Quadratic life span of periodic gravity-capillary water waves
Massimiliano Berti, Roberto Feola, Luca Franzoi

TL;DR
This paper rigorously reduces the gravity-capillary water waves equations to Birkhoff normal form, demonstrating that small initial data solutions persist for long times despite potential resonances and chaotic dynamics.
Contribution
It provides a Birkhoff normal form reduction for the system and proves long-time existence of solutions for small initial data, accounting for possible resonances.
Findings
Normal form reduction up to cubic degree.
Long-time stability for small initial data.
Finite 3-wave resonances and chaotic dynamics possible.
Abstract
We consider the gravity-capillary water waves equations for a bi-dimensional fluid with a periodic one-dimensional free surface. We prove a rigorous reduction of this system to Birkhoff normal form up to cubic degree. Due to the possible presence of 3-waves resonances for general values of gravity, surface tension and depth, such normal form may be not trivial and exhibit a chaotic dynamics (Wilton-ripples). Nevertheless we prove that for all the values of gravity, surface tension and depth, initial data that are of size in a sufficiently smooth Sobolev space lead to a solution that remains in an -ball of the same Sobolev space up to times of order . We exploit that the -waves resonances are finitely many, and the Hamiltonian nature of the Birkhoff normal form.
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Quadratic life span
of periodic gravity-capillary water waves
M. Berti, R. Feola, L. Franzoi
Abstract
We consider the gravity-capillary water waves equations for a bi-dimensional fluid with a periodic one-dimensional free surface. We prove a rigorous reduction of this system to Birkhoff normal form up to cubic degree. Due to the possible presence of -waves resonances for general values of gravity, surface tension and depth, such normal form may be not trivial and exhibit a chaotic dynamics (Wilton-ripples). Nevertheless we prove that for all the values of gravity, surface tension and depth, initial data that are of size in a sufficiently smooth Sobolev space lead to a solution that remains in an -ball of the same Sobolev space up times of order . We exploit that the -waves resonances are finitely many, and the Hamiltonian nature of the Birkhoff normal form.
1 Introduction and main results
We consider an incompressible and irrotational perfect fluid, under the action of gravity, occupying at time the bi-dimensional domain
[TABLE]
periodic in the horizontal variable, with depth which may be finite or infinite. The time-evolution of the fluid is determined by a system of equations for the free surface and the function where is the velocity potential in the fluid domain. Given the shape of the domain and the Dirichlet value of the velocity potential at the top boundary, one recovers as the unique solution of the elliptic problem
[TABLE]
According to Zakharov [35] and Craig-Sulem [13], the variables evolve under the system
[TABLE]
where is the acceleration of gravity, the surface tension, and is the nonlocal Dirichlet-Neumann operator defined by .
As observed by Zakharov [35], the equations (1.1) are the Hamiltonian system
[TABLE]
where denotes the -gradient, with Hamiltonian
[TABLE]
given by the sum of the kinetic and potential energy of the fluid and the energy of the capillary forces. We remind that the Poisson bracket between two functions , is
[TABLE]
The “mass” is a prime integral of (1.1) and, with no loss of generality, we can fix it to zero by shifting the coordinate. Moreover (1.1) is invariant under spatial translations and Noether’s theorem implies that the momentum is a prime integral of (1.1).
Let , , denote the Sobolev spaces of -periodic functions of . The variable belongs to the subspace of of zero average functions (for some positive ). On the other hand, the variable belongs to the homogeneous Sobolev space obtained by the equivalence relation if and only if is a constant. This is coherent with the fact that only the velocity field has physical meaning, and the velocity potential is defined up to a constant. For simplicity we denote the equivalence class in by and, since the quotient map induces an isometry of onto , we conveniently identify with a function with zero average.
The water waves equations (1.1) are a quasi-linear system. In the last years, they have been object of intense research both in the periodic setting , , and in the dispersive case with data decaying at infinity. A fundamental difference between these cases concerns the dynamical behavior of the linearized water waves equations at = 0. In they are
[TABLE]
with dispersion relation
[TABLE]
Notice that, if , the Dirichlet-Neumann operator is and the dispersion relation . In the case , the solutions of (1.4) disperse to zero as . On the contrary, if , all the solutions of the linear system (1.4) are time periodic, or quasi-periodic, or almost periodic in time, with linear frequencies of oscillations , . In such a case a natural tool to analyze the nonlinear dynamics of (1.1), at least for small amplitude solutions, is normal form theory, that is particularly difficult due to the quasi-linear nature of the nonlinearity. In [14], Craig and Sulem developed a Birkhoff normal form analysis for (1.1) starting from the Taylor expansion of the Hamiltonian (1.2),
[TABLE]
where (up to a constant)
[TABLE]
and collects all the terms of homogeneity in greater or equal than . Unfortunately, in this Taylor expansion there is a priori no control of the unboundedness of the Hamiltonian vector field associated to .
