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Two blow-up criteria of solutions to a modified two-component Camassa-Holm system
Journal of Inequalities and Applications volume 2014, Article number: 54 (2014)
Abstract
In this paper, we establish two sufficient conditions on the initial data to guarantee a blow-up phenomenon for the modified two-component Camassa-Holm (MCH2) system.
MSC:37L05, 35Q58, 26A12.
1 Introduction
In this paper, we consider the Cauchy problem of the following modified two-component Camassa-Holm (MCH2) system:
where , u denotes the velocity field, g is the downward constant acceleration of gravity as applied to shallow water waves, is the average density, and is taken to be a constant. For convenience we let in this paper. The MCH2 system does admit peaked solutions in the velocity and average density; we refer to Ref. [1] for details. There the authors analytically identified the steepening mechanism that allows the singular solutions to emerge from smooth spatially confined initial data. They found that wave breaking in the fluid velocity does not imply a singularity in the pointwise density ρ at the point of vertical slope. Some other recent works can be found in [2, 3]. We find that the MCH2 system is expressed in terms of an averaged or filtered density in analogy to the relation between momentum and velocity by setting . Note that the MCH2 system is a version of the CH2 system modified to allow for a dependence on the average density (or depth, in the shallow water interpretation) as well as the pointwise density ρ.
Let , then , where the sign ∗ denotes the spatial convolution, is the associated Green’s function of the operator . Therefore system (1.1) is equivalent to the following one:
The MCH2 may not be integrable unlike CH2. The characteristic is that it will amount to strengthening the norm for from to in the potential energy term [4]. It means we have the following conserved quantity:
We cannot obtain the conservation of the norm for the CH2 system, which reads
The CH2 system appeared initially in [5], and recently Constantin and Ivanov in [6] gave a demonstration about its derivation in view of the fluid shallow water theory from the hydrodynamic point of view. This generalization, similar to the Camassa-Holm equation, possesses the peakon, multi-kink solutions and the bi-Hamiltonian structure [7, 8] and is integrable. Well-posedness and the wave breaking mechanism were discussed in [9–11] and the existence of global solutions was analyzed in [6, 10, 12]. The geometric investigation can be found in [13, 14].
Obviously, under the constraint of , this system reduces to the Camassa-Holm equation, which was derived physically by Camassa and Holm in [15] (found earlier by Fokas and Fuchssteiner [16] as a bi-Hamiltonian generalization of the KdV equation) by directly approximating the Hamiltonian for Euler’s equation in the shallow water region with representing the free surface above a flat bottom. Some satisfactory results have been obtained recently, for instance, see Refs. [17–21]. Moreover, wave breaking criteria for a large class of initial data have been established in [18, 20–22]. In [20], McKean established the necessary and sufficient condition of wave breaking, while Zhou and his collaborators gave a new and direct proof in [22] for McKean’s theorem. In [23], Xin and Zhang showed global existence of weak solutions but uniqueness was obtained only under a priori assumption that is known to hold only for initial data such that is a sign-definite random measure. The solitary waves of the Camassa-Holm equation are peaked solutions and are orbitally stable [24]; see also [25] for a very related rod equation. Recently, an asymptotic analysis was given in [26]. If , the CH2 system which includes both velocity and density variables in the dynamics is actually an extension of the CH equation. Although possessing peaked solutions in the velocity, the CH2 system does not admit singular solutions in the density profile. Its mathematical properties have been studied further in many works [6–10, 27, 28].
In Section 2, we recall some preliminary results on well-posedness and blow-up scenario. In Section 3, two detailed blow-up criteria are presented.
2 Preliminaries
In this section, for completeness, we recall some elementary results and skip their proofs. Local well-posedness for the MCH2 system can be obtained by Kato’s semi-group theory [29]. In [2], the authors gave a detailed description on the well-posedness theorem.
Theorem 2.1 [2]
Give , , there exist a maximal and a unique solution to system (1.2) such that
Moreover, the solution depends continuously on the initial data, i.e. the mapping
is continuous.
The next result describes the precise blow-up scenario for sufficiently regular solutions to system (1.2).
Theorem 2.2 [2]
Let , , and Let T be the maximal existence time of the solution to system (1.2) with the initial data . Then the corresponding solution blows up in finite time if and only if
We also need to introduce the classical particle trajectory method for later use. Let be the particle line evolved by the solution; that is, it satisfies
Differentiating the first equation with respect to x, one has
Hence
which is always positive before the blow-up time. Therefore, the function is an increasing diffeomorphism of the line.
