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The Cauchy problem for a generalized Camassa–Holm equation with the velocity potential

Lin, Bohuan; Yin, Zhaoyang

Published in: Applicable Analysis

DOI:

10.1080/00036811.2016.1267342

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Publication date: 2018

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Lin, B., & Yin, Z. (2018). The Cauchy problem for a generalized Camassa–Holm equation with the velocity potential. Applicable Analysis, 97(3), 354–367. https://doi.org/10.1080/00036811.2016.1267342

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The Cauchy problem for a generalized

Camassa–Holm equation with the velocity

potential

Bohuan Lin & Zhaoyang Yin

To cite this article: Bohuan Lin & Zhaoyang Yin (2018) The Cauchy problem for a generalized Camassa–Holm equation with the velocity potential, Applicable Analysis, 97:3, 354-367, DOI: 10.1080/00036811.2016.1267342

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https://doi.org/10.1080/00036811.2016.1267342

The Cauchy problem for a generalized Camassa–Holm equation

with the velocity potential

Bohuan Linaand Zhaoyang Yina,b

aDepartment of Mathematics, Sun Yat-sen University, Guangzhou, China;bFaculty of Information Technology,

Macau Univercity of Science and Technology, Macau, China

ABSTRACT

In this paper, we discuss a generalized Camassa–Holm equation whose solutions are velocity potentials of the classical Camassa–Holm equation. By exploiting the connection between these two equations, we first establish the local well-posedness of the new equation in the Besov spaces and deduce several blow-up criteria and blow-up results. Then, we investigate the existence of global strong solutions and present a class of cuspon weak solutions for the new equation.

ARTICLE HISTORY Received 12 October 2016 Accepted 28 November 2016 COMMUNICATED BY A. Constantin KEYWORDS A generalized Camassa–Holm equation with the velocity potential; local well-posedness; blow-up; cuspon weak solutions

AMS SUBJECT CLASSIFICATIONS

35G25; 35L05

1. Introduction

Equations of the following form are quite common in physics and of great interests:

ut = F(u, u1,. . . , un). (1.1)

Among them, the Camassa–Holm (CH) Equation (1.2) and the Degasperis-Procesi (DP) Equation (1.3) have drawn much attention since the time they were proposed [1,2]:

ut− utxx+ 3uux = 2uxuxx+ uuxxx, (1.2)

(1 − D2

x)ut = 4uux− 3uxuxx− uuxxx. (1.3)

Both the CH and DP equations describe the motion of shallow water waves with one dimension in space and have the same asymptotic accuracy [3,4]. They are integrable and possess bi-Hamitonian structures, which makes them to be important mathematical objects for study [5–9]. It is worth pointing out that both CH and DP equations admit peaked solutions [1,10,11]. The peakons are of hydrodynamical relevance since the Stokes waves of greatest height (extreme wave solutions of the governing equations for water waves) are peaked [12–14], and this type of patterns also arise as solutions to the governing equations for gravity water waves [15,16] as well as for equatorial ocean waves [17–20].

The local well-posedness of the Cauchy problem for the CH equation in Sobolev spaces and Besov spaces was proved in [21–24], and some blow-up criteria were proposed in [21,25–27]. The existence

CONTACT Zhaoyang Yin mcsyzy@mail.sysu.edu.cn

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of the global strong solutions and finite time blow-up solutions were shown in [21,22,26,28], while the global existence and uniqueness of the weak solutions were discussed in [29,30].

As for the DP equation, the local well-posedness of its Cauchy problem was discussed in [31–33]. Like the CH equation, it also possesses global strong solutions, finite time blow-up solutions and global weak solutions [33–40].

As we know, when talking about the shallow water waves, the fluid is always considered adiabatic and inviscid, and acted by the gravity. This indicates that the flow should preserve the circulation of its velocity field according to Kelvin’s theorem. So it is interesting to consider the case where it is a potential flow. Besides, when considering the waves in the space with one dimension, we are actually referring to motions of fluid in a two-dimensional space. The vertical component of the velocity is always considered negligible compared to the horizontal component and thus is omitted, while the latter one is assumed to be constant along the vertical direction. So the potential we are looking for is actually a function with two variables, t ∈ R+ and x ∈ R. In 2009, Novikov used the perturbative symmetry approach to deduce a series of generalized CH equations [41], which are integrable and possess an infinite hierarchy of quasi-local higher symmetries. Among them, the following two equations happen to be the ones that we are interested in:

(1 − D2 x)ut = 1 2(3u 2 x− 2uxuxxx− u2xx), (1.4) (1 − D2 x)ut = (4 − D2x)u2x. (1.5)

This paper mainly aims at solving (1.4) in Besov spaces by exploiting its connection with the classical CH equation. More explicitly, we are dealing with the following Cauchy problem:

⎧ ⎨ ⎩ (1 − D2 x)ut = 12(3ux2− 2uxuxxx− u2xx), u t=0 = u0. (1.6)

As we will see in the paper, applying our method in Section 3for establishing the local well-posedness of the Cauchy problem (1.6), we can easily obtain the blow-up criteria and some blow-up results for (1.6) in Section4. As pointed out in the later discussion, a similar argument can be applied to (1.5). In the last section, a class of weak solutions to (1.6) is presented.

