Well-Posedness and Infinite Propagation Speed for the Fifth-Order Camassa-Holm Equation with Weakly Dissipative Term

In this paper, we study the fifth-order Camassa-Holm equation with weakly dissipative term. We first give the local well-posedness result and the blow up criterion. Then, we establish sufficient conditions to guarantee that the solution exists globally in time. Finally, the infinite propagation speed of this equation is also investigated.

• Blow up Criterion
• Global Existence
• Infinite Propagation Speed

1. Introduction

In 1993, Camassa and Holm [1] derived an integrable shallow water equation taking the form as

u t − u x x t + 3 u u x = 2 u x u x x + u x u x x x , (1.1)

where u ( x , t ) denotes the height of the water above the flat bottom. Equation (1.1) describes wave motion in shallow water regime. Due to its mathematical importance and wide applications in physics, such equation has been intensively studied in the past decades and many interesting results have been obtained. Local well-posedness for the initial datum in H s with s > 3 / 2 was proved in [2] [3] . The blow-up phenomenon was studied in [2] - [7] . McKean [7] (see also [6] for a simple proof) proved that the Camassa-Holm equation breaks if and only if some portion of the positive part of y 0 lies to the left of some portion of its negative part, here y 0 = ( 1 − ∂ x 2 ) u 0 . The hierarchy properties and algebro-geometric solutions of the Camassa-Holm equation were proposed in [8] . Global weak solution was studied in [9] [10] [11] .

Later, researchers are concerned with the Camassa-Holm equation with weakly dissipative term

y t + u y x + 2 u x y + λ y = 0 ,     y = ( 1 − ∂ x 2 ) u . (1.2)

Wu and Yin proved in [12] [13] that the solution of (1.2) decays to zero as time goes to infinity if the initial momentum density y 0 does not change its sign. Unlike the Camassa-Holm equation, there are no traveling wave solutions of (1.2) (see [12] ). Global existence and blow-up phenomena were studied in [12] - [17] .

In recent years, the following fifth-order Camassa-Holm equation was studied by Liu and Qiao [18] :

y t + u y x + b u x y = 0 ,   y = ( 1 − α 2 ∂ x 2 ) ( 1 − β 2 ∂ x 2 ) u ,   α β ≠ 0 , (1.3)

where b , α , β are real constants. In [18] , the authors studied peakon solutions including single pseudo-peakons, two-peakons and three-peakons interactional solutions of (1.3). In [19] , Tang and Liu proved that the Cauchy problem of this equation is locally well-posed in the critical Besov space B 2,1 7 / 2 or in B p , r s with 1 ≤ p , r ≤ + ∞ , s > max { 3 + 1 / p , 7 / 2 } when α = β = 1 . Zhu, Cao, Jiang and Qiao [20] studied the global existence of the solution of (1.3) with α ≠ β ≠ 0 . For more mathematical studies of (1.3), we refer to [21] [22] [23] [24] [25] .

So far, there have been many researches on Camassa-Holm equation. However, the results on the fifth-order Camassa-Holm equation are few. In this paper, we consider the Cauchy problem of the fifth-order Camassa-Holm equation with weakly dissipative term

y t + u y x + b u x y + λ y = 0 ,   t > 0 ,   x ∈ ℝ , (1.4)

y = ( 1 − α 2 ∂ x 2 ) ( 1 − β 2 ∂ x 2 ) u ,   t > 0 ,   x ∈ ℝ , (1.5)

u ( x , 0 ) = u 0 ( x ) , (1.6)

where b ∈ ℝ is a constant and α , β ∈ ℝ are two parameters satisfying α β ≠ 0 . Our main purpose is to study the existence of global solution for this problem and investigate the properties of the solution.

Throughout the paper, we denote by L p ( ℝ ) the Lebesgue space equipped with the norm

‖ u ‖ L p = ( ∫ ℝ | u ( x ) | p d x ) 1 p     if   1 ≤ p < + ∞

and

‖ u ‖ L ∞ = esssup { | u ( x ) | ; x ∈ ℝ } .

