Abstract
In this essay, we investigate the blow-up scenario, global solution and propagation speed for a modified Camassa–Holm (MCH) equation both dissipation and dispersion in Sobolev space \(H^{s,p} (\mathbb {R})\), \(s\ge 1\), \(p\in (1,\infty )\). First of all, by the mathematical induction of index s, we establish the precise blow-up criteria, which extends the result obtained by Gui et al. in article (Comm Math Phys 319: 731–759, 2013). Secondly, we derive the global existence of the strong solution of MCH equation both dissipation and dispersion. Eventually, the propagation speed of the equation is studied when the initial data are compactly supported.
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1 Introduction
In 1993, by using Hamiltonian methods, Camassa and Holm [3] derived the following new completely integrable dispersive shallow water equation:
i.e., the classical Camassa-Holm (CH) equation, where k denotes a constant related to the critical shallow water wave speed, and the subscripts of \(y=v-v_{xx},\;v\) indicate the partial derivative. Although Fuchssteiner et al. [17] researched the bi-Hamiltonian equation using recursive operators as early as 1981 and derived the CH equation, the work received little attention at that time.
As is known to all, the CH equation has been widely studied. This model simulates the unidirectional propagation of shallow water waves on a flat bottom and the axisymmetric wave propagation in a hyperelastic rod [3, 13]. The CH equation, in contrast to the KdV equation, simulates the breaking phenomenon of shallow water waves. Moreover, scholars have demonstrated the global existence and the blow-up phenomenon of the solution [6, 8, 23]. The remarkable feature of the CH equation is its peaked solitons at the form \(v(t,x)=ce^{-\left| x-ct \right| },\) where c is a wave speed and \(c\in \mathbb {R} \) [4]. At the same time, Constantin et al. [5, 11, 12, 17] not only studied the Hamiltonian structure and integrability of the CH equation, but also proved the orbital stability of peaked solitons. In recent years, many researchers have been greatly interested in the CH equation and have conducted a great deal of research on it [1, 2, 7, 9, 14, 15, 28, 29].
The integrable modified Camassa-Holm (MCH) equation with cubic nonlinearity was first introduced in 1996 by Fuchssteiner [16] and Olver et al. [25] using the bi-Hamiltonian representation of the classical integrable system:
where \(m =\omega -\omega _{xx}\), \(\omega =\omega \left( t,x \right) \) is the fluid velocity and subscripts of \(m,\ \omega \) denote the partial derivatives, \(\omega _{0}\) is the initial data. Until now, Fu and Gui et al. [18] demonstrated that the MCH equation is locally well-posed in the Besov space \(B_{p,r}^{s}(\mathbb {R})\), obtained the blow-up scenario and the lower bound of the maximum existence time. Futhermore, they proved that the nonexistence of smooth traveling wave solutions. The creation of singularities and the presence of peaked traveling-wave solutions to MCH equation were studied by Gui and Liu et al. [20]. Moreover, they proved the existence of single peak solution and multi-peak solution. When \(\alpha =0\), Wu and Guo [30] investigated the persistence, infinite propagation and traveling wave solutions of MCH equation. The local well-posedness and asymptotic behavior of MCH equation solution were studied by Wu and Zhang [31, 32] successively.
In this essay, we discuss the Cauchy problem of the modified Camassa-Holm equation both dissipation and dispersion:
where \(m =\omega -\omega _{xx}\), \(k\in \mathbb {R}\) is a dispersion parameter, and \(\lambda > 0\) is a dissipation coefficient. Recently, a number of researchers have investigated nonlinear models with dissipation. Ott and Sudan [24] studied how the KdV equation was modified by the existence of dissipation and what the influence of such a dissipation was on soliton solutions of the KdV equation. Wu and Yin [26] discussed the local well-posedness, blow-up rate and the global solutions of the weakly dissipative periodic CH equation. In addition, the local well-posedness, blow-up rate and decay of solutions to the weakly dissipative Degasperis-Procesi equation were also established by them [27]. Hu [21] investigated the local well-posedness, the global existence and blow-up phenomena for a weakly dissipative periodic two-component CH equation. Thereafter, Hu and Qiao [22] studied the local well-posedness, the precise blow-up scenario, the global existence and propagation speed for a generalized CH model with both dissipation and dispersion.