Notation 1.1: In the following, since all spaces of functions are over R, for simplicity, we drop R

in our notations of function spaces if there is no ambiguity.

2. Preliminaries

The main tools of this paper are based on the Littlewood–Payley decomposition and theories of the Besov spaces. Let’s denote by C the annulusξ ∈ R34 <|ξ| <83. Then there exist radial functions

χ ∈ D(B(0,4

3)) and ϕ ∈ D(C) which take value in [0, 1] such that

χ(ξ) +

j≥0

ϕj(ξ) = 1. (2.1)

Denote by F the Fourier transform. For∀u ∈ S, we have the following definition: −1u= F−1(χFu),

ϕj(ξ) = ϕ(2−jξ),

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Sju=



k≤j−1

ku.

Then for 1≤ p, r ≤ ∞ and any real number s, the nonhomogeneous Besov spaces can be defined as follows: Bsp,r = u∈ S 2js ju p r <.

When p, r= 2, the corresponding Besov spaces are actually the Sobolev spaces Hs. The following propositions and lemmas are fundamental and necessary to our work.

Proposition 2.1 [42]: 1 ≤ p ≤ q ≤ ∞, 1 ≤ r ≤ ∞, then Bs p,r → B s−(1 p−1q) q,r . Proposition 2.2 [42]: If s > 1 p, then Bsp,ris an algebra.

Lemma 2.3 [42]: Suppose that p, p, r, rsatisfy : 1

p+p1 = 1, 1r +r1 = 1. Then B−sp,ris isomorphic to

the dual space of C0Bsp,r ⊂ Bsp,r. More specifically, the duality can be expressed in the following way

(u, φ) = 

|j−j|≤1

ju,jφ .

Lemma 2.4 [42]: Let C be an annulus. Suppose that u ∈ Sandˆu is supported on λC. Let σ be a smooth

function onR, and possess the following property: for any α ∈ N,

|∂ασ(ξ)| ≤ Cα|ξ|m−|α|.

Then there exists some constant C such that

σ (D)u p≤ Cλm u p.

The operators mentioned above are called Smmultipliers. We have the following important fact for the this kind of operators.

Lemma 2.5 [42]: Assume that σ(D) is an Smmultiplier, then it is a bounded linear map from Bs−m p,r

to Bsp,r.

We would like to point out here thatσ(D) = (1 − D2x)−1is an S−2multiplier withσ = 1+|ξ|1 2.

Denote by p(x) = 12e−|x|. Then p= F−1(σ).

Lemma 2.6 (Commutator Estimates [42]): Let v be a vector field, and Rj= [v · ∇, j]f . Then there

exists some constant C dependent of s, p such that: if s > 0, then

2js R j p r≤ C ∇v f Bs p,r+ ∇v Bsp,r−1 ∇f ∞ ; if−1p< s < 1+1p, then 2js R j p r≤ C ∇v B 1 p p,r∩L f Bs p,r.

Lemma 2.7 [42]: Let E be a Banach space, and be an open set in E. If v ∈ C([0, T], C0,1( , E)), then

there exists a mapψ ∈ C([0, T], C0,1( , E)) ∩ C1([0, T] × , E) such that

ψ(t, x) = x +

 t

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Lemma 2.8 [42]: Assume s > 1 + 1

p, v ∈ C([0, T], Bsp,r) ∩ C1([0, T], Bsp,r−1), g ∈ C([0, T], S) ∩

L1([0, T], Bsp,r). Then for any f0∈ Bsp,r, the Cauchy problem



∂tf + v · ∇f = g,

f(0, x) = f0,

(2.2)

has a unique solution in

 C([0, T], Bs p,r), r <∞,  t<sC([0, T], Btp,)  Cw([0, T], Bsp,r), r = ∞.

Besides, the following estimate holds:

f (t) Bs p,rexp( − CV(t)) ≤ f0 Bsp,r+  t 0 exp( − CV(τ))g(τ)dτ, (2.3) where V(t) =t 0 ∇v Bsp,r−1dτ.