For s ∈ ℝ , H s ( ℝ ) denotes the nonhomogeneous Sobolev space defined by

H s ( ℝ ) = { u ∈ S ′ ( ℝ ) | ‖ u ‖ H s ( ℝ ) 2 = ∫ ℝ ( 1 + | ξ | 2 ) s | u ^ ( ξ ) | 2 d ξ < + ∞ } ,

where u ^ ( ξ ) is the Fourier transform of u.

This paper is organized as follows. In Section 2, we present the local well-posedness result and the blow up criterion. In Section 3, we discuss the problem of global existence. Finally, we consider the infinite propagation speed in Section 4.

2. Blow up Criterion

In this section, we discuss the blow up criterion for the solution to (1.4) - (1.6). To this aim, we first give the following existence theorem.

Theorem 2.1. Let u 0 ∈ H s ( ℝ ) with s > 7 2 . Then the Cauchy problem (1.4) - (1.6) admits a unique solution u ( x , t ) such that

u ∈ C ( [ 0, T ) ; H s ( ℝ ) ) ∩ C 1 ( [ 0, T ) ; H s − 1 ( ℝ ) ) ,

where T = T ( ‖ u 0 ‖ H s ) > 0 .

Theorem 2.1 can be proved by applying Kato’s method [26] . Since the argument is standard, we omit the details for simplicity. If T < ∞ and

l i m t → T − ‖ u ‖ H s = ∞ ,

we say the solution blows up in finite time. If the norm ‖ u ‖ H s is bounded at any large time, we say the solution exists globally.

Define

G ( x ) = { α 2 ( α 2 − β 2 ) e − | x | α − β 2 ( α 2 − β 2 ) e − | x | β , α ≠ β , 1 4 α ( 1 + | x | α ) e − | x | α , α = β , (2.1)

then the function [ ( 1 − α 2 ∂ x 2 ) ( 1 − β 2 ∂ x 2 ) ] − 1 y can be expressed as

u ( t , x ) = [ ( 1 − α 2 ∂ x 2 ) ( 1 − β 2 ∂ x 2 ) ] − 1 y ( t , x ) = G ∗ y .

Now we state the main result of this section.

Theorem 2.2. Assume that u 0 ∈ H 4 ( ℝ ) , and T is the maximal existence time of the solution obtained by Theorem 2.1.

1) If b > 1 2 , then the solution blows up in finite time if and only if

lim t → T inf x ∈ ℝ u x = − ∞ . (2.2)

2) If b < 1 2 , then the solution blows up in finite time if and only if

lim t → T sup x ∈ ℝ u x = + ∞ . (2.3)

Proof: Using (1.5), we obtain

‖ y ‖ L 2 2 = ∫ ℝ [ u − ( α 2 + β 2 ) u x x + α 2 β 2 u x x x x ] 2 d x = ∫ ℝ [ u 2 + ( α 2 + β 2 ) 2 u x x 2 − 2 ( α 2 + β 2 ) u u x x + α 4 β 4 u x x x x 2 + 2 α 2 β 2 u u x x x x   − 2 ( α 2 + β 2 ) α 2 β 2 u x x u x x x x ] d x

= ∫ ℝ [ u 2 + ( α 2 + β 2 ) 2 u x x 2 + 2 ( α 2 + β 2 ) u x 2 + α 4 β 4 u x x x x 2 + 2 α 2 β 2 u x x 2   + 2 ( α 2 + β 2 ) α 2 β 2 u x x x 2 ] d x ,

then

C 0 ‖ u ‖ H 4 2 ≤ ‖ y ‖ L 2 2 ≤ C ‖ u ‖ H 4 2 . (2.4)

In case of b > 1 2 , we have

1 2 d d t ∫ ℝ   y 2 d x = − 1 2 ∫ ℝ   u ( y 2 ) x d x − b ∫ ℝ   y 2 u x d x − ∫ ℝ   λ y 2 d x = ( 1 2 − b ) ∫ ℝ   y 2 u x d x − ∫ ℝ   λ y 2 d x ,

which implies

d d t ‖ y ‖ L 2 2 + 2 λ ‖ y ‖ L 2 2 = ( 1 − 2 b ) ∫ ℝ   y 2 u x d x ≤ ( 1 − 2 b ) inf x ∈ ℝ u x ∫ ℝ   y 2 d x .