In this essay, we study the blow-up scenario, global solution and propagation speed of strong solution for the IVP of Eq. (1.3). Our study shows that the blow-up scenario for the solution of Eq. (1.3)(\(k,\ \lambda \ne 0\)) is similar to that of Eq. (1.2)(\(k=\lambda =0\)). In addition, different from Gui’s approach, we used mathematical induction to study the blow-up criterion in Theorem 2.1. It is worth noting that the dissipation term \(\lambda m\) and the dissipation term \(km_{x}\) in Eq. (1.3) have an impact on the global existence and the propagation speed of its solution, see Theorem 3.1 and Theorem 4.1. In particular, the propagation speed is heavily influenced by the dispersion parameter k and the dissipation coefficient \(\lambda \).
The essay is structured as follows. In Sect. 2, we first give three important lemmas and establish the blow-up criterion for the solution of Eq. (1.3). The global existence of strong solutions of Eq. (1.3) is studied in Sect. 3. In the last section, we study the propagation speed of strong solutions to Eq. (1.3) provided the initial data have compact support.
Notation: For convenience, all function spaces are over \(\mathbb {R}\), and if there is no ambiguity, we exclude \(\mathbb {R}\) from our notation of function spaces. For \(1\le p\le \infty \), \(\Vert \cdot \Vert _{L^{p}}\) will stand for the norm in the Banach space \(L^{p} (\mathbb {R} )\), while the norm in the classical Sobolev spaces \(H^{s,p} (\mathbb {R} )\) will be written by \(\Vert \cdot \Vert _{H^{s,p}}, s\in \mathbb {R}\). Furthermore, the norm of \(H^{s,p}(\mathbb {R})\) is defined as follows
where \(\widehat{D^{s}f}(\xi ) =\left| \xi \right| ^{s} \widehat{f}(\xi )\) and \(\widehat{f}(\xi )\) represents the Fourier transformation.
2 Blow-up scenario
In this section, we will show some significant results in order to achieve our goal. Let the potential \(m =\omega -\omega _{xx}\), \(\left( t,x \right) \in \mathbb {R}^{+} \times \mathbb {R}\), then we rewrite Eq. (1.3) in the form of a quasi-linear evolution equation of hyperbolic type:
Furthermore, Eq. (2.1) can be reformulated in the following form:
where we used \((1-\partial ^{2}_{x})^{-1}g=G*g\) for all \( g\in L^{p}\), \(G(x)=\frac{1}{2}e^{-|x|},\ x\in \mathbb {R},\) namely \((1-\partial ^{2}_{x})^{-1}m =G*m=\omega \), here we represent by \(*\) the convolution.
Apparently, similar to [32], the local well-posedness of the Cauchy problem Eq. (1.3) in \(H^{s,p} (\mathbb {R})\), \(s\ge 1\) can be obtained by applying the Kato’s semigroup theorem.
Lemma 2.1
[32] Suppose that \(m_{0} \in H^{s,p} (\mathbb {R})\), \(s\ge 1\), \(p\in (1,\infty )\), in other words, the initial datum \(\omega _{0} \in H^{s+2,p} (\mathbb {R})\). Then there exist a time \(T=T(m_{0})>0\) and a unique strong solution m(t, x) to Eq. (1.3) such that
Moreover, the solution m(t, x) depends continuously on \(m_{0}\), i.e., the mapping
is continuous.
In particular, the unique strong solution m(t, x) to Eq. (1.3) satisfies
Next, we consider the following ordinary differential system:
where \(\omega \) is the corresponding strong solution to Eq. (1.3). It should be pointed out that a similar system for Camassa-Holm defines the re-expression of that equation as geodesic flow (a detail discussion can be found in [10]). The following several lemmas, which are essential in the demonstration of global existence, can be obtained by applying classical results in the theory of ordinary differential equations.
Lemma 2.2
Assume that \(\omega _{0} \in H^{s,p} (\mathbb {R}),\ s\ge 3\), \(p\in (1,\infty )\). Then there exist a \(T=T(\omega _{0} )>0\) and a unique strong solution \(\rho \in \mathcal {C} (\left[ 0,T \right) \times \mathbb {R};\mathbb {R} )\) to Eq. (2.3) such that the function \(\rho (t,\cdot )\) is an increasing diffeomorphism of \(\mathbb {R}\) with
Proof. Differentiating Eq.(2.3) with respect to x, it follows that
Solving the above equation derives the result of Lemma 2.2.
Lemma 2.3
Suppose that \(\omega _{0} \in H^{s,p} (\mathbb {R}),\ s\ge 3\), \(p\in (1,\infty )\), and let \(T=T(\omega _{0} )>0\) be the maximal existence time of the solution \(\omega \) to Eq. (1.3) corresponding to the initial data \(\omega _{0}\). Then we have
For all \(\left( t,x \right) \in [0, T) \times \mathbb {R}\), if there exists \(M> 0\) such that \(-m\omega _{x}\left( t,x \right) \le M \), then we obtain
Proof. Differentiating the left-hand side of Eq. (2.5) with respect to t, by virtue of Eqs. (1.3) and (2.3), it follows that
Solving the above equation, one obtains
In addition, it follows that
Therefore, the proof of Lemma 2.3 have been completed.
