Abstract
This work deals with the homogenization of two dimensions’ tidal equations. We study the asymptotic behavior of the sequence of the solutions using the sigma-convergence method. We establish the convergence of the sequence of solutions towards the solution of an equivalent problem of the same type.
MSC:
35B40; 46J10
1. Introduction
Ocean tides have been investigated by many authors, starting from [1,2]. The last decades have been marked by rapid progress in both theoretical and experimental studies of ocean tidal phenomena. Today, experimental and theoretical knowledge of ocean tides are used in order to address important problems in Oceanography, Atmospheric Sciences, Geophysics, as well as in Electronics and Telecommunications. It is important to point out that Laplace [3] was the first author to make the first major input in the theoretical formulation for tides of water on a rotating globe. Indeed, he formulated a system of partial differential equations that relate the horizontal flow to the surface height of the ocean. The existence and uniqueness of solutions of the deterministic tidal equation while using the classical compactness method have been proven in [2,4]. In our work, we consider the deterministic counterpart of a model of tidal dynamics that was studied by Manna et al. [5] and originally proposed by Marchuk and Kagan [2], where they considered the model of tidal dynamics derived by taking the shallow water model on a rotating sphere, with the latter being a slight generalization of the one considered earlier by Laplace.
Our objective is to carry out the homogenization of (2)–(5) under a suitable structural assumption on the coefficients of the operator that is involved in (2). These assumptions cover several physical behaviors, such as the periodicity, the almost periodicity, and much more. In order to achieve our goal, we shall use the concept of sigma-convergence [6], which is roughly a formulation of the well-known two-scale convergence method [7,8,9,10,11,12,13] in the context of algebras with mean value [6,14,15,16]. Therefore, our study falls within the framework of homogenization beyond the periodic setting, but including the periodic study as a special case.
The outline of the paper is as follows. The statement of the model problem, together with the derivation of appropriate uniform estimates, are the objectives of Section 2. Section 3 deals with the fundamentals of the sigma-convergence method. The homogenization process is performed in Section 4, while, in Section 5, we provide some applications of the main homogenization result.
2. Setting of the Problem and Uniform Estimates
2.1. Statement of the Problem
The tidal dynamics system that was developed by Manna et al. [5] for suitably normalized velocity and tide height z reads as
where is an open bounded subset, where and are defined by
and (the Coriolis parameter) being positive constants, a given function and .
In our work, we ignore the Coriolis parameter (), so that . However, instead of the Laplace operator, we rather consider a general linear elliptic operator of order 2 in divergence form, leading to the investigation of the limiting behavior (when ) of the generalized sequence of solution to the system (2)–(5), below
where is a Lipschitz bounded domain of and T is a positive real number. Here, and stand, respectively, for the total transport 2-D vector (the vertical integral of the velocity) and the deviation of the free surface with respect to the ocean bottom. We have chosen the Dirichlet boundary condition in order to simplify the presentation. It is worth noticing that other boundary conditions can be considered, such as the Robin one: the difficulties may be only of technical types, with the method being the same.
In (2)–(5), ∇ (resp. div) is the gradient (resp. divergence) operator in and the functions , h, , , and are constrained, as follows:
- (A1)
- The function is defined by (), where is a symmetric matrix withwhere is a given constant independent of x, y and .
- (A2)
- The operator is defined on by (), where is a given function and (for a fixed real number ), h being a continuously differentiable function satisfyingwhere is a given constant, which is equal to zero at a constant ocean depth. The functions , and are such that , , , and g is the gravitational constant.
- (A3)
- We assume further that, for all , the matrix-function has its entries in , where is an algebra with mean value on in , while stands for the generalized Besicovitch space that is associated to .
Remark 1.
The operator continuously sends into with the following properties (see ([5], Lemma 3.3)): for , we have
The assumption (A3), which depends on the algebra with a mean value , is crucial in the homogenization process. It shows how the microstructures are distributed in the medium and, therefore, allows for us to pass to the limit.
