Smooth stationary water waves with exponentially localized vorticity
Mats Ehrnstr\"om, Samuel Walsh, Chongchun Zeng

TL;DR
This paper demonstrates the existence of large families of stationary water waves with finite energy and exponentially localized vorticity, using advanced mathematical techniques from elliptic equations and water wave theory.
Contribution
It introduces a novel construction of stationary water waves with localized vorticity, expanding understanding of wave solutions with specific vorticity distributions.
Findings
Existence of large families of such waves.
Waves carry finite energy.
Vorticity is exponentially localized.
Abstract
We study stationary capillary-gravity waves in a two-dimensional body of water that rests above a flat ocean bed and below vacuum. This system is described by the Euler equations with a free surface. Our main result states that there exist large families of such waves that carry finite energy and exhibit an exponentially localized distribution of (nontrivial) vorticity. This is accomplished by combining ideas drawn from the theory of spike-layer solutions to singularly perturbed elliptic equations, with techniques from the study of steady solutions of the water wave problem.
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Taxonomy
TopicsNavier-Stokes equation solutions · Ocean Waves and Remote Sensing · Aquatic and Environmental Studies
Smooth stationary water waves with exponentially localized vorticity
Mats Ehrnström
Department of Mathematical Sciences, Norwegian University of Science and Technology, 7491 Trondheim, Norway
,
Samuel Walsh
Department of Mathematics, University of Missouri, Columbia, MO 65211
and
Chongchun Zeng
School of Mathematics, Georgia Institute of Technology, Atlanta, GA 30332
Abstract.
We study stationary capillary-gravity waves in a two-dimensional body of water that rests above a flat ocean bed and below vacuum. This system is described by the Euler equations with a free surface. A great deal of recent activity has focused on finding waves with nontrivial vorticity . There are now many results on the existence of solutions to this problem for which the vorticity is non-vanishing at infinity, and several authors have constructed waves with having compact support. Our main theorem states that there are large families of stationary capillary-gravity waves that carry finite energy and exhibit an exponentially localized distribution of vorticity. They are solitary waves in the sense that the free surface is asymptotically flat. Remarkably, while their amplitude is small, the kinetic energy is . In this and other respects, they are strikingly different from previously known rotational water waves.
To construct these solutions, we exploit a previously unobserved connection between the steady water wave problem on the one hand and singularly perturbed elliptic PDE on the other. Indeed, our result expands the study of spike-layer solutions to free boundary problems with physical relevance.
ME was supported by grant nos. 231668 and 250070 from the Research Council of Norway.
SW was supported by the National Science Foundation through the awards DMS-1514910 and DMS-1812436.
CZ was supported in part by the National Science Foundation through the award DMS-1900083.
1. Introduction
We consider waves in a two-dimensional body of water that has finite depth. Mathematically, they are modeled as solutions to the incompressible Euler equation
[TABLE]
The kinematic boundary conditions state that the velocity field does not penetrate the bed:
[TABLE]
and, along the free surface, we have
[TABLE]
Lastly, on the surface we impose the dynamic condition according to the Young–Laplace law that
[TABLE]
where is a constant measuring the surface tension and
[TABLE]
is the signed curvature. Because , we always presume that surface tension is present on the interface and that gravity acts in the bulk. Solutions of (1.1) are therefore called capillary-gravity waves.
A stationary water wave is a solution to (1.1) that is independent of time. More generally, one can consider steady or traveling waves, which are solutions that become time independent after shifting to a moving frame of reference. These are among the oldest and most important examples of nonlinear wave phenomena studied in mathematics.
Perhaps the central object of interest for this paper is the vorticity
[TABLE]
which is the third component of . The earliest rigorous constructions of steady water waves were given by Levi-Civita [30] and Nekrasov [33], who worked in the irrotational regime where vanishes identically. This assumption permits several elegant reformulations of the problem that are far more tractable; see, for example, the survey [41]. However, beginning in the early 2000s, substantial inroads have been made in the rigorous analysis of rotational water waves. With a few exceptions, these results pertain to waves without interior stagnation, meaning that the streamlines (the integral curves of ) are never closed, and hence the vorticity does not vanish at infinity.
In practice, though, many of the effects that generate vorticity are local — wind blowing over a section of the water or a boundary layer caused by an immersed body, for example. This naturally leads us to seek waves for which is concentrated in the near field. A completely different analytical approach is necessary to treat this situation, however. Consequently, there are comparatively very few rigorous results for waves with localized vorticity, and those that are available concern either periodic waves or waves with compactly supported vorticity; see the overview below.
Another important quantity associated to the system is the total energy defined by
[TABLE]
The first term on the right-hand side represents the kinetic energy, while the second is gravitational potential energy, and the third is the surface energy. It is well-known that is conserved by sufficiently smooth solutions of the time-dependent problem. It is physically desirable, therefore, to construct waves that carry a finite amount of total energy, which in particular means that must be in .
As the main contribution of this paper, we prove the existence of large families of solitary stationary water waves with a smooth, highly localized vorticity and a finite energy : in a perturbed disk around the origin the vorticity is large and negative, and outside it is positive and exponentially decaying. Qualitatively, this represent an entirely novel species of water wave that we call a vortex spike. Our method establishes a connection between singularly perturbed elliptic equations and physical problems with free boundaries. This application to water waves is at once quite natural and yet completely new.
1.1. Main theorem
We now state the result more precisely. In two dimensions, divergence free vector fields can be represented through a stream function, namely,
[TABLE]
One can easily confirm that from (1.3) that .
As mentioned above, our interest is in smooth finite energy stationary waves with spatially highly localized vorticity. For the momentum equation (1.1a), we see satisfies
[TABLE]
and hence the vorticity is transported by the Lagrangian flow. In terms of the stream function, for the stationary case this becomes
[TABLE]
The kinematic boundary conditions (1.1c)–(1.1d) imply that is a constant along each component of . Without loss of generality, we take
[TABLE]
see Section 1.3 for more discussion about this. At the same time, the dynamic condition (1.1e) can be expressed in terms of as the well-known Bernoulli equation
[TABLE]
Together, (1.6)–(1.8) are equivalent to the (stationary) Euler equations (1.1). We seek to construct waves for which the stream function and the vorticity will have the leading order forms
[TABLE]
where , is roughly the location of the vorticity to be determined in the proof which will turn out to be very close to the origin in out coordinate system, and is a smooth solution to (1.6) on the whole of , exponentially decaying as . It is well known that (1.6) is satisfied provided that , for some vorticity function . We therefore construct as the solution to
[TABLE]
with a solution to
[TABLE]
We will assume that satisfies the following.