3 Blow-up
Before giving blow-up theorems, we rewrite the system (1.1) by as follows:
As and as is given by the convolution with , we have
from which we get
Thus,
Now we give our two blow-up theorems.
Theorem 3.1 Suppose , , for some point , and initial data satisfies the following conditions:
-
(i)
and ,
-
(ii)
,
where . Then the solution to system (1.2) with the initial value blows up in finite time.
Remark 3.1 In fact the condition (ii) can be reduced to
If , the theory becomes the blow-up theorem in [21] for the Camassa-Holm. As has nothing to do with the initial data, so we add the initial energy to condition (ii).
Proof Differentiating the first equation in system (1.2) with respect to x, we obtain
Applying to the above equation yields
This equation gives
where we used the fact
As regards we can deduce that
Due to (3.2), we obtain
Owing to , we have the following inequality:
Then using (3.3) and (3.4), we can turn the inequality (3.1) into
In order to reach our result, we need the following claim.
Claim 1 is decreasing, for all , where T is the maximal existence time of the solution.
Suppose not, i.e., there exists a such that on and . Now let
and
Firstly for , differentiating , we have
where we used (3.3) and (3.4).
Secondly, by the same argument, we get
Hence, it follows from (3.6) and (3.7) and the continuity property of the ODEs that
for all , where we have used the condition (i) and (ii). The continuity property implies that, when , we have
This is an obvious contradiction. Then can be extended to T. On the other hand
Then the initial assumption makes obvious. So our claim is proved.
Using (3.6) and (3.7) again, we have the following equation for :
where we used . Due to (3.5), we can obtain
Now, substituting (3.9) into (3.8), it yields
Before completing the proof, we need the following technical lemma.
Lemma 3.1 [30]
Suppose that is a twice continuously differential satisfying
Then blows up in finite time. Moreover the blow-up time T can be estimated in terms of the initial datum as
Let , then given the condition (i) and due to the claim and the expression of , we get and . Using the above lemma, (3.10) is an equation of type (3.11) with . We can conclude that under the conditions (i) and (ii), the solution to system (1.2) blows up in finite time. □
Theorem 3.2 Suppose , , there exists δ satisfying when , , when , and when , . Some portion of the positive part of lies to the left of some portion of its negative part with the changing sign point at , then the solution to system (1.2) with the initial value blows up in finite time.
Before we prove the above theorem, we draw a picture of in Figure 1.
Proof In order to prove the theorem, we define the following quantities:
Then concerning the sign of and , we have four cases.
Case 1: , .
Case 2: , .
Case 3: , .
Case 4: , .
The cases for or are easy to handle.
First, we can find that Case 3 is equivalent to Case 2.
In fact, if is a solution, let and , then is also a solution with and . Let with positive part on and negative part on , then we have
By the same reasoning, we have .
Set
for any , then we have
In order to get the monotonous property of and , we need the following claim.
Claim 2 Under the condition of from the theorem, for all we have
and .
From the first equation of system (1.1) we have the following equivalent form:
Applying the particle trajectory method and the second equation in (1.1), we obtain
and
which implies
Due to the condition of from the theorem and , we get
for all . Then
Thus is independent on time t. By taking , we have
Since and from the above equation, we get . Therefore the claim holds.
Claim 3 For any fixed t, , for any and all .
As , where G is the Green’s function, it can be expressed as , and then one has the equation for and :
Therefore,
By direct computation, if , for any , then from the above two equations we can get
where we used the above claim as regards . Similarly, if , for any , we also have
This completes the proof of the claim.
For any , by applying our claim to (3.12) and (3.13), we obtain
which implies is a strictly increasing function, while is a strictly decreasing one for a nontrivial solution.
Now we prove Case 1.
From (3.1) and Claim 3, we have
Due to the increasing property of and the decreasing property of ((3.14) and (3.15)), if we let
then
Suppose the corresponding solution exists globally in time. Since is strictly decreasing with initial assumption , there exists a such that for all , we have
where
Thanks to (3.16) and the following fact:
we have the following inequality for :
Then we need the following lemma to finish our proof for Case 1.
Lemma 3.2 [31]
Assume that a differentiable function satisfies
with constant . If we have the initial datum , then the solution goes to −∞ before t tends to .
Through this lemma, we can see that goes to −∞ within finite time and Case 1 has been proved.
Now we prove Case 2.
We will prove that after some time Case 2 will change to Case 1. So it is sufficient to show that there exists a time , such that as .
Suppose not, i.e., for any . As in Case 2, we have
Then
which shows that, for , there exists a , and for any , we have
That is to say
If we set and (see Figure 2), then
Therefore, for any ,
When , we see that is increasing and is decreasing, then from the hypothesis we know for all
and
Then we obtain
That is to say .