Normal form theory for gravity-capillary water waves, even in , has been developed in Berti-Delort [6], proving, for most values of the parameters , an almost global existence result for the solutions of (1.1) in Sobolev spaces. A key point is, in analogy with the KAM theory approach in [8], to transform the unbounded water waves vector field to a paradifferential one with constant coefficient symbols, up to smoothing operators. Very recently, Birkhoff normal form and long time existence results for periodic pure gravity water waves in infinite depth, where no parameters are available, have been proved in Berti-Feola-Pusateri [7]. A key point is a normal form uniqueness argument which allows to identify the paradifferential normal form with the formal Hamiltonian Birkhoff normal form up to fourth degree, which turns out to be completely integrable.
Complementing these works, the goal of this paper is to prove that, for any value of , , the gravity-capillary water waves system (1.1) is conjugated to its Birkhoff normal form, up to cubic remainders that satisfy energy estimates (Theorem 1.1), and that all the solutions of (1.1), with initial data of size in a sufficiently smooth Sobolev space, exist and remain in an -ball of the same Sobolev space up times of order , see Theorem 1.2. Let us state precisely these results.
Main results. To state our first main result, concerning the rigorous reduction of system (1.1) to its Birkhoff normal form up to cubic degree, let us assume that, for large enough and some , we have a classical solution
[TABLE]
of the Cauchy problem for (1.1). The existence of such a solution, at least for small enough , is guaranteed by local well-posedness theory, see the literature at the end of the section.
Theorem 1.1**.**
(Cubic Birkhoff normal form)*
Let , and . There exist and , such that, if is a solution of (1.1) satisfying (1.7) with*
[TABLE]
then there exists a bounded and invertible linear operator , which depends (nonlinearly) on , such that
[TABLE]
and the variable satisfies the equation
[TABLE]
where:
* is the Fourier multiplier with symbol defined in (1.5) and is defined in (5.3),*
* the Hamiltonian has the form*
[TABLE]
where , and denotes the -th Fourier coefficient of the function (see (2.2)), and the coefficients
[TABLE]
with defined in (3.2) and ;
* satisfies and the “energy estimate”*
[TABLE]
The main point of Theorem 1.1 is the construction of the bounded and invertible transformation in (1.9) which recasts (1.1) in the Birkhoff normal form (1.10), where the cubic vector field satisfies the energy estimate (1.13). We remark that Craig-Sulem [14] constructed a bounded and symplectic transformation that conjugates (1.1) to its cubic Birkhoff normal form, but the cubic terms of the transformed vector field do not satisfy energy estimates.
We underline that, for general values of gravity, surface tension and depth , the “resonant” Birkhoff normal form Hamiltonian in (1.11) is non zero, because the system
[TABLE]
for , may possess integer solutions , known as -waves resonances (cases with absence of -waves resonances are discussed in remark 4.5). The resonant Hamiltonian gives rise to a complicated dynamics, which, in fluid mechanics, is responsible for the phenomenon of the Wilton ripples. Nevertheless we are able to prove the following long time stability result.
Theorem 1.2**.**
(Quadratic life span)* For any value of , , , , there exists and, for all , there are , , , such that, for any , any initial data*
[TABLE]
there exists a unique classical solution of (1.1) belonging to
[TABLE]
satisfying . Moreover
[TABLE]
Before presenting the literature about existence results for water waves, we describe some key points concerning the proof of these results:
-
The long time existence Theorem 1.2 is deduced by the complete conjugation of the water waves vector field (1.1) to its Birkhoff normal form up to degree , Theorem 1.1, and not just on the construction of modified energies.
-
Since the gravity-capillary dispersion relation is superlinear, the water waves equations (1.1) can be reduced, as in [6], to a paradifferential system with constant coefficient symbols, up to smoothing remainders (see Proposition 3.2). At the beginning of Section 4 we remark that, thanks to the -translation invariance of the equations, the symbols in (3.9) of the quadratic paradifferential vector fields are actually zero. For this reason, in Section 4, it just remains to perform a Poincaré- Birkhoff normal form on the quadratic smoothing vector fields, see Proposition 4.3.
-
Despite the fact that our transformations are non-symplectic (as in [6], [7]), we prove, in Section 5.1, using a normal form identification argument (simpler than in [7]), that the quadratic Poincaré-Birkhoff normal form term in (4.9) coincides with the Hamiltonian vector field with Hamiltonian (1.11).
