{p})}_{1,1}\),
2.2 \(L^p\)-norm decay
Proposition 2.3
(Hardy–Littlewood–Sobolev [10]) Let \(0< \alpha < n\) and \(1<p<r<\infty \), such that \(\frac{1}{r} = \frac{1}{p} - \frac{\alpha }{n}\). Then there exists a constant \( C > 0\) such that
Proposition 2.4
Let \(n \in {\mathbb {N}}\), \(p \in [1,\infty ]\), \(k \in {\mathbb {N}}\), \(\alpha \in [1,2]\). Then there exists \(C>0\) such that, for all \(1 \le j \le n\), and \(t > 0 \),
The decay rate is easily obtained by a change of variables, recalling (1.2). The overall boundedness is proven using the Hausdorff-Young inequality.
Proposition 2.5
Let \(\theta _0 \in W^{1,1} \cap W^{1,\infty }\), and \(1 \le p \le \infty \). Let \(\theta \) be a solution to (1.1).
-
(i)
For all \(\alpha \in [1,2]\), there exists \(C >0\) such that, for all \(t>0\),
$$\begin{aligned} \Vert \theta (t)\Vert _{p} \le C ( t + 1 )^{-\frac{2}{\alpha }(1-\frac{1}{p}) }. \end{aligned}$$(2.2) -
(ii)
For \(\alpha = 1\), \(\beta > 0\), there exists \(C_\beta > 0\) such that, for all \(t \ge 1\),
$$\begin{aligned} \Vert |\nabla |^{\beta } \theta (t)\Vert _p \le C_{\beta } t^{-2(1-\frac{1}{p}) - \beta }, \end{aligned}$$(2.3)where
$$\begin{aligned} |\nabla |^\beta \theta (t) :=\mathcal {F}^{-1} [|\xi |^\beta \hat{\theta }(t)]. \end{aligned}$$
For the proof of (i), see [6]. For the proof of (ii), see Proposition 4.3 in [12].
3 Large-time behaviour
We will now begin to discuss the large-time behaviour of the solution \(\theta \). Before beginning our proof of Theorem 1.2, we begin with a less strong approximation of the solution. Results similar to the below have been proven with respect to the N-dimensional convection-diffusion equations [8] and the critical Burger’s equations [13].
3.1 Approximation by the fractional heat kernel
Proposition 3.1
Let \(\alpha \in [1,2]\) and \(p \in [1,\infty ]\). Let \(\theta _0 \in W^{1,1} \cap W^{1,\infty }\), and also assume \(|x| \theta _0 \in L^1\). Then the solution \(\theta \) to (1.4) satisfies
In order to prove the above proposition, it is useful to split the norm into linear and nonlinear parts as follows:
We then prove the bound (3.1) in parts as two separate lemmas. The first concerns the linear part, and has been adapted from Escobedo-Zuazua [8] to apply to the fractional heat kernel.
Lemma 3.2
[8] Let \(p \in [1,\infty ]\), and \(\alpha \in [1,2]\). Let \(\phi , |x|\phi \in L^1\), with \(M := \int _{{\mathbb {R}}^2}\phi (x) \mathop {}\!\mathrm {d}x\). Then there exists \(C>0\), such that
Lemma 3.3
Let \( 1 \le p \le \infty \), and \(\alpha \in [1,2]\). Suppose that \(\theta \) is a mild solution satisfying the decay properties in Proposition 2.5. Then there exists \(C >0\) such that, for all \(t\ge 1\),
where \(b_{\alpha ,p}\) is defined by (1.8).
Proof
Step 1. (\(p \ge 2\) case) We will need to split the time interval into two halves, and handle the \(\alpha = 1\) and \(\alpha > 1\) cases separately. The proof below is only for the \(p < \infty \) case, as the \(p = \infty \) case is almost identical.
We utilise the \(L^p\) decay of the solution and its derivative. For values \(t \in (0,1]\), we can increase the powers of s in our estimates by taking
by which we ensure that the time-integral does not blow up locally.
We start on the second half of the time-interval, with \(\alpha >1.\) By the boundedness of the Riesz transform,
In the \(\alpha = 1\) case,
where we have used (2.3) to handle the derivative of \(\theta \).
For the first half of the time-interval, we will distinguish between the \(\alpha >1\) and \(\alpha =1\) cases when it becomes necessary. We will take the Fourier transform inside the norm, and manipulate the resulting multipliers from the derivative and Riesz transform. In particular, let us first note that the following Fourier multiplier can be written in the following forms
Now we begin estimating our \(L^p\) norm.
We start with the \(p=2\) case. By the Plancherel theorem,
The large multiplier inside the \(\eta \) integral is easily estimated from above by
Next, we take the Littlewood-Paley decomposition of both \(\theta \) functions:
We also split the \(L^2\) norm by Hölder’s inequality.
