Instability of $H^1$-stable peakons in the Camassa-Holm equation
Fabio Natali, Dmitry E. Pelinovsky

TL;DR
This paper demonstrates that despite $H^1$-orbital stability of peakons in the Camassa-Holm equation, certain perturbations grow over time, revealing an instability not captured by linear analysis.
Contribution
It shows the instability of peakons under piecewise $C^1$ perturbations using characteristics, challenging the traditional stability understanding.
Findings
Piecewise $C^1$ perturbations grow over time.
Linearized stability analysis contradicts $H^1$-orbital stability.
Passage from linear to nonlinear stability in $H^1$ is invalid.
Abstract
It is well-known that peakons in the Camassa-Holm equation are -orbitally stable thanks to the presence of conserved quantities and properties of peakons as constrained energy minimizers. By using the method of characteristics, we prove that piecewise perturbations to peakons grow in time in spite of their stability in the -norm. We also show that the linearized stability analysis near peakons contradicts the -orbital stability result, hence passage from linear to nonlinear theory is false in .
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Instability of -stable peakons
in the Camassa–Holm equation
Fábio Natali
Departamento de Matemática - Universidade Estadual de Maringá, Avenida Colombo 5790, CEP 87020-900, Maringá, PR, Brazil
and
Dmitry E. Pelinovsky
Department of Mathematics and Statistics, McMaster University, Hamilton, Ontario, Canada, L8S 4K1
Abstract.
It is well-known that peakons in the Camassa–Holm equation are -orbitally stable thanks to the presence of conserved quantities and properties of peakons as constrained energy minimizers. By using the method of characteristics, we prove that piecewise perturbations to peakons grow in time in spite of their stability in the -norm. We also show that the linearized stability analysis near peakons contradicts the -orbital stability result, hence passage from linear to nonlinear theory is false in .
Key words and phrases:
Peakons, Camassa–Holm equation, characteristics, stability, instability
1. Introduction
The Camassa-Holm (CH) equation [5]
[TABLE]
can be rewritten in the convolution form
[TABLE]
where is the Green function satisfying with being Dirac delta distribution and being the convolution operator. It is clear that for , where is the standard Sobolev space of squared integrable distributions equipped with the norm with and being the Fourier transform of on .
The purpose of function is not only to rewrite the evolution problem for the CH equation (1.1) in the convolution form (1.2) that depends on the first derivative of in and does not depend on its higher-order derivatives. In addition, expresses a particular family of solutions with which are referred to as peakons (or peaked solitary waves). Indeed, the validity of these peakons as solutions to the CH equation in the convolution form (1.2) can be checked directly from the identity
[TABLE]
which is piecewise on both sides from the peak at .
Cauchy problem for the CH equation (1.1) with the initial data was studied in the series of papers [7, 8, 9]. It was shown in Theorem 4.1 in [7] that if does not change sign on , then the corresponding solution exists globally in time. If there exists such that on , the same conclusion applies (Theorem 4.4 in [7]), whereas if on , the local solution breaks in a finite time in the sense that the slope of the solution becomes unbounded from below in a finite time (Theorems 5.1 and 5.2 in [7]).
The condition on the initial data was used in [7, 8, 9] to control the auxiliary quantity and to extend local solutions to global solutions of the CH equation (1.1). Without these requirements, local well-posedness of the Cauchy problem can be proven for initial data in for every [22, 28] but cannot be pushed below and at because of lack of uniform continuity of the local solution with respect to initial data and the norm inflation [4, 16].
Cauchy problem for the CH equation in the convolution form (1.2) with the initial data in was studied in [2] (similar results appear also in [17]) by means of a coordinate transformation of the quasilinear equation to an equivalent semilinear system. It was proven that the Cauchy problem for the equivalent semilinear system admits a unique global solution (Theorem 1 in [2]), which provides a global conservative solution to the CH equation (Theorem 2 in [2]) such that
[TABLE]
This global conservative solution is consistent with the two conserved quantities of the CH equation:
[TABLE]
Moreover, it was proven in [3] that the global conservative solution to the CH equation (1.2) is unique for every initial data in . Continuous dependence from initial data and local well-posedness of the weak solutions
[TABLE]
to the CH equation (1.2) was established very recently in [24] for every , where is the Sobolev space of functions with bounded first derivatives and is a local existence time.