Before dealing with the well-posedness of (2)–(5), we first need to define the concept of solutions that we will deal with.
Definition 1.
In the above definition, stands for the duality pairings between any Hilbert space X and its topological dual . We also recall that the operator acts in a diagonal way, which is, for , we have
where . This being so, the following existence and uniqueness result holds.
Theorem 1.
Proof.
We note that, in the problem stated in [5], if we replace the Laplace operator by and we neglect therein the Coriolis parameter, then the proof follows exactly the lines of that of ([5], Propositions 3.6 and 3.7). □
2.2. A Priori Estimates
The following result will be useful in deriving the uniform estimates for
Lemma 1
([5], Lemma 3.1). For any real-valued smooth function φ compactly supported in , we have
The following lemma provides us with the a priori estimates.
Lemma 2.
Proof.
We first deal with Equation (2). In the variational form of (2), we choose the test function associated to (4) to obtain
By the divergence theorem, we have
Applying Young’s inequality in the form
to (19) (with ), we obtain
In (7) if we take and to get , which yields
Using again (20), but this time with , we get
Putting together (6), (21)–(23), we derive, from (18), the following
Integrating (24) with respect to t, we obtain
Next. dealing with (3), which we multiply by and then integrate the resulting equality over , we get
However,
Taking (27) into account and integrating (26) in t gives
Summing up inequalities (25) and (28), gives readily
where
and
Now, appealing to inequality (12) (in Lemma 1) and owing to the fact that , we have
so that
We are, therefore, led to
Applying the Gronwall inequality leads to
3. Fundamentals of the Sigma-Convergence Method
Here, we are concerned with the main features of the sigma-convergence method, which we define. The reader may find more details in [14,15].
We first recall that by an algebra with mean value on is meant any Banach algebra consisting of bounded uniformly contiuous functions on , satisfying
- (i)
- contains the constants;
- (ii)
- for any and ; and,
- (iii)
- for any , the limit BR u(y)dy exists and is called the mean value of u.
In (iii), above, BR is the integral mean over the open ball BR centered at 0 and of radius R: BR = |BR|−1 ∫BR.
For obvious purposes, we define the generalized Besicovitch space () associated to a given algebra with mean value , as the completion with respect to the seminorm defined on by (). It is worth noticing that is well defined, since for any and . We may also define the Banach counterpart of by cutting with the kernel of the seminorm : with .
In the current work, we assume that all of the algebras with a mean value are ergodic (see [6,17] for the definition). We also need a further space, say , which is defined, as follows:
We identify two elements of by their gradients, which is, in if . Equipped with the gradient norm , is a Banach space ([18], Theorem 3.12).
We are now able to define the concept of sigma-convergence.
Definition 2.
A sequence is said to:
- (i)
- weakly Σ-converge in to as if we havefor every , . We express this by writing in -weak Σ;
- (ii)
- We express this by writing in -strong Σ.
Remark 2.
(1) We can prove that the weak Σ-convergence in implies the weak convergence in . (2) The convergence (30) still holds true for , where , .
The following results are the main properties of sigma-convergence and they can be found in [6,14,17]. Before we can state them, we need to define what we call a fundamental sequence. By a fundamental sequence, we term any ordinary sequence (denoted here, below, by E) of real numbers satisfying and when .
- (SC)
- For , any sequence that is bounded in possesses a weakly -convergent subsequence.
- (SC)
- Let () be a bounded sequence in . Afterwards, up to a subsequence from E, there exists a couple with and , such that, as ,and
- (SC)
- Let and be such that . Assume that is weakly -convergent in to some and is strongly -convergent in to some . Subsequently, the sequence is weakly -convergent in to .
4. Homogenization Result
4.1. Passage to the Limit
First, we set
The spaces and are Hilbert spaces with obvious norms. Moreover, the imbedding is compact.
Now, in view of a priori estimates in Lemma 2, the sequences and are bounded in and in , respectively. Thus, given a fundamental sequence E, there exist a subsequence of E and a couple , such that, as ,
Using the estimates (13)–(17), it follows that there exist a subsequence of (not relabeled) and a function , such that, as ,
It follows that .
