Well-posedness of the initial value problem for the Ostrovsky-Hunter equation with spatially dependent flux
Giuseppe Maria Coclite, Neelabja Chatterjee, Nils Henrik Risebro

TL;DR
This paper establishes the well-posedness of the initial value problem for the Ostrovsky-Hunter equation with a spatially dependent flux, proving existence and uniqueness of entropy solutions under certain smoothness conditions.
Contribution
It extends the analysis of the Ostrovsky-Hunter equation to flux functions depending on space, providing new existence and uniqueness results.
Findings
Existence of entropy solutions under smoothness conditions.
Uniqueness of solutions via doubling of variables.
Use of compensated compactness for existence proof.
Abstract
In this paper we study the Ostrovsky-Hunter equation for the case where the flux function may depend on the spatial variable with certain smoothness. Our main results are that if the flux function is smooth enough (specified later), then there exists a unique entropy solution. To show the existence, after proving some a priori estimates we have used the method of compensated compactness and to prove the uniqueness we have employed the method of doubling of variables.
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Wellposedness of the initial value problem for the Ostrovsky-Hunter Equation with spatially dependent flux
G. M. Coclite
Dipartimento di Meccanica, Matematica e Management
Politecnico di Bari
Via E. Orabona 4
70125 Bari, Italy
,
N. Chatterjee
Department of mathematics
University of Oslo
P.O. Box 1053, Blindern
N–0316 Oslo, Norway
and
N. H. Risebro
Department of mathematics
University of Oslo
P.O. Box 1053, Blindern
N–0316 Oslo, Norway
Abstract.
In this paper we study the Ostrovsky-Hunter equation for the case where the flux function may depend on the spatial variable with certain smoothness. Our main results are that if the flux function is smooth enough (namely is uniformly Lipschitz locally in and is uniformly bounded), then there exists a unique entropy solution. To show the existence, after proving some a priori estimates we have used the method of compensated compactness and to prove the uniqueness we have employed the method of doubling of variables.
2010 Mathematics Subject Classification:
Primary: 35L35, 35G25; Secondary: 45M10
This project has received funding from the European Union’s Horizon 2020 research and innovation programme under the Marie Skłodowska-Curie grant agreement No 642768 for NC’s work and GMC’s work was supported by the Research Council of Norway (project 250674/F20). GMC is member of the Gruppo Nazionale per l’Analisi Matematica, la Probabilita’ e le loro Applicazioni (GNAMPA) of the Istituto Nazionale di Alta Matematica (INdAM). This work was initiated while GMC visited Department of Mathematics at the University of Oslo. He is grateful for Department’s financial support and excellent working conditions.
1. Introduction
To model numerous physical phenomena such as the propagation of undular bores in shallow water, the flow of liquids containing gas bubbles, the propagation of waves in an elastic tube filled with a viscous fluid, weakly nonlinear plasma waves with certain dissipative effects etc. the following nonlinear evolution equation, known as Korteweg-deVries-Burgers equation
[TABLE]
has been extensively investigated in the recent years (see [17, 23, 30] and references therein). Also considering the effects of background rotation through the Coriolis force ( being the force parameter and is the linear shallow water speed) (1.1) takes the following form
[TABLE]
To model small-amplitude long waves in a rotating fluid of finite depth [27] and to study long internal waves in a rotating fluid [20] both the viscous dissipation term and the high-frequency dispersion term has to be dropped, i.e. ; which leads to
[TABLE]
which is known as the Ostrovsky-Hunter equation, as Ostrovsky also independently derived them [27]. This equation is also used to model high frequency waves in a relaxing medium [33]. In the cases described above the flux is considered to be of Burger’s type, i.e. .
Also by including the effects of background rotation in the shallow water equation, and then using singular perturbation methods (1.3) has been derived previously (see [15], [21]). In the recent years enormous amount of research has been carried out investigating (1.3). Among those works in [27], [29], [31] the equation (1.3) is also known as the reduced Ostrovsky equation, in [20] it is called short wave equation, whereas in [4], [5] (1.3) is known as Ostrovsky-Vakhnenko equation and as Vakhnenko equation in [34]. Moreover, the equation (1.2) is used to model ultra short light pulses in silica optical fibres (see [2], [25]), in which case . In this case equation (1.2) is sometimes referred to as the short-pulse-equation.