-
The Hamiltonian is a prime integral of the resonant Birkhoff normal form . Moreover, since (1.14) admits at most finitely many integer solutions (Lemma 4.4) the Hamiltonian where , for some finite . Therefore, any solution of the Birkhoff normal form satisfies, for any ,
[TABLE]
and remains bounded for all times. Finally we deduce the energy estimate (5.27) for the solution of the whole system (1.10), where we take into account the effect of , which implies stability for all .
Literature. Local existence results for the initial value problem of the water waves equations go back to the pioneering works of Nalimov [27], Yosihara [34], Craig [12] for small initial data, Wu [30, 31] without smallness assumptions, and Beyer-Günther [9] in presence of surface tension. For some recent results about gravity-capillary waves we refer to [4, 26, 11, 28, 10, 1]. Clearly, specializing these results for initial data of size , the solutions exist and stay regular for times of order .
Global well-posedness. In the case and the initial data decay sufficiently fast at infinity, global in time solutions have been constructed exploiting the dispersive effects of the system. The first global in time solutions were proved in by Germain-Masmoudi-Shatah [17] and Wu [33] for gravity water waves, by Germain-Masmoudi-Shatah [18] for the capillary problem, and for gravity-capillary water waves by Deng-Ionescu-Pausader-Pusateri [15]. In an almost global existence result for gravity waves was proved by Wu [32], improved to global regularity by Ionescu-Pusateri [23], Alazard-Delort [2], Hunter and Ifrim-Tataru [20, 21]. For capillary waves, global regularity was proved by Ionescu-Pusateri [24] and Ifrim-Tataru [22].
Normal forms. For space periodic water waves in absence of -waves resonances, existence results for times of order have been obtained in [32, 29, 23, 2, 20] for pure gravity waves, in [24, 22] for pure capillarity waves, and in [19] for gravity waves over a flat bottom. If we refer to [25] for an result. The only existence result for parameter independent water waves is proved in [7], and it is based on the complete integrability of the fourth order Birkhoff normal form for pure gravity water waves in infinite depth.
An almost global existence result of periodic gravity-capillary water waves, even in , for times has been proved by Berti-Delort [6], for almost all values of . The restriction on the parameters arises to verify the absence of -waves interactions at any . The restriction to even in solutions arises because the transformations in [6] are reversibility preserving but not symplectic. Almost global existence results for fully nonlinear reversible Schrödinger equations have been proved in [16].
We finally mention that time quasi-periodic solutions for (1.1) have been constructed in Berti-Montalto [8] and, for pure gravity waves, in Baldi-Berti-Haus-Montalto [5].
Acknowledgements. The research was partially supported by PRIN 2015 KB9WPT-005 and ERC project FAnFArE, n. 637510.
2 Functional Setting and Paradifferential calculus
In this section we recall definitions and results of para-differential calculus following Chapter of [6], where we refer for more information. In the sequel we will deal with parameters
[TABLE]
Given an interval , symmetric with respect to , and , we define the space C^{K}_{*}(I,{\dot{H}}^{s}(\mathbb{T},\mathbb{C}^{2})):=\bigcap_{k=0}^{K}C^{k}\big{(}I;\dot{H}^{s-\frac{3}{2}k}(\mathbb{T};\mathbb{C}^{2})\big{)} endowed with the norm
[TABLE]
With similar meaning we consider . We denote by the subspace of functions in such that U={\bigl{[}\begin{smallmatrix}u\\ \overline{u}\end{smallmatrix}\bigr{]}}. Given we set
[TABLE]
We expand a -periodic function , with zero average in , (which is identified with in the homogeneous space), in Fourier series as
[TABLE]
We also use the notation and . We set and .
For we denote by the orthogonal projector from to the subspace spanned by , i.e. and we denote by also the corresponding projector in . If is a -tuple of functions, , we set .
We deal with vector fields which satisfy the -translation invariance property
[TABLE]
Para-differential operators. We first give the definition of the classes of symbols, collecting Definitions , and in [6]. Roughly speaking, the class contains homogeneous symbols of order and homogeneity in , while the class contains non-homogeneous symbols of order which vanish at degree at least in , and that are -times differentiable in .
Definition 2.1**.**
(Classes of symbols)* Let , with , in with , .*
* -homogeneous symbols. We denote by the space of symmetric -linear maps from to the space of functions of , , satisfying the following. There is and, for any , there is such that*
[TABLE]
for any in , and . Moreover we assume that, if for some , , then there exists a choice of signs such that . For we denote by the space of constant coefficients symbols which satisfy (2.3) with and the right hand side replaced by . In addition we require the translation invariance property
[TABLE]
* Non-homogeneous symbols. Let . We denote by the space of functions , defined for , for some large enough , with complex values such that for any , any , there are , and for any and any , with *
[TABLE]
* Symbols. We denote by the space of functions such that there are homogeneous symbols , , and a non-homogeneous symbol such that . We denote by the space matrices with entries in .*
As a consequence of the momentum condition (2.4) a symbol in the class , for some , can be written as
[TABLE]
for some coefficients , see [7].