The previous study of stability of peakon solutions in [10, 11] relies on the existence of conserved quantities (1.5). It was proven in [10] that the peakon is a unique (up to translation) minimizer of in subject to the constraint (Proposition 3.6 in [10]), where and . Consequently, global smooth solutions which are close to in remains close to the translated orbit in for all (Theorem 3.1 in [10]).
A different result on stability of peakons was proven in [11], which we reproduce here.
Theorem 1**.**
[11*]**
Assume existence of a solution to the CH equation (1.1) with either finite or infinite . For every small , if the initial data satisfies*
[TABLE]
then the solution satisfies
[TABLE]
where is a point of maximum for .
In Theorem 1, the local solution to the CH equation (1.1) may break in a finite time in the sense of Theorem 5.1 in [7]:
[TABLE]
Nevertheless, the -norm of the solution remains finite as thanks to the energy conservation in time up to the blowup time . This implies that the bound (1.8) remains valid in the limit and allows us to say that peakons of the CH equation are orbitally stable.
Various extensions of the orbital stability of peakons have been made recently. Orbital stability of peaked periodic waves in the CH equation was proven in [19, 20]. Stability of peakons in another integrable equation called the Degasperis–Procesi equation was established in [23] by extending ideas of [11]. Asymptotic stability of peakons in the class of functions with being a non-negative finite measure is proven in [26]. Asymptotic stability of trains of peakons and anti-peakons with being a sign-indefinite finite measure was constructed recently in [27].
Multi-peakon solutions were constructed by many analytical and numerical tools [1, 6, 18, 25]. The local characteristic curve for the Camassa–Holm equation (1.2) is defined by the equation
[TABLE]
Since the multipeakon solution is known in the closed form , where satisfies the finite-dimensional Hamiltonian system
[TABLE]
it is clear that the single peakons move along the local characteristic curves [25] so that
[TABLE]
Global conservative solutions to the CH equation with multi-peakons were studied with the inverse scattering transform method in [12], where the long-time behavior of solutions with peakons was investigated (see also [1, 21]) and details of collisions between peakons and anti-peakons were given (see also [2, 27]).
The purpose of this work is to address the question of stability of a single peakon in the time evolution of the CH equation beyond the orbital stability result of Theorem 1. We start with the linearized stability analysis and study evolution of the linearized equation around the peakons by using the method of characteristics. The same method is also useful to prove nonlinear instability of piecewise perturbations to peakons. This instability develops in spite of the orbital stability result of Theorem 1.
The previous works avoid the question of linearized stability of peakons. It was noticed in [10] that “the nonlinearity plays a dominant role rather than being a higher-order correction”, so that “the passage from the linear to the nonlinear theory is not an easy task, and may even be false”. The authors of [23] added that the peakons are not differentiable in , which makes it difficult to analyze the spectrum of the linearized operator around the peakons.
By adding a perturbation to the single peakon moving with the normalized speed and dropping the quadratic term in , we obtain the linearized equation for from the CH equation in the convolution form (1.2):
[TABLE]
In what follows, we use instead of thanks to the translational invariance of the convolution operator. After the change, the location of the peak of is placed at . The following theorem represents the first main result of this work.
Theorem 2**.**
For every initial data satisfying , there exists a unique global solution to the linearized equation (1.11) satisfying ,
[TABLE]
and
[TABLE]
for every .
In Theorem 2, we confirm the expectation from [11] that the passage from the linear to the nonlinear theory may be false in . Indeed, the sharp exponential growth of in (1.12) for the solution of the linearized equation (1.11) contradicts the bound (1.8) in Theorem 1 obtained for the solution of the full nonlinear equation (1.2).
On the other hand, by solving the linearized equation (1.11) with a method of characteristics, we discover the intrinsic instability associated with the peaked profile of the traveling wave (Lemma 3). This instability is related to the characteristics to the right of the peak for but not to the left of the peak for .
Within the linearized equation (1.11), we also discover that if , the continuous initial data generates a finite jump discontinuity in the solution at the peak for every small (Lemma 2). This finite jump discontinuity is allowed in the domain of the linearized operator associated with the linearized equation (1.11) in (Remark 1), however it prevents the solution to stay in for every . Related to this fact, we prove that the single peak of a perturbed peakon in the CH equation in the convolution form (1.2) moves with the speed equal to the local characteristic speed as in (1.10) (Lemma 6). This allows us to show that the constraint on the solution at the peak required in Theorem 2 is satisfied identically in the time evolution of the full nonlinear equation (1.2) (Remark 3).