In his seminal paper [20], Hunter showed the connection between the KdV equation (1.2) and the Ostrovsky-Hunter equation (1.3) as the no-rotation and no-long wave dispersion limits of the same equation. When the oceanic waves approach shore, the waves usually propagate through a background with varying properties. It is natural to expect the linear phase speed of the wave which encoded in the flux function, in such a variable medium, should have a spatial dependecy. In the context of KdV equation, Johnson [22] for water waves and Grimshaw [18] for internal waves derived the variable coefficient equation (see also [19] for a detailed review). Motivated by this, it is immediate to pose the question of design and analysis of numerical scheme for the Ostrovsky-Hunter equation with a spatial dependency in the flux function. In [6], we investigated the spatially dependent Ostrovsky-Hunter equation in the fully-discretized setting to prove convergence of the corresponding numerical method to the unique entropy solution and we proved its order of convergence. Whereas in this paper, our aim is to establish well-posedness of the problem in continuous set up.
The results obtained in this paper are the following. If the function is uniformly Lipschitz continuous locally in , the function to be uniformly locally bounded, and the initial data are square integrable and satisfy zero-mean condition, then there exists an entropy solution via method of compensated compactness. Furthermore, for two entropy solutions and , with initial data and respectively, we establish the following estimate
[TABLE]
for some constants to be specified later. The rest of this paper is organized as follows. In Section 2 we give detailed descriptions of the notations used, the precise assumptions of the regularity of the flux funxtion and the initial data. Also, apart from stating our main result as a theorem, we state the definition of entropy solution to be used. In Section 3 we prove few useful a priori estimates (namely energy estimate and bound) for the purpose of compensated compactness technique. In Section 4 we first state the two results due to Murat and Tartar in the form of two lemmas, using which we will employ a compensated compactness argument to show the existence of entropy solution of the equation under consideration. Moreover, we establish an contraction type estimate mentioned above using the technique of doubling of variables.
2. Preliminaries and Notation
Throughout this paper is the conserved quantity and is the flux which is dependent on the spatial variable and , denoted by . For notational consistency, we mention the following chain rule keeping the notation of
[TABLE]
We are interested in the initial boundary value problem for (1.3), but with spatially dependent flux, and hence we augment the equation with the initial datum
[TABLE]
Keeping that in mind, following the works of [10], [7] and [35] integrating the equation (1.3) on the interval we get the integro-differential formulation of the problem under consideration and setting ,
[TABLE]
Denoting , we get the following equivalent formulation
[TABLE]
For the initial datum, we assume the following zero-mean condition and regularity assumption respectively
[TABLE]
and
[TABLE]
where will be denoting the unbounded positive half line throughout the paper. Similarly will be used to denote . Also the flux is assumed to satisfy the following hypothesis:
- (A1)
is genuinely nonlinear, i.e. for a.e. and for all , 2. (A2)
a constant such that and for all , 3. (A3)
a constant such that , for all , 4. (A4)
a constant such that , for all .
Even if the initial data is smooth enough, solutions of (2.3) generically develop discontinuities. Hence solutions must be considered in the weak sense. A function is a weak solution of (2.3) if
[TABLE]
for all test functions . Moreover, from (2.3) we have that
[TABLE]
Following [3] we define entropy solutions as
Definition 1** (Entropy Solution).**
We say that u\in L^{\infty}_{\mathrm{loc}}\Big{(}\Pi\Big{)} is an entropy solution of the initial boundary value problem (2.3), if
- •
* satisfies (2.6) ;*
- •
for every smooth, non negative test function and
[TABLE]
As an immediate consequence of (2.7) if a map satisfies the following equivalent entropy inequality for every convex entropy/entropy flux pair (i.e. for )
[TABLE]
in the sense of distributions, then by Theorem of [13] on the boundary strong trace exists. By a standard approximation argument equivalently any convex entropy/entropy flux pair in (2.9) can be replaced by Kružkov entropy pair namely for , and . The main result of this paper is the following theorem.
Theorem 2**.**
Assuming (2.4) and (2.5), the Cauchy problem (2.2), or equivalently (2.3) possesses a unique entropy solution in the sense of Definition 1. Moreover, if and are two entropy solutions of (2.2), or equivalently (2.3) in the sense of Definition 1, the following estimate holds for a given
[TABLE]
for almost every , and being the bound , where the constant depends on , , and .