The final step is obtained by applying the Hausdorff–Young inequality and the following Hölder inequality
where \(\hat{\psi }_k :=\hat{\phi }_{k-1} + \hat{\phi }_k +\hat{\phi }_{k+1}. \) The above sum in (3.4) can be written as the product of Besov norms of the solution \(\theta \). We give estimates for the necessary Besov norms next.
Recall that \(\theta \) is made up of a linear and nonlinear term. We will take the norms of each separately, and will see that both hinge on the Besov norm of the fundamental solution, \(P_{\alpha /2}\). We start with the linear term. Clearly
Let us now consider the Besov norms of the whole solution \(\theta \). In the following, we must distinguish between the noncritical and critical cases. We start with the noncritical \(\alpha \in (1,2]\) case.
We now look at the critical case, \(\alpha =1\). Here, the only difference is that we leave the derivative on the right hand side of the convolution for the second half of the time-integral, and apply the decay estimate of the derivative.
Returning to (3.4), we get
The above result is easily extended to all \(p>2\) by Young’s convolution inequality. We simply split the fundamental solution into two parts as follows, and then proceed through the exact same steps as above.
Step 2 (\(1 \le p < 2\) case) We take the \(j=1\) term of the Fourier multiplier in (3.3):
For simplicity of notation, we also only take one term from the dot product above. We then split the Fourier multiplier into two parts:
and we focus on the first term above, as both cases have almost identical proofs. We write
Next, the most crucial step to this method is to split the Euclidean space into squares, whose size depends on time. For \(k = (k_1,k_2) \in {\mathbb {Z}}^2\), define the set
Then we can once again fit our inverse Fourier transform into an \(L^2\) norm, and thus estimate away the Riesz transforms. That is,
where we have used Hölder’s inequality. We are able to eliminate the Riesz transform by taking advantage of the Plancherel theorem, and split one of the solution functions \(\theta \) into parts defined on squares \(Q_{t,l}\) as follows:
Next, we split up the above double sum into two cases: \(k=l,\) and \(k\ne l.\)
In the case when \(k=l\),
The steps above have used Young’s convolution inequality and the Hardy–Littlewood–Sobolev inequality, as we have seen before in our original estimations of the nonlinear term of \(\theta \).
In the \(k \not = l\) case, we multiply by 1 by inserting \(|t^{1/\alpha }k - t^{1/\alpha }l|^{2} \text {/} |t^{1/\alpha }k - t^{1/\alpha }l|^{2}\), and thus write
The step (3.7) was obtained by simply using Hölder’s inequality for sequences, noting that
Our next concern is with the boundedness of the sum over l. The key points to the following steps are that \(t^{1/\alpha } k\) is close to x, where x is the variable of our \(L^2(Q_{t,k})\) norm; and that we thus treat \(t^{1/\alpha } k\) as a derivative in \(\xi \) after moving it inside the inverse Fourier transform. For each l,
Briefly, the \(\xi \) derivative results in a factor of \(t^{1/\alpha },\) which simply cancels with the inverse factor emerging from the \(\xi _1^2\) already present inside the integral. The resulting estimate is thus essentially similar to
Returning to (3.8),
It is a delicate process to prove that the above sums (3.6) and (3.9) are bounded properly. As such, we provide an outline of the proof, beginning with the following estimates.
where here we have applied the decay estimate of the solution and its derivative, and the elementary inequality \(t^{-1} \le C (1+s)^{-1}\), for \(t \ge \max \{ 1, s \}\). By Grönwall’s inequality we have the same decay as in \(L^{\frac{4}{3}}\),
We apply the decay above to the inequalities (3.6) and (3.9), and so (3.5) is bounded by
This completes the proof in the case when \(1 \le p < 2\). \(\square \)
We thus have completed the proof of (3.1), and also obtained a useful bound on the nonlinear term of our solution, which we will use later. For all \(p \in [1,\infty ]\), and with initial data satisfying (1.3),
for all \(\alpha \in [1,2], \ t \ge 1\).
3.2 Improving the decay rate
We now begin our proof of Theorem 1.1. We will show convergence for the linear and nonlinear approximations separately. The convergence of the linear part is expressed in the next lemma.
Lemma 3.4
Let \(\alpha \in [1,2]\) and \(p \in [1,\infty ]\). Let \(\phi , |x|^2\phi \in L^1\) and \(M := \int _{{\mathbb {R}}^2}\phi (x) \mathop {}\!\mathrm {d}x\). Then
Proof
This lemma is proven analogously to Lemma 3.2. Indeed, by the Taylor expansion
the convergence result becomes clear; and so we omit the details. \(\square \)
Finally, we discuss the nonlinear approximation.
Lemma 3.5
Let \(\alpha \in [1,2]\) and \(p \in [1,\infty ]\).
Then
Proof
The convergence can be shown by a similar method to the bounds from above that we have calculated up to this point. We split the time interval into two halves. The second half is estimated simply using Hölder’s inequality and Young’s convolution inequality. The first half is estimated using the same method as in Sect. 3.1.