Similarly, we show for the linearized equation (1.11) that if with and , then for every small because of the finite jump discontinuity of at for (Remark 2). Compared to the constraint on at the peak, there is no way to maintain a constraint on at the peak and to prevent the finite jump discontinuity of at in the time evolution of the full nonlinear equation (1.2).
The above facts suggest that the -based spaces like or may not be the best spaces to study the intrinsic instability of peakons in the CH equation. Instead, we work in the space of bounded continuous functions on which are piecewise continuous differentiable with a finite jump discontinuity of the first derivative at and bounded first derivatives away from . This space is denoted by :
[TABLE]
The linear instability result of Theorem 2 is easily extended to prove exponential instability of because of the characteristics to the right of the peak (Lemma 4). Unlike the linear instability in of Theorem 2, which cannot be true in the nonlinear evolution due to the result of Theorem 1, the linear instability in persists in the full nonlinear equation (1.2) as the nonlinear instability of peakons with respect to piecewise perturbations (Lemma 9). The following theorem represents the second main result of this work.
Theorem 3**.**
For every , there exist and satisfying
[TABLE]
such that the global conservative solution to the CH equation (1.2) with the initial data satisfies
[TABLE]
where is a point of peak of for .
We note that the peakon is located on the boundary between global and breaking solutions to the Camassa–Holm equation in the sense that is zero everywhere except at the peak. It is expected that some perturbations to the peakons lead to global solutions whereas some others break in a finite time in the same sense as (1.9). The nonlinear instability result in Theorem 3 does not distinguish between these two possible scenarios because the bound (1.16) is attained before the blowup time . Note that we measure the instability of peakons in the same norm as the one used to study wave breaking in the Camassa–Holm equation in [7]. Although perturbations to the peakons are not smooth in , we have justified the same blow-up criterion in the method of characteristics for the solutions in as the criterion (1.9) for the smooth solutions (Lemma 7).
A general global conservative solution to the CH equation (1.2) satisfies (1.4) and may have finite jumps of the energy in (1.5) at some time instances, which correspond to collision between peakons and anti-peakons [2]. The initial data in Theorem 3 exclude anti-peakons and hence no jumps of the energy occur in the time evolution of the global conservative solution, which hence satisfies . Since , this unique global conservative solution coincides for with the local solution (1.6) constructed in [24] where the maximal existence time may be finite because of the blow-up of the norm of the local solution. Again, this blow-up of the norm agrees well with the instability criterion (1.16) in Theorem 3.
Study of the instability of peakons in the CH equation is inspired by the recent work [13, 14, 15] on smooth and peaked periodic waves in the reduced Ostrovsky equation,
[TABLE]
which is another generalization of the inviscid Burgers equation . While smooth periodic waves are linearly and nonlinearly stable [13, 14], peaked periodic waves were found to be linearly unstable because the -norm of the perturbation grows exponentially in time [15]. The linear instability was found from the solution of the truncated linearized equation obtained by the method of characteristics and from the estimates on the solution of the full linearized equation. Nonlinear instability was not studied in [15] due to the lack of global well-posedness results on solutions of the reduced Ostrovsky equation (1.17) in .
Compared to [15], we show here that the full linearized equation (1.11) can be solved by method of characteristics without truncation and that the nonlinear instability of peakons in the CH equation (1.2) can be concluded from the linear instability of perturbations in .
The remainder of the article is organized as follows. Linearized evolution near a single peakon is studied in Section 2, where the proof of Theorem 2 is given. Nonlinear evolution of piecewise perturbations to a single peakon is studied in Section 3, where the proof of Theorem 3 is given. Section 4 concludes the article with ideas for further work.
2. Linearized evolution near a single peakon
Let us first simplify the linearized equation (1.11) by using the following elementary result.
Lemma 1**.**
Assume that . Then, for every ,
[TABLE]
Proof.
Since integrals of absolutely integrable functions are continuous and since , the map
[TABLE]
is continuous for every . Now, is continuously embedded into the space of bounded continuous functions on decaying to zero at infinity and thus, . Integrating by parts yields the following explicit expression for every :
[TABLE]
which simplifies the left-hand side of (2.1) to the form:
[TABLE]
Furthermore, we obtain
[TABLE]
which completes the proof of (2.1). ∎
The Cauchy problem for the linear equation (1.11) can be written in the evolution form:
[TABLE]
where the linearization near the single peakon for a perturbation in is given by
[TABLE]
thanks to Lemma 1 and the translational invariance.
