Optimal estimates for far field asymptotics of solutions to the quasi-geostrophic equation
Masakazu Yamamoto, Yuusuke Sugiyama

TL;DR
This paper provides uniform estimates for the far field asymptotics of solutions to the critical and supercritical two-dimensional dissipative quasi-geostrophic equation, highlighting the slow decay due to anomalous diffusion.
Contribution
It offers new uniform estimates for the far field behavior of solutions, advancing understanding of decay properties in critical and supercritical cases.
Findings
Established uniform estimates for solutions' far field asymptotics
Demonstrated slow decay of solutions due to anomalous diffusion
Enhanced understanding of decay behavior in quasi-geostrophic equations
Abstract
The initial value problem for the two dimensional dissipative quasi-geostrophic equation of the critical and the supercritical cases is considered. Anomalous diffusion on this equation provides slow decay of solutions as the spatial parameter tends to infinity. In this paper, uniform estimates for far field asymptotics of solutions are given.
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**Optimal Estimates for Far Field Asymptotics of Solutions to the Quasi-Geostrophic Equation
** Masakazu Yamamoto111Graduate School of Science and Technology, Niigata University, Niigata 950-2181, Japan Yuusuke Sugiyama222Department of Engineering, The University of Shiga Prefecture, Hikone 522-8533, Japan
Abstract.
The initial value problem for the two dimensional dissipative quasi-geostrophic equation of the critical and the supercritical cases is considered. Anomalous diffusion on this equation provides slow decay of solutions as the spatial parameter tends to infinity. In this paper, uniform estimates for far field asymptotics of solutions are given.
1. Introduction
We derive far field asymptotics of solutions of the following initial-value problem:
[TABLE]
where for , and for . The unknown function stands for the potential temperature and is the stream function (cf.[8]). The fluid velocity is represented by and is the Riesz transform. When and , the scaling property of (1.1) is in the critical and the supercritical, respectively. In those cases, it is well-known that some smallness and smoothness for the initial-data are required to obtain the global existence of solutions in time. Global existence of solutions in scale-invariant spaces is important problem also in the study for the Navier-Stokes flow. Especially the critical quasi-geostrophic equation has similar stracture as the Navier-Stokes equations. Furthermore, in the critical and the supercritical cases, the quasi-geostrophic equation seems to be elliptic and hyperbolic, respectively. Hence the several methods for parabolic equations are not working for (1.1). Because of those reasons, the quasi-geostrophic equation is considered by many authors (see [5, 6, 7, 9, 13, 14, 17, 22]). In this paper, we treat the global solution in time which satisfies that
[TABLE]
Then the mass-conservation and the uniform decay in time hold:
[TABLE]
Those properties are confirmed initial data that is small and smooth. In the recent paper [30], the smoothness and the upper bound of spatial decay of the solution are proved. Namely, upon the condition for and for , the solution satisfies that
[TABLE]
and
[TABLE]
Those estimates are optimal since the fundamental solution of the linear equation fulfills that and . When , this fundamental solution is given by the Poisson kernel . Moreover the lower bound of spatial decay is derived in [30]:
[TABLE]
where , and for and for . Since and , (1.6) intends that and are canceled in far field. Therefore the asymptotic profile of as is presented by . This idea is developed from pointwise-estimates for Navier-Stokes flow via Miyakawa [23], and Miyakawa and Schonbek [24], and firstly applied by Brandolese [2], and Brandolese and Vigneron [3]. A main goal of this paper is to show the uniform estimate of the spatial decay of the solution. Specifically, we provide the similar estimate as (1.6) in . For solutions to the fractional diffusion equation with and some suitable , general theory of spatial decay is given by Brandolese and Karch [4]. This theory is based on the - estimates for and available for (1.1) in the subcritical case since (1.1) is parabolic in this case. However, since the nonlinearity balances to the dissipation in , the general theory does not work in the case that . More precisely, it is diffucult to estimate the nonlinear term in the integral equation in usual way, since is not integrable near , which requires to estimate in the weighted Sobolev spaces with some positive differential order. In particular, we estimate by using the energy method (cf.[29]). Furthermore we prepare some uniform decay properties for (see Lemmas 2.6 and 2.7). We note that the Moser-Nash iteration method is not used, which is usually employed in order to obtain estimate from (e.g.[10, 18, 26]). In [30], the estimate (1.6) is derived by the energy method. The proof of the uniform estimate (1.7) in the main theorem is based on the - argument. We can express the spatial decay of the solution both in the critical and the supercritical cases.
Theorem 1.1**.**
Let and . Assume that is sufficiently small, and the solution fulfills (1.2) and (1.3). Then
[TABLE]
where .
We emphasize that . Thus Theorem 1.1 states that and are canceled uniformly in far field. We remark that the assertions in this theorem is sharp in time. Indeed, (1.7) for instead of is fulfilled (see Lemma 2.7 in Section 2), and the scaling property of guarantees the sharpness of those estimates. Namely, from the mean value theorem, we expect that the decay-rate of the top term of is given by one of , and and . The details are in the proof of Lemma 2.7. Furthermore (1.7) is optimal also in since for any . A coupling of this theorem and the property of provides the obvious decay as follows.