If inf x ∈ ℝ u x ≥ − M , then

d d t ‖ y ‖ L 2 2 ≤ [ − ( 1 − 2 b ) M − 2 λ ] ‖ y ‖ L 2 2 . (2.5)

By Gronwall’s inequality, there holds

‖ y ‖ L 2 2 ≤ e [ − ( 1 − 2 b ) M − 2 λ ] t ‖ y 0 ‖ L 2 2 . (2.6)

Hence, ‖ u ( x , t ) ‖ H 4 is bounded for all t ∈ [ 0, T ) , which contradicts the maximal property of T.

In case of b < 1 2 , we can obtain similar result with the same arguments as above. This completes the proof of Theorem 2.2.

3. Global Existence Results

In this section, we will show two global existence results. To begin with, motivated by Mckean’s deep observation for the Camassa-Holm equation [7] , we define the particle trajectory by

( q t = u ( q , t ) , 0 < t < T ,   x ∈ ℝ , q ( x , 0 ) = x , x ∈ ℝ , (3.1)

where T is the lifespan of the solution. From (3.1), we get

d q t d x = q t x = u x ( q , t ) q x ,   t ∈ ( 0 , T ) ,

which yields

( q x = exp { ∫ 0 t   u x ( q , s ) d s } , 0 < t < T , x ∈ ℝ , q x ( x , 0 ) = 1 , x ∈ ℝ . (3.2)

The relation (3.2) implies that q x is always positive, hence q ( x , t ) is an increasing function. A direct calculation gives

d d t ( y ( q ) q x b ) = [ y t ( q ) + u ( q , t ) y x ( q ) + b u x ( q , t ) y ( q ) ] q x b = − λ y ( q ) q x b ,

so we have

y ( q ) q x b = e − λ t y 0 ( x ) . (3.3)

From (3.3), we also get

e λ t b ∫ ℝ   y 1 b d x = ∫ ℝ   y 0 1 b d x . (3.4)

Theorem 3.1. Assume b = 1 2 or b = 2 , and u 0 ∈ H s ( ℝ ) with s > 7 2 , then the solution of (1.4) - (1.6) exists globally in time.

Proof: We first consider the case b = 1 2 . Multiplying both sides of Equation (1.4) by y and integrating with respect to x, we have

d d t ‖ y ‖ L 2 2 + 2 λ ‖ y ‖ L 2 2 = 0,

hence, we obtain ‖ y ‖ L 2 = e − λ t ‖ y 0 ‖ L 2 . By (2.4) and Sobolev’s inequality, we see that ‖ u x ‖ L ∞ is bounded by ‖ y ‖ L 2 , so we can extend the local solution to be a global solution.

Then, we give the proof for b = 2 . Let

E ( t ) = ∫ ℝ [ u 2 + ( α 2 + β 2 ) u x 2 + α 2 β 2 u x x 2 ] d x ,

then

d d t E ( t ) = ∫ ℝ [ 2 u u t + 2 ( α 2 + β 2 ) u x u x t + 2 α 2 β 2 u x x u x x t ] d x = ∫ ℝ [ 2 u u t − 2 ( α 2 + β 2 ) u u x x t + 2 α 2 β 2 u u x x x x t ] d x = 2 ∫ ℝ   u y t d x = − 2 ∫ ℝ   u ( u y x + 2 u x y + λ y ) d x = − 2 λ E ( t ) .

The above identity gives E ( t ) = e − 2 λ t E ( 0 ) , so once again we can see ‖ u x ‖ L ∞ is bounded. This ends the proof of Theorem 3.1.

Theorem 3.2. Let α ≠ β and u 0 ∈ H s ( ℝ ) with s > 7 2 . Assume that y 0 = ( 1 − α 2 ∂ x 2 ) ( 1 − β 2 ∂ x 2 ) u 0 does not change sign, then the solution of (1.4) - (1.6) exists globally in time.