Lemma 2.9 [42]: Suppose f1(t, x), f2(t, x) are two solutions for the Cauchy problem (2.2) with the initial

data h1, h2, respectively. Then the following inequality holds:

f1− f2 Lt (Bs

p,r)≤ h1− h2 Bsp,rexp CV(t). (2.4) Before recalling the basic results for the CH equation, we first introduce some notations:

Ep,rs (T)  C([0, T]; Bsp,r)  C1([0, T]; Bsp,r−1), if r < ∞, Ep,s(T)  Cw([0, T]; Bsp,)  C0,1([0, T]; Bsp,−1), if r = ∞.

The CH equation (1.2) can also be written as:

ut+ u∂xu= −∂xp∗  u2+1 2u 2 x  .

Lemma 2.10 [42,43]: Assume s > 1 + max{1 p,

1

2}. Then for any u0 ∈ Bsp,r, there is some T > 0 such

that the Cauchy problem



ut+ u∂xu= −∂xp∗ (u2+12u2x),

u(0, x) = u0,

(2.5)

has a unique solution in Esp,r(T). When r < ∞, the solution map is continuous with respect to the initial data.

Lemma 2.11 [42]: Suppose that Tis the lifespan of the solution for the Cauchy problem (2.5) in Bs p,r. Then we have  T∗ 0 uxdt= ∞, (2.6)  T∗ 0 u B1∞,∞ dt= ∞. (2.7)

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Lemma 2.12 [25]: Assume s > 3

2. If there exists some point x0such that∂xu0(x0) < −|u0(x0)|, then

the corresponding solution for the Cauchy problem (2.5) will blow up in finite time. Suppose thatγ is

the streamline of the velocity field u which starts at x0. Then

lim

t→T∂xu0◦ γ (t) = −∞. (2.8) Lemma 2.13 [27]: Denote by m = u − uxx. Assume that u0∈ H3. Then the corresponding solution to

(2.5) blows up in finite time if and only if there exist x1< x2such that m0(x1) > 0 > m0(x2).

3. Local well-posedness

In this section, we will establish the local well-posedness of the Cauchy problem (1.6). Rewrite (1.4) in the following form

ut− 1 2u 2 x = (1 − D2x)−1  u2x+ 1 2u 2 xx  . (3.1)

Applying Dxto both sides of the above equation yields

(ux)t− ux∂xux = ∂xp∗  u2x+1 2u 2 xx  ,

which indicates that−uxsatisfies the CH equation (1.2). Thus, solutions to (3.1) or (1.4) are actually

the velocity potentials of the solutions to the CH equation. By exploiting such a relation between the two equations, we give the following theorem.

Theorem 3.1: Let s > 2 + max{1

p,12} and u0 ∈ Bsp,r. Then there exists some T > 0 such that the

following Cauchy problem

⎧ ⎨ ⎩ ut −12u2x= (1 − D2x)−1(u2x+12u2xx), u t=0 = u0, (3.2)

has a unique solution in Es

p,r(T). When r < ∞, the continuity dependence of the solution with respect

to the initial data holds.

Proof: Let’s focus on the existence first, and the uniqueness and the continuity dependence with

respect to the initial data will be proved later. Consider the following Cauchy problem:

⎧ ⎨ ⎩ vt− vvx= ∂xp∗ (v2+12vx2), v t=0 = ∂xu0. (3.3)

According to Lemma 2.8, there exists some T > 0 such that it has a unique solution in Ep,rs−1(T). Then

when r <∞, v ∈ C([0, T], Bsp,r−1); when r = ∞, for any t < s, v ∈ C([0, T], Btp,1−1)

L([0, T], Bsp,−1∞).

Then, consider the next Cauchy problem: ⎧ ⎨ ⎩ ut−12vux= (1 − D2x)−1(v2+12v2x), u t=0 = u0. (3.4)

Notice that(1 − Dx2)−1is an S−2-multiplier. Since s > 2+1p, Bsp,rand Bsp,r−1are Banach algebras, we

have(1 − D2

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problem has a solution u∈  C([0, T], Bs−1 p,r ), r <∞, C([0, T], Bt−1 p,r ) L([0, T], Bsp,r−1), r = ∞.

Next, we are going to prove that u is a solution to (3.2). In order to do so, we just need to prove that ux= v. Applying Dxto (3.4) and then subtracting (3.3) from it, we get



(ux− v)t−12v∂x(ux− v) −12vx(ux− v) = 0,

(ux− v)t=0= 0.