In order to define a strong solution to the Cauchy problem (2.2), we consider the operator with the maximal domain given by
[TABLE]
Since as exponentially fast and , is equivalent to
[TABLE]
Remark 1*.*
Since , is continuously embedded into but it is not equivalent to . In particular, if with a finite jump discontinuity at then but . However, the representation (2.1) in Lemma 1 does not hold for solutions in with a finite jump discontinuity at .
Let us consider the linearized Cauchy problem (2.2) in the space defined by (1.14). The following lemma shows that unless satisfies the constraint , solutions to the Cauchy problem (2.2) do not remain in for .
Lemma 2**.**
Assume that with and that there exists a strong solution to the Cauchy problem (2.2). Then, for every with sufficiently small.
Proof.
Assume that for with some and obtain a contradiction. If , then it follows from (2.2) and (2.3) for every that
[TABLE]
and since , we have for every with sufficiently small because of the finite jump discontinuity at . Consequently, for every . ∎
Due to the reason in Lemma 2, we set for the initial condition in the Cauchy problem (2.2). Note that . If and , then in (2.3) is continuous at and its definition can be extended for every by
[TABLE]
The next result shows that the condition on is not only necessary but also sufficient for existence of the unique global solution in to the Cauchy problem (2.2) with (2.5).
Lemma 3**.**
Assume that with . There exists the unique global solution to the Cauchy problem (2.2) with (2.5) satisfying for every .
Proof.
We solve the evolution problem (2.2) with (2.5) by using the method of characteristics piecewise for and . The family of characteristic curves satisfying the initial-value problem
[TABLE]
are uniquely defined for every thanks to the Lipschitz continuity of on . The peak location at is the critical point which remains invariant under the time flow of the initial-value problem (2.6). For and , we obtain the family of characteristic curves in the exact form
[TABLE]
with for every . Let us define
[TABLE]
then with . We are looking for the solution with for every . Substituting into yields
[TABLE]
which can be integrated as follows:
[TABLE]
where the integration constant is zero thanks to the boundary condition for every . Along each characteristic curve satisfying (2.6), satisfies the initial-value problem:
[TABLE]
which can be solved uniquely in the exact form:
[TABLE]
with for every thanks to . Note the different limits if , hence if . Also note that
[TABLE]
and
[TABLE]
Finally, we solve (2.2) with (2.5) by using (2.7) and (2.10). Along each characteristic curve satisfying (2.6), satisfies the initial-value problem:
[TABLE]
which can be solved uniquely in the exact form:
[TABLE]
with for every thanks to . Furthermore, is continuously differentiable in piecewise for and for every since and . Hence, for every . Also, thanks to the properties (2.11) and (2.12), we have for every since and .
Finally, thanks again to the properties (2.11), (2.12), and for every , the change of coordinates is a invertible transformation so that the solution belongs to and satisfies for every . ∎
By analyzing the exact solution of Lemma 3 in , we show that grows in due to characteristics with . At the same time, if we add an additional constraint on the initial data, we can also show that remains bounded in the supremum norm as .
Lemma 4**.**
Assume that with and . Then, we have for every :
[TABLE]
and
[TABLE]
Proof.
If with , we have for every by Lemma 3. If in addition , then thanks to the bound .
We obtain by elementary computations:
[TABLE]
While the proof of the first equality is obvious, the proof of the second equality consists of several steps. For fixed , the function
[TABLE]
is monotonically increasing in so that
[TABLE]
Then, is monotonically decreasing in attaining the maximal value as . It follows from (2.14) and (2.17) that
[TABLE]
and
[TABLE]
where it follows from (2.8) that
[TABLE]
Bounds (2.15) follow from the estimates (2.18) and (2.19).
By using the chain rule for , we obtain from (2.14) the exact solution for and :
[TABLE]
If , then the first bound in (2.16) follows from the estimate
[TABLE]
thanks to .
Similarly, we obtain from (2.14) the exact solution for and :
[TABLE]
By using the second equality in (2.17), we obtain from (2.22) that
[TABLE]
which yields the second bound in (2.16). ∎
Remark 2*.*
If with and , then so that for . Consequently, for .
The exponential growth of as in Lemma 4 discovers the linear instability of the peakon in the supremum norm on . The same instability is observed in the norm, as formulated in Theorem 2. Below we prove equalities (1.12) and (1.13) in Theorem 2 for with without additional requirements and .
