Internal doubly periodic gravity-capillary waves with vorticity
Douglas Svensson Seth

TL;DR
This paper proves the existence of three-dimensional steady gravity-capillary waves with vorticity in a multi-fluid system, using bifurcation theory and explicit conditions for in-phase and off-phase motions across interfaces.
Contribution
It introduces a multi-parameter bifurcation framework for steady gravity-capillary waves with vorticity, including explicit conditions for different interface motions.
Findings
Existence of 3D steady gravity-capillary waves with vorticity.
Explicit conditions for in-phase and off-phase motions.
A general bifurcation theorem applicable to similar problems.
Abstract
We consider a multi-fluid system with several free interfaces. For this system we prove existence of three-dimensional steady gravity-capillary waves with non-zero vorticity. We obtain non-zero vorticity by prescribing the relative velocity fields to be Beltrami fields, for which the vorticity and velocity are parallel. The main result is a multi-parameter bifurcation result for small amplitude waves given in two variants: a first theorem guaranteeing existence under some general parameter assumptions; and a second specific but less exhaustive theorem, for which the assumptions may be explicitly verified, yielding the existence of both in-phase and off-phase motions in the different layers. The proof relies on an implicit function theorem corresponding to multi-parameter bifurcation. This theorem is presented in an appendix as an abstract result that can be applied directly to other…
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Taxonomy
TopicsOcean Waves and Remote Sensing · Coastal and Marine Dynamics · Navier-Stokes equation solutions
Internal doubly periodic gravity-capillary waves with vorticity
Douglas Svensson Seth
Abstract.
We consider a multi-fluid system with several free interfaces. For this system we prove existence of three-dimensional steady gravity-capillary waves with non-zero vorticity. We obtain non-zero vorticity by prescribing the relative velocity fields to be Beltrami fields, for which the vorticity and velocity are parallel. The main result is a multi-parameter bifurcation result for small amplitude waves given in two variants: a first theorem guaranteeing existence under some general parameter assumptions; and a second specific but less exhaustive theorem, for which the assumptions may be explicitly verified, yielding the existence of both in-phase and off-phase motions in the different layers. The proof relies on an implicit function theorem corresponding to multi-parameter bifurcation. This theorem is presented in an appendix as an abstract result that can be applied directly to other problems.
Department of Mathematical Sciences, Norwegian University of Science and Technology, [email protected]
1. Introduction
In this paper we consider immiscible fluids separated by free boundaries. All the fluids are contained within the domain
[TABLE]
which itself is separated into the layers given by
[TABLE]
for different interface profiles ( as well as ); see fig. 1.
contains the :th fluid. In each layer we assume that the fluid has constant density and that the velocity field of the fluid satisfies the Euler equations with an external gravitational force . In the remainder of the paper we assume that the densities always satisfy the condition . We also work under the traveling wave assumption, that is, the velocity fields and interface profiles are time independent in some frame of reference moving with constant speed . In other words, the waves travel with speed . Instead of working directly with we will work with the relative velocity field in the frame of reference moving with the waves . This relative velocity field is obtained by setting and it solves the steady Euler equations
[TABLE]
From now on we will just refer to as the velocity field. We assume that the velocity fields are Beltrami fields, which means that the vorticity is parallel to the velocity. In particular, we shall assume that the velocity field is a strong Beltrami field in each layer. Here strong means that the proportionality factor between velocity and vorticity is a constant. In other words, in for some constant . However, we do allow for . For mathematical reasons this is a very suitable vorticity assumption when working with the Euler equations. The identity
[TABLE]
means that the momentum equation of the Euler equations, eq. 1.1, is satisfied with pressure given by
[TABLE]
if is a Beltrami field, for an arbitrary constant ; like in the irrotational case, which is the special case . Moreover, we introduce two linearly independent vectors and , which allows us to define the lattice
[TABLE]
We shall assume that our solutions, whence the waves, are periodic with respect to this lattice; see fig. 1. For future reference we also introduce the dual lattice
[TABLE]
where . For our analysis it is suitable to express the vectors in the dual lattice in polar form, so we let for some general vector and in particular , . We also denote ‘one period’ with respect to by
[TABLE]
and one period of by
[TABLE]
In summary, the velocity fields satisfy the equations
[TABLE]
for , and since the fluids are assumed to be immiscible we get the boundary conditions
[TABLE]
for and the (upwards) unit normal of . Moreover, the pressure difference between and at their shared boundary satisfies the Young–Laplace law
[TABLE]
for . Here denotes an interfacial tension parameter. We can substitute the pressure using eq. 1.3 and obtain
[TABLE]
for . We normalize the pressure, that is, choose the , in Section 1.3. The eqs. 1.4 to 1.7 constitute a free boundary problem with several undetermined interfaces .