- (A)
, , , , and (1.11) has a nontrivial radial solution satisfying as , and 2. (B)
the kernel of is equal to .
We would like to point out that the asymptotic vanishing of and at can be ensured by further asking that or , see Remark 3.4. Also, as a consequence of (A), and its derivatives up to order decay exponentially, and so in particular, , see Proposition 3.1. Prototypical functions fulfilling assumptions (A) and (B) are , for integers , but many others will do as well. Classical results for dimension may be found in for example [2, 3, 28], and a modern summary including the non-degeneracy results in [1].
Under the above assumptions, our main theorem is as follows.
Theorem 1.1**.**
For any as in Assumptions (A) and (B), there exists such that, for each , there is a finite energy solution
[TABLE]
to the stationary water wave problem (1.7), (1.8), and (1.10). Both and are even in . Moreover, there exists a constant , independent of but depending on , such that for each there exists with satisfying
[TABLE]
where
[TABLE]
and
[TABLE]
with
[TABLE]
We first comment on the vorticity and the surface profile given in the above theorem. On the one hand, from Proposition 3.1, Corollary 3.5 and (1.12), we see that the kinetic energy is of . Roughly,
[TABLE]
while the corresponding vorticity is spiked in the sense that
[TABLE]
On the other hand, the total vorticity is exponentially small in :
[TABLE]
By (1.12) and the definition of , for any as , where is the characteristic function of . Then from the above integral estimate we can readily prove as for any continuous compactly supported in . Therefore, as a measure, converges weakly to [math] as . However, the vorticity has a rich spatial structure in a domain on the scale of where its point-wise value is . Moreover, as is in , these waves exhibit a highly localized but strong rotational vector field with kinetic energy of order .
Since concentrates far away from and the total vorticity is exponentially small, is only weakly impacted by the spike. This fact is reflected in the exponential smallness of in (1.13). According to Proposition 3.1, the leading term given in (1.13) satisfies for for some independent of , while its tail is much smaller. Therefore the concentrated vorticity creates a surface depression in the near field with rapid decay as ; see Figure 1.
1.2. History and relation to our construction
Rotational steady water waves have been a very active area of research for nearly two decades, beginning with the construction of large-amplitude periodic gravity waves by Constantin and Strauss [11]. These authors used bifurcation theory starting from a fixed shear flow, and their methodology has since been adapted and expanded upon in many ways, see [9]. It is important to note that, while there do exist explicit rotational water waves (for example, [22, 15, 26, 6, 24]), they are exceedingly rare. From that perspective, the main contribution of [11] was its systematic treatment of a broad class of vorticity distributions. However, Constantin–Strauss — and most of the works that followed them — require both that is non-localized and that there are no interior stagnation points. In particular, smooth perturbation of a shear flow could never yield decaying vorticity. Interior stagnation and critical layers (regions of closed streamlines), however, can be constructed using variants of this approach. Early papers of Simmem and Saffman [38] and da Silva and Peregrine [16] considered this regime through formal asymptotic analysis and numerical bifurcation theory. In [18], it was rigorously shown that the nonlinear particle paths in the linearized system can have closed orbits, and the behavior of small waves with constant vorticity was studied. Based on it, Wahlén [44] constructed exact periodic waves with one critical layer, and similar waves were subsequently constructed using a harmonic-functions approach, globally, in [13]. These works all treat constant vorticity and the situation where the linearized problem at the shear flow has a one-dimensional kernel. One can also find steady waves with critical layers bifurcating from two-dimensional [17], three-dimensional [19], and even arbitrarily high dimensional kernels [27] of affine or near-affine vorticity functions, as well as from one-dimensional kernels of constant vorticity with one discontinuity [32]. Very recently, a global theory for analytic vorticity functions allowing for several critical layers has been presented in [43] (one might note that even affine vorticity can yield arbitrarily many vertically aligned stagnation points.) The waves built in this paper have vorticity functions of the next order in this development, as Assumption (A) implies that is nonlinear with leading-order linear term, although the method of proof is very different.
The first rigorous construction of traveling capillary-gravity waves with localized vorticity in infinite depth is due to Shatah, Walsh, and Zeng [37]. In that paper, two classes of compactly supported vorticity were studied: solitary and periodic waves with a submerged point vortex, and solitary waves with a vortex patch. In the former case, is a Dirac measure supported in the interior of . This can be viewed as a solution to a suitably weakened version of the Euler equations. The proof in [37] was based on a splitting of the velocity field into a rotational and irrotational component, followed by a bifurcation argument beginning at the trivial solution with the total vorticity serving as the parameter. While the vortex patch solutions were small amplitude, the authors obtained a global curve of periodic traveling waves with a point vortex. The vortex patches have finite energy and the corresponding vorticity is and smooth on its support. Later, Varholm [42] extended the ideas in [37] to the finite-depth case with arbitrarily many point vortices, and Le [29] studied the existence and orbital stability of finite dipoles inside an infinite-depth capillary-gravity wave. Earlier work in the 50s and 60s that treated point vortices carried by gravity waves in finite depth include [40, 21, 20]. A vortex patch situated near a shoreline and such that the velocity vanishes completely outside a ball has also been constructed in [8], using dynamical systems tools.
The capillary-gravity waves in the current work can be said to live between the above-mentioned types. They can be viewed, for , as smoothed vortex patches or as the limit, as the period tends to infinity, of steady periodic waves with critical-layers. We note that in [37], (i) is single-signed and either a Dirac measure or in ; and (ii) the measure vanishes absolutely as one approaches the point of bifurcation. By contrast, in the present paper, the vorticity changes sign and is smooth throughout . Moreover, converges to [math] weakly as , while the norm of and the kinetic energy both remain order . This surprising feature results from the fact that we do not perturb from a shear flow, but singularly from of (1.11) which has fixed, positive energy. In all these respects, the vortex spikes constructed in Theorem 1.1 contrast starkly with the literature described above.
When is not compactly supported, it is of little help to decompose the velocity field into rotational and irrotational parts. We are also barred from using shear flows as a model for the stream function. The main new idea is to instead look to the theory of spike and spike-layer solutions to singular perturbations of semi-linear elliptic PDE. These equations typically have the form
[TABLE]
where is a smooth bounded domain, , and Dirichlet or Neumann conditions are prescribed on . Beginning in the late 80s, versions of (1.14) were investigated intensively by the elliptic PDE community resulting in a vast literature; see, for example, [34, 31, 36, 35].
Drawing inspiration from these works, we model our stream function as a rescaled and translated on the unknown fluid domain represented by a conformal mapping . The translation invariance of the problem leads to a degeneracy — as can be seen in Assumption (B) — which is resolved through a Lyapunov–Schmidt reduction. We outline heuristically how to solve the resulting highly degenerate bifurcation equation for in the next subsection.