Before proceeding to prove this theorem, it is worth mentioning that Coclite et al. [10], [7] have showed the well-posedness of the initial-boundary value problem and the Cauchy problem for the Ostrovsky-Hunter Equation (2.2), but without any spatial dependency in the flux. Throughout the next section we will extend their results following the papers cited just above.
3. A-Priori Estimates
The existence argument is based on passing to the limit in the following vanishing viscosity approximation of (2.3) (see [11]). Fix a small number , and let be the unique classical solution of the following problem
[TABLE]
where is a approximation of such that
[TABLE]
and on the viscous source term for we assume that
[TABLE]
Clearly, (3.1) is equivalent to the integro-differential problem
[TABLE]
The existence of such solutions can be obtained by fixing a small number and considering the further approximation of (3.4) (see for the whole real line [7, 10]; for the half line [8, 9, 11] and the references therein). We are going to use the following result from previous works of Coclite et al. (see [7, 12] and references therein).
Theorem 3**.**
Let . Assuming that conditions (3.2) and (3.3) hold, there exists a unique classical solution to the Cauchy problem of (3.4) such that
[TABLE]
Now let us prove some a priori estimates on .
Lemma 4**.**
We have the equivalence of following two equalities
[TABLE]
Proof.
Let . First we will prove that (LABEL:eq:ViscousZeroMeanCondition) implies (3.7). Multiplying equation (3.4) by we get
[TABLE]
In this equality, consider the term . We are going to show that after integration this term vanishes. Clearly the equation (LABEL:eq:ViscousZeroMeanCondition) implies that
[TABLE]
Using into (3.8) we get
[TABLE]
Integrating this expression over and invoking (3.9) we get
[TABLE]
And finally integrating over the we obtain
[TABLE]
which proves (3.7). Now we are going to prove the opposite implication. Assume that for some , which implies
[TABLE]
which results in
[TABLE]
ultimately contradicting our assumption (3.7). This concludes the proof. ∎
Lemma 5**.**
For each , (LABEL:eq:ViscousZeroMeanCondition) holds. In particular we have that for a constant coming from (A2), independent of
[TABLE]
where is any constant greater than .
Proof.
From the equation (3.4) we have
[TABLE]
Integrating both sides with respect to we get
[TABLE]
Observe that from of (3.1) we have which, due to (A1)
[TABLE]
Invoking the property (A1), (3.12) and the smoothness of from Theorem 3 we can conclude , which proves (LABEL:eq:ViscousZeroMeanCondition). So by Lemma 5 the relation (3.7) holds. To estimate the last term of the relation (3.7) due to our assumption (A2) for any constant we get
[TABLE]
Consequently in (3.7) inserting (3.2) and (3.13) we have:
[TABLE]
which concludes the proof. ∎
Remark 6**.**
It follows from (5) that
[TABLE]
Thus by an application of Gronwall’s inequality, we have
[TABLE]
Lemma 7**.**
The family
[TABLE]
And consequently the family
[TABLE]
Proof.
By Hölder inequality we have the following estimate
[TABLE]
Now assume and be the solutions of the following equations respectively
[TABLE]
[TABLE]
Then and are respectively a solution, a supersolution, and a subsolution of the parabolic problem (3.4). Following [16, Theorem , Chapter ] we have that . Moreover from [1], and are uniformly bounded in . Define the following two functions:
[TABLE]
Clearly therefore and they satisfy the inequality
[TABLE]
This proves (3.15).
Now since |P_{\epsilon}(t,x)|=\Big{|}\int_{0}^{x}u_{\epsilon}(t,y)dy\Big{|}\leq\int_{0}^{x}|u_{\epsilon}(t,y)|dy, (3.16) follows from (3.15). This completes the proof. ∎
4. Proof of the Main Theorem
In this section we prove Theorem 2. Using the compensated compactness method, (see [32, 28]) we are going to construct a solution of (2.2) or equivalently of (2.3) by passing to the limit in sequence of the viscosity approximations (3.1). The compensated compactness method due to Panov (see Theorem of [28], or Lemma of [14]) to be used here can be stated as the following lemma
Lemma 8**.**
Let be a family of functions defined on . If is uniformly bounded in and the family is compact in for every convex , where . Then there exist a sequence , as , and a map such that a.e. and in , as .