Denote ux− v by w. Since ux ∈ C([0, T], Btp,r−2) and v ∈ C([0, T], Btp,r−1), we have w ∈ C([0, T], Btp,r−2),

where s > t > 2+max{12,1p}. Thus, what we need descends to the uniqueness of the following Cauchy problem:



wt−12v∂xw−12vxw= 0,

wt=0= 0.

This is a fact ensured by the following lemma:

Lemma 3.2: Assume t > max{1

2,1p}, v ∈ C([0, T], B t+1

p,r ) and f , g ∈ L1([0, T], Btp,r). Suppose that

w∈ C([0, T], Btp,r) is the solution to the following Cauchy problem:



wt + v∂xw+ fw = g,

wt=0= w0.

(3.5)

Then for any 0 < < min{t − 1p, 1}, the following inequality holds with some constant C:

w ˜ Lt(B 1 p + p,r ) ≤  w0 B 1 p + p,r +  t 0 g B 1 p + p,r ds  exp  C  t 0 vx B 1 p + p,r + f B 1 p + p,r ds  .

Proof: Applying jto (3.5) yields

∂tjw+ v∂xjw+ [j, v∂x]w + j(fw) = jg.

If p <∞, multiplying both sides of the above equation by sgn(jw)|jw|p−1and integrating with

respect to x and t, we have

jw(t) pp≤ jw0 pp+  t 0 vx ∞ j w ppds +  t 0 ( Rj p+ j g p+ j(fw) p) jw pp−1ds, jw(t) p sup s∈(0,t) jw(s) pp−1 ≤ jw0 pp+ sup s∈(0,t) jw(s) pp−1  t 0 vx ∞ j w pds + sup s∈(0,t) jw(s) p−1 p  t 0 ( Rj p+ jg p+ j(fw) p) ds.

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Then jw(t) p≤ jw0 p+  t 0 vx ∞ jw pds +  t 0 Rj p+ j g p+ j(fw) pds. (3.6)

If p= ∞, since v ∈ C([0, T], Btp,r+1) → C([0, T], C0,1), we can utilize its flow ψ(t, x) in [0, T] × R to

get

d

dtjw= −j(fw) + jg+ Rj.

Integrating with respect to t and taking L− norm with respect to x, we obtain jw(t) ∞≤ jw0 ∞+

 t

0 j(fw) ∞+ j

g + Rjds. (3.7)

Multiplying (3.6) and (3.7) by 2j(p1+), and taking the lr− norm with respect to j, we get w(t) B 1 p + p,r ≤ w0 B 1 p + p,r +  t 0 vx w B 1 p + p,r ds +  t 0 2 j(1 p+) Rj p r+ g B 1 p + p,r + (fw) B 1 p + p,r ds.

Exploiting the commutator estimate yields: w(t) B 1 p + p,r ≤ w0 B 1 p + p,r +  t 0 vx w B 1 p + p,r ds +  t 0 vx B 1 p + p,r L w B 1 p + p,r + g B 1 p + p,r + f B 1 p + p,r w B 1 p + p,r ds.

Then the lemma is proved by applying the Gronwall inequality. Now let’s go onto prove Theorem 3.1.

From Lemma 3.2, we know that u∈ 

C([0, T], Bs−1

p,r ), r <∞,

t<sC([0, T], Btp,r−1), r = ∞,

is the solution to the Cauchy problem (3.2). Due to the fact that

ux = v ∈  C([0, T], Bs−1 p,r ), r <∞, t<sC([0, T], Btp,−1∞) L([0, T], Bsp,−1∞), r = ∞, we know actually u∈  C([0, T], Bs p,r), r <∞, t<sC([0, T], Btp,) L([0, T], Bsp,), r = ∞.

Because Bsp,r−1and Bsp,r−2are both Banach algebras, we have

ut ∈  C([0, T], Bs−1 p,r ), r <∞, t<sC([0, T], Btp,−1∞) L([0, T], Bsp,−1∞), r = ∞.

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It still remains to prove u ∈ Cw([0, T], Bsp,) in the case r = ∞. For any φ ∈ B−sp,1, u(t), φ =

Sju(t), φ + u(t), (id − Sj)φ . Since u ∈ C([0, T], Btp,), we have Sju ∈ C([0, T], Bsp,), and thus

Sju(t), φ is continuous with respect to t. On the other hand, (id − Sj)φ B−sp,1 → 0, j → ∞, and

| u(t), (id − Sj)φ | ≤ u L([0,T],Bs

p,) (id − Sj)φ B−sp,1, then together we can draw the conclusion

that u(t), φ is continuous with respect to t, and thus u ∈ Cw([0, T], Bsp,).