Corollary 1.2**.**
Let be radially symmetric and monotone increasing in , and satisfy that as . Let and . Assume that the solution fulfills (1.2), (1.3), and (1.4) for . Then, for any fixed ,
[TABLE]
as , where and .
We should remark that on Theorem 1.1 and Corollary 1.2 fulfill (1.5) for any . Indeed, if , then Proposition 2.6 in Section 2 yields (1.5), and we confirm that
[TABLE]
Notation. The Fourier transform and its inverse are defined by and , where . The derivations are abbreviated by for and . The fractional Laplacian and its inverse, and the Riesz transform are defined by for , and for , respectively. The Hölder conjugate of is denoted by , i.e., . For . For some operators and . Various positive constants and suitable fuctions are denoted by and , respectively.
2. Preliminaries
The Duhamel principle yields that
[TABLE]
where . It is well-known that
[TABLE]
for , and
[TABLE]
for and (see[19, 30]). The spatial decay of is published as the following (cf.[1]):
[TABLE]
as , where is introduced in Corollary 1.2. The following lemma plays a crucial role in the energy estimates.
Lemma 2.1** (Stroock-Varopoulos inequality [9, 13, 20]).**
Let and . Then
[TABLE]
holds.
We need the following inequalities of Sobolev type.
Lemma 2.2** (Hardy-Littlewood-Sobolev’s inequality [28, 31]).**
Let and . Then there exists a positive constant such that
[TABLE]
for any .
Lemma 2.3** (Gagliardo-Nirenberg inequality [11, 15, 25]).**
Let and . Then
[TABLE]
holds.
To care the Riesz transforms, we call the following Hörmander-Mikhlin type estimate.
Lemma 2.4** (Hörmander-Mikhlin inequality [12, 21, 27]).**
Let and . Assume that satisfies the following conditions:
- •
* for any with ;*
- •
* for and with .*
Then
[TABLE]
holds.
For the details of this Lemma, see [27]. The following proposition is confirmed in [9, 14, 30].
Proposition 2.5**.**
Let and be small. Assume that the solution satisfies (1.2) and (1.3). Then (1.4) holds.
The authors proved the following proposition in [30].
Proposition 2.6**.**
Let and . Assume that the solution of (1.1) satiefies (1.2) and (1.3). Then (1.5) holds.
The term of initial-data on (2.1) satisfies the following lemma.
Lemma 2.7**.**
Let and . Then
[TABLE]
for , where .
Proof.
The mean value theorem gives that
[TABLE]
The first term fulfills that
[TABLE]
From (2.2) and (2.3), for and , we see that and then
[TABLE]
Thus, we have that
[TABLE]
and conclude the proof. ∎
Lemma 2.8**.**
Let and , where is defined in Corollary 1.2. Then, for any ,
[TABLE]
as , where .
Proof.
We use (2.5). For the first term, we see that
[TABLE]
as . For the second term on (2.5), we choose sufficiently small and , then we have by the similar argument as in the proof of Lemma 2.7 that
[TABLE]
as . Here we remark that and
[TABLE]
Hence we complete the proof. ∎
3. Proof of main theorems
To show our main assertions, we prepare the estimate for the nonlinear effect. We denote the nonlinear term on (2.1) by , i.e.,
[TABLE]
Then decay-rate of as is published as follows.
Proposition 3.1**.**
Let and . Assume that the solution fulfills (1.3) and (1.4) for . Then defined by (3.1) satisfies that .
Proof.
From the definition, we see for that
[TABLE]
where is the -th component of . Hence
[TABLE]
From (1.3)-(1.5), (2.2) and (2.3), we see that the first and the third terms are bounded by . We estimate the second, the fourth and the fifth terms later. To care the last term, we prepare the estimate for . We derivate the first equality on (1.1) in and multiply . Then, by integrating it in and employing Lemma 2.1, we see for the second and the last terms that
[TABLE]
and
[TABLE]
Here we used the relation . Therefore we have that
[TABLE]
From (2.1) and Hausdorf-Young’s inequality, we see that
[TABLE]
Here we used the scaling property . We remark that Lemma 2.4 guarantees that . The relation and the smallness of conclude that . Hence for the second term on (3.3) and some small , we have that
[TABLE]
For the third term on (3.3), we see for that
[TABLE]
Here we used the Sobolev inequality for . Lemma 2.3 with Proposition 2.5 guarantees that and . Hence
[TABLE]
Calculus on the Fourier symbol yield that . Thus, for ,
[TABLE]
Since , we have from the Sobolev inequality with (1.5) that
[TABLE]
Therefore
[TABLE]
Consequently, applying (3.4)-(3.6) to (3.3),
[TABLE]
We back to the estimate for the last term on (3.2). Since , this term fulfills that
[TABLE]
Here (1.4) and (3.7) yield that
[TABLE]
Concurrently, if we choose sufficiently near from , then for ,
[TABLE]
Therefore
[TABLE]
Similarly, for the second term on (3.2), we obtain that
[TABLE]
The fourth term on (3.2) also is bouded by . For the fifth term on (3.2), we see from (3.7) that
[TABLE]
Applying those estimates to (3.2), we complete the proof. ∎
Finally, Lemma 2.7 and Proposition 3.1 show Theorem 1.1. Also we conclude Corollary 1.2 from (2.4), Lemma 2.8 and Proposition 3.1.
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