To the best of our knowledge, ours is the first work exploring singularly perturbed elliptic equations in the hydrodynamical context. The method bears certain similarities to Li and Nirenberg’s treatment of (1.14) in [31], in particular, the use of a Lyapunov–Schmidt reduction, bundle coordinates in a tubular neighborhood of a family of translates, and boundary correction projections. However, we stress that the steady water wave problem presents substantial new difficulties: the upper boundary is free, the Bernoulli condition (1.8) imposed there is completely nonlinear, and the domain is horizontally unbounded.
1.3. Heuristic discussions
In this subsection, we discuss several issues related to the finite energy/spatial decaying assumptions on smooth steady (stationary or traveling) solutions on fluid domains extending to horizontal infinity. We first observe that the support of the vorticity of such solutions should be the whole of . Otherwise, one expects that the vorticity will not be smooth over the boundary of its support, as a consequence of the Hopf lemma for the elliptic equation (1.10).
Traveling waves.
While we focus on stationary capillary-gravity waves in the current paper, by shifting to a moving reference frame, Theorem 1.1 immediately furnishes families of traveling capillary-gravity waves with exponentially localized vorticity. The velocity field for these waves will be an perturbation of a fixed uniform background current , and the vorticity will be spiked in the same sense as before.
On the other hand, smooth finite-energy waves with a non-zero wavespeed are unlikely to exist. In fact, the vorticity level curves for such waves would be closed loops , which are transported by the velocity field . Therefore
[TABLE]
where is the unit outward normal vector of . This implies that if , which usually happens on an proportion of most level curves. Consequently, is likely to be bounded from below on a set with infinite measure, which is prevented by the finite energy assumption.
Fluid depth and the boundary condition of the stream function.
In [37], traveling capillary-gravity waves with compact vortex patches were constructed in fluids of infinite depth. Slightly modifying the formula of the rotational part of the velocity fields, actually the same construction should also work with finite depth. However, we do not expect smooth spatially localized stationary waves to exist in infinite depth unless the free surface is overturned.
In fact, let us temporarily not preclude the possibility of with infinite depth. Let a solution of (1.10) be given satisfying and with the outward unit normal to . The latter condition implies that is locally constant on . Fix on .
Much as in the proof of Proposition 3.1, and its derivatives decay exponentially as . Let be the antiderivative of with . We multiply (1.10) by and integrate to find
[TABLE]
where in the last step above we used that is locally constant on and thus holds there.
The first implication of this equality is that if is nontrivial, then . Otherwise we would have with , which is impossible. This argument does not rely on anything but the regularity of , in particular, we do not need the full strength of Assumption (A) or (B). Non-existence of deep water solitary waves in the presence of algebraically localized vorticity has been more thoroughly investigated in the recent paper [4]; see also [14, 39, 25, 45] for results on the irrotational case.
Now suppose instead that the domain is finite depth, and set , with denoting the flat rigid lower boundary. Suppose also that . The properties (i) as ; (ii) ; and (iii) is locally constant on , together imply that based on a simple Hölder estimate on along vertical lines. Therefore, from (1.15), we infer that
[TABLE]
The reduced (degenerate) equation from the Lyapunov–Schmidt reduction.
Equation (1.16) is the key to the proof of our main theorem. As mentioned above, we first carry out a Lyapunov–Schmidt reduction argument to reduce the problem to a highly degenerate one-dimensional “bifurcation” equation with the parameter as in Theorem 1.1. One of the usual techniques to handle those somewhat degenerate bifurcation equations is to first use a blow-up argument to search for a non-degenerate direction of the linearized problem, then employ the implicit function theorem. Even though Proposition 4.5 does imply such linear invertibility of the bifurcation equation, the non-degeneracy we find is far too weak for an (obvious) application of the implicit function theorem to be effective.
Instead, in Section 5 we show that the bifurcation equation is equivalent to the above (1.16). Now, on the free surface, , while on the flat bed . If is highly localized close to the surface, then the integral there should dominate so that the left-hand side of (1.16) would be positive, and conversely for concentrated near the bed. This mandates a balancing between the contributions on the surface and bed. That observation is at the heart of the analysis in the last part of Section 5. It also reveals the importance of the translation parameter .
Non-flat bottom and more.
With some modifications, the approach of the current paper should also apply when the bed has nontrivial topography111This question was also raised by Shuangjie Peng and Shusen Yan during a talk given by the third author.. Indeed, suppose , where is now a horizontally asymptotically flat rigid bottom, for simplicity taken even in . Thus we expect the vorticity to be localized at for some . We can parametrize the unknown by a conformal mapping defined on a fixed domain above and below . Based on Proposition 3.1, one may adjust the basic estimates in Sections 3 and 4 accordingly to carry out the Lyapunov–Schmidt reduction and arrive at a highly degenerate one-dimensional reduced bifurcation equation that would still turn out to be equivalent to (1.16). As in the current paper, the distance from would again play a crucial role. Let
[TABLE]
Much like [31], stationary solutions are expected to exist with a localized vorticity concentrated near strict local maximums of . However, when multiple localized vorticity locations are considered or when is not necessarily even in , a sphere packing problem arises. See, for example, [23].
Lastly, we remark that it would be very interesting, though quite difficult, to study gravity water waves with a spike vortex. Surface tension allows us to treat the Bernoulli condition (1.8) essentially as an elliptic problem on the boundary. In fact, the linear part is invertible, which greatly simplifies the analysis; see the proof of Lemma 5.2. Perhaps with much more careful estimates it would be possible to allow for .
1.4. Plan
We begin, in Section 2, by rewriting the stationary water wave problem into an analytically more tractable form. Using a conformal mapping , the fluid domain is pulled back to a fixed slab of width ; this mapping becomes one of the unknowns, taking the place of . We impose the desired ansatz (1.9) on the stream function, thereby reformulating the problem in terms of the deviation of from a translated and rescaled solution to (1.11).
In Section 3, we obtain leading-order approximations of and a boundary correction operator as well as rather precise exponentially small bounds on the remainders.
Section 4 is devoted to the study of the linearized problem at an approximate solution. Specifically, we prove that there is a small simple eigenvalue related to the direction of . The linearized problem is uniformly non-degenerate in the complementary codimension-1 directions.
All of these tools are used in Section 5 to prove Theorem 1.1. Adopting bundle-type coordinates over , we carry out a Lyapunov–Schmidt reduction in the non-degenerate codimension-1 directions to reduce the problem to a one-dimensional bifurcation equation. As mentioned above, this bifurcation equation is equivalent to (1.16) and the proof is completed by invoking the intermediate value theorem. Here the idea of balancing the two surface integrals is made rigorous through careful estimates of all the quantities involved. Indeed, while this analysis is quite delicate, the simple identity (1.16) is the key to the argument.