Remark 2.2**.**
A symbol of the form (2.6), independent of , is actually .
We also define classes of functions in analogy with our classes of symbols.
Definition 2.3**.**
(Functions)* Fix with , with , . We denote by , resp. , , the subspace of , resp. , resp. , made of those symbols which are independent of . We write , resp. , , to denote functions in , resp. , , which are real valued.*
Paradifferential quantization. Given we consider functions and , even with respect to each of their arguments, satisfying, for ,
[TABLE]
For we set . We assume moreover that , , and , .
If is a smooth symbol we define its Weyl quantization as the operator acting on a -periodic function (written as in (2.2)) as
[TABLE]
where is the Fourier coefficient of the periodic function .
Definition 2.4**.**
(Bony-Weyl quantization)* If a is a symbol in , respectively in , we set*
[TABLE]
where in the last equality stands for the Fourier transform with respect to the variable, and we define the Bony-Weyl quantization of as
[TABLE]
If is a symbol in , we define its Bony-Weyl quantization
Paradifferential operators act on homogeneous spaces. If is in , the corresponding para-differential operator is bounded from to , for all , see Proposition 3.8 in [6].
Definition 2.4 is independent of the cut-off functions , , up to smoothing operators that we define below (see Definition in [6]). Roughly speaking, the class contains smoothing operators which gain derivatives and are homogeneous of degree in , while the class contains non-homogeneous -smoothing operators which vanish at degree at least in , and are -times differentiable in .
Given we denote by the second largest among the integers .
Definition 2.5**.**
(Classes of smoothing operators)* Let , with , and .*
(i) -homogeneous smoothing operators.* We denote by the space of -linear maps from to , symmetric in , of the form that satisfy the following. There are , such that*
[TABLE]
for any , , , any . Moreover, if
[TABLE]
then there is a choice of signs such that . In addition we require the translation invariance property
[TABLE]
(ii) Non-homogeneous smoothing operators. We denote by the space of maps defined on which are linear in the variable and such that the following holds true. For any there are and such that, for any , any , any and any , we have
[TABLE]
(iii) Smoothing operators. We denote by the space of maps that may be written as for some in , and in .
We denote by the space of matrices with entries in the class .
Below we introduce classes of operators without keeping track of the number of lost derivatives in a precise way (see Definition 3.9 in [6]). The class denotes multilinear maps that lose derivatives and are -homogeneous in , while the class contains non-homogeneous maps which lose derivatives, vanish at degree at least in , and are -times differentiable in .
Definition 2.6**.**
(Classes of maps)* Let , with , , with and .*
(i) -homogeneous maps.* We denote by the space of -linear maps from to which are symmetric in , of the form and that satisfy the following. There is such that*
[TABLE]
for any , any , in , any . Moreover the properties (2.8)-(2.9) hold.
(ii) Non-homogeneous maps. We denote by the space of maps defined on which are linear in the variable and such that the following holds true. For any there are and such that for any , any , any , , we have that is bounded by the right hand side of (2.10).
(iii) Maps. We denote by the space of maps that may be written as for some in , and in . Finally we set , , .
We denote by the space of matrices whose entries are maps in . We set .
Given an operator in (or in ), and , , the momentum condition (2.9) implies that
[TABLE]
for some , see [7].
Proposition 2.7**.**
(Compositions)* Let , with , , and . Let , and . Then:*
* , are in ;*
* and are smoothing operators in ;*
* If , , then belongs to .*
Proof.
See Propositions 3.16, 3.17 in [6]. The translation invariance properties for the composed operators and symbols in items (i)-(ii) follow as in [7]. ∎
Real-to-real operators. Given a linear operator acting on (it may be a smoothing operator in or a map in ) we associate the linear operator defined by
[TABLE]
We say that a matrix of operators acting on is real-to-real, if it has the form
[TABLE]
If is a real-to-real matrix of operators then, given V={\bigl{[}\begin{smallmatrix}v\\ \overline{v}\end{smallmatrix}\bigr{]}}, the vector has the form Z={\bigl{[}\begin{smallmatrix}z\\ \overline{z}\end{smallmatrix}\bigr{]}}, i.e. the second component is the complex conjugated of the first one.
Given two linear operators (either two operator-valued matrices acting on as in (2.12)), we denote their commutator by .
The notation means that for some positive constant .