Proof: Differentiating ∫ ℝ   y d x with respect to t and using (1.5), we have

d d t ∫ ℝ   y d x = − ∫ ℝ ( u y x + b u x y + λ y ) d x = − ( b − 1 ) ∫ ℝ   u x y d x − λ ∫ ℝ   y d x = − ( b − 1 ) ∫ ℝ   u x ( u − ( α 2 + β 2 ) u x x + α 2 β 2 u x x x x ) d x − λ ∫ ℝ   y d x = − λ ∫ ℝ   y d x ,

which yields

∫ ℝ   y d x = e − λ t ∫ ℝ   y 0 d x . (3.5)

When α ≠ β , using the expression of G (see (2.1)), u ( x , t ) and u x ( x , t ) can be represented as

u = α 2 ( α 2 − β 2 ) ( e − x α ∫ − ∞ x   e ξ α y ( ξ , t ) d ξ + e x α ∫ x + ∞   e − ξ α y ( ξ , t ) d ξ )   − β 2 ( α 2 − β 2 ) ( e − x β ∫ − ∞ x   e ξ β y ( ξ , t ) d ξ + e x β ∫ x + ∞   e − ξ β y ( ξ , t ) d ξ ) , (3.6)

and

u x = 1 2 ( α 2 − β 2 ) ( − e − x α ∫ − ∞ x   e ξ α y ( ξ , t ) d ξ + e x α ∫ x + ∞   e − ξ α y ( ξ , t ) d ξ )   + 1 2 ( α 2 − β 2 ) ( e − x β ∫ − ∞ x   e ξ β y ( ξ , t ) d ξ − e x β ∫ x + ∞   e − ξ β y ( ξ , t ) d ξ ) . (3.7)

Without loss of generality, we may assume y 0 ≥ 0 as the case y 0 ≤ 0 can be discussed similarly. If α > β > 0 , by (3.5) and (3.7), we have

u x ≤ 1 2 ( α 2 − β 2 ) ( e x α ∫ x ∞   e − ξ α y ( ξ , t ) d ξ + e − x β ∫ − ∞ x   e ζ β y ( ξ , t ) d ξ ) ≤ 1 2 ( α 2 − β 2 ) ( ∫ ℝ   y ( ξ , t ) d ξ + ∫ ℝ   y ( ξ , t ) d ξ ) = 1 α 2 − β 2 e − λ t ∫ ℝ   y 0 ( ξ , t ) d ξ ,

and

u x ≥ 1 2 ( α 2 − β 2 ) ( − e − x α ∫ − ∞ x   e ξ α y ( ξ , t ) d ξ − e x β ∫ x + ∞   e − ξ β y ( ξ , t ) d ξ ) = − 1 α 2 − β 2 e − λ t ∫ ℝ   y 0 ( ξ , t ) d ξ .

Similarly, if β > α > 0 , we can also obtain

− 1 β 2 − α 2 e − λ t ∫ ℝ   y 0 ( ξ , t ) d ξ ≤ u x ( x , t ) ≤ 1 β 2 − α 2 e − λ t ∫ ℝ   y 0 ( ξ , t ) d ξ .

Hence, by Theorems 2.1 - 2.2, we know that the problem (1.4) - (1.6) has a unique global solution.

4. Infinite Propagation Speed

In this section, we study the infinite propagation phenomenon for the Equation (1.4). To this aim, we set

E 1 ( t ) = ∫ ℝ   e x α y ( x , t ) d x ,   F 1 ( t ) = ∫ ℝ   e − x α y ( x , t ) d x ,

and

E 2 ( t ) = ∫ ℝ   e x β y ( x , t ) d x ,   F 2 ( t ) = ∫ ℝ   e − x β y ( x , t ) d x .

The main result of this section is stated as follows.

Theorem 4.1. Let b ≥ 0, λ ∈ ℝ . Suppose that the initial value u 0 ( x ) ≡ 0 is supported in the interval [ a , c ] . Then for any t ∈ ( 0, T ] , the solution u ( x , t ) of (1.4) - (1.6) can be expressed by

u ( x , t ) = ( α 2 ( α 2 − β 2 ) e − x α E 1 ( t ) − β 2 ( α 2 − β 2 ) e − x β E 2 ( t ) , x > q ( c , t ) , α 2 ( α 2 − β 2 ) e x α F 1 ( t ) − β 2 ( α 2 − β 2 ) e x β F 2 ( t ) , x < q ( a , t ) .