Lemma 2.4
[19] For \(s\ge 0\), \(p\in (1,\infty )\), there exists a constant \(C_s\) such that the following estimate holds:
Next, we will provide the precise blow-up criteria.
Theorem 2.1
Suppose \(m_{0} \in H^{s,p} (\mathbb {R})\), \(s\ge 1\), \(p\in (1,\infty )\). Then the solution m of Eq. (1.3) blows up in the finite time \(T> 0\) if and only if
Proof. Sufficiency: If \(\liminf _{t\uparrow T}{(m\omega _{x})(t,\cdot )}=-\infty \), and \(m\omega _{x}\) is continuous with respect to x, by the Sobolev’s embedding theorem, then the solution m of Eq. (1.3) will blow-up in finite time.
Necessity: Without loss of generality, we only prove the necessity when \(s\ge 1,\ s\in \mathbb {N}\). If there exists a positive constant \(M> 0\) such that \(-m\omega _{x}(t,x)\le M\) for all \(t\in [0,T)\), then we need to prove that \(\left\| m(t,\cdot ) \right\| _{H^{s,p}}< \infty \). For the convenience of writing, let \(A=e^{(2M-\lambda )t}\left\| m_{0}\right\| _{L^{\infty }}\). We will use mathematical induction for s to demonstrate this statement.
(i) Let \(s=1\), we shall estimate \(\left\| m(t,\cdot ) \right\| _{H^{1,p}}< \infty \).
Multiplying Eq. (1.3) by \(\left| m \right| ^{p-2}m\) with \(p\ge 2\), and integrating over \(\mathbb {R}\) with respect to x, integration by parts, then we have
i.e.,
Differentiating Eq. (1.3) with respect to x, we get
Applying Eq. (2.8) by \(\left| m_{x} \right| ^{p-2}m_{x}\) with \(p\ge 2\), and integrating over \(\mathbb {R}\) with respect to x, integration by parts leads to
where the second inequality comes from
By virtue of (2.9), one can easily deduce that
Add up (2.7) and (2.10), it follows that
where \(c_{1}=\max \{2A^{2}+(2p-2)M+\lambda p,\ 2A^{2}(p-1)+(6p-2)M+\lambda p\}.\)
By virtue of Gronwall’s inequality, one gets
(ii) Let \(s=2\), we will estimate \(\left\| m(t,\cdot ) \right\| _{H^{2,p}}< \infty \).
Differentiating Eq. (1.3) twice with respect to x, we have
Multiplying Eq. (2.13) by \(\left| m_{xx} \right| ^{p-2}m_{xx}\) with \(p\ge 2\), and integrating over \(\mathbb {R}\) with respect to x, then we obatin
where the constant \(c_{2}=6Ae^{\frac{c_{1}t}{p}}\left\| m_{0}\right\| _{H^{1,p}}\) and the third inequality comes from
Then we have
where the constant \(c_{3}=(p-1)(12A^{2}+c_{2})+(8p-2)M+\lambda p\).
Combining (2.11) with (2.16), it yields that
Thanks to Gronwall’s inequality, one has
(iii) Suppose that \(\left\| m(t,\cdot ) \right\| _{H^{s-1,p}}< \infty \), thus we will prove \(\left\| m(t,\cdot ) \right\| _{H^{s,p}}< \infty \). In other words, we only need to prove \(\left\| \partial _{x}^{s}m(t,\cdot ) \right\| _{L^{p}}< \infty \).
Differentiating Eq. (1.3) with respect to x variable s times, applying the result by \(\left| \partial _{x}^{s}m \right| ^{p-2}\partial _{x}^{s}m\) with \(p\ge 2\), and integrating by parts, we obtains
Obviously, one gets
and
Note that in the following inequalities, we applied \(\left\| m \right\| _{H^{2,p}}< \infty \) and the assumption \(\left\| m \right\| _{H^{s-1,p}}< \infty \).
As \(i=0\) and \(i=1\), it follows that
When \(i=s\), we have
where
For \(2\le i\le s-1,\ i\in \mathbb {N}\), it yields that
where the above inequality comes from
When \(j=0\), one shows that
where
As \(j=1\), one gets that
When \(j=s\), it follows that
For \(2\le j\le s-1,\ j\in \mathbb {N}\), we have
Plugging the above inequalities into (2.19) yields that
In view of Gronwall’s inequality, there exists a constant \(c(M,\ p,\ s,\ \lambda )> 0\) such that
In summary, we have completed the proof of Theorem 2.1.