The following compact embedding result of Murat [26] will be also used,
Lemma 9**.**
Let be a bounded open set of , . Suppose that the sequence of distributions is bounded in . In addition, suppose that ; where lies in a compact subset of and lies in a bounded subset of . Then lies in a compact subset of .
First we are going to extract a limit function from the collection and then we are going to show that this satisfies (• ‣ 1).
Lemma 10**.**
The family has a subsequence and a limit function such that
[TABLE]
Moreover, we have
[TABLE]
where
[TABLE]
Moreover, (• ‣ 1) is satisfied.
Proof.
Let . Multiplying the equation (3.4) by , we get
[TABLE]
which can be rewritten as
[TABLE]
From the definition of we have . Inserting this into the above expression we get
[TABLE]
This can be written as
[TABLE]
From Lemma 5 we have
[TABLE]
To show is uniformly bounded in , let be any bounded subset of . Then, by Lemma 7,
[TABLE]
So it remains to show that and are uniformly bounded in . To that end observe that
[TABLE]
So is uniformly bounded in . Similarly we have
[TABLE]
Consequently, is uniformly bounded in .
Therefore, by Lemma 9 we can conlcude that
[TABLE]
Therefore using the bound obtained from Lemma 7, (4.4) and Lemma 8 we can conclude that there exists a subsequence and a limit function such that (4.1) holds. By the Hölder inequality and the definition of , (4.2) follows from (4.1).
We remark that the entropy inequality (2.9) can be obtained from (10) by the standard argument of letting and using convexity of . Thus by [13, Theorem ], strong trace for on does exist. Now we are going to prove (• ‣ 1). From the Definition 1 for (3.4) and using (2.9) we get for Krǔzkov entropy/entropy flux pair
[TABLE]
Multiplying by a non-negative test function and integrating over , we get
[TABLE]
Invoking Lemmas 5, 7, and 10, letting , we have
[TABLE]
Consequently to show (• ‣ 1) it is enough to prove that
[TABLE]
In order to prove this we need to employ a particular choice of test function. Let be a sequence of non-negative test functions satisfying
[TABLE]
Multiplying the equation (3.4) by the test function we get after an integration by parts
[TABLE]
Employing the strong convergence from Lemma 10, passing to the limit , respectively and using the properties of in the above relation (10) we get
[TABLE]
which in turn proves (4.6). Combining (10) and (4.6) we have obtained the desired inequality (• ‣ 1).
This completes the proof. ∎
Consequently we have established the existence of an entropy solution (in the sense of Definition 1) of the equation (2.2) or equivalently of (2.3). Now in order to prove the uniqueness of entropy solutions we are going to prove (2.10), i.e. we will prove Theorem 2.
Proof.
(of Theorem 2 :) Let and be two entropy solutions of (2.2) or equivalently (2.3). We will use the doubling of variables. For and let be a non-negative test function. Since and are entropy solutions of (2.3), we have
[TABLE]
and
[TABLE]
Then integrating (4) with respect to , ; (4) with respect to , ; and adding the two outcomes we obtain,
[TABLE]
For as , where is the Dirac mass concentrated at [math], where
[TABLE]
for some non-negative with total mass being . Now let us define the particular test function
[TABLE]
where is a non-negative, test function. Inserting the function (4.13) into the last inequality (4), we get
[TABLE]
By standard limiting argument of doubling of variable technique, passing to the limit as we obtain from the previous inequality (4) that for all test functions as mentioned above,
[TABLE]
Following Kružkov’s argument [24] if we consider the sets for ,
[TABLE]
and define the following non-negative test function
[TABLE]
where is defined in (4.12) and is defined in (A4). Clearly observe that is an approximation of the characteristic function of . From definition . Using as the test function in (4) and similarly as before letting , we get
[TABLE]
With
[TABLE]
note that
[TABLE]
Since
[TABLE]
and,
[TABLE]
We consider the following continuous function:
[TABLE]
Then we can combine (4), (4), (4) and (4.21) to obtain
[TABLE]
Consequently, by Gronwall’s inequality we can conclude:
[TABLE]
i.e.
[TABLE]
Consequently we have the estimate (2.10), namely
[TABLE]
where the constant depends on , , and .
This completes the proof. ∎
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