3 Paradifferential reduction to constant symbols
up to smoothing operators
The first step in order to prove Theorem 1.1 is to write (1.1) in paradifferential form, to symmetrize it, and reduce to paradifferential symbols which are constant in , see Proposition 3.2. These results are proved in [6] (up to minor details). We denote the horizontal and vertical components of the velocity field at the free interface by
[TABLE]
and the “good unknown” of Alinhac
[TABLE]
as introduced in Alazard-Metivier [3]. The function belongs to , for any (see Proposition 7.4 in [6]). Then, by the action of a paraproduct, if and then the good unknown is in .
Define the Fourier multiplier of order as
[TABLE]
and consider the complex function
[TABLE]
where acts on functions modulo constants in itself.
Let . We first remark that, if solves the gravity-capillary system (1.1), then the function defined in (3.3) satisfies, by Proposition in [6], for , as long as stays in the unit ball of ,
[TABLE]
As a consequence, if (1.8) holds then
[TABLE]
Proposition 3.1**.**
(Paradifferential complex form of the water waves equations)*
Let , . Assume that solves the gravity-capillary system (1.1) and satisfy (1.8) for some and . Then the function U:={\bigl{[}\begin{smallmatrix}u\\ \overline{u}\end{smallmatrix}\bigr{]}}, with defined in (3.3), solves*
[TABLE]
where and
* where is the dispersion relation symbol defined in (1.5). the matrix of symbols has the form*
[TABLE]
where
* the function is in ;*
* the symbols are in , , and are in for ;*
* the matrix of smoothing operators is in ;*
* the operators and are real-to-real, according to (2.12).*
Proof.
It is Corollary and Proposition in [6]. The only difference is that is not even in . The property that the homogeneous components , , , of the matrices , satisfy (2.4) and (2.9) is checked as in [7]. ∎
System (3.6) has the form
[TABLE]
where is a real-to-real map in for some (using that paradifferential operators and smoothing remainders are maps, see (4.2.6) in [6]).
As in [6], since the dispersion law (1.5) is super-linear, system (3.6) can be transformed into a paradifferential diagonal system with a symbol constant in , up to smoothing terms.
Proposition 3.2**.**
(Reduction to constant coefficients up to smoothing operators)* Fix arbitrary. There exist , such that, for any , for all small enough, for all and any solution of (3.6), there is a family of real-to-real, bounded, invertible linear maps , , such that the function*
[TABLE]
solves the system
[TABLE]
where
* the function and the diagonal matrix of symbols are independent of ;*
* the symbol belongs to ;*
* is matrix of smoothing operators in *
* the operators and are real-to-real, according to (2.12);*
* the map satisfies, for all , for any ,*
[TABLE]
uniformly in . Moreover the map where is in and with estimates uniform in .
Proof.
This statement collects the results of Propositions , and in [6]. The remainder in (5.2.9) in [6] has the form (3.9) expressing and using the estimates (3.10), which follow by Lemma 3.22 in [6]. Another difference is that is not even in . The -invariance properties (2.4) for the symbols and (2.9) for the smoothing operators are checked as in [7]. The last statement follows using Lemma A.2 in [7]. ∎
4 Poincaré - Birkhoff normal form at quadratic degree
From this section the analysis strongly differs from [6].
- •
Notation: for simplicity in the sequel we omit to write the dependence on the time in the symbols, smoothing remainders and maps, writing , , instead of , , .
The aim of this section is to transform system (3.9) into its quadratic Poincaré-Birkhoff normal form, see system (4.9). We first observe that the paradifferential vector field in (3.9) of quadratic homogeneity is actually zero.
Lemma 4.1**.**
(Quadratic Poincaré-Birkhoff normal form up to smoothing vector fields)* The system (3.9) with has the form*
[TABLE]
where and
[TABLE]
where is a diagonal matrix of symbols independent of , such that
[TABLE]
and . The operators and are real-to-real.
Proof.
We expand in homogeneity the function , , the diagonal matrix of symbols , , and the smoothing remainder , . Since the function and admit an expansion as (2.6) and are independent of (see Proposition 3.2), Remark 2.2 implies that , . This proves (4.1)-(4.3). ∎
System (4.1) is yet in Poincaré-Birkhoff normal form at degree 2 up to smoothing remainders and the cubic term in (4.2) admits an energy estimate as (1.13), since is independent of and purely imaginary up to symbols of order [math], see (4.3).