Proof of Theorem 2. By working on , wee use the exact solutions in (2.14) and (2.20), integrate by parts, and obtain
[TABLE]
and
[TABLE]
In order to obtain (2.24), we use (2.14) and the chain rule to write
[TABLE]
We expand the square and integrate the middle term by parts with the boundary conditions and thanks to the Hölder inequality:
[TABLE]
As a result, straightforward computations yield (2.24). The computations for (2.25) are similar but longer with three terms integrated by parts with the boundary conditions and . Summing (2.24) and (2.25) yields (1.12).
Computations on are similar from the exact solutions in (2.14) and (2.22). Integration by parts yield
[TABLE]
and
[TABLE]
Summing (2.26) and (2.27) yields (1.13).
3. Nonlinear evolution near a single peakon
Global existence and uniqueness of the conservative solution (1.4) to the Cauchy problem for the CH equation in the convolution form (1.2) with initial data was proven in [2, 3]. Continuous dependence of the conservative solution (1.6) for initial data was proven in [24]. We rewrite the Cauchy problem in the form:
[TABLE]
where
[TABLE]
The following lemma shows that is continuous for every if .
Lemma 5**.**
For every , we have .
Proof.
We can rewrite (3.2) in the explicit form:
[TABLE]
Each integral is a continuous function for every since it is given by an integral of the absolutely integrable function. Hence is continuous on . ∎
The unique global conservative solution (1.4) to the Cauchy problem (3.1) satisfies the weak formulation
[TABLE]
where the equality is true for every test function . We consider the class of solutions with a single peak placed at the point so that for every , where is defined by (1.14). The following lemma shows that the single peak moves with its local characteristic speed as in (1.10).
Lemma 6**.**
Assume that there exists such that the weak global conservative solution (1.4) to the equation (3.3) satisfies for every with a single peak located at . Then, satisfies
[TABLE]
Proof.
Integrating (3.3) by parts on and and using the fact that , we obtain the following equations piecewise outside the peak’s location:
[TABLE]
Since for every , is a continuous function of on for every by Lemma 5. Therefore, the function satisfies:
[TABLE]
where is the jump of across the peak location. On the other hand, since is continuous and , we differentiate continuously on both sides from and obtain
[TABLE]
Since if , then satisfies (3.4) and since due to Sobolev embedding of into , then . ∎
In order to study the nonlinear evolution near a single peakon, we decompose the weak global conservative solution (1.4) as the following sum of the peakon and its small perturbation:
[TABLE]
where for every is the perturbation and is the deviation of the perturbed peakon’s peak from its unperturbed position moving with the unit speed. If there exists such that for every , the global conservative solution (1.4) satisfies for every , that is, it has a single peak at . By Lemma 6, satisfies the equation
[TABLE]
Substituting (3.5) and (3.6) into the Cauchy problem (3.1) yields the following Cauchy problem for the peaked perturbation to the peakon :
[TABLE]
where and the linear evolution has been simplified by using (2.1) in Lemma 1. Note that in (3.5) becomes in (3.7) thanks to the translational invariance of the system (3.1) with (3.2).
Remark 3*.*
The dynamical equation (3.6) cancels the last term in the linearization at the peakon (2.3) without additional requirement of imposed in Lemmas 3 and 4.
Related to the Cauchy problem (3.7), we define the family of characteristic coordinates satisfying the initial-value problem:
[TABLE]
Along each characteristic curve parameterized by , let us define . It follows from (3.7) and (3.8) that on each characteristic curve satisfies the initial-value problem:
[TABLE]
The following lemma transfers well-posedness theory for differential equations to the existence, uniqueness, and smoothness of the family of characteristic coordinates and the solution surface.
Lemma 7**.**
Assume . There exists (finite or infinite) such that the unique family of characteristic coordinates to (3.8) and the unique solution surface to (3.9) exist as long as for . Moreover, and are in and in for every .
Proof.
A simple extension of the proof of Lemma 5 implies that if , then . Every function is Lipschitz continuous at . In addition, since for every , then , hence the function is globally Lipschitz continuous when it is locally Lipschitz continuous. Since have the same properties on and if , the right-hand-sides of systems (3.8) and (3.9) are global Lipschitz continuous functions of as long as the solution remains for with some (finite or infinite) . Existence and uniqueness of the classical solutions and for every follows from the ODE theory. By the continuous dependence theorem, and for every .