Notation.
Throughout the paper , and indicate relations that are valid up to a positive factor which can be chosen uniformly in small enough and . Complex scalars are sometimes viewed as 2-d real vectors, hence “” between complex quantities denotes their dot product. For a given function defined on certain domain, we often use to denote the -orthogonal complement of . We also use .
2. Reformulation
As the first step toward proving Theorem 1.1, the stationary water wave problem (1.10), (1.7), and (1.8) will be reformulated on a fixed domain, and we will build in the spike ansatz for the stream function mentioned in (1.9). The final product of these efforts is an equivalent transformed problem (2.24) that is posed on an infinite strip.
2.1. Rescaling and parametrization
We start by introducing new coordinates that eliminate the free boundary. As mentioned in the introduction, this can be achieved at little cost in the irrotational regime; see, for example, [12, 7]. With vorticity, however, one expect to pay a price in the form of increased complexity of the equations. Given that the highest-order operator in the semi-linear equation (1.10) is the Laplacian, it is natural to work with conformal mappings. With that in mind, define the reference domain to be , which we identify with the complex strip
[TABLE]
We will look for fluid domains that are expressed as the image of the reference domain under a near-identity holomorphic mapping. Specifically, let be holomorphic and satisfy
[TABLE]
Note this implies that is odd and is even. Such a conformal mapping is uniquely determined by . In fact, since is harmonic,
[TABLE]
where denotes the Fourier transform in the variable. By construction, vanishes on the bottom of the domain, and hence it depends analytically upon its trace on the upper boundary, . Explicitly,
[TABLE]
so we have
[TABLE]
and
[TABLE]
Observe that above is the Dirichlet–Neumann operator on the strip with a homogeneous Dirichlet condition imposed on the lower boundary. The real part is a harmonic conjugate of whose one degree of freedom is fixed by the symmetry in .
The corresponding fluid domain is taken to be
[TABLE]
It follows that the free surface is parameterized by , for ranging over . This curve can also be written as the graph
[TABLE]
The stream function can be pulled back,
[TABLE]
yielding a new unknown defined on the fixed reference domain. Then the water wave problem (1.10), (1.7), and (1.8) become
[TABLE]
together with the transformed Bernoulli condition
[TABLE]
where we used that along due to the boundary condition on . Here in view of the fact that is holomorphic, and
[TABLE]
is the signed curvature of the interface.
Recalling the scaling in (1.9), we define
[TABLE]
which then solves a non-dimensionalized version of the problem for set on the slab
[TABLE]
It is important to realize that this domain is decreasing in , so that in particular . Now it is easy to compute that satisfies the elliptic equation
[TABLE]
and the Bernoulli condition translates to
[TABLE]
2.2. Boundary correction
Our overarching strategy is to model , and by extension , on a rescaled of (1.11). However, while is exponentially localized, it does not satisfy the homogeneous boundary conditions in (2.9). We therefore perform a boundary correction, modeled on Assumption (A), subtracting a function from that shares its trace but is exceedingly smaller in the interior.
For any real-valued function in a reasonable Sobolev space (see below) defined on , we introduce the extension operator
[TABLE]
defined uniquely by
[TABLE]
where is the restriction of on , and we are using the Japanese bracket notation . Provided that , , the function is an -solution222In general the solution of (2.12) need not be unique, as is an infinite slab. of
[TABLE]
Observe that, due to the localization of and the assumption , the above problem closely resembles the linearized operator away from the origin. It is worth noting that, for any ,
[TABLE]
2.3. The perturbed problem
Let be given by Assumption (A). As discussed in Section 1, it will be important to consider vertical translates of this function. For each , let
[TABLE]
With a slight abuse of notation we shall still write to denote the function , except when the precise value of becomes important. At other times, it will be more convenient to use the notation rather than . The value is unimportant; we will find waves for exceedingly much smaller. What is important is that the center of vorticity remains closer to the origin than to the boundary of the reference domain, but has no special significance.
We proceed with the ansatz
[TABLE]
where bc denotes the boundary correction from (2.12). Thus measures the deviation of from the rescaled, translated, and boundary corrected . Inserting this into (2.9), we see that it solves the following elliptic PDE set on :
[TABLE]
Here, we have made use of the facts that and . Similarly, the kinematic condition in (2.9) takes the form
[TABLE]
since there.
Consider next the Bernoulli condition (2.10). Direct substitution yields
[TABLE]
From the Cauchy–Riemann equations and
[TABLE]
any derivatives involving can be expressed in terms of derivatives of . Making this replacement in (2.17) yields
[TABLE]
Here, all terms involving are evaluated at . The idea is that, to the leading order in terms of , the right-hand side of (2.18) is determined by the operator acting on , which is invertible for all . To make this rigorous, let
[TABLE]
be the trace of on the top of the reference domain . We have from (2.18) and (2.3)
[TABLE]
where , , and . Let be a linear operator depending on acting on as
[TABLE]
Notice also that preserves the even-odd parity. For a given smooth , is a zero-order operator on any Sobolev space , , where here and elsewhere the subscript ‘e’ indicates that the functions are even in . More precisely, if for , then the map333Note here that the lower right used in stands for ‘surface’, while the slanted is a (general) regularity index.
[TABLE]
Recall here that is the continuous dual of , whence the lower bound is needed to ensure that products can be made sense of when applying to . Now and we have the bound
[TABLE]
Thus is invertible for . We can now isolate the leading-order terms in (2.20) by applying to it:
[TABLE]
which is valid as long as .
Now we are roughly in a position to make a rigorous statement of our problem. For any , we define
[TABLE]
Summarizing the analysis of this section, we see that if , , and satisfy
[TABLE]
where and are the mappings
[TABLE]
and
[TABLE]
then , reconstructed via (2.5), (2.7), (2.14), (2.1), (2.19), and the Cauchy-Riemann equations, will solve the stationary water wave problem (1.10), (1.7), and (1.8). Recall here that is a shorthand for . For the class of satisfying Assumption (A) and Assumption (B), the mappings and are well defined and continuously differentiable given some basic estimates on and that are derived in the next section. For that reason, we postpone making a precise statement, or offering a proof, until Lemma 3.8.
3. Estimates of and its boundary corrections
This section is devoted to the estimates of , its derivatives, and boundary corrections of the same functions, assuming that Assumptions (A) and (B) from Section 1 hold. Finally, we give some estimates of the nonlinearities and , defined in (2.25) and (2.26), in the elliptic system (2.24), which is equivalent to the original problem (1.10), (1.7), and (1.8) of finding stationary water waves.
