Abstract
We study a Camassa–Holm-type equation with a prescribed, time-independent bottom profile, The model is considered here as a mathematically motivated bottom-modified Camassa–Holm equation. The bottom modifies the transport velocity and the lower-order term is chosen so that the basic momentum balance keeps the same cancellation structure as in the flat-bottom case. We clarify the meaning of a gentle bottom in terms of bounded multiplier norms of the prescribed profile and do not claim a complete asymptotic derivation from the Euler equations. Under suitable regularity assumptions on h, we prove local well-posedness in Sobolev spaces by verifying the hypotheses of Kato’s quasilinear semigroup theorem. We also derive an momentum identity and a continuation criterion based on the integrability of . The proof of the continuation criterion is strengthened by combining the momentum bound with a high-order energy estimate.
1. Introduction
The Camassa–Holm equation
is an important nonlinear dispersive equation arising in shallow-water theory. It has been extensively studied due to its remarkable mathematical structure, including complete integrability, peaked solitary waves, and wave-breaking phenomena. It also plays a significant role in the asymptotic description of unidirectional water waves [1,2,3,4].
In many realistic situations, wave propagation occurs over a non-flat bottom. Bottom topography can affect the wave speed, the dispersive properties, and the balance between nonlinear and dispersive effects. This motivates the study of Camassa–Holm-type models in which the flat-bottom structure is perturbed by prescribed spatially varying coefficients. Variable-depth shallow-water models and related asymptotic approximations have been studied in different regimes, and these works show that topography generally enters through modified transport, variable coefficients, and additional lower-order terms [5,6,7,8].
The aim of the present work is more modest than a complete physical derivation from the full water-wave problem. We introduce and analyze the following mathematically motivated bottom-modified Camassa–Holm-type equation:
where is a prescribed time-independent spatial coefficient, motivated by a fixed bottom profile. The term h modifies the transport velocity, while the lower-order term is included in order to preserve a favorable cancellation in the basic momentum identity. Thus, Equation (2) should be understood as a mathematically defined bottom-modified Camassa–Holm equation designed to retain a tractable quasilinear and energy structure. We do not claim that (2) is derived from the Euler water-wave equations or that it is the unique asymptotic model associated with a variable-depth regime.
To avoid any ambiguity, the results of this paper are formulated as a purely mathematical study of the class of equations represented by (2). The terminology “bottom” and “topography” is used only to motivate the fixed coefficient h; all theorems below depend solely on the stated Sobolev and multiplier assumptions. The coefficient in front of is therefore part of the model definition and is chosen to preserve the momentum cancellation. Other coefficients, or a model derived by a different asymptotic procedure, would require a separate analysis.
We also clarify the terminology used in the paper. In this work, “gentle bottom” is a technical mathematical assumption, not a small-amplitude physical scaling. More precisely, for the local theory at the index , a technical gentle bottom means
Thus h has bounded derivatives up to the order required by the Sobolev estimates, and multiplication by and is continuous on the spaces used below. No smallness condition such as is used in the proofs. If one wants to interpret h as a physically gentle bottom, then an additional small-slope assumption may be imposed, but it is not needed for the mathematical well-posedness and continuation results established here. The constants in the estimates depend on the bounded multiplier norm of h, not on smallness of .
The main contribution of this paper is the rigorous local well-posedness analysis of (2). We rewrite the equation as a quasilinear evolution equation of Kato type and verify the required semigroup, Lipschitz, and source estimates. In response to the technical issues raised by the referees, the proof of the nonlinear Lipschitz estimate is now written in full at both the and levels, and the continuation criterion is justified by a high-order energy estimate rather than only by the momentum bound. The continuation criterion has the classical form familiar from the flat-bottom Camassa–Holm theory; it is included to show that the prescribed bottom coefficient does not destroy this standard continuation mechanism, and no independent novelty claim is made for the criterion itself.
The first main result is the following local well-posedness theorem.
Theorem 1
(Local well-posedness). Let and assume that . For every , there exists a maximal time and a unique solution u to (2) such that
Moreover, the data-to-solution map is continuous from into
The second result is a continuation criterion. As noted above, this criterion has the same form as in the flat-bottom Camassa–Holm theory. Its role here is to make explicit that the added bounded coefficient h does not introduce a different breakdown mechanism under the assumptions of the theorem.
Theorem 2
(Continuation criterion). Let u be the solution given by Theorem 1, defined on its maximal interval of existence . If
then the solution can be continued beyond . Equivalently, if , then necessarily
We also derive the following a priori momentum estimate.
Proposition 1
Remark 1
(conditional global continuation). If the corresponding solution satisfies
then Theorem 2 excludes finite-time breakdown and hence the maximal existence time is infinite. This observation is only a direct consequence of the continuation criterion and is not stated as an independent corollary or as a new global-existence theorem.
The paper is organized as follows. In Section 2, we recall the analytical tools needed for the local theory. In Section 3, we rewrite the equation in quasilinear form and check the algebra leading to the source term. In Section 4, we prove local well-posedness by verifying Kato’s hypotheses. In Section 5, we establish the momentum estimate, the continuation criterion, and the conditional global continuation statement.
2. Preliminaries
We first recall two standard tools used throughout the paper.
Lemma 1.
If , then is an algebra. Moreover,
Lemma 2.
Let . Then
where .
We shall also use the following multiplier estimate. If and , then multiplication by a is bounded on ; in particular,
This estimate is used for the fixed coefficients and .
We use the following standard Kato-type local well-posedness theorem for quasilinear evolution equations. The formulation below records explicitly the domain, density, range and Lipschitz assumptions used in the proof.
Lemma 3.