Moreover, if α > 0 , 0 < β ≤ 3 2 α , 0 ≤ b ≤ min { 3 − 2 β 2 α 2 , 5 3 } , then e λ t E 1 ( t ) is a strictly increasing function and e λ t F 1 ( t ) is a strictly decreasing function. Similarly, if β > 0 , 0 < α ≤ 3 2 β , 0 ≤ b ≤ min { 3 − 2 β 2 α 2 , 5 3 } , then e λ t E 2 ( t ) is a strictly increasing function and e λ t F 2 ( t ) is a strictly decreasing function.

Proof: By (3.3), we have

y ( q ( x , t ) , t ) = 0 ,   x < a   or   x > c .

Since

u ( x , t ) = ( α 2 α 2 − β 2 p 1 − β 2 α 2 − β 2 p 2 ) ∗ y ( x , t ) = α 2 ( α 2 − β 2 ) ∫ ℝ   e − | x − ξ | α y ( ξ ) d ξ − β 2 ( α 2 − β 2 ) ∫ ℝ   e − | x − ξ | β y ( ξ ) d ξ = α 2 ( α 2 − β 2 ) ∫ q ( a , t ) q ( c , t )   e − | x − ξ | α y ( ξ ) d ξ − β 2 ( α 2 − β 2 ) ∫ q ( a , t ) q ( c , t )   e − | x − ξ | β y ( ξ ) d ξ , (4.1)

when x > q ( c , t ) , we get

u ( x , t ) = α 2 ( α 2 − β 2 ) ∫ q ( a , t ) q ( c , t )   e − x − ξ α y ( ξ ) d ξ − β 2 ( α 2 − β 2 ) ∫ q ( a , t ) q ( c , t )   e − x − ξ β y ( ξ ) d ξ = α 2 ( α 2 − β 2 ) e − x α ∫ q ( a , t ) q ( c , t )   e ξ α y ( ξ ) d ξ − β 2 ( α 2 − β 2 ) e − x β ∫ q ( a , t ) q ( c , t )   e ξ β y ( ξ ) d ξ = α 2 ( α 2 − β 2 ) e − x α E 1 ( t ) − β 2 ( α 2 − β 2 ) e − x β E 2 ( t ) .

Similarly, when x < q ( a , t ) , we have

u ( x , t ) = α 2 ( α 2 − β 2 ) e − x α F 1 ( t ) − β 2 ( α 2 − β 2 ) e − x β F 2 ( t ) .

Note that

d E 1 ( t ) d t = ∫ ℝ   e ξ α y t ( ξ , t ) d ξ . (4.2)

By

y = ( 1 − α 2 ∂ x 2 ) ( 1 − β 2 ∂ x 2 ) u = u − ( α 2 + β 2 ) u x x + α 2 β 2 u x x x x ,

then we get

y t = − u y x − b y u x − λ y = − ( b + 1 ) u u x + ( α 2 + β 2 ) u x x x u − α 2 β 2 u x x x x x u     + b ( α 2 + β 2 ) u x x u x − b α 2 β 2 u x x x x u x − λ y . (4.3)

Inserting (4.3) into (4.2), we have

d E 1 ( t ) d t = − ( b + 1 ) ∫ ℝ   e x α u u x d x + ( α 2 + β 2 ) ∫ ℝ   e x α u x x x u d x − α 2 β 2 ∫ ℝ   e x α u x x x x x u d x     + b ( α 2 + β 2 ) ∫ ℝ   e x α u x x u x d x − b α 2 β 2 ∫ ℝ   e x α u x x x x u x d x − λ E 1 ( t ) ,

then

d ( e λ t E 1 ( t ) ) d t = e λ t ( b + 1 2 α ∫ ℝ   e x α u 2 d x − α 2 + β 2 2 α 3 ∫ ℝ   e x α u 2 d x + 3 ( α 2 + β 2 ) 2 α ∫ ℝ   e x α u x 2 d x   + β 2 2 α 3 ∫ ℝ   e x α u 2 d x − 5 β 2 2 α ∫ ℝ   e x α u x 2 d x + 5 α β 2 2 ∫ ℝ   e x α u x x 2 d x   − b ( α 2 + β 2 ) 2 α ∫ ℝ   e x α u x 2 d x + b β 2 2 α ∫ ℝ   e x α u x 2 d x − 3 b α β 2 2 ∫ ℝ   e x α u x x 2 d x ) = e λ t ( b 2 α ∫ ℝ   e x α u 2 d x − ( b − 3 ) α 2 + 2 β 2 2 α ∫ ℝ   e x α u x 2 d x   + ( 5 − 3 b ) α β 2 2 ∫ ℝ   e x α u x x 2 d x ) . (4.4)