Estimates for , , and
We start with some basic estimates on . Recall from Assumption (A) that , for a fixed integer .
Proposition 3.1**.**
Under Assumptions (A) and (B), there exists such that
[TABLE]
Remark 3.2*.*
As
[TABLE]
and
[TABLE]
when applied to radial functions, we have
[TABLE]
Proposition 3.1 readily induces signs on the Cartesian derivatives of these functions. In particular, globally with
[TABLE]
when . Note also that
[TABLE]
Remark 3.3*.*
For , the function from (2.13) is just a translation of the center and global maximum of the radial function from the origin to . It follows that Proposition 3.1 applies to with changed accordingly.
Remark 3.4*.*
The solution to (1.11) is often obtained through a variational approach carried out in space. In fact, for any satisfying , any radial solution automatically satisfies the decay assumption in (A). This is due to the inequality
[TABLE]
which implies hence also bounded. The boundedness of yields and thus . Therefore follows from the same argument. Obviously one may also replace by .
Proof of Proposition 3.1.
The decay rate (3.1) is stated by Li and Nirenberg [31] for the case , with a reference to an earlier paper of Berestycki and P. L. Lions [3]. However, while that work could be extended to our setting, as written it does not contain the same sharp result and it is restricted to three or higher dimensions. Here we provide a sketch of a proof that does cover the case of interest; it is based on invariant manifold methods rather than variational techniques. For a reference, see for example [5].
In polar coordinates the semi-linear problem for is
[TABLE]
and thus it suffices to obtain the estimate for , due to the fact . Letting
[TABLE]
we rewrite (3.3) as
[TABLE]
Clearly is an unstable equilibrium of the ODE system with , , and being in the unstable, stable, and the center directions, respectively. Therefore there exists a center-stable manifold in a neighborhood of given by a graph
[TABLE]
Even though the center-stable manifold is usually not unique, the subset is indeed unique because of its positive invariance under the ODE flow. Due to Assumption (A), both the orbit corresponding to as well as the trivial state converge to as . Hence they both belong to . This implies
[TABLE]
Therefore the only orbit on intersecting is the one corresponding to the trivial solution. On , the equation in (3.4) and the above properties of yield
[TABLE]
Using this, we first calculate that
[TABLE]
Therefore is decreasing in for and thus converges absolutely. Moreover the above estimate of on further implies
[TABLE]
Since , the above estimate implies that exists and belongs to , which along with the fact that yields (3.1) for . ∎
The following corollary will be used to analyze the boundary correction operator. For this and the coming results, especially Corollary 3.7, it can be good to consult Figure 2. Note, in particular, that the estimate below essentially concerns the behavior of outside of the slab (on the slab reflected over its own boundaries, modulo the translation .)
Corollary 3.5**.**
For any , , and , and satisfy
[TABLE]
Proof.
We shall focus on as the others can be handled similarly. Consider the following subset of
[TABLE]
Let be the polar coordinates of so that
[TABLE]
Since , we have in , and
[TABLE]
Along with Proposition 3.1, this implies
[TABLE]
Again, it follows from Proposition 3.1 and (3.6) that
[TABLE]
while
[TABLE]
This completes the proof of the corollary. ∎
In order to estimate the boundary correction operator defined in (2.12), we will need the following auxiliary lemma.
Lemma 3.6**.**
Suppose is an integer, , and satisfies
[TABLE]
and
[TABLE]
Then
[TABLE]
satisfies
[TABLE]
Intuitively, this says that the boundary correction of is, to leading order, found by subtracting the reflections of over the top and bottom boundaries of the slab.
Proof.
From the definition of in (2.12), we see that satisfies
[TABLE]
One can immediately deduce the energy estimate
[TABLE]
An upper bound of the first term on the right-hand side above can be obtained much as in the proof of Corollary 3.5, and so we only provide a sketch and focus on the “” case. Let be given as in (3.5), and split the slab . From the properties assumed on , we see that
[TABLE]
The norm can be estimated by interpolating it between and and then appealing to the assumptions on :
[TABLE]
where the substitution was used to evaluate the integral on . Combining the above inequalities concludes the proof of the lemma. ∎
Lemma 3.6 is mainly applied to and for . In fact, (1.11) yields
[TABLE]
and so the assumption that together with Proposition 3.1 ensures that and satisfy the hypotheses of Lemma 3.6. Therefore, in addition to Corollary 3.5 we obtain the following estimates, which will be essential to us later.
Corollary 3.7**.**
For any , and satisfy
[TABLE]
Proof.
The first two inequalities follow directly from Proposition 3.1 and Lemma 3.6. To obtained the estimate on based on the first inequality and Corollary 3.5, we only need to show the almost orthogonality
[TABLE]
In fact, for
[TABLE]
due to the convexity of , there exists independent of , and small such that
[TABLE]
It is also clear that
[TABLE]
Applying these inequalities to and we obtain
[TABLE]
Together with Proposition 3.1 it immediately implies (3.8) and completes the proof of the corollary. ∎
Estimating the nonlinearity
Finally, we give some estimates of the nonlinearities and occurring in the reformulated water wave problem (2.24).
Lemma 3.8**.**
For as in Assumptions (A) and (B) and any integer , there exists depending only on and , such that the operators and given in (2.25) and (2.26) satisfy
[TABLE]
where is the ball in centered at [math] with radius and if and can be any number smaller than if . Moreover, for any , , , and , we have
[TABLE]
and
[TABLE]
Proof.
Verifying the smoothness of and is tedious but straightforward. The argument is based on (i) standard regularity results on products in Sobolev spaces, properties of the harmonic extension, the trace theorem, and (ii) the smoothness of the mapping for a given , which holds for and in dimensions. The limitation on the smoothness of and with respect to is only due to the dependence of in . The small is chosen such that the denominator in the definition of is bounded away from zero and has a bounded inverse, which can be done independent of and small . We omit the details and focus on the quantitative estimates related to and . In what follows, let be the conformal mapping determined by through (2.1) and (2.19). Note that this involves just the harmonic extension (2.2) and harmonic conjugate operators.
From the definition of ,
[TABLE]
which, along with Corollary 3.7, implies that
[TABLE]
Without loss of generality, we only need to consider the “+” term in the summation. According to Assumption (A) and Proposition 3.1, for any and ,
[TABLE]
which can be estimated much as (3.8). Applying (3.9) and (3.10) to and , we have
[TABLE]
and so we have that
[TABLE]
This further implies
[TABLE]
which, with (3.11), furnishes the desired estimate of .