Thanks to the result for the CH equation, the argument for the uniqueness is quite simple. Suppose that u1, u2are two solutions to (3.2), then∂xu1,∂xu2are solutions to (3.3) with the same initial data

∂xu0. Due to the uniqueness of the Cauchy probelm for the CH equation, we have∂xu1 = ∂xu2.

Plugging into (3.2) yields∂tu1= ∂tu2. Since u1, u2share a common initial data, they are actually the

same.

Now let’s prove the continuity dependence with respect to the initial data in the case r < 0. Suppose that u1, u2 ∈ Esp,r are two solutions to (3.2) with respect to the initial data h1, h2, respectively. Then

∂xu1,∂xu2 are the two solutions to (3.3) with respect to∂xh1,∂xh2, respectively. Denote u1− u2by

w. And now we need to show that w Bs

p,r → 0, as h1− h2 Bp,rs → 0. Plugging u1, u2into equation, respectively, and subtracting one from the other, we get

∂tw− 1 2(∂xu1+ ∂xu2)∂xw = (1 − D2 x)−1  (u1− u  2)(u  1+ u  2) + 1 2(u  1− u  2)(u  1+ u  2)  = P(u1, u  2). Since w∈ Es p,r(T) → C  [0, T], W2,p C2and ∂xu1+ ∂xu2∈ L([0, T], Bsp,r−1) → L([0, T], C1,),

then it follows that: if p < ∞ , multiplying both sides of the above equation by sgn(w)|w|p−1 and integrating with respect to x and t, or if p= ∞, utilizing the flow of ∂xu1+ ∂xu2, we get

w(t) p≤ w0 p+  t 0 2 xu1(s) + ∂x2u2(s) w(s) pds+  t 0 P(u  1, u  2) pds.

Applying the Gronwall inequality yields w(t) p≤  w0 p+ C  t 0  u1− u  2 Bsp,r−1  u1 Bsp,r−1+ u  2 Bsp,r−1  ds  × exp  C  t 0 2 xu1(s) + ∂x2u2(s) ds  .

Thanks to the continuity dependence with respect to the initial data of the CH equation, we know that when h2 → h1in Bsp,r, w0 p+ C t 0  u1− u2 Bs−1 p,r  u1 Bs−1 p,r + u  2 Bsp,r−1 

ds tends to zero and expC0t ∂x2u1(s) + ∂x2u2(s) ds



is bounded. Then w Lt (Lp) → 0, and thus S0w L

t (Bsp,r)

C w Lt (Lp) → 0. On the other hand, due to the Bernstein inequality, and again by the continuity dependence with respect to the initial data of the CH equation, we deduce

(id − S0)w Lt (Bs

p,r)≤ C ∂xu1− ∂xu2 Lt (Bsp,r−1)→ 0.

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4. Blow-up

By exploiting the method used to prove the existence of the solution to (3.2) in Section 3, we have the following theorem:

Theorem 4.1: For any u0 ∈ Bsp,r, s > 2+ max{21,1p}, the corresponding solutions to (3.2) and (3.3)

with the same initial data u0have the same lifespan.

Proof: It is clear that the lifespan of the solution to (3.3) is at least as long as that of (3.2). This is because that once u∈ Esp,r(T) is a solution to (3.2),∂xu∈ Esp,r−1(T) is a solution to (3.3) on[0, T].

So we need to show that if v∈ Ep,rs−1(T) is the solution to (3.3) for any T> 0, then there is some

u∈ Esp,r(T) satisfying (3.2). This is also true. In the proof of Theorem 3.1, we find u by solving (3.4). Note that v∈ Esp,r−1(T) implies (1−Dx2)−1(v2+12v2x) ∈ L([0, T], Bp,rs ) and v ∈ L([0, T], Bsp,r−1).

So by Lemma 2.8, u∈ Ep,rs−1(T). As is shown in the proof, we have v = ux, which yields u∈ Ep,rs (T).

Thus the solutions to (3.2) and (3.3) have the same lifespan.

Thanks to Theorem 4.1 and Lemmas 2.11–2.13, the blow-up criteria and some blow-up results of the CH equation can be easily transferred into the ones that fit (1.6).

Theorem 4.2: Suppose that Tis the lifespan of the solution to (3.2) and T<∞. Then

 T∗ 0 uxxdt= ∞,  T∗ 0 ux B1∞,∞ dt= ∞.

Theorem 4.3: Assume that s > 5

2, and u0 ∈ Hs. If there is some point x0 such that∂x2u0(x0) >

|∂xu0(x0)|, then the solution to the Cauchy problem (3.2) blows up in finite time. Ifγ is the streamline

of the velocity field which starts from x0, then

lim

t→T 2

xu0◦ γ (t) = +∞.