Remark 2.1
Theorem 2.1 shows that the dispersion coefficient k and the dissipation parameter \(\lambda \) have no effect on the blow-up criterion of solution of Eq. (1.3). That is to say, when \(k=\lambda =0\), Theorem 2.1 also holds.
Lemma 2.5
Let \(m_{0} \in H^{s,p} (\mathbb {R})\), \(s\ge 1\), \(p\in (1,\infty )\). Then as long as the solution \(\omega (t)\) given by Lemma 2.1 exists for any \(t\in [0, T)\), we have
Proof. Multiplying Eq. (1.3) by \(\omega \) and integration by parts, it yields that
Owning to
and
one can easily check that
Applying Gronwall’s inequality, we have
This completes the proof of Lemma 2.5.
3 Global existence of solution
In this section, we provide global existence result for strong solutions to Eq. (1.3).
Theorem 3.1
Let \(m_{0} \in H^{s,p} (\mathbb {R})\), \(s\ge 1\), \(p\in (1,\infty )\), and \(m_{0} =\omega _{0}-\omega _{0,xx}\). If \(m_{0}(x)\ne 0,\ x\in \mathbb {R}\) and \(\left\| m_{0} \right\| _{H^{1}}\le (\frac{2\lambda }{c})^{\frac{1}{2}}\), then the solution m(t, x) of Eq. (1.3) globally exists in time.
Proof. Multiplying Eq. (1.3) by m, and integrating over \(\mathbb {R}\) with respect to x, integration by parts, then we have
Applying Eq. (2.8) by \(m_{x}\), and integrating over \(\mathbb {R}\) with respect to x, integration by parts leads to
Add up (3.1) and (3.2), it yields that
Applying both side of Eq. (3.3) by \(e^{2\lambda t}\), one gets
By using Sobolev embedding theorem \(H^{1}\hookrightarrow L^{\infty }\), we have
and
where constant \(c> 0\) and (3.6) comes from
So, plugging (3.5) and (3.6) into (3.4), it follows that
Set \(g(t)\doteq e^{2\lambda t}\int _{\mathbb {R}}(m^{2}+m_{x}^{2})dx\). For all \(t\in \mathbb {R}\) and \(m_{0}(x)\ne 0,\ x\in \mathbb {R}\), then we have \(g(t)> 0\). If \(m_{0}(x)\ne 0,\ x\in \mathbb {R}\), then \(m(t,\rho (t,x))\ne 0,\ x\in \mathbb {R}\) from (2.5). Obviously, \(g(t)> 0\).
Replacing \(e^{2\lambda t}\int _{\mathbb {R}}(m^{2}+m_{x}^{2})dx\) in (3.7) with g(t), one obtains
Solving the above equation implies that
Integrating Eq. (3.9) with respect to t, we can derive
namely, it follows that
where \(g(0)^{-1}-\frac{c}{2\lambda }\ge 0\) is guaranteed by the assumption \(\left\| m_{0} \right\| _{H^{1}}\le (\frac{2\lambda }{c})^{\frac{1}{2}}\).
In addition, we have
i.e.,
Thus, it yields that
Combining (3.5), (3.6) with (3.10), we can easily obtain that m and \(m\omega _{x}\) are bounded, namely,
Therefore, we can obtain the solution m(t, x) of Eq. (1.3) globally exists in time. This completes the proof of Theorem 3.1.
Remark 3.1
From Theorem 3.1, one can easily check that the dissipation term \(\lambda m\) affects the global existence of the strong solution of Eq. (1.3), however the dispersion term \(km_{x}\) does not affect the global solution.
4 Propagation speed
The effect of the dispersion coefficient k and the dissipation parameter \(\lambda \) on the propagation speed of the strong solutions to Eq. (1.3) will be examined in this section.
Theorem 4.1
Let \(m_{0} \in H^{s,p} (\mathbb {R})\), \(s\ge 1\), \(p\in (1,\infty )\). The maximal existence time that the solution \(\omega (t, x)\) to Eq. (1.3) with the initial data \(\omega _{0}\) can exist is given by \(T = T(\omega _0)\). If the initial data \(\omega _{0}\) are compactly supported in \([a_{\omega _{0}}, b_{\omega _{0}}]\), for all \(t\in [0, T)\), then we have
where the compact support [q(t, a), q(t, b)] of \(m(t, \cdot )\) is contained in the interval \([q(t, a_{\omega _{0}}), q(t, b_{\omega _{0}})]\). Furthermore, if the initial potential \(m_{0} =\omega _{0}-\omega _{0,xx}\) does not change sign on \(\mathbb {R}\) and for any \(t\in [0, T)\) the solution \(\omega \not \equiv 0\), then for \(m_{0}\ge 0\), we have \(E^{+}(t)>0\) and \(E^{-}(t)<0\); on the contrary, for \(m_{0}\le 0\), one obtains \(E^{+}(t)<0\) and \(E^{-}(t)>0\), where \(E^{+}(t)\), \(E^{-}(t)\) are continuous non-vanishing functions, and \(E^{+}(0)=E^{-}(0)=0\).