The key point is that a faster decay is achieved when taking the difference between the two terms above than when they are estimated separately. This is accomplished by splitting the difference of the integrand as follows:
where
We know that there are faster decay estimates for the two terms in the right hand side of (3.11) than for \((u \cdot \nabla ) \theta \), since the nonlinear part I decays faster than the linear part.
We split the time interval into two halves again. The second half is simply calculated using estimates of \(\theta ,U,I\) that we have seen above. For the first half of the time interval, we again split up the proof into the \(p\ge 2\) and \(1\le p <2\) cases.
Step 1 (First half of time interval, \(p\ge 2\) case) We will show the proof for \(p=2,\) and again the result can be easily extended to all greater values of p afterwards. We handle the two terms in (3.11) separately.
which proves that
The convergence of the second term \(N\big ( I(s), \theta (s) \big )\) follows from almost the same argument as above, by applying the decay of \(\theta \) instead of U.
Step 2 (First half of time interval, \(1 \le p < 2\) case) We again take the terms from (3.11), and use the same technique as was used for the bound from above in Sect. 3.1. That is, we split the Fourier multiplier and divide the time-integral into two halves, and split the space into squares \(Q_{t,k}\). We omit the details. \(\square \)
3.3 Optimal decay of nonlinear term
We lastly discuss the optimality (in the \(p=2\) case) of our estimate in Lemma 3.3. The decay rate for our estimate from above is optimal if we can bound the nonlinear estimate from below by the same power of t. That is, we need
for all \(\alpha \in [1,2]\), and \(t>0\) sufficiently large.
Since we are taking the \(L^2\)-norm, taking the Fourier Transform inside the norm does not change its value.
We rewrite the divergence operator and Riesz transform as two separate Fourier multipliers.
Let
The key difference between these two multipliers is that the numerator of \(m_1\) features a second-order derivative, whereas that of \(m_2\) has a third-order derivative. We show that, for some initial data \(\theta _0\), the first part with \(m_1\) has the optimal decay and the remainder with \(m_2\) is smaller.
Lemma 3.6
Let \(\delta , \epsilon > 0\). Let \(\theta _0 \in W^{1,1} \cap W^{1,\infty }\) as before, but with the following additional conditions:
-
\(\hat{\theta }_0 \ge 0, \text { on } {\mathbb {R}}^2\),
-
\(\text { supp }\hat{\theta }_0 \subseteq \{ \xi \in {\mathbb {R}}^2 \ | \ |\xi _2| < \delta |\xi _1| \}\),
-
\(\hat{\theta }_0(\xi ) \ge C, \text { for some } C>0, \text { for all } \xi \in \text { supp }\hat{\theta }\cap \{ \xi \in {\mathbb {R}}^2 \ | \ |\xi | \le 1 \}\).
Then, for sufficiently small \(\delta \) and \(\epsilon \), we have
Proof
We consider (3.14) and (3.13) separately. Beginning with (3.14), we consider just the \(j=1\) part, as the estimates of both terms are identical.
as \(\hat{\theta }_0\) is bounded. We bound the above norm by considering the integral
Note that, by making the substitution \(\eta \rightarrow \xi - \eta \), we can rewrite the integral as
where we have split the integral into three parts with \(|\eta |\) small, \(|\eta |\) close to \(|\xi |\), and \(|\eta |\) large. We start with the small part.
Next we take \(|\eta |\) large.
and finally we take \(|\eta |\) close to \(|\xi |\).
Therefore, we obtain
We note that all of these terms are smaller than
for \(\epsilon < 1\) and \(t > 1\), and thus we have (3.14).
We next will show (3.13), for sufficiently small \(\epsilon \), and for sufficiently large t. We begin by labelling the two terms in our integral.
Our plan is to make (L) the larger term. This is accomplished by the conditions on \(\theta _0\) that we have imposed. Taking the norm of (L) on its own,
where in the first step we made use of the shape of\(\text { supp }\hat{\theta }_0\), and in the second we used the fact that the integrands are positive and the bound from below for \(\hat{\theta }_0\) on\(\text { supp }\hat{\theta }_0\) close to 0. We next convert the integral over \(\eta \) to polar coordinates and use substitution of variables to produce the final powers of t in the subcritical case, and the \(\ln \) function in the critical case.
Finally, by our setting of\(\text { supp }\hat{\theta }_0\), we obtain
by estimations of integrals similar to before. Thus we obtain (3.13). \(\square \)
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Acknowledgements
T. Iwabuchi was supported by JSPS Grant-in-Aid for Young Scientists (A) (No. 17H04824).
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Ó hAodha, D., Iwabuchi, T. Large-time behaviour of solutions to the surface quasi-geostrophic equation. Partial Differ. Equ. Appl. 3, 60 (2022). https://doi.org/10.1007/s42985-022-00197-w
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DOI: https://doi.org/10.1007/s42985-022-00197-w