Theorem 4.4: Let m = u − uxx. Assume that u0∈ H4. Then the solution to (3.2) blows up in finite

time if and only of there exist x1< x2such that∂xm0(x1) < 0 < ∂xm0(x2).

5. A few remarks

Although the local well-posedness has been proved in Section 3, we still want to introduce the following proposition which implies some kind of stability of (3.2), and also yields the uniqueness in a different way.

Proposition 5.1: Suppose that s > 2 + max{1

2,1p}, and u1, u2 ∈ Esp,r(T) are solutions to (3.4) with

the initial data h1, h2∈ Bsp,r, respectively. Then the following estimate holds:

u1− u2 Bs−1 p,r exp  −C  t 0 ∂xx u1− ∂xxu2 Bs−2 p,r dτ  ≤ h1− h2 Bs−1 p,r exp  C  t 0 ∂x u1+ ∂xu2 Bs−1 p,r dτ  , (5.1)

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Proof: Denotet

0 ∂xxu1− ∂xxu2 Bs−2

p,r dø by V

(t). Plugging u

1, u2 into equation, respectively, and

subtracting one from another, we obtain

∂t(u1− u2) −1 2(∂xu1+ ∂xu2)(∂xu1− ∂xu2) = p ∗  (∂xu1− ∂xu2)(∂xu1+ ∂xu2) +1 2(∂xxu1− ∂xxu2)(∂xxu1+ ∂xxu2)  .

By (2.3) and the product law of the Besov spaces, we have u1− u2 Bs−1 p,r exp  − V(t) ≤ h1− h2 Bs−1 p,r +  t 0 exp− V(τ) u1− u2 Bs−1 p,r u1+ u2 B s p,rdτ.

Applying the Gronwall inequality, we get (5.1).

As we know, if u∈ Bsp,r+1, then ux ∈ Bp,rs . Conversely, if v∈ Bsp,r, we may not have some u∈ Bsp,r+1

such that v= ux. Let’s denote by∂Bsp,r+1the subspace



v∈ Bsp,r∃u∈ Bsp,r+1such that v= ux



. Theorem 4.1 actually tells us that once u0belongs to the subspace∂Bsp,r+1, then the solution remains in it until

blowing up. And that the velocity field shares the same lifespan with its potential in corresponding spaces seems to be a reasonable result. We would like to point out that if the initial data u0takes on

the following shape, then (3.2) has a global solution.

The local well-posedness of (3.2) has been proved under the assumption that s > 2+ max{12,1p} by exploiting the results for the CH equation in the Besov space Btp,rwhere t > 1+ max{12,

1

p}. However,

according to [24], the local well-posedness of the CH equation also holds for B

3 2

2,1. So actually we can

deduce the results for (3.2) in B

5 2

2,1by applying the same argument in Theorem 3.1.

As mentioned before, the DP equation (1.3) is the other well-known equation which also describes the shallow water waves and is integrable and (1.5) is the other equation proposed by Novikov [41]. Rewrite it in the following form

ut − ux2= (1 − D2x)−1(3u2x).

Applying Dxto both sides of equation yields

(ux)t− 2ux∂xux = ∂xp∗ (3u2x),

which is actually the DP equation. Obviously, the same discussions in Sections 3-4 can be applied to the above two equations to get desired results.

6. Cuspon weak solutions

In this section, we intend to give a class of cuspon weak solutions to (1.4). Let’s first state the definition of weak solutions:

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Definition 6.1: u ∈ C1([0, T], C1) C([0, T], C2) is called a weak solution to (1.4) if for any

φ(x, t) ∈ C1[0, T], C∞ 0 (R)



, it satisfies the following condition:  RuT(1 − ∂ 2 x)φTdx−  Ru0(1 − ∂ 2 x)φ0dx−  T 0  Ru(1 − ∂ 2 x)φtdxdt (6.1) =1 2  T 0  Ru 2 x(1 − ∂x2)φdxdt +  T 0  Ru 2 xφdxdt + 1 2  T 0  Ru 2 xxφdxdt. (6.2)

Theorem 6.2: (1.4) has a class of weak solutions of the following form:

u=



c− cect−x, ct < x,

cex−ct− c, x ≤ ct. (6.3)