The goal is now to transform the quadratic smoothing term in (4.1) to Poincaré-Birkhoff normal form at degree , see Definition 4.2. The remainder in (4.1) is real-to-real (i.e. has the form (2.12)), satisfies the momentum condition (2.9), thus it has the form (2.11), and so we write it as
[TABLE]
for . For any we expand
[TABLE]
where, for , and is the homogeneous smoothing operator
[TABLE]
with entries
[TABLE]
for suitable scalar coefficients . The restriction is due to the momentum condition.
Definition 4.2**.**
(Poincaré-Birkhoff Resonant smoothing operator)* Given a real-to-real, smoothing operator as in (4.4)-(4.7), we define the Poincaré-Birkhoff resonant, real-to-real, smoothing operator with matrix entries defined as in (4.7) such that, for any , ,*
[TABLE]
In the next Proposition we conjugate (4.1) into its complete quadratic Poincaré-Birkhoff normal form.
Proposition 4.3**.**
(Quadratic Poincaré-Birkhoff normal form)* There exists such that, for all , with given by Proposition 3.2, there exists such that, for any , for all small enough, and any solution of the water waves system (3.6), there is a family of real-to-real, bounded, invertible linear maps , , such that, if solves (4.1), then the function*
[TABLE]
solves
[TABLE]
where:
* is the matrix in (3.6) and has symbol (1.5);*
* is the real-to-real Poincaré-Birkhoff resonant smoothing operator introduced in Definition 4.2;*
* has the form*
[TABLE]
where is defined in (4.2) and satisfies (4.3), while is a matrix of real-to-real smoothing operators in ;
* the map satisfies, for any , ,*
[TABLE]
uniformly in . Moreover the map where is in and with estimates uniform in .
In order to prove Proposition 4.3 we first provide lower bounds on the “small divisors” which appear in the Poincaré-Birkhoff reduction procedure.
4.1 Three waves interactions
We analyze the possible three waves interactions among the linear frequencies (1.5). We first notice that they admit an expansion as
[TABLE]
for some constant .
Lemma 4.4**.**
(-waves interactions)*
There exist , such that for any , , such that*
[TABLE]
and , we have
[TABLE]
If , then, either the phase is zero, or (4.14) holds.
Proof.
If then the bound (4.14) is trivial for all . Assume and (the cases and are the same, up to reordering the indexes). Then, by (4.13), we have and we may suppose that , otherwise the bound (4.14) is trivial. Without loss of generality we assume , thus, also and are positive. In conclusion we assume that . By (4.12),
[TABLE]
Now
[TABLE]
using that . By (4.15) and (4.16) we deduce that the phase
[TABLE]
if , in particular, since , if
[TABLE]
Recall that . Therefore and we conclude that
[TABLE]
For the finitely many integers satisfying such that the phase , the lower bound (4.14) is trivial. ∎
Remark 4.5**.**
The constant in (4.12) is bounded by , for some constant independent of . Then, there are such that, if , , then (4.17) holds, for all . As a consequence there are no -waves interactions, i.e. (4.14) holds for all .
Notice that, for some values of the parameters , there could be -waves interactions.
4.2 Poincaré-Birkhoff normal form of the
smoothing quadratic terms
In order to prove Proposition 4.3, we conjugate (4.1) with the flow
[TABLE]
with an operator in , of the same form of in (4.4)-(4.7), to be determined. We introduce the new variable Y:={\bigl{[}\begin{smallmatrix}y\\ \overline{y}\end{smallmatrix}\bigr{]}}=\big{(}\mathfrak{C}^{\theta}(U)[Z]\big{)}_{|_{\theta=1}}.
Lemma 4.6**.**
If solves the homological equation
[TABLE]
where is the Poincaré-Birkhoff resonant operator in Definition 4.2, then
[TABLE]
where is the same diagonal matrix of symbols in (4.2) and is a real-to-real smoothing operator in with (fixed below (3.8)).
*The flow map in (4.18) satisfies (4.11) and where is in and with estimates uniform in . *
Proof.
Since is a smoothing operator then the flow in (4.18) is well-posed in Sobolev spaces and satisfies the estimates (4.11), as well as the last statement, by e.g. Lemma in [7]. To conjugate (4.1) we apply the usual Lie expansion up to the first order (see for instance Lemma in [7]). Denoting , we have
[TABLE]
Using that belongs to , Proposition 2.7 and (4.11), the integral term in (4.21) is a smoothing operator in . Similarly, we obtain
[TABLE]
up to a matrix of smoothing operators in . Finally
[TABLE]
plus a smoothing operator in .
Next we consider the contribution coming from the conjugation of . Applying again a Lie expansion formula (see Lemma in [7]) we get
[TABLE]
Recalling (3.8) we have
[TABLE]
up to a term in , where we used Proposition 2.7. By (4.23), the fact that is in and (4.11), we deduce that the term in (4.22) belongs to . Collecting all the previous expansions, and using that solves (4.19), we deduce (4.20). ∎
We now solve the homological equation (4.19).