In the present paper we will also allow , to be able to capture interaction between surface waves and internal waves. Note that with and we recover the classical water wave problem for surface waves. Setting completely decouples the problem from the uppermost layer, so we introduce
[TABLE]
to be able to handle both cases simultaneously. Moreover, we will use the following notation
[TABLE]
1.1. Background
This type of free boundary problem has been extensively studied in two dimensions. Especially the case with two fluids separated by one free interface, that is, ; see for example [1, 6, 18, 22]. One of the common applications of a multi-fluid system like this is the study of internal waves in an ocean stratified by, for example, temperature or salinity; see [11, section 7] for an overview. However, the two-layer model that is usually studied gives an idealized version of an ocean with almost constant, but different, densities in two layers separated by a sharp density gradient. If the gradient is sufficiently sharp then it is intuitive to approximate it with a single layer given by a free interface; this has also been rigorously justified under certain conditions by Chen and Walsh [4]. Naturally with this approximation we may lose some of the finer detail from a varying density, which has been studied numerically by Vanden-Broeck and Turner [23]. To recapture some of that detail is one of the reason we study more than two layers. This have been proposed before, by for example Rusås and Grue [20], and there is at least numerical support that several layers allows us to recapture some phenomena lost by collapsing the change in density to a single layer; see for example Nakayama and Lamb [16].
In three dimensions most existing results treat only surface waves. The first rigorous existence result for doubly periodic waves on a symmetric lattice is due to Reeder and Shinbrot [19]; this was extended to general lattices Craig and Nicholls [5]. Both these results are based on bifurcation theory, albeit Craig and Nicholls also employs a variational approach to the problem. Another method that has proven useful is that of spacial dynamics; first used for the water wave problem in three dimensions by Groves and Mielke [10] and Groves and Haragus [9]. All these are results for gravity-capillary waves. This is due to a small-divisor problem that appears for pure gravity waves in three dimensions, making the problem in many ways easier with surface tension. The existence of surface gravity waves has however been proven by Iooss and Plotnikov [12, 13] using Nash-Moser techniques. In the present paper interfacial tension is included as it resolves the small-divisor problem. Similarly, in the dynamical setting nonzero interfacial tension resolves the Kelvin–Helmholtz instability for high frequencies; see Lannes [14]. Since our result is valid for arbitrarily small, although non-zero, interfacial tension we should be able to provide solutions were the interfacial tension brings stability without having a large impact on the wave profiles. For internal waves in three dimensions there is one existence result relying on spacial dynamics, due to Nilsson [17].
The problem studied in this paper includes vorticity, due to the assumption that the velocity fields are Beltrami fields. Waves with vorticity have been studied extensively in two dimensions, but in three dimensions the results are more sparse. For surface waves in three dimensions with vorticity there is a non-existence result for constant vorticity due to Wahlén [24]. There are also two existence results in the same setting; the first due to Lokharu, Seth and Wahlén [15], which is similar in nature to the present contribution in that the velocity is assumed to be a Beltrami field; the second, by Seth, Varholm and Wahlén [21], is based on a different vorticity assumption, which is inspired by a mathematically equivalent problem in plasma physics. There is one result considering internal waves in three dimensions with vorticity. Chen, Fan, Walsh and Wheeler [3] show that if the vorticity is constant then the solutions are very restricted.
1.2. Main result and structure of the article
In the present paper we obtain an existence result for three dimensional, internal waves with nonzero vorticity. The main result requires additional technical definitions to be stated precisely, but we give a summarized version here.
Theorem 1.1**.**
Under appropriate assumptions on the parameters, , there exists an , such that for every there exist solutions , , and , to eqs. 1.4 to 1.7. Moreover, the interface profiles are given by
[TABLE]
for some real numbers , , depending on the parameters.
The detailed version of this result is given in Theorem 5.3. The assumptions referenced in the theorem is not obviously satisfied, and do indeed fail for some parameter values. For this reason we show that there exists a non-empty subset of the parameter space where the assumptions are satisfied, with the corresponding existence results given in Propositions 6.2 and 6.4. These results cover a large part of the parameter space, but a complete characterization lies beyond the scope of this paper.