The solution depends continuously on the initial data, and it can be continued as long as its Y-norm remains finite. This is the form of Kato’s theorem applied below with and ; see Kato [9,10].
Let Y and X be Hilbert spaces with continuously and densely. Consider
Assume that for every bounded subset the following conditions hold.
- (i)
- For each , is a densely defined operator on X with domain , and generates a -semigroup on X with a growth bound depending only on B. Equivalently, the usual quasi-m-accretivity and range condition hold for sufficiently small .
- (ii)
- The map is locally Lipschitz from Y into .
- (iii)
- The source term f is locally Lipschitz from Y to X and from Y to Y.
- Then, for each , there exists a time and a unique solution
3. Quasilinear Formulation
Let
Since , Equation (2) becomes
Applying , we obtain
Using the identity
and the fact that , the commutator term can be simplified to obtain
Therefore Equation (2) can be rewritten as
where
and
For completeness, we give the algebra leading to the simplified expression for f. Since
we compute
Moreover,
and
Adding the three contributions gives
4. Local Well-Posedness
In this section, we prove Theorem 1 with
Lemma 4.
Let and . For each , the operator
with domain , is quasi-m-accretive on . In particular, generates a -semigroup on .
Proof.
For ,
We decompose
Hence,
By the commutator estimate and the multiplier bound for the fixed function h,
Therefore,
For the second term, integration by parts gives
Hence,
The operator is densely defined because is dense in . Together with the standard closedness and range properties for first-order transport operators with coefficient , this quasi-accretivity implies, by the Lumer–Phillips theorem in the form used in Kato’s framework, that generates a -semigroup on . □
Lemma 5.
Let . Then
and for all ,
Proof.
Since
Lemma 1 yields
□
Lemma 6.
Proof.
First we prove the Lipschitz estimate in . Since is bounded, it is enough to estimate in . Whenever a product is first estimated in , we use explicitly the continuous Sobolev embedding . On a ball , we have
and
For , write
Since , the product estimate gives
For , write
Again using , the Sobolev product estimate first gives a bound in . The embedding then yields
Combining the estimates and applying yields
We now prove the Lipschitz estimate in . Since is bounded, it is enough to estimate the same quantities in . The terms containing h are controlled by the multiplier estimate (6):
and
For , the algebra property of gives
For , using
we obtain, because is an algebra and ,
Therefore,
The two estimates (11) and (12) verify the required local Lipschitz properties. □
Proof of Theorem 1.
The embedding is continuous and dense. Lemma 4 verifies the semigroup generation hypothesis for on . Lemma 5 verifies the local Lipschitz property of A from to . Lemma 6 verifies the required local Lipschitz properties of the source map f in both the X and Y topologies. Hence all hypotheses of Kato’s theorem, Lemma 3, are satisfied, and the Cauchy problem is locally well-posed in . □
5. A Priori Estimate, Continuation, and Conditional Global Continuation
Proof of Proposition 1.
We next establish the high-order estimate needed for the continuation criterion.
Lemma 7.
Proof.
Apply to (7), take the inner product with , and use the usual commutator decomposition for the transport term. We get
The transport term satisfies
For the source term, we separate the classical Camassa–Holm part and the bottom part. The classical part may be written as
Since is bounded,
We estimate the two terms separately, without using to control the high Sobolev norm. By the product estimate,
while
Therefore,
The bottom-dependent terms are estimated using (6):
Combining the preceding bounds gives (13). □
Proof of Theorem 2.
Let be the maximal existence time given by Theorem 1. By the local theory, the solution can be continued as long as its norm remains finite.
Assume that
By Proposition 1, remains bounded on . Since , the norm is equivalent to . Therefore,
Using Lemma 7, we then obtain
where C is finite on . Gronwall’s lemma gives
Thus the continuation principle from the local well-posedness theorem allows the solution to be extended beyond , contradicting maximality. Hence, if , one must have
□
6. Conclusions
We studied a mathematically motivated Camassa–Holm-type equation with a prescribed gentle bottom. The bottom profile enters the model through a variable transport velocity and a lower-order term chosen to preserve a useful momentum cancellation. We clarified that the model is not presented as a full asymptotic derivation from the Euler water-wave equations; rather, it is a purely mathematical bottom-modified Camassa–Holm equation designed for rigorous Sobolev analysis. Under the uniform assumption , , we proved local well-posedness by verifying Kato’s semigroup hypotheses, including the full and Lipschitz estimates for the source term. We also established a momentum identity and a continuation criterion based on . The conditional global statement is now presented only as a remark following the continuation criterion and is not intended as an independent global-existence theorem.
Future work may include deriving related models from a systematic asymptotic expansion over variable bottom, studying sharper blow-up criteria, and identifying additional sign or smallness conditions on the initial momentum and bottom profile that lead to genuine global existence results.
Author Contributions
Conceptualization, S.I. and C.G.A.; methodology, S.I., C.G.A. and B.A.Y.A.; formal analysis, S.I., C.G.A. and B.A.Y.A.; investigation, S.I., C.G.A. and B.A.Y.A.; writing—original draft preparation, S.I. and C.G.A.; writing—review and editing, S.I., C.G.A. and B.A.Y.A. All authors have read and agreed to the published version of the manuscript.
Funding
This research received no external funding.
Institutional Review Board Statement
Not applicable.
Informed Consent Statement
Not applicable.
Data Availability Statement
No new data were created or analyzed in this study. Data sharing is not applicable to this article.
Acknowledgments
The authors thank the reviewers for their careful reading and constructive comments, which helped improve the manuscript.
Conflicts of Interest
The authors declare no conflicts of interest.
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