Let us now show that for if for . By differentiating (3.8) piecewise for and , we obtain
[TABLE]
with the solution
[TABLE]
If for , then for piecewise for and , hence the change of coordinates is a invertible transformation. As a result, implies that for . ∎
Since and for every , is a critical point of the initial-value problem (3.8). Therefore, the unique solution of Lemma 7 for satisfies . This limiting characteristic curve separates the family of characteristic curves with and . Since is in for every and Lipschitz continuous at by Lemma 7, the limiting value is in and satisfies
[TABLE]
where we have used .
In order to control for needed in the condition of Lemma 7, we differentiate (3.7) in and obtain
[TABLE]
where we have used and have defined
[TABLE]
It follows from (3.8) and (3.12) that on each characteristic curve satisfies the initial-value problem:
[TABLE]
Although has a jump discontinuity at , the regions and for are separated from each other thanks to the fact that the limiting characteristic curve at corresponds to the critical point of the initial-value problem (3.8). As a result, we consider the initial-value problem (3.14) separately for and .
Lemma 8**.**
Assume and (finite or infinite) be given by Lemma 7. There exist unique solutions and to (3.14) as long as for . Moreover, are in and for every .
Proof.
Similarly to the proof of Lemma 5, it follows that if , then . In addition, are functions of and for and separately for and . Existence and uniqueness of solutions and to (3.14) follow from the ODE theory. By the continuous dependence theorem, are in and for every . ∎
By Lemma 8, we are allowed to define the one-sided limits for . The functions are in and satisfy for :
[TABLE]
By analyzing the time evolution (3.11) and (3.15), we finally prove the nonlinear instability of peaked perturbations to the -orbitally stable peakon.
Lemma 9**.**
For every , there exist and satisfying
[TABLE]
such that the unique solution to the Cauchy problem (3.7) in Lemmas 7 and 8 satisfies
[TABLE]
Proof.
Combining (3.11) and (3.15) together yields the following equation for :
[TABLE]
where
[TABLE]
and we have used , . By using an integrating factor, we rewrite (3.18) in the equivalent form
[TABLE]
where the last inequality is due to . Integrating the differential inequality yields the bound:
[TABLE]
Since as and as , whereas is small in the norm at least for , the coordinate for the peak’s location coincides with the location of the maximum of in the decomposition (3.5) for . By Theorem 1, for every small , if , then
[TABLE]
By Sobolev’s embedding, we have
[TABLE]
Let us assume that the initial data satisfies and
[TABLE]
The initial bound (3.16) is consistent with (3.21) if for every small , the small value of satisfies
[TABLE]
which just specifies in terms of . With these constraints on , the bound (3.19) yields
[TABLE]
or equivalently, . Hence, for every small there exists sufficiently large
[TABLE]
such that . This implies thanks to the bound (3.20).
If , then for some as by the condition of Lemma 7. Therefore, there exists such that the bound (3.17) is true. If , then the differential equation (3.18) is valid for by Lemmas 7 and 8 so that the bound (3.17) is true at thanks to the bound
[TABLE]
In both cases, the bound (3.17) is proven. ∎
Remark 4*.*
The result of Lemma 9 gives the proof of Theorem 3 thanks to the representation (3.5) and the characteristic equation (3.6) at the peak’s location at .
4. Conclusion
We have shown that the passage from linear to nonlinear stability of peakons in is false for the Camassa–Holm equation because the linear result of Theorem 2 gives linearized instability in whereas the result of Theorem 1 gives nonlinear stability of peakons in . On the other hand, we show that the linearized instability in persists as the nonlinear instability result of Theorem 3. The latter result is natural for the Camassa–Holm equation where smooth solutions may break in a finite time with the slopes becoming unbounded from below.
We conclude the paper with possible extensions of our main results. It is quite natural to prove instability of the peaked periodic waves with respect to the peaked periodic perturbations in the framework of the CH equation (1.1). Furthermore, the same instability is likely to hold for peakons in the Degasperis–Procesi equation, although the linearized evolution may not be as simple as the one for the CH equation. Finally, the method of characteristics is likely to work to prove nonlinear instability of peaked periodic wave in the reduced Ostrovsky equation (1.17), which has been an open problem up to now.
Acknowledgements. This project was initiated in collaboration with Y.Liu and G. Gui during the visit of D.E. Pelinovsky to North-West University at Xi’an in June 2018. DEP thanks the collaborators for useful comments. The project was completed during the visit of F. Natali to McMaster University supported by CAPES grant. D.E. Pelinovsky is supported by the NSERC Discovery grant.
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