The overall structure of the proof of Theorem 1.1 is reminiscent of [15] and relies on multi-parameter bifurcation. To this end, we finish the introduction by defining the trivial solutions that the non-trivial solutions in Theorem 1.1 bifurcate from. In section 2 we set up suitable function spaces for the remaining analysis. In Section 3 we change coordinates to a flattened domain and reduce the problem to a single equation for the free interfaces. In Section 4 we study the linearized version of this reduced problem. With the results from Section 4 we state a purely algebraic assumption used for the main existence result. Both the assumption and main existence result are given, and in the latter case proved, in Section 5. We end by showing that this assumption is satisfied in certain subsets of the parameter space in Section 6. We focus on two cases: limiting the number of layers to two, that is , and considering weak vorticity, that is . However, we also include an informal discussion and some examples of other cases in Section 6.3. Appendix A contains a multi-parameter bifurcation result that is integral in the proof of the main theorem. Similar techniques have been used repeatedly in the literature (for example in [7, 8, 15]), but only for special cases. Here, on the other hand, we have abstracted the previously used ideas and present them in a general result. This will give a handy tool for future research, since it can be directly applied to similar problems.
1.3. Trivial solutions
For flat interfaces, , we can find laminar flows that are explicit solutions with nonzero velocity by considering the basis functions
[TABLE]
With any and we can construct a solution to eqs. 1.4 to 1.6 which is given by
[TABLE]
Now we pick the in such a way that these velocity fields also satisfy eq. 1.7. This can be done by setting
[TABLE]
where the satisfy
[TABLE]
This leaves us with one degree of freedom in the pressure, that is, we can add the same constant to all . This does not effect the mathematical problem, though, and we can remove this freedom by simply setting . To further decrease the degrees of freedom we will only keep and as free parameters and define the other and as functions of these through the recursive relationships
[TABLE]
These are the relations that leaves us with a continuous trivial solution if we glue together all to one function in . However, there is no mathematical requirement for continuity and all and could be kept as free parameters. In fact, keeping them all as free parameters could potentially let us handle bifurcation from a point were the kernel of the linearization has higher dimension. However, in this paper we restrict ourselves to a two-dimensional kernel, which means two bifurcation parameters and are sufficient. For notational simplicity we drop the indices from and , and let . With these choices eq. 1.7 become
[TABLE]
which is satisfied by and .
Now we impose the following integral conditions
[TABLE]
for , in addition to the equations eqs. 1.4 to 1.7. They will allow us to find unique solving eqs. 1.4 to 1.6 for given and , which allows us to reduce the problem to eq. 1.7 with and as unknowns. In particular, for we obtain , that solve eq. 1.7 for all .
2. Functional analytic setting
We work in the real valued Hölder spaces , where for the velocity fields and for the interfaces. These are Banach spaces equipped with the norm
[TABLE]
where is a fixed number in . The subscript per denotes that they are restricted to functions that are periodic with respect to . Moreover, we want the velocity fields and interfaces to satisfy certain symmetry conditions. By a subscript we denote functions that are even with respect to and by a subscript we denote functions that are odd with respect to . That is,
[TABLE]
and likewise for . After the flattening transform in the next section it is clear that the natural relation between and is . Therefore we seek solutions in and , which is the lowest regularity in these spaces that allow solutions in the classical sense. We also let
[TABLE]
so that and . For future reference we also introduce the lower regularity spaces and .
Due to the periodicity and symmetries we can express as a Fourier series
[TABLE]
where are real valued and satisfy , for and are imaginary and satisfy . An analogous Fourier series representation exist for
For an operator , where , and are Banach spaces, we denote the Fréchet derivative at by . Moreover, by and we denote the Fréchet derivatives of and at and at , respectively. Finally, we note that
[TABLE]
for .
3. Flattening
To avoid unnecessarily complicated notation after we change variables, we change notation for the physical frame, and denote the coordinates and functions expressed in these coordinates with a bar, for example . We flatten the domains using a naive flattening given by
[TABLE]
Since we only are concerned with small amplitude waves this flattening transformation is sufficient, and it is conceptually easy to understand. maps
[TABLE]
to as long as the interfaces do not intersect, that is, if for . The flattening transformation has Jacobian matrix
[TABLE]
with determinant
[TABLE]
For scalar functions, we define through
[TABLE]
and for vectors fields, , we define through
[TABLE]
which corresponds to expressing the vector fields in terms of a position-dependent, and not necessarily orthonormal, basis. We also note that this transformation preserves the regularity and symmetry, that is, if then if and only if . We also define analogously to . We use this flattening to transform our original free boundary problem to a problem in the fixed domains.
Proposition 3.1**.**
Assume , then the equations
[TABLE]
for , with , and are equivalent to the eqs. 1.4 to 1.8 with and , where
[TABLE]
and and are some operators that satisfy
[TABLE]
Proof.