Lemma 4.7**.**
(Homological equation)* Let be an operator of the form (4.4)-(4.7) with coefficients*
[TABLE]
for any , , satisfying
[TABLE]
and otherwise. Then is in and solves the homological equation (4.19).
Proof.
The coefficients in (4.24) are well defined by (4.25) and, by Lemma 4.4, they satisfy the uniform lower bound . Then the operator is in , see e.g. Lemma of [7].
Next, recalling (4.4), the homological equation (4.19) amounts to the equations
[TABLE]
for , and, setting to the equations, for any , ,
[TABLE]
Expanding as in (4.5)-(4.7) with entries
[TABLE]
we have that satisfies
[TABLE]
Hence the left hand side in (4.26) has coefficients
[TABLE]
for and with . Recalling Definition 4.2 we deduce that with coefficients in (4.24) solves the homological equation (4.19). ∎
Proof of Proposition 4.3.
We apply Lemmata 4.6 and 4.7. The change of variables that transforms (4.1) into (4.20) is where is the flow map in (4.18) that satisfies (4.11) and the last statement in Lemma 4.6. Moreover, using also the last item of Proposition 3.2 we may express
[TABLE]
Then system (4.20) can be written as system (4.9) with given in (4.10) and
[TABLE]
By (4.27) and Proposition 2.7- we have that where . ∎
5 Birkhoff normal form and quadratic life-span of solutions
In this section we prove Theorems 1.1 and 1.2. We first recall the Hamiltonian formalism in the complex symplectic variables
[TABLE]
where is the Fourier multiplier defined in (3.2).
A vector field and a function assume the form
[TABLE]
The Poisson bracket in (1.3) reads .
Given a Hamiltonian , expressed in the complex variables , the associated Hamiltonian vector field is
[TABLE]
that we also identify, using the standard vector field notation, with
[TABLE]
If is the Hamiltonian vector field of the Hamiltonian , we have
[TABLE]
The push-forward acts naturally on the commutator of nonlinear vector fields, defined in (5.14), namely
[TABLE]
Recalling (1.6), the Hamiltonian (1.2) admits, in complex coordinates, the expansion
[TABLE]
where, recalling (3.3), (1.5), (2.2),
[TABLE]
and are computed in (1.12), for .
5.1 Normal form identification and proof of Theorem 1.1
A normal form uniqueness argument allows to identify the quadratic Poincaré-Birkhoff resonant vector field in (4.9) as the cubic resonant Hamiltonian vector field obtained by the formal Birkhoff normal form construction in [14].
Proposition 5.1**.**
(Identification of the quadratic resonant Birkhoff normal form)* The Birkhoff resonant vector field defined in (4.9) is equal to*
[TABLE]
where is the cubic Birkhoff normal form Hamiltonian in (1.11).
The proof follows the ideas developed in Section in [7]. Recalling (1.6), we first expand the water waves Hamiltonian vector field in (1.1)-(1.2) in degrees of homogeneity
[TABLE]
and collects the higher order terms. System (4.9) has been obtained conjugating (1.1) under the map
[TABLE]
where is the good-unknown transformation (see (3.1))
[TABLE]
the map is defined in (5.1) (see (3.3) and Proposition 3.1), and
[TABLE]
where , are defined respectively in Propositions 3.2 and 4.3. In order to identify the quadratic vector field in system (4.9), we perform a Lie commutator expansion, up to terms of homogeneity at least . Notice that the quadratic term in (4.9) may arise by only the conjugation of under the homogeneous components of the paradifferential transformations and , neglecting cubic terms.
We use the following Lemma 5.2 that collects Lemmata , and in [7]. The variable may denote both the couple of complex variables or the real variables .
Lemma 5.2** ( [7]).**
(Lie expansion)* Consider a map , , of the form*
[TABLE]
Then:
* the family of maps is such that*
[TABLE]
where is a polynomial in and finitely many monomials for , ;
* the family of maps satisfies*
[TABLE]
where with and is a polynomial in and finitely many monomials for maps , .
(iii) Let for some map where is in and in . If solves , then the function solves
[TABLE]
up to terms of degree of homogeneity greater or equal to , where we define the nonlinear commutator
[TABLE]
- •
Notation. Given a homogeneous vector field , we denote by the induced (formal) push forward (see (5.13))
[TABLE]
where the dots denote cubic terms.
Proof of Proposition 5.1.