Proof. If \(\omega _{0}\) is compactly supported in the closed interval \([a_{\omega _{0}}, b_{\omega _{0}}]\), then \(m(t, \cdot )\) has compact support with its support contained in the interval \([q(t, a), q(t, b)]\subseteq [q(t, a_{\omega _{0}}), q(t, b_{\omega _{0}})]\) according to Lemma 2.3. We define the following two necessary functions:
In view of \(\omega (t,x)=G*m=\frac{1}{2}e^{-\left| x \right| }*m\), it yields that
Due to (4.2) and (4.3), we can derive
Combining (4.2) with (4.4), we have
Apparently, \(\omega _{0}(x)\) is compactly supported in the interval \([a_{\omega _{0}}, b_{\omega _{0}}]\), with \(E^{+}(0)=E^{-}(0)=0\). Thanks to
Since \(m(t, \cdot )\) is compactly support in the interval [q(t, a), q(t, b)] and \(\omega (t,x)=\omega _{x}(t,x)\) as \(x< q(t,a)\). Differentiating Eq. (4.2) with respect to t, combining with Eq. (1.3) yields
It follows from (4.6) that
where \(f\doteq -\int _{\mathbb {R}}\left[ \left( \omega ^{2} -\omega _{x}^{2}\right) m \right] _{x}e^{-x}dx\). We can easily check that
Since \(m_{0}\) does not change sign on \(\mathbb {R}\), we have
Now we consider the case \(m_{0}\ge 0\). As \(\omega _{x}\ge 0\), then \(0\le \omega _{x}\le \omega \), we can easily get
otherwise, as \(\omega _{x}\le 0\), then \(0\le -\omega _{x}\le \omega \), i.e., \(\omega ^{3}+\omega _{x}^{3}\ge 0\), one has
Combining the above two inequalities and (4.8), it follows that
which means
namely,
then from (4.12) we obtain
Thus it follows that \(E^{-}(t)\le 0\) for the case \(m_{0}\ge 0\). Analogous to the above process, if \(m_{0}\le 0\), we can get \(E^{-}(t)\ge 0\).
Obviously, similar to (4.6), it follows that
From the above relation (4.14), we deduce
where \(g\doteq -\int _{\mathbb {R}}\left[ \left( \omega ^{2} -\omega _{x}^{2}\right) m \right] _{x}e^{x}dx\). Thus one can get
When \(m_{0}\ge 0\), one has \(g\le 0\), similar to (4.10–4.13), it yields that \(E^{+}(t)\ge 0\). For the same reason, as \(m_{0}\le 0\), we can get \(E^{+}(t)\le 0\). In summary,
This completes the proof of Theorem 4.1.
Remark 4.1
From the proof of Theorem 4.1, it follows that the dispersion coefficient k and the dissipation parameter \(\lambda \) have an effect on the propagation speed of the solution to Eq. (1.3). When \(k=\lambda =0\) in [30], \(E^{+}(t)\) and \(E^{-}(t)\) are both non-vanishing functions. For \(m_{0}\ge 0\), \(E^{+}(t)\) is strictly increasing function and \(E^{-}(t)\) is strictly decreasing function; conversely, for \(m_{0}\le 0\), \(E^{+}(t)\) is strictly decreasing function and \(E^{-}(t)\) is strictly increasing function.
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Acknowledgements
This work was partially supported by NSFC(Grant No.:11771442) and the Fundamental Research Funds for the Central University(WUT:2021III056JC). The authors thank the professor Boling Guo, Zhen Wang and Doctor Zhengyan Liu for their helpful discussions and constructive suggestions.
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Wu, X., Zhang, X. & Du, L. Blow-up, global existence and propagation speed for a modified Camassa–Holm equation both dissipation and dispersion in \(H^{s,p}(\mathbb {R})\). Monatsh Math 205, 371–390 (2024). https://doi.org/10.1007/s00605-024-01966-y
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DOI: https://doi.org/10.1007/s00605-024-01966-y