By directly applying the flatting transformation to eqs. 1.4 to 1.8 turns the equations into
[TABLE]
for . where
[TABLE]
and
[TABLE]
These equations are very similar to eqs. 3.1 to 3.6, but there are two vital differences. The first is that and the second is that the right hand side of eq. 3.10 is nonzero. To rectify this we introduce and , defined below, which will give equations with the desired properties for
[TABLE]
The velocity field gives the right hand side of eq. 3.1 the properties we want, but introduces the nonzero right hand sides of the boundary conditions in eqs. 3.3 to 3.4, while makes the right hand side of eq. 3.5 zero. Specifically, is given by
[TABLE]
and is a laminar flow such that , that is, for flat interfaces it coincides with the solution from Section 1.3. Moreover, is chosen in such a way that
[TABLE]
To show that this choice is possible we begin by computing
[TABLE]
and similarly
[TABLE]
Since
[TABLE]
we find
[TABLE]
and similarly
[TABLE]
By setting and integrating we obtain that we need and to satisfy
[TABLE]
If these equations are solvable and we get
[TABLE]
We note that is of quadratic order with respect to . Moreover, for obvious modifications to the calculations give , which coincide with the limit in the formula above. In fact, setting for gives an analytic function (with respect to ) around [math]. Thus we can find the desired for .
We move on to check what happens with the other equations. First note that
[TABLE]
Then we define and and find that
[TABLE]
and
[TABLE]
Combining these two equations above with eqs. 3.12 to 3.17 we see that eqs. 3.7 to 3.11 turn into eqs. 3.1 to 3.6 with as a variable instead of , where, and . From these definitions it also directly follows that
[TABLE]
∎
In light of this proposition we focus our attention to eqs. 3.1 to 3.6 in the remainder of the paper.
3.1. Reduction to the interfaces
We define the spaces
[TABLE]
and the operator by
[TABLE]
For a given the eqs. 3.1 to 3.5 are equivalent to
[TABLE]
To find a unique solving eqs. 3.1 to 3.5 if and are given we need to impose the non-resonance condition
[TABLE]
Doing so allows us to substitute this solution, , into eq. 3.6, which reduces the problem to the interfaces. We also note that eq. 3.18 is a stricter condition than the assumption in Proposition 3.1; for in eq. 3.18 implies that the assumption in Proposition 3.1 is satisfied. To solve eqs. 3.1 to 3.5 we begin by proving that has the following properties.
Lemma 3.2**.**
- (i)
* is an isomorphism.*
- (ii)
* is a Fredholm operator with index 0.*
- (iii)
* is an isomorphism if and only if the non-resonance condition in eq. 3.18 is satisfied.*
Proof.
Clearly is a bounded linear map. To prove we begin by proving that is injective. If
[TABLE]
then so , which means that
[TABLE]
By continuity and satisfy Laplace equation with Neumann boundary conditions on and . Together with the fact that and are periodic and satisfy the integral conditions
[TABLE]
we obtain . Hence is injective. To show that is surjective pick a general element . We introduce satisfying
[TABLE]
By standard elliptic theory we can solve both these problems in the appropriate function spaces and it is not hard to check that satisfies
[TABLE]
For property we note that is of the from ‘identity plus a compact operator’. Thus is Fredholm with index [math] and it follows that so is .
Part follows from part and the fact that is injective if and only if eq. 3.18 is satisfied. Indeed, if we consider
[TABLE]
then the Fourier coefficients of must satisfy
[TABLE]
Under the condition in eq. 3.18 this implies in for all . With this in mind we find that
[TABLE]
which implies in for all , . Moreover, eq. 3.19, the condition in eq. 3.18 and the integral conditions , give in . Hence, we have shown is injective under the condition in eq. 3.18. On the other hand, if eq. 3.18 is not satisfied we can a find non-trivial solution to eqs. 3.19 to 3.21 for the that breaks the condition in eq. 3.18. This in turn gives a non-trivial element in the kernel of . ∎
Proposition 3.3**.**
Assume the non-resonance condition in (3.18) holds, then for any , , and there exists a unique solution to the problem given by eqs. 3.1 to 3.5 provided that and . Furthermore, depends analytically on and . If is constant in the direction of then so is .
Proof.
We can write eqs. 3.1 to 3.5 as
[TABLE]
where is given by
[TABLE]
for the spaces and . The Fréchet derivative at is given by
[TABLE]
By lemma 3.2 every component of is an isomorphism, whence so is . This means we can apply the analytic implicit function theorem [2, Theorem 4.5.4] to obtain the result.