Case 3.1 For any x, y satisfying , there exists a constant , such that .
For any , assume that . In view of for , we have
On the other hand, from the boundedness of u and , it follows that
which implies that
From the expression of , we know that
Hence
Fix some points (see Figure 3), such that , and is small enough. Because of the convexity of , we can deduce that
Therefore, there exist and , such that
Similarly, we also get
Combining (3.18) and (3.19), it follows that
Then a contradiction is obtained from (3.17): is summable with respect to t, but is not.
Case 3.2. There exist some points, say , such that is unbounded.
Different from (3.17), we can deal with the same term as
According to the convexity of , we have
Next we will consider the first term in (3.20),
From the hypothesis, we know that may reach ∞, which means that there exist some times and , such that
Let with (see Figure 4). Thanks to , we know that the above points all belong to the interval . First, we prove the following claim.
Claim 4 For any two adjacent points belong to , say e and f with , it satisfies as .
In fact, there exist , and , such that
According to and the convexity of , we have
So the claim is true.
Therefore,
for all , which implies
Since ,
Then
Summarizing these estimates and using the convexity of , we can get
for large enough and in the time interval it is increasing.
Putting (3.21) and (3.22) into (3.20), we know that becomes negative. This is a contradiction.
Therefore, we finish the proof for Case 2.
Finally we finish the proof of our theorem with proving Case 4.
We want to prove that Case 4 can be reduced to the first or the third case, so it is sufficient to prove that there exists a time , such that as .
We suppose that for all , we have , then get a contradiction. For any ,
Summarizing the above two inequalities, we obtain
After the above preparation, we have
which implies
On the other hand, by (3.14), we have
Since
which yields
we get
Then a contradiction is obtained from (3.23): taken at is summable with respect to t, but is not.
So there exists a time T, such that when , . This completes the proof for Case 4.
Remark 3.2 Scrutinizing the proof, we find that the condition of guarantees that Claim 3 holds. Therefore it can be replaced by
for all . Then the theorem still holds.
Remark 3.3 This blow-up theorem has nothing to do with the initial energy . It is the sign of the initial density and the sign of that play an important role in wave breaking, it is not the size of them that affects it. It is very similar to the necessary and sufficient blow-up condition for the Camassa-Holm equation given by McKean in [20]. □
References
Holm D, Náraigh LÓ, Tronci C: Singular solutions of a modified two-component Camassa-Holm equation. Phys. Rev. E 2009.,3(79): Article ID 016601
Guan C, Karlsen KH, Yin Z: Well-posedness and blow-up phenomena for a modified two-component Camassa-Holm equation. Contemp. Math. 526. In Nonlinear Partial Differential Equations and Hyperbolic Wave Phenomena. Am. Math. Soc., Providence; 2010:199–220.
Guo Z, Zhu M: Wave breaking for a modified two-component Camassa-Holm system. J. Differ. Equ. 2012,252(3):2759–2770. 10.1016/j.jde.2011.09.041
Guo Z, Zhu M, Ni L: Blow-up criteria of solutions to a modified two-component Camassa-Holm system. Nonlinear Anal., Real World Appl. 2011, 12: 3531–3540. 10.1016/j.nonrwa.2011.06.013
Olver P, Rosenau P: Tri-Hamiltonian duality between solitons and solitary-wave solutions having compact support. Phys. Rev. E 1996, 53: 1900–1906.
Constantin A, Ivanov R: On an integrable two-component Camassa-Holm shallow water system. Phys. Lett. A 2008, 372: 7129–7132. 10.1016/j.physleta.2008.10.050
Chen M, Liu S, Zhang Y: A two-component generalization of the Camassa-Holm equation and its solutions. Lett. Math. Phys. 2006, 75: 1–15. 10.1007/s11005-005-0041-7
Falqui G: On a Camassa-Holm type equation with two dependent variables. J. Phys. A 2006, 39: 327–342. 10.1088/0305-4470/39/2/004
Escher J, Lechtenfeld O, Yin Z: Well-posedness and blow-up phenomena for the 2-component Camassa-Holm equation. Discrete Contin. Dyn. Syst. 2007, 19: 493–513.