Next, observe that, for any with ,
[TABLE]
Now, for any we have the the scaling identity
[TABLE]
and, for and , it holds that
[TABLE]
Thus, the norm of the last line of (3.13) has the upper bound
[TABLE]
Corollary 3.7 therefore gives the claimed estimate of .
Regarding , we have for any that
[TABLE]
where is the complex holomorphic function determined by . The estimate on follows from this expression and the scaling of the Sobolev norms explained above.
From the definition of , one can directly compute
[TABLE]
Recall the one-dimensional scaling property,
[TABLE]
which holds for all . The term can be estimated by approximating by . From Corollary 3.7 and the trace theorem, we then have, for any ,
[TABLE]
Using Proposition 3.1 and the change of variables , we can estimate while the terms on the right hand-side are obviously much smaller,
[TABLE]
This implies that
[TABLE]
We therefore obtain the estimate on from the scaling property as
[TABLE]
Consider next the bound on . It is easy to see from the definition of that,
[TABLE]
By the trace theorem and (3.17), we have
[TABLE]
The desired bound on then follows from the scaling property.
Finally, for any ,
[TABLE]
Since and with , straightforwardly we obtain
[TABLE]
where the scaling property and the trace theorem have been used. The estimate on now follows immediately from (3.17). ∎
One notices that is not small no matter how small and are. Fortunately this is an “off diagonal term” in the linearization, which will be handled by a simple rescaling argument in Section 5.
4. Spectral properties
Having the necessary estimates on and the boundary correction operator now in hand, we next consider the linear operator
[TABLE]
in the elliptic equation (2.24a). Recall that the Dirichlet boundary conditions on are encoded in the definition of the space , and that we usually suppress the dependence on the translation parameter in the notation for .
The inherent difficulty here is that equation (1.11) implies
[TABLE]
so that is in the kernel of viewed as an operator with domain . Working in the strip breaks the vertical translation symmetry and eliminates this kernel direction. It is therefore expected that will be invertible from , and, indeed, this is proved in Lemma 4.6. However, as , heuristically the strip approximates , and so we cannot hope to obtain bounds for that are uniform in . Another way to see this is to note that
[TABLE]
as and its derivatives decay exponentially. Thus, is nearly degenerate in the direction close to .
In order to proceed, it is therefore necessary to have detailed information about the behavior of as . We will prove that there is a positive (simple) eigenvalue that is exponentially small in for fixed , and whose eigenfunction approaches as . In the orthogonal complement of , the inverse of is bounded uniformly in . In the next section, we will make use of this fact to perform a Lyapunov–Schmidt type reduction to (2.24a), first solving the problem on a codimension subspace where is well-behaved, and then studying the reduced equation on the near-degenerate direction.
4.1. An approximate eigenfunction
As a preparation for proving the existence of and , we first study the function
[TABLE]
which results from taking and perturbing it slightly so that the homogeneous boundary condition on is satisfied, see Figure 2. In what follows, the dependence of on will be suppressed when there is no risk of confusion. While is not likely to be an eigenfunction itself, we will see that it does help in identifying the asymptotically degenerate direction. Observe that it solves the elliptic problem
[TABLE]
as and by the definition of the boundary correction operator. Recall also that according to Assumption (A).
Lemma 4.1**.**
For , we have and
[TABLE]
Proof.
Simply from the exponential decay of as , Proposition 3.1, Corollary 3.7, and its definition, it is clear that in for . On the other hand, from (4.2) and Corollary 3.7, we obtain the estimate
[TABLE]
Without loss of generality, we only need to consider the “+” case. According to Assumption (A) and Proposition 3.1, for any and ,
[TABLE]
and thus the claimed bound on follows from (3.12).
Likewise, using the above estimate on in conjunction with Corollary 3.7, (4.1), and (4.2), one can estimate
[TABLE]
We concentrate on the first term on the right-hand side, as it will clearly dominate as . Using the identities
[TABLE]
and integrating by parts twice yields:
[TABLE]
The first of the boundary integrals we treat by integrating back to the interior domain and using the definition of the boundary correction operator:
[TABLE]
where Corollary 3.5 and 3.7 are used in the above last step. The second integral we instead estimate by integrating into the outer domain , where and its derivatives are well defined and exponentially decaying in all radial directions. In analogy to above, we use the elliptic equation that satisfies to find
[TABLE]
where the last bound is from Corollary 3.5. Observe also that both boundary integrals are positive. This implies the positivity of for small enough, and so the proof is complete. ∎
We wish to show that is well behaved as except in a one-dimensional near-degenerate direction that anticipates the kernel of on . To be more precise, define the function spaces
[TABLE]
Then, under Assumption (B) we see that has a one-dimensional kernel spanned by . Note that here the even symmetry restriction eliminates the kernel direction generated by . Let denote the orthogonal projection of onto ; abusing notation somewhat, we use the same symbol for the induced projection .
The following non-degeneracy result is a direct consequence of Assumption (B).
Lemma 4.2** (Non-degeneracy in ).**
The operator is an isomorphism with bounds uniform in .
Next, we establish an estimate for . Let be a smooth cut-off function with
[TABLE]
Given a function we define its (odd) extension by
[TABLE]
Notice that
[TABLE]
and hence if and only if . By a standard property of odd extensions, we have in fact that if and only if .
Now, let
[TABLE]
For any and , we see that and
[TABLE]
Using the bounds of and given in Corollary 3.5 and 3.7, we estimate that
[TABLE]
uniformly for and all small values of . In other words, the extension is nearly orthogonal to in . Combining these observation leads to the bound
[TABLE]
which holds for all .
Lemma 4.3** (Non-degeneracy in ).**
- (a)
There exists and such that, for all and ,
[TABLE] 2. (b)
For every , there exists and such that, for all , , and satisfying
[TABLE]
we have
[TABLE]
Proof.
First observe that in light of (4.8), for any fixed , any element will satisfy (4.10) for sufficiently small. It therefore suffices to prove part (b). Fix as above and let satisfy the near orthogonality condition (4.10) be given. By linearity, we can assume without loss of generality that .
From the definition (4.4) of the extension ,
[TABLE]
We compute that, for , one has
[TABLE]
This leads directly to the following expression for the commutator on the set
[TABLE]
Now, measuring the left- and right-hand sides of (4.12) in , taking into account the estimates of for small and Proposition 3.1, we find that
[TABLE]
The term above can be eliminated via interpolation:
[TABLE]
Inserting this inequality into (4.12), we arrive at the commutator bound
[TABLE]
independent of , , and .