The analysis can be repeated in function spaces where the elements are constant in the direction of . This gives the result that if is constant in the direction of then so is . ∎
With the solution from this proposition we can write eqs. 3.1 to 3.6 as the single equation
[TABLE]
where is the operator defined through
[TABLE]
4. The linearised problem
The aim is to apply the bifurcation theorem in Appendix A to find nontrivial solutions to Equation 3.22. To this end we have to study the linearised problem to obtain the Fréchet derivatives and . If we set , , then
[TABLE]
To show that this satisfies the properties required to apply Theorem A.1 we will rewrite it in a more workable form summarized in lemma 4.1 at the end of this section. We cannot immediately give the result since we need to find in terms of and first. solves the linearised version of eqs. 3.1 to 3.5 given by
[TABLE]
for . We express in terms of its Fourier series
[TABLE]
where . Since the problem is linear we can consider every Fourier mode of separately. Thus assume for some and recall the polar form . Then the solution will be of the form
[TABLE]
Combining eqs. 4.2 and 4.3 gives the equation
[TABLE]
for . This equation together with the boundary conditions
[TABLE]
obtained from eqs. 4.4 and 4.5, has a unique solution when the non-resonance condition (3.18) is satisfied. When we obtain . Moreover, in this case we also get due to the integral conditions in eq. 4.6 together with the non-resonance condition. Substituting this into eq. 4.1 gives
[TABLE]
To express the solution for we introduce and which solve
[TABLE]
respectively, where prime denotes derivative with respect to . Explicitly is given by
[TABLE]
and from the equation it can easily be seen that we can obtain by interchanging and in the expression for . In terms of these functions we get
[TABLE]
where satisfying
[TABLE]
We have also used the fact that our choice of means that
[TABLE]
For future reference we also define , which satisfies
[TABLE]
where . Using the expression for we find
[TABLE]
Substituting these expressions for into eq. 4.1 gives
[TABLE]
where we have used the identities and to replace all instances of with .
Lemma 4.1**.**
The Fréchet derivative of can be expressed as
[TABLE]
where is a matrix defined by eqs. 4.7 and 4.8. In particular, is a tridiagonal symmetric matrix.
Proof.
Because only depends on , and the matrix is tridiagonal. To show that the matrix is symmetric we consider
[TABLE]
that is, . Hence the matrix is symmetric. ∎
5. Existence result
We will begin with stating an assumption on the matrix from lemma 4.1 that will immediately allow us to apply Theorem A.1 in Appendix A to obtain an existence result.
Assumption 5.1*.*
There exists such that:
- (i)
and .
- (ii)
The matrix with entries given by
[TABLE]
is invertible.
- (iii)
[TABLE]
Remark 5.2*.*
Since we immediately get and from part (i) of this assumption. Together with part (iii) this implies
[TABLE]
because is an operator the space consisting of even functions
5.1 is specifically designed to make from eq. 3.22 satisfy the assumptions in Theorem A.1. So proving an existence result at this point under the assumption is rather straightforward. The difficulty lies in proving the validity of the assumption itself, which is a problem studied in Section 6. However, the analysis of the assumption in this paper is not completely exhaustive, which means that the existence theorem below remains valid in a larger subset of the parameter space than shown in Section 6. With this assumption in hand we are ready to prove the first and more abstract version of the main result.
Theorem 5.3**.**
If 5.1 and eq. 3.18 holds then there exits an such that for every there exist parameters and corresponding solutions and to eqs. 3.1 to 3.6 such that the map
[TABLE]
is real analytic and
[TABLE]
In particular, this means that there exist nontrivial solutions to eqs. 1.4 to 1.8.
Proof.
We prove the theorem by checking conditions (i)–(iv) of Theorem A.1 for
[TABLE]
from eq. 3.22. Where and are the subspaces of and spanned by and respectively. It follows from the fact that is symmetric that the kernel and cokernel of are spanned by the same functions.
Condition (i) of Theorem A.1 is trivially satisfied. That the derivative is a well defined linear bounded operator mapping to follows from the fact that for large . Moreover, by part (i) and (iii) of 5.1 the kernel is two dimensional and given by as defined above and the cokernel is also two dimensional and given by . Hence it is a Fredholm operator and condition (ii) of Theorem A.1 is satisfied. Condition (iii) of Theorem A.1 is exactly the same as part (ii) of 5.1. Finally, condition (iv) of Theorem A.1 is satisfied if we pick and such that and are the subspaces of functions that are constant in the direction for . ∎
6. On 5.1
This section is dedicated to show that 5.1 is satisfied in large parts of the parameter space of the problem. To this end we note that, due to fact that is tridiagonal, it is sufficient to find such that and check that the sub- and superdiagonal consist of nonzero elements for part of 5.1. Then to check parts and it is sufficient to check that a finite number of quantities are nonzero. This is due to the fact that for large the terms are dominant so for all sufficiently large .