Applying similar arguments as above, we can obtain

d ( e λ t F 1 ( t ) ) d t = e λ t ( − b 2 α ∫ ℝ   e x α u 2 d x + ( b − 3 ) α 2 + 2 β 2 2 α ∫ ℝ   e x α u x 2 d x   − ( 5 − 3 b ) α β 2 2 ∫ ℝ   e x α u x x 2 d x ) . (4.5)

According to (4.4) and (4.5), it is easy to see that if α > 0 , 0 < β ≤ 3 2 α and 0 ≤ b ≤ min { 3 − 2 β 2 α 2 , 5 3 } , the function e λ t E 1 ( t ) is strictly increasing and the function e λ t F 1 ( t ) is strictly decreasing. In the same way, we can obtain the desired result when β > 0 , 0 < α ≤ 3 2 β and 0 ≤ b ≤ min { 3 − 2 β 2 α 2 , 5 3 } .

Acknowledgements

The author is extremely appreciative of the reviewers valuable suggestions and comments on the manuscript.

Conflicts of Interest

The author declares no conflicts of interest regarding the publication of this paper.

References

1. Camassa, R. and Holm, D.D. (1993) An Integrable Shallow Water Equation with Peaked Solitons. Physical Review Letters, 71, 1661-1664. https://doi.org/10.1103/PhysRevLett.71.1661

2. Constantin, A. and Escher, J. (1998) Well-Posedness, Global Existence, and Blowup Phenomenon for a Periodic Quasi-Linear Hyperbolic Equation. Communications on Pure and Applied Mathematics, 51, 475-504. https://doi.org/10.1002/(SICI)1097-0312(199805)51:5<475::AID-CPA2>3.0.CO;2-5

3. Li, Y. and Olver, P. (2000) Well-Posedness and Blow-Up Solutions for an Integrable Nonlinear Dispersive Model Wave Equation. Journal of Differential Equations, 162, 27-63. https://doi.org/10.1006/jdeq.1999.3683

4. Constantin, A. (2000) Existence of Permanent and Breaking Waves for a Shallow Water Equation: A Geometric Approach. Annales de l’Institut Fourier, 50, 321-362. https://doi.org/10.5802/aif.1757

5. Constantin, A. and Escher, J. (1998) Wave Breaking for Nonlinear Nonlocal Shallow Water Equations. Acta Mathematica, 181, 229-243. https://doi.org/10.1007/BF02392586

6. Jiang, Z., Ni, L. and Zhou, Y. (2012) Wave Breaking of the Camassa-Holm Equation. Journal of Nonlinear Science, 22, 235-245. https://doi.org/10.1007/s00332-011-9115-0

7. McKean, H. (1998) Breakdown of a Shallow Water Equation. Asian Journal of Mathematics, 2, 867-874. https://doi.org/10.4310/AJM.1998.v2.n4.a10

8. Qiao, Z. (2003) The Camassa-Holm Hierarchy, N-Dimensional Integrable Systems, and Algebro-Geometric Solution on a Symplectic Submanifold. Communications in Mathematical Physics, 239, 309-341. https://doi.org/10.1007/s00220-003-0880-y

9. Constantin, A. and Escher, J. (1998) Global Weak Solutions for a Shallow Water Equation. Indiana University Mathematics Journal, 47, 1527-1546. https://doi.org/10.1512/iumj.1998.47.1466

10. Xin, Z. and Zhang, P. (2000) On the Weak Solutions to a Shallow Water Equation. Communications on Pure and Applied Mathematics, 53, 1411-1433. https://doi.org/10.1002/1097-0312(200011)53:11<1411::AID-CPA4>3.0.CO;2-5