Proof: Plugging (6.3) into both sides of (6.2), we get  Ru 2 x(1 − ∂x2)φdxdt =  −∞u 2 xφdxdt −  ct c2e2ct−2x∂x2φdxdt −  ct −∞c 2e2x−2ct2 xφdxdt =  −∞u 2 xφdxdt +  ct ( − 2)c 2e2ct−2x xφdxdt +  ct −∞2c 2e2x−2ct xφdxdt − u2x∂xφ  ctct+ =  −∞u 2 xφdxdt −  ct 4c2e2ct−2xφdxdt −  ct −∞4c 2e2x−2ctφdxdt + 4c2φ(ct, t) = −  ct 3c2e2ct−2xφdxdt −  ct −∞3ce 2x−2ctφdxdt + 4c2φ(ct, t), and  Ru 2 xφdx + 1 2  Ru 2 xxφdx =  ct 3 2c 2e2ct−2xφdx +  3 2ce 2x−2ctφdx. Thus 1 2  T 0  Ru 2 x(1 − ∂x2)φdxdt +  T 0  Ru 2 xφdxdt + 1 2  T 0  Ru 2 xxφdxdt =  T 0 2c2φ(ct, t)dt.

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On the other hand,  RuT(1 − ∂ 2 x)φTdx−  Ru0(1 − ∂ 2 x)φ0dx =  RuTφTdx−  Ru0φ0dx+  R∂xuT∂xφTdx−  R∂xu0∂xφ0dx −  uT∂xφT  cTcT+ − u0∂xφ0  0− 0+  =  RuTφTdx−  Ru0φ0dx+ ∂xuTφT  cTcT+ − ∂xu0φ0  0− 0+ −   R 2 xuTφTdx−  R 2 xu0φ0dx  = −  ct c(φT− φ0)dx +  ct −∞c(φT− φ0)dx. Similarly,  Ru(1 − ∂ 2 x)φtdx = − c  ct ∂tφ(t, x)dx + c  ct −∞∂tφ(t, x)dx = − cd dt  ct φ(t, x)dx − c 2φ(t, ct) + cd dt  ct −∞φ(t, x)dx − c 2φ(t, ct). Then  T 0  Ru(1 − ∂ 2 x)φtdxdt = − c  ct (φT− φ0)dx + c  ct −∞(φT− φ0)dx − 2c 2  T 0 φ(t, ct)dt. Thus, we have  RuT(1 − ∂ 2 x)φTdx−  Ru0(1 − ∂ 2 x)φ0dx−  T 0  Ru(1 − ∂ 2 x)φtdxdt = 2c2  T 0 φ(t, ct)dt =1 2  T 0  Ru 2 x(1 − ∂x2)φdxdt +  T 0  Ru 2 xφdxdt + 1 2  T 0  Ru 2 xxφdxdt.

This completes the proof of the theorem.

Acknowledgement

The authors thank the referees for their valuable comments and suggestions.

Disclosure statement

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Funding

This work was partially supported by NNSFC [grant number 11671407], [grant number 11271382]; FDCT [grant number 098/2013/A3]; Guangdong Special Support Program [grant number 8-2015]; the key project of NSF of Guangdong province [grant number 2016A030311004].

References

[1] Camassa R, Holm DD. An integrable shallow water equation with peaked soliton. Phys Rev Lett.

1993;71(11):1661–1664.

[2] Degasperis A, Holm DD, Hone AN. A new integrable equation with peakon solutions. Theor Math Phys.

2002;133(2):1463–1474.

[3] Constantin A, Lannes D. The hydrodynamical relevance of the Camassa-Holm and Degasperis–Procesi equations. Arch Ration Mech Anal.2009;192(1):165–186.

[4] Dullin H, Gottwald GA, Holm DD. On asymptotically equivalent shallow water wave equations. Physica D.

2004;190(1):1–14.

[5] Constantin A. On the scattering problem for the Camassa–Holm equation. R Soc Lond Proc Ser A Math Phys Eng Sci.2001;457(2008):953–970.

[6] Constantin A, Gerdjikov VS, Ivanov RI. Inverse scattering transform for the Camassa-Holm equation. Inverse Prob.2006;22(6):2197–2207.

[7] Constantin A, Ivanov RI, Lenells J. Inverse scattering transform for the Degasperis–Procesi equation. Nonlinearity.2010;23(10):2559–2575.

[8] Constantin A, McKean H. A shallow water equation on the circle. Commun Pure Appl Math.1999;52(8):949–982. [9] De Monvel AB, Kostenko A, Shepelsky D, et al. Long-time asymptotics for the camassa-holm equation. SIAM J

Math Anal.2009;41(4):1559–1588.

[10] Lenells J. Traveling wave solutions of the Camassa-Holm equation. J Differ Equ.2005;217(2):393–430. [11] Lenells J. Traveling wave solutions of the Degasperis–Procesi equation. J Math Anal Appl.2005;306(1):72–82. [12] Constantin A. The trajectories of particles in stokes waves. Inventiones Math.2006;166(3):523–535.

