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Radu Precup
Tiberiu Popoviciu Institute of Numerical Analysis, Romanian Academy, Romania
Department of Mathematics, Babes-Bolyai University, Cluj-Napoca, Romania
Andrei Stan
Tiberiu Popoviciu Institute of Numerical Analysis, Romanian Academy, Romania
Department of Mathematics, Babes-Bolyai University, Cluj-Napoca, Romania
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[1,3]Andrei Stan These authors contributed equally to this work. [1] Faculty of Mathematics and Computer Science, Babeș-Bolyai University, Cluj-Napoca, 400084, Romania
2] Institute of Advanced Studies in Science and Technology, Babeş-Bolyai University, Cluj-Napoca, 400110, Romania
3] Tiberiu Popoviciu Institute of Numerical Analysis, Romanian Academy, Cluj-Napoca, 400110, Romania
MSC Classification]35J91, 35J60, 37N10, 35B45, 35B33
Existence, uniqueness, and localization results for a Dirichlet problem in geophysics
Abstract
In the present paper, we investigate the existence, uniqueness, and localization of solutions for a recently derived model for gyres, formulated as a Dirichlet problem. This problem is studied from two perspectives. In the first part, we establish the existence and uniqueness of a weak solution by means of the Minty–Browder theorem. For the nonlinear term, we assume a suitable monotonicity condition together with an exponential growth condition. Here, the growth condition is admissible since the problem is posed in dimension two, which allows us to use the Trudinger–Moser inequality. In the second part, we prove the existence of a localized positive solution within a conical annular region by means of the Moser–Harnack inequality. This approach also yields multiplicity results when the required conditions are satisfied on disjoint sets. From a physical perspective, an upper bound for the solution reflects the dynamical intensity of the flow, while a lower bound