11. Xin, Z. and Zhang, P. (2002) On the Uniqueness and Large Time Behavior of the Weak Solutions to a Shallow Water Equation. Communications in Partial Differential Equations, 27, 1815-1844. https://doi.org/10.1081/PDE-120016129

12. Wu, S. and Yin, Z. (2006) Blow-Up, Blow-Up Rate and Decay of the Solution of the Weakly Dissipative Camassa-Holm Equation. Journal of Mathematical Physics, 47, Article ID: 013504. https://doi.org/10.1063/1.2158437

13. Wu, S. and Yin, Z. (2009) Global Existence and Blow-Up Phenomena for the Weakly Dissipative Camassa-Holm Equation. Journal of Differential Equations, 246, 4309-4321. https://doi.org/10.1016/j.jde.2008.12.008

14. Guo, Z. (2008) Blow up, Global Existence, and Infinite Propagation Speed for the Weakly Dissipative Camassa-Holm Equation. Journal of Mathematical Physics, 49, Article ID: 033516. https://doi.org/10.1063/1.2885075

15. Lenells, J. and Wunsch, M. (2013) On the Weakly Dissipative Camassa-Holm, Degasperis-Procesi, and Novikov Equations. Journal of Differential Equations, 255, 441-448. https://doi.org/10.1016/j.jde.2013.04.015

16. Park, S. (2015) Local Well-Posedness and Blow-Up Result for Weakly Dissipative Camassa-Holm Equations. Advances in Differential Equations, 20, 983-1008. https://doi.org/10.57262/ade/1435064519

17. Zhu, M. and Jiang, Z. (2012) Some Properties of Solutions to the Weakly Dissipative b-Family Equation. Nonlinear Analysis: Real World Applications, 13, 158-167. https://doi.org/10.1016/j.nonrwa.2011.07.020

18. Liu, Q. and Qiao, Z. (2018) Fifth Order Camassa-Holm Model with Pseudo-Peakons and Multi-Peakons. International Journal of Non-Linear Mechanics, 105, 179-185. https://doi.org/10.1016/j.ijnonlinmec.2018.05.024

19. Tang, H. and Liu, Z. (2015) Well-Posedness of the Modified Camassa-Holm Equation in Besov Spaces, Zeitschrift für angewandte Mathematik und Physik, 66, 1559-1580. https://doi.org/10.1007/s00033-014-0483-9

20. Zhu, M., Cao, L., Jiang, Z. and Qiao, Z. (2021) Analytical Properties for the Fifth Order Camassa-Holm (FOCH) Model. Journal of Nonlinear Mathematical Physics, 28, 321-336. https://doi.org/10.2991/jnmp.k.210519.001

21. Coclite, G., Holden, H. and Karlsen, K. (2009) Well-Posedness of Higher-Order Camassa-Holm Equations. Journal of Differential Equations, 246, 929-963. https://doi.org/10.1016/j.jde.2008.04.014

22. Han, L. and Cui, W. (2019) Infinite Propagation Speed and Asymptotic Behavior for a Generalized Fifth-Order Camassa-Holm Equation. Applicable Analysis, 98, 536-552. https://doi.org/10.1080/00036811.2017.1395868

23. McLachlan, R. and Zhang, X. (2009) Well-Posedness of Modified Camassa-Holm Equations. Journal of Differential Equations, 246, 3241-3259. https://doi.org/10.1016/j.jde.2009.01.039

24. Tian, L., Zhang, P. and Xia, L. (2011) Global Existence for the Higher-Order Camassa-Holm Shallow Water Equation. Nonlinear Analysis: Theory, Methods & Applications, 74, 2468-2474. https://doi.org/10.1016/j.na.2010.12.002

25. Zhu, M., Jiang, Z. and Qiao, Z. (2022) Analytical Properties for the Fifth-Order b-Family Novikov Model. Journal of Evolution Equations, 22, Article No. 19. https://doi.org/10.1007/s00028-022-00781-y

26. Kato, T. (1975) Quasi-Linear Equations of Evolution, with Application to Partial Differential Equations. In: Everitt, W.N., Ed., Spectral Theory and Differential Equations, Lecture Notes in Mathematics, Vol. 448, Springer, Berlin, 25-70. https://doi.org/10.1007/BFb0067080