We are now prepared to prove the estimate (4.11). From Lemma 4.2 we have that
[TABLE]
where the last inequality follows from hypothesis (4.10) and (4.5). On the other hand, together (4.5) and the commutator estimate (4.13) reveal that
[TABLE]
Combined, (4.14) and (4.15) imply that (4.11) holds when is taken sufficiently small, which completes the proof. ∎
4.2. Construction of a near-degenerate eigenfunction
In Section 4.1, it was shown that the function roughly aligns with the near-degenerate direction of in the sense that the restriction is uniformly positive according to (4.9), where is defined in (4.6). We now refine our analysis to find a (very small) eigenvalue and corresponding eigenfunction near that limits to in some sense as . Similar as above, denote by the orthogonal projection and also the projection it induces from .
Lemma 4.4**.**
Consider the operator
[TABLE]
defined by
[TABLE]
There exists such that, for all and , we have that is an isomorphism and is self-adjoint as an unbounded and densely defined operator on with .
Proof.
Throughout the proof, all norms and inner products are evaluated on the domain . By definition, and if and only if
[TABLE]
which holds if and only if
[TABLE]
for all and . Since on , we obtain that and if and only if
[TABLE]
Thus , and . This implies that is indeed self-adjoint on its domain in .
Next, we improve slightly the bound of in (4.9): observe that, for all ,
[TABLE]
But, due to equation (4.2) satisfied by and Lemma 4.1, we know that
[TABLE]
and thus
[TABLE]
This implies that is an isomorphism from to its range — a closed subspace of . It follows from the self-adjointness of on that it is an isomorphism from to . ∎
Proposition 4.5** (Existence of ).**
For each and sufficiently small, there exists an eigenfunction
[TABLE]
of with a real eigenvalue :
[TABLE]
They obey the estimates
[TABLE]
Moreover, for fixed , is in and is in for , respectively.
Here is simply a normalizing constant so that .
Proof.
From Lemma 4.4, we know that there exists such that, for any , is an isomorphism from to . By (4.16), its inverse satisfies
[TABLE]
for some independent of and small . A function , with , is an eigenfunction corresponding to if
[TABLE]
Taking the inner product of the above equation with yields
[TABLE]
On the other hand, applying to the eigenfunction equation and recalling that , we see that
[TABLE]
This motivates us to consider the mapping defined by
[TABLE]
where
[TABLE]
is the presumptive eigenvalue. Clearly a small fixed point of yields an eigenfunction of close to associated to the eigenvalue .
It is straightforward to estimate
[TABLE]
and
[TABLE]
Likewise, we have
[TABLE]
and
[TABLE]
where all above inequalities are uniform in and small . Consequently, Lemma 4.1 and (4.18) imply is a contraction map that sends , the closed unit ball centered at the origin in , to itself. It therefore has a unique fixed point . This yields the eigenvalue defined by (4.21) and the corresponding eigenfunction whose higher Sobolev regularity is due to the ellipticity in (4.19). The normalizing constant is chosen such that . Since and with exponential decay, it is easy to see that is in for . From standard spectral theory, the simple eigenvalue is in and the unit eigenfunction of is in for . As is a fixed point of the contraction , its definition (4.20) and Lemma 4.1 imply
[TABLE]
The higher Sobolev norms satisfy similar estimates due to the elliptic regularity given in (4.19). Finally, we conclude from (4.21), the above inequality, and Lemma 4.1, that
[TABLE]
Along with Lemma 4.1, this yield the desired estimate on . The positivity of is a consequence of the sign of proved in Lemma 4.1. ∎
Using the estimates just obtained, we can now confirm that is invertible (with near-degeneracy in the direction) and, more important, that the inverse of its restriction to the orthogonal complement of is bounded independently of . That said, let be given as in Proposition 4.5 and denote its orthogonal complement in by .
Lemma 4.6** (Invertibility of ).**
There exists such that, for all and ,
[TABLE]
Moreover, there exists such that
[TABLE]
where is the complement of in .
Proof.
Since is self-adjoint and is an eigenfunction of the eigenvalue , it is standard that is invariant under in the sense that
[TABLE]
Because of and again the self-adjointness of , it suffices to prove that has a lower bound independent of and small . In fact, recall
[TABLE]
Any can be written as
[TABLE]
We have
[TABLE]
and thus
[TABLE]
It implies that and are isomorphic through
[TABLE]
where was also used. Together with Lemmas 4.1 and 4.3 we obtain
[TABLE]
which completes the proof. ∎
The invertibility of also holds in higher Sobolev spaces due to elliptic theory.
Corollary 4.7**.**
There exists such that, for all , , and ,
[TABLE]
Moreover, there exists such that
[TABLE]
5. Proof of the main result
In this section we complete the argument leading to the proof of Theorem 1.1.
5.1. Normal bundle coordinates
Recall from Section 2 that the waves we study are represented by two quantities: the boundary value of a conformal mapping, that determines the fluid domain, and a (rescaled) stationary stream function that gives the velocity field. Our basic approach is to construct waves for which and is a perturbation of , where the parameter selects the approximate altitude of the center of vorticity.
At this stage, we have obtained detailed information regarding the spectrum of the linearized operator
[TABLE]
and its dependence on and . In particular, we proved in Proposition 4.5 that there exists a unique simple eigenvalue , associated to an eigenfunction , that converges to [math] exponentially fast as . This presents an obvious obstruction to a naïve fixed point scheme. We will see that is the key to ameliorating the issue.
To see the connection, observe that the family
[TABLE]
can be viewed as a curve in the ambient space . At a fixed , the tangent vector to is
[TABLE]
where the second equality follows from the linearity of the boundary correction operator. The above calculation shows that the tangent direction along the curve is almost parallel to the near-degenerate subspace.
Therefore, our strategy is to seek a (rescaled) stationary stream function of the form
[TABLE]
with the unknowns
[TABLE]
This ensures that avoids the near-degenerate direction of . While the linear part of the Bernoulli boundary condition (2.24b) is already invertible. We may then perform a Lyapunov–Schmidt reduction: for each fixed , we solve for and , leaving a one-dimensional problem of the form , for a certain bifurcation function . Finally, we will appeal to an intermediate value theorem argument to infer the existence of solutions to this reduced problem, as anticipated by the model calculation carried out in Section 1.
It is therefore imperative that the Lypanuov–Schmidt reduction be performed in such a way that is continuous (or even smooth). Because the near-degenerate and non-degenerate subspaces vary as we change , it is natural to view as a smooth vector bundle over the base , with the fibers being the non-degenerate subspaces
[TABLE]
see also Figure 4. According to Proposition 4.5, the -regularity of ensures that is for , and hence the orthogonal projection onto enjoys the same regularity with respect to . It then follows that each is contained in a neighborhood such that the mapping
[TABLE]
is a local trivialization of . Note that here and in the sequel, we reserve cursive script for bundles. In the Lyapunov–Schmidt reduction, we fix , while tracking the continuous dependence on it.