The results here are by no means exhaustive, since the parameter space is very large and a complete characterization of the subset where 5.1 is satisfied may not even be possible to do in a simple way. We focus on giving results with relatively simple assumptions in this section, because it is not difficult to check numerically if 5.1 is satisfied for a given set of parameter values. Thus a characterization of the the set where 5.1 is satisfied in terms of equally complicated algebraic expressions would be of little use.
For this section we also make the following definition
Definition 6.1**.**
We call a lattice a symmetric lattice if its generators and satisfy
[TABLE]
Moreover, we call it non-degenerate if
[TABLE]
The conditions on the lattice are exclusively required for part of 5.1. Even under this assumption we may still have to redefine in some arbitrarily small neighborhood. However, it should be noted that it is plausible part of 5.1 is true for a general lattice, such that parts and of 5.1 is satisfied, and almost all parameter values. As stated above, part of 5.1 is equivalent to a finite subset of does not solve . For any given set of parameters it is unlikely that any of these solve . However, we can expect this to happen for some set of particular parameter values. Although in general we expect this set to be very small.
6.1. The case
The case and , was considered in [15]. The case when can be treated similarly. To make this paper more self-contained we give an adapted result below; prescribing sufficient conditions for 5.1 to be satisfied in the latter case. For the former case and a more detailed discussion we refer to [15]. When the matrix is simply a scalar and if, in addition, it is given by
[TABLE]
For the following result we shall assume that and . This can be done without loss of generality because we can always rotate the coordinate system and change to if necessary. This equation can be analyzed as a hyperbola in the variables and , and we obtain the result below.
Proposition 6.2** ([15]).**
If
- (i)
, and ;
- (ii)
;
then there exist such that part and of 5.1 are satisfied; if, additionally,
- (iii)
* is a symmetric lattice;*
then part of 5.1 is also satisfied for and almost every .
Remark 6.3*.*
The first condition is more or less a matter of proper labeling, but the second condition requires us to be in this setting. We can also replace the conditions and , by . See [15] for further details.
This proposition can be combined with Theorem 5.3 to obtain solutions under the assumptions given in the proposition.
6.2. Irrotational and small vorticity
In the previous section we only considered the case . Here we also allow any . Unfortunately, lifting the restriction leads to a substantial increase of complexity and we have to impose some other restrictions; specifically small vorticity. The result of this section is the second main theorem of this paper and gives an existence result without supposing 5.1 holds. Instead more direct assumptions on the parameters are given, which in turn imply that 5.1 holds. This gives us the second and more concrete version of the main result. However, before we state this theorem we make the following observation to introduce some necessary notation. If , then , , so we can write
[TABLE]
where is a diagonal matrix with elements given by
[TABLE]
This allows us to state the main result of this section.
Theorem 6.4**.**
Assume that is a non-degenerate symmetric lattice, the non-resonance condition in eq. 3.18 holds, and that . Then, after possibly redefining in an arbitrarily small neighborhood, there exist parameter values , , and an such that for every there exist parameters and corresponding solutions , and to eqs. 3.1 to 3.6 such that the map
[TABLE]
is real analytic and
[TABLE]
Moreover, the vectors and that span and respectively, are also given by
[TABLE]
*where and are eigenvectors of and
with corresponding eigenvalues , satisfying*
[TABLE]
Remark 6.5*.*
This theorem means that there exist different nontrivial solutions to eqs. 1.4 to 1.8. In fact we expect there to exist more than values of that yield solutions. However, these additional values give rise to solutions that are qualitatively similar to the ones in the Theorem. For we illustrate and example of the two modes in Figure 2 and the four different waves they can be combined to in Figure 3. It should also be noted that for , the solution for is a reflection of the solution for . Consider for example a square lattice with and . Let
[TABLE]
then . For we still get a solution to the Euler equations under this reflection, but the reflected velocity fields, , are Beltrami fields with constants ; that is, if then .
The rest of this section is dedicated to the proof of this theorem. We begin working under the assumption and extend this to through an implicit function theorem argument. In the proofs we will also make use of submatrices and thus make the following definition.
Definition 6.6**.**
For an matrix we define as the matrix obtained by removing the last rows and the last columns. We call a leading principal submatrix of and a leading principal minor of .
Now we can prove the following properties of the matrix .
Lemma 6.7**.**
If and , then the matrix in eq. 6.1 has negative elements on the diagonal, positive elements on the sub- and superdiagonal, and all eigenvalues of are negative.