Now, for an element , we set
with . The smooth counterpart of is defined by .
Proposition 1.
Let and . Afterwards, and solve the following variational problem:
for all and .
Proof.
Let and be, as above, and define
Taking as a test function in the variational form of (2)–(5), we obtain
and
While using the identities
we infer that, as ,
Let us consider each of the Equations (39) and (40) separately. We first consider (39) and, using the convergence results (34) and (41), we obtain
Because , we use it as test function together with property (SC) (recall that we have (36) and (42)) to obtain
Let us show that
First, we have, from (34), that, up to a subsequence of not relabeled, a.e. in Q. Hence, from the continuity of , we entail
we infer, from the boundedness of the sequence , that in -weak. Putting this together with (43), we obtain (46). We also easily obtain
Next, the convergence results (35) and (43) yield
As for Equation (40), we use the weak convergence (35) that is associated to (43) to obtain
Concerning the second term in (40), we infer, from (34), that
thereby completing the proof of the proposition. □
4.2. Homogenized Problem
Here, we intend to derive the problem whose the couple is solution. In order to achieve this, we first uncouple Equation (37), which is equivalent to the system consisting of (49) and (50), below:
Choosing in (50)
we obtain
Let us deal with (52). To this end, fix and consider the corrector problem:
Subsequently, in view of the properties of the matrix , we infer, from [19,20], that (53) possesses a unique solution in . Coming back to (53) and taking there , testing the resulting equation with as in (51), we get, by the uniqueness of the solution of (53), that . This shows that belongs to . Clearly, if is the solution of (53) corresponding to (that is all of the entries of are zero, except the entry occupying the jth row and the ℓth column, which is equal to 1), then
We recall again that depends on x, as it is the case for . In the variational form of (49), we insert the value of that was obtained in (54) to obtain the equation
where , with ( the ℓth vector of the canonical basis of ) and
Additionally, Equation (38) is equivalent to
Finally, putting together the Equations (55) and (56) associated to the boundary and initial conditions, we are led to the homogenized problem, viz.
It can be easily shown that the matrix of homogenized coefficients has entries in , and it is uniformly elliptic, so that, under the conditions (A1)–(A2), the problem (57) possesses a unique solution with and . Because the solution of (57) is unique, we infer that the whole sequence converges in a suitable space towards , as stated in the following result, which is the main result of the work.
Theorem 2.
Proof.
The proof is a consequence of the previous steps. □
5. Some Concrete Applications of Theorem 2
The homogenization of problem has been made possible under the fundamental assumption (A3). Some of the physical situations that lead to (A3) are listed below.
Problem 1 (Periodic Homogenization).
The homogenization of (2)–(5) holds under the periodicity assumption that the matrix-function is periodic with period 1 in each coordinate, for any . In that case, we have , where and is the algebra of continuous Y-periodic functions defined in . It is easy to see that is Y-periodic}, and the mean value expresses as . Hence, the homogenized matrix is defined by , with ( the ℓth vector of the canonical basis of ) and
where, here, is the solution of the cell problem
with , and .
Problem 2 (Almost periodic Homogenization).
We may consider the homogenization problem for (2)–(5) under the assumption that the coefficients of the matrix are Besicovitch almost periodic functions [21]. In that case, hypothesis (A3) holds true, with , where is the algebra of Bohr almost periodic functions on [22]. The mean value of a function is the unique constant that belongs to the close convex hull of the family of the translates .
Problem 3 (Weakly almost periodic Homogenization).
Author Contributions
G.C., A.F. and J.L.W. contributed in writing the original draft. All authors have read and agreed to the published version of the manuscript.
Funding
This research received no external funding.
Acknowledgments
The third author is very grateful to the Alexander von Humboldt Foundation for the Equipment’s Grant he received.
Conflicts of Interest
The authors declare no conflict of interest.
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