Remark 5.1*.*
While continuity in is sufficient for our purpose, in differential geometry, there are standard notions of smoothness of mappings related to vector bundles based on the smoothness of the trivializations, which allow implicit function theorem type arguments to be carried out as on flat spaces or manifolds. Moreover, it is standard to prove that
[TABLE]
defines a local coordinate map (usually referred to as the transversal bundle coordinates) near .
To simplify notation, we introduce the set
[TABLE]
and endow it with the structure of a vector bundle over having fibers
[TABLE]
and locally trivialized in the obvious way.
5.2. Lyapunov–Schmidt reduction
Let us now reconsider the elliptic system (2.24),
[TABLE]
from this geometrical standpoint. In the previous subsection, we argued that this system is equivalent to finding together with a scaled stream function having the ansatz
[TABLE]
As before, we suppress the dependence of and on whenever there is no risk of confusion. With a slight abuse of notation we also as above view
[TABLE]
from (2.25) and (2.26) to be the bundle map from a subset (with small) of to . It is easily seen that the slightly reinterpreted enjoy the same regularity as in Lemma 3.8.
Projecting the semilinear elliptic problem into the near-degenerate and non-degenerate subspaces (which are invariant under ), we can reconfigure the governing equations as the following system:
[TABLE]
Notice that for a fixed , (5.5b)–(5.5c) are solved on the fiber . In the next lemma, we prove that one can always do this, and the solution depends smoothly on . We therefore reduce the system to the one-dimensional equation (5.5a) related to the near-degenerate subspace.
Lemma 5.2** (Lyapunov–Schmidt reduction).**
There exists such that, for all and , there exists a solution to (5.5b)–(5.5c) which is unique in the set
[TABLE]
and satisfies
[TABLE]
where
[TABLE]
Moreover, depends continuously on .
Remark 5.3*.*
As a consequence, the system (5.5) is locally equivalent to the one-dimensional problem
[TABLE]
Also, it is worth noting that, since for any , the above lemma holds for all such . The uniqueness property of implies that it is independent of .
Proof.
Let be given, where will determined over the course of the proof, which is largely based on the estimates given in Lemma 3.8. To tame the singular bound of , we introduce the rescaled variable
[TABLE]
where will be determined independent of and , and the corresponding scaling of the nonlinearities
[TABLE]
Denote by
[TABLE]
where we recall that the existence and boundedness of were established in Corollary 4.7. In particular, notice that, because is self-adjoint with respect to the inner product and is an eigenfunction, the range of is contained in . Then we see that solve (5.5b) and (5.5c) if and only if is a fixed point of the mapping
[TABLE]
given by
[TABLE]
on the set
[TABLE]
From Lemma 3.8, we have
[TABLE]
Therefore, for a sufficiently large , which can be chosen independently of and , is a contraction on , and so it possesses a unique fixed point
[TABLE]
Moreover, we have the estimate
[TABLE]
The continuity of and follows from the continuity of in , where we can view it as a mapping defined on a smooth bundle.
Finally, we identify the leading order term of . Due to the fixed point property, we have
[TABLE]
Lemma 3.8 and the above upper bounds of imply
[TABLE]
From (3.14), (3.15), (3.16), and the scaling property, we have
[TABLE]
which along with the above inequality yields the desire estimate on . ∎
5.3. Proof of the main result
Proof of Theorem 1.1.
The Lyapunov–Schmidt reduction carried out in Lemma 5.2 shows that it suffices to find with , where is defined in (5.6). Our strategy will be to relate the bifurcation equation to the model calculation (1.16).
With that in mind, fix and recall
[TABLE]
recalling that , , , and were obtained in Section 4. In particular, is a normalizing constant introduced to ensure that .
Since solves (5.5b), we have
[TABLE]
Now, let
[TABLE]
where is the holomorphic function constructed from through (2.19). According to Lemma 5.2, the domain of is the (slightly) perturbed strip
[TABLE]
For clarity, we use as the coordinate variable in . It is easy to compute
[TABLE]
where the complex number is understood as a two-dimensional vector. Corollary 3.7, Proposition 4.5, and Lemma 5.2 together imply that
[TABLE]
In view of (5.8), we have that (5.6) holds for if and only if
[TABLE]
By the definitions of and the boundary correction operator,
[TABLE]
which, along with the coordinate change , gives
[TABLE]
Following the same calculation leading to (1.16), we then find that
[TABLE]
where
[TABLE]
is the outward unit normal vector on the upper/lower component of , and
[TABLE]
the length element along . We can rewrite as an integral on by reversing the coordinate change:
[TABLE]
Notice that tangential derivatives do not appear because . Without loss of generality, we just consider the first term. From the definition of , (3.15), (3.16), Lemma 5.2 (taking ), and the trace theorem, we obtain
[TABLE]
and
[TABLE]
Therefore, again Lemma 5.2 implies
[TABLE]
where
[TABLE]
Here we have used the radial symmetry of to slightly simplify the expression. Clearly, it also implies that is odd.
Due to the exponential localization, can be effectively determined by integrating only over a -dependent but compact interval. Indeed, from Proposition 3.1, it is easy to see
[TABLE]
where
[TABLE]
Since is also odd, we consider . Using Proposition 3.1 once more, along with (3.2), we compute that
[TABLE]
where we used the fact that in this integral region. Let
[TABLE]
which has the polar coordinates representation
[TABLE]
where, because we are restricting to ,
[TABLE]
Therefore we have
[TABLE]
This implies that, for ,
[TABLE]
and thus we obtain from (5.10) that there exists independent of such that
[TABLE]
From the oddness of , we can then conclude that there exists with and such that is a solution to (5.5), and thus corresponds to a solution to the stationary capillary-gravity wave problem. The stream function is given by
[TABLE]
defined on
[TABLE]
From the estimate , Corollary 3.7, and Lemma 5.2, we have
[TABLE]
and
[TABLE]
where
[TABLE]
The desired estimate on in Theorem 1.1 follows immediately.
Finally, the corresponding free surface profile is given by
[TABLE]
which clearly satisfies
[TABLE]
Using (3.16) and Lemma 5.2, it is straightforward to identify the leading order term of coinciding with that of and to obtain the same remainder estimate much as in the above procedure for . This completes the proof of the main theorem. ∎
Acknowledgements
The authors wish to thank one of the referees whose extraordinarily thorough reading and many suggestions lead to substantial improvements.
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