Proof.
If then , which means we can write
[TABLE]
is a diagonal matrix with diagonal elements given by
[TABLE]
and is tridiagonal with nonzero elements given by
[TABLE]
Moreover, can be further decomposed into , where
[TABLE]
and
[TABLE]
Computing the leading principal minors of and is straightforward. We obtain
[TABLE]
and
[TABLE]
Both being positive for all if , which means and are positive definite, whence and are negative definite and so is their sum . If , then either or have only zeros in the last row and column. However, and are still negative definite. Thus one of and is negative definite, while the other is negative semi-definite. The conclusion is that their sum is negative definite still holds in this case as well. ∎
With these properties we can prove that 5.1 and are satisfied. In fact there are several for .
Proposition 6.8**.**
If , then there exist parameter values , , such that 5.1 (i) and (ii) are satisfied with distinct .
Remark 6.9*.*
It should be noted that the for fixed and is not unique in general. The proposition only ensures us that there exists at least one for every possible choice of and .
Proof.
By Lemmas 6.7 and 4.1 the matrices are symmetric, tridiagonal, negative definite with nonzero elements on the sub- and superdiagonals. Thus there exist eigenvalues and , and corresponding orthogonal eigenvectors and , . Moreover, if because
[TABLE]
for all . This follows from the rank-nullity theorem and the fact that
[TABLE]
because the elements of on the sub- and superdiagonals are nonzero. We obtain by solving
[TABLE]
It follows that is a solution to
[TABLE]
which always exist because and as a function of maps onto . In fact this equation has several solutions in , so for simplicity we pick to be the smallest such solution. Then is simply given by
[TABLE]
5.1 (i) follows by setting and
giving
[TABLE]
and similarly for . Moreover the kernels of and are both one dimensional due to eq. 6.2.
For 5.1 (ii) we calculate
[TABLE]
which is zero only if . However, this would require
[TABLE]
for some , but this contradicts the fact that and are linearly independent. ∎
Under stricter assumptions on the lattice we can also prove 5.1 is satisfied. At least if we modify by an arbitrarily small amount. On the other hand we can drop the assumption that the vorticity is small for the following proposition.
Proposition 6.10**.**
If , is a non-degenerate symmetric lattice, and is such that parts (i) and (ii) of 5.1 are satisfied, then for every there exist and corresponding , such that and 5.1 is satisfied for and .
Proof.
First note that we always have . For can define by replacing with , where
[TABLE]
We also define
[TABLE]
and obtain
[TABLE]
Clearly and , so for and all . On the other hand, if there exists some such that , then
[TABLE]
where is the diagonal matrix with entries given by
[TABLE]
Now is a polynomial with respect to . Moreover, it is not identically [math]; for example,
[TABLE]
whence for all but a finite number of . Thus we can find such that for all . Since only a finite number of can satisfy , we repeat this a finite number of times, shrinking if necessary. Moreover, by continuity, 5.1 (ii) remains satisfied for all in some neighborhood of [math]. Thus, after possibly shrinking again, we find that 5.1 is satisfied for if we choose for any . Choosing any such that is sufficiently small gives the desired result. ∎
We can now extend these results to small .
Proposition 6.11**.**
If 5.1 holds for some with , then there exist for every such that 5.1 holds for as well.
Proof.
Defining
[TABLE]
we can find
[TABLE]
where and . We have , because , due to the fact that is a polynomial and is a root with multiplicity and, as above, only if . Since we can define such that and for all . This means 5.1 (i) remains true. It is clear that part (ii) remains true by continuity. The same is true for part (iii) and any finite set of , but since for all large this is sufficient. ∎
Combining Propositions 6.8 to 6.11 with the existence result in Theorem 5.3 gives Theorem 6.4.
6.3. Discussion of large vorticity
This subsection does not include any definite results about existence of solutions, but rather exemplifies some of the possibilities that can occur if we relax the assumption . We also exclusively focus on part (i) and (ii) of 5.1 because both and part (iii) can reasonably be assumed true for most parameter values. There is no assumption on in Proposition 6.10 and it is not unreasonable to suspect a similar result to hold true even for general . In the discussion below we implicitly consider part (iii) of 5.1 to be satisfied when mentioning ‘solutions’ or ‘interfaces’.