Gui G, Liu Y: On the global existence and wave-breaking criteria for the two-component Camassa-Holm system. J. Funct. Anal. 2010, 258: 4251–4278. 10.1016/j.jfa.2010.02.008
Guo Z, Zhou Y: On solutions to a two-component generalized Camassa-Holm equation. Stud. Appl. Math. 2010, 124: 307–322. 10.1111/j.1467-9590.2009.00472.x
Guo Z: Blow-up and global solutions to a new integrable model with two components. J. Math. Anal. Appl. 2010, 372: 316–327. 10.1016/j.jmaa.2010.06.046
Escher J, Kohlmann M, Lenells J: The geometry of the two-component Camassa-Holm and Degasperis-Procesi equations. J. Geom. Phys. 2011, 61: 436–452. 10.1016/j.geomphys.2010.10.011
Holm D, Ivanov R: Two component CH system: inverse scattering, peakons and geometry. Inverse Problems 2011., 27: Article ID 045013
Camassa R, Holm D: An integrable shallow water equation with peaked solitons. Phys. Rev. Lett. 1993, 71: 1661–1664. 10.1103/PhysRevLett.71.1661
Fuchssteiner B, Fokas AS: Symplectic structures, their Backlund transformations and hereditary symmetries. Physica D 1981/1982.,4(1): Article ID 4766
Bressan A, Constantin A: Global conservative solutions of the Camassa-Holm equation. Arch. Ration. Mech. Anal. 2007, 183: 215–239. 10.1007/s00205-006-0010-z
Constantin A, Escher J: Well-posedness, global existence, and blow-up phenomena for a periodic quasi-linear hyperbolic equation. Commun. Pure Appl. Math. 1998, 51: 475–504. 10.1002/(SICI)1097-0312(199805)51:5<475::AID-CPA2>3.0.CO;2-5
Himonas A, Misiolek G, Ponce G, Zhou Y: Persistence properties and unique continuation of solutions of the Camassa-Holm equation. Commun. Math. Phys. 2007, 271: 511–522. 10.1007/s00220-006-0172-4
McKean HP: Breakdown of a shallow water equation. Asian J. Math. 1998, 2: 767–774.
Zhou Y: Wave breaking for a shallow water equation. Nonlinear Anal. 2004, 57: 137–152. 10.1016/j.na.2004.02.004
Jiang Z, Ni L, Zhou Y: Wave breaking of the Camassa-Holm equation. J. Nonlinear Sci. 2012,22(2):235–245. 10.1007/s00332-011-9115-0
Xin Z, Zhang P: On the weak solutions to a shallow water equation. Commun. Pure Appl. Math. 2000, 53: 1411–1433. 10.1002/1097-0312(200011)53:11<1411::AID-CPA4>3.0.CO;2-5
Constantin A, Strauss W: Stability of peakons. Commun. Pure Appl. Math. 2000, 53: 603–610. 10.1002/(SICI)1097-0312(200005)53:5<603::AID-CPA3>3.0.CO;2-L
Zhou Y: Stability of solitary waves for a rod equation. Chaos Solitons Fractals 2004, 21: 977–981. 10.1016/j.chaos.2003.12.030
Jiang Z, Zhou Y, Zhu M: Large time behavior for the support of momentum density of the Camassa-Holm equation. J. Math. Phys. 2013., 54: Article ID 081503
Mustafa OG: On smooth traveling waves of an integrable two-component Camassa-Holm shallow water system. Wave Motion 2009, 46: 397–402. 10.1016/j.wavemoti.2009.06.011
Zhang P, Liu Y: Stability of solitary waves and wave-breaking phenomena for the two-component Camassa-Holm system. Int. Math. Res. Not. 2010, 2010: 1981–2021.
Kato T Spectral Theory and Differential Equations. In: Proc. Sympos., Dundee, 1974. Lecture Notes in Math., vol. 48, p. 25. Springer, Berlin (1975), dedicated to Konrad Jorgens
Zhou Y: On solutions to the Holm-Staley b-family of equations. Nonlinearity 2010, 23: 369–381. 10.1088/0951-7715/23/2/008
Zhou Y: Blow-up of solutions to a nonlinear dispersive rod equation. Calc. Var. Partial Differ. Equ. 2006, 25: 63–77. 10.1007/s00526-005-0358-1
Acknowledgements
This work is partially supported by ZJNSF (Grant No. LQ13A010008) and NSFC (Grant No. 11226176). Thanks are also given to the anonymous referees for careful reading and suggestions.
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LJ proposed the problems and finished the whole manuscript. YJ proved Theorem 3.1. CM proved Theorem 3.2. All authors read and approved the final manuscript.
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Ma, C., Jin, L. & Jin, Y. Two blow-up criteria of solutions to a modified two-component Camassa-Holm system. J Inequal Appl 2014, 54 (2014). https://doi.org/10.1186/1029-242X-2014-54
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DOI: https://doi.org/10.1186/1029-242X-2014-54
Keywords
- MCH2 system
- blow-up