[13] Constantin A, Escher J. Particle trajectories in solitary water waves. Bull Am Math Soc.2007;44(3):423–431. [14] Constantin A, Escher J. Analyticity of periodic traveling free surface water waves with vorticity. Ann Math.

2011;173(1):559–568.

[15] Constantin A. Edge waves along a sloping beach. J Phys A: Math Gen.2001;34(45):9723–9731. [16] Henry D. On gerstner¸a´rer wave. J Nonlinear Math Phys.2008;15(sup2):87–95.

[17] Constantin A. An exact solution for equatorially trapped waves. J Geophys Res: Oceans.2012;117(C5):C05029 (8pp).

[18] Constantin A, Germain P. Instability of some equatorially trapped waves. J Geophys Res: Oceans.

2013;118(6):2802–2810.

[19] Henry D. An exact solution for equatorial geophysical water waves with an underlying current. Eur J Mech-B/Fluids.2013;38:18–21.

[20] Henry D. Equatorially trapped nonlinear water waves in a-plane approximation with centripetal forces. J Fluid Mech.2016;804:R1.

[21] Constantin A, Escher J. Global existence and blow-up for a shallow water equation. Anal Scuola Normale Superiore Pisa-Classe Scienze.1998;26(2):303–328.

[22] Constantin A, Escher J. Well-posedness, global existence, and blowup phenomena for a periodic quasi-linear hyperbolic equation. Commun Pure Appl Math.1998;51(5):475–504.

[23] Danchin R. A few remarks on the Camassa–Holm equation. Differ Integral Equ.2001;14(8):953–988. [24] Danchin R. A note on well-posedness for Camassa–Holm equation. J Differ Equ.2003;192(2):429–444. [25] Brandolese L. Local-in-space criteria for blowup in shallow water and deispersive rod equation. Commun Math

Phys.2014;330(1):401–414.

[26] Constantin A, Escher J. Wave breaking for nonlinear nonlocal shallow water equations. Acta Math.

1998;181(2):229–243.

[27] McKean HP. Breakdown of the Camassa–Holm equation. Commun Pure Appl Math.2004;57(3):416–418. [28] Constantin A. Existence of permanent and breaking waves for a shallow water equation: a geometric approach.

Ann lnst Fourier.2000;50(2):321–362.

[29] Bressan A, Constantin A. Global conservative solutions of the Camassa-Holm equation. Arch Ration Mech Anal.

2007;183(2):215–239.

[30] Bressan A, Constantin A. Global dissipative solutions of the Camassa-Holm equation. Anal Appl.2007;5(01): 1–27.

[31] Gui G, Liu Y. On the Cauchy problem for the Degasperis–Procesi equation. Q Appl Math.2011;69(3):445–464. [32] Himonas AA, Holliman C. The Cauchy problem for the Novikov equation. Nonlinearity.2012;25(2):449–479.

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[33] Yin Z. On the Cauchy problem for an integrable equation with peakon solutions. Illinois J Math.2003;47(3): 649–666.

[34] Coclite GM, Karlsen KH. On the well-posedness of the Degasperis–Procesi equation. J Funct Anal.

2006;233(1):60–91.

[35] Escher J, Liu Y, Yin Z. Global weak solutions and blow-up structure for the Degasperis–Procesi equation. J Funct Anal.2006;241(2):457–485.

[36] Escher J, Liu Y, Yin Z. Shock waves and blow-up phenomena for the periodic Degasperis–Procesi equation. Indiana Univ Math J.2007;56(1):87–117.

[37] Liu Y, Yin Z. Global existence and blow-up phenomena for the Degasperis–Procesi equation. Commun Math Phys.2006;267(3):801–820.

[38] Liu Y, Yin Z. On the blow-up phenomena for the Degasperis–Procesi equation. Int Math Res Not.

2007;2007:rnm117.

[39] Yin Z. Global existence for a new periodic integrable equation. J Math Anal Appl.2003;283(1):129–139. [40] Yin Z. Global solutions to a new integrable equation with peakons. Indiana Univ Math J.2004;53(4):1189–1209. [41] Novikov V. Generalizations of the Camassa–Holm equation. J Phys A: Math Theor.2009;42(34):342002 (14pp). [42] Bahouri H, Chemin J-Y, Danchin R. Fourier analysis and nonlinear partial differential equations. Vol. 343. Beriln

Heidelberg: Springer-Verlag;2011.

[43] Li J, Yin Z. Well-posedness and global existence for a generalized Degasperis–Procesi equation. Nonlinear Anal: Real World Appl.2016;28:72–90.

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