In the general case we can write the matrix as
[TABLE]
where
[TABLE]
From this we can define the matrix
[TABLE]
which is symmetric, whence it has linearly independent eigenvectors , with corresponding real eigenvalues , . We can find such that 5.1 (i) is satisfied by finding such that for some . This is because
[TABLE]
implies
[TABLE]
for if
[TABLE]
Conversely it is not difficult to check that a vector in gives rise to an eigenvector of with negative eigenvalue given by eq. 6.3. So 5.1 part is satisfied if and only if we have such that . If, in addition, then 5.1 part (ii) is also satisfied. We can see this by considering
[TABLE]
so . Similarly we obtain , which means
[TABLE]
It is not difficult to show that , whence 5.1 part (ii) is satisfied if . In summary, if there exists such that
[TABLE]
then parts (i) and (ii) of 5.1 are satisfied for
[TABLE]
Moreover, if we have such an intersection point between and , then by Theorem 5.3 the solution to eqs. 1.4 to 1.8 will have interface profiles given by
[TABLE]
for some .
Theorem 6.4 gives us the existence of at least such intersection points in the case , that is, intersects in this manner for all . In fact, there will in general be more intersections points. Since is -periodic we can expect an even number of intersection points on the interval ; see Figure 4(a). However, for we also know that all the additional intersection points corresponds to a surface profile that is identical to one of the original . This is because is completely independent of in this case and in eq. 6.4 is the same as in Theorem 6.4. For this is not necessarily true, but for we have at least different solutions and the surface profile corresponding to any additional intersection point is very similar to the surface profile of one of these solutions. For larger we can no longer guarantee the same amount of intersection points. What we can say is that if , then and are the same function shifted by the angle between and . This means and intersects if is a symmetric lattice. Moreover, if and are such that then is negative semi-definite so the intersection points will also almost surely satisfy . This means we should at least have solutions with surface profiles , in this case; see Figure 4(b). It should also be noted that when is not small, all different intersection points can correspond to more substantially different eigenvectors and thus different surface profiles. Finally, when the eigenvalues can be positive and one or more of the intersection points may satisfy , which means we cannot find a corresponding real satisfying eq. 6.3; see Figure 4(c). If this is the case for all intersection points, then there are no satisfying 5.1 and we cannot obtain any solutions with Theorem 5.3; see Figure 4(d). It should be noted that this does not exclude small amplitude solutions to eqs. 1.4 to 1.8. For example we could find solutions that are constant in one horizontal direction when has a one dimensional kernel, giving so called 2$$\nicefrac{{1}}{{2}}-dimensional waves.
Appendix A A multi parameter bifurcation theorem
Let , and be Banach spaces, and and , be one dimensional subspaces of and respectively. This means that we can write
[TABLE]
where and are closed subspaces. This decomposition allows us to define the projections and , , which are projections onto and along
[TABLE]
respectively. Moreover, in this section we let and . Below is a bifurcation result to solve an equation of the form
[TABLE]
for an operator . When this result coincides with the Crandall-Rabinowitz bifurcation theorem.
Theorem A.1**.**
If , with , such that , or (that is is analytic), is an operator with the following properties:
- (i)
* for all and there exists such that is a Fredholm operator of index [math]*
- (ii)
The kernel of is -dimensional and given by .
- (iii)
If , then the matrix given by
[TABLE]
is invertible.
- (iv)
There exist closed subspaces of and of for each such that
[TABLE]
and
[TABLE]
is a Fredholm operator of index [math] with kernel .
Then there exists an such that for every equation (A.1) has a solution . Moreover, and
[TABLE]
Remark A.2*.*
The conditions (i),(ii), and (iii) are clear analogues to the standard local bifurcation theorem by Crandall & Rabinowitz. Condition (iv) has no analogue because it is superfluous if . In the case when it is necessary unless we also relax the conclusion of the theorem. Moreover, separates the domain and codomain of the operators in a way that makes the proof of the theorem quite straightforward.
Proof.
We begin by performing a Lyapunov Schmidt reduction. Writing where and we obtain the equations
[TABLE]
By assumption (i) we can apply the implicit function theorem to obtain that solves the first equation. We note that and , . Moreover, by assumption (iv) we can consider the restricted operator and perform a Lyapunov-Schmidt reduction. It follows that . Due to this fact and assumption (iv) we get that
[TABLE]
This means that we can write
[TABLE]
and solve
[TABLE]
instead. The functions are differentiable and
[TABLE]
Since is invertible this means we can apply the implicit function theorem to obtain a differentiable function defined in that solves eq. A.2.
We end by noting that we do not obtain uniqueness due to the fact that if then is not equivalent to . ∎
acknowledgements
This work was carried out during the tenure of an ERCIM ’Alain Bensoussan’ Fellowship Programme. The Author would also like to thank Mats Ehrnström for constructive comments on the structure of the article.
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