Step . The good unknown change of variable in (5.10). First of all we note that where
[TABLE]
Since is a function in we have that has an expansion as in (5.12) up to cubic terms. Hence, by Lemma 5.2--, we regard the inverse of the map , obtained truncating up to cubic remainders, as the (formal) time one flow of a quadratic vector field
[TABLE]
By (5.8), (5.15) and (5.16), we get
[TABLE]
Step . Complex coordinates in (5.1). In the complex coordinates (5.1), the vector field (5.17) reads, recalling (5.2) and (5.5),
[TABLE]
where, by (5.4), (5.8), (5.6),
[TABLE]
Step . The transformation in (5.11). By the last items of Proposition 3.2 and Proposition 4.3, the map has the form (5.12) up to cubic terms. Thus, by Lemma 5.2--, the approximate inverse of the truncated map can be regarded as the (formal) time-one flow of a vector field
[TABLE]
By (5.18), (5.19), (5.15), we get
[TABLE]
Comparing (4.9) and (5.21) we deduce that
[TABLE]
The vector field is in Poincaré-Birkhoff normal form, recall Definition 4.2. Therefore, defining the linear operator acting on a quadratic monomial vector field as
[TABLE]
we have that
[TABLE]
In addition, since
[TABLE]
we deduce
[TABLE]
In conclusion, (5.24), (5.22) and (5.25) imply that
[TABLE]
where is the Hamiltonian in (1.11). This proves (5.7).
**Proof of Theorem 1.1. ** Hypothesis (1.8) implies that the variable defined in (3.3) satisfies (3.5) and therefore the function U={\bigl{[}\begin{smallmatrix}u\\ \overline{u}\end{smallmatrix}\bigr{]}} belongs to the ball (recall (2.1)) with and . By Proposition 3.1 the function solves system (3.6). Then we apply Proposition 3.2 and the Poincaré-Birkhoff Proposition 4.3 with and given by Proposition 3.2, taking small enough. The map in (5.11) transforms the water waves system (3.6) into (4.9), which, thanks to Proposition 5.1, is expressed in terms of the Hamiltonian in (1.11) as
[TABLE]
where is the first component of in (4.10). Renaming , the above equation is (1.10). We define as the first component of the change of variable (5.9), namely of , with written in terms of by (3.3), (3.1). By (4.11) and (3.10) with , and using that , we get
[TABLE]
and (1.9) follows, using also (3.3), (3.1). The cubic vector field in (4.10) satisfies the estimate by Proposition 3.8 in [6] (recall that ), by (2.10) with , and (3.4), (5.26). Moreover, the vector field satisfies the energy estimate (1.13) since the symbol is independent of and purely imaginary up to symbols of order [math], see (4.3) (for the detailed argument we refer to Lemma in [7]).
5.2 Energy estimate and proof of Theorem 1.2
We now deduce Theorem 1.2 by Theorem 1.1 and the following energy estimate for the solution of the Birkhoff resonant system (1.10). By time reversibility, without loss of generality, we may only look at positive times .
Lemma 5.3**.**
(Energy estimate)* Fix as in Theorem 1.1 and assume that the solution of (1.1) satifies (1.8). Then the solution of (1.10) satisfies*
[TABLE]
Proof.
By Lemma 4.4, the Birkhoff resonant Hamiltonian in (1.11) depends on finitely many variables , , because
[TABLE]
For any function we define the projector on low modes, respectively the projector on high modes, as
[TABLE]
We write and we define the norm
[TABLE]
where (see (5.6))
[TABLE]
Since , , and is supported on finitely many Fourier modes , we have that, for some constant ,
[TABLE]
i.e. the norms and are equivalent. We now prove the estimate (5.27) for the equivalent norm .
We first note that, by (5.28), . Therefore and the equation (1.10) amounts to the system
[TABLE]
Moreover since the Hamiltonian in (1.11) is in Birkhoff normal form, it Poisson commutes with the quadratic Hamiltonian in (5.29), i.e.
[TABLE]
We have
[TABLE]
using that by item of Theorem 1.1. Moreover, since and project on -orthogonal subspaces,
[TABLE]
by item of Theorem 1.1. Integrating in the inequalities (5.2), (5.2), we deduce
[TABLE]
which, together with the equivalence (5.30), implies (5.27). ∎
Conclusion of the Proof of Theorem 1.2.
Consider initial data satisfying (1.15) with given by Theorem 1.1. Classical local existence results imply that
[TABLE]
for some and thus (1.8) holds with and . A standard bootstrap argument based on the energy estimate (5.27) (see for instance Proposition in [7]) implies that the solution of (1.10) can be extended up to a time for some , and satisfies
[TABLE]
We deduce (1.16) by (5.35), the equivalence (5.26), and going back to the original variables by (3.3) and (3.1). ∎
The reference list from the paper itself. Each links out to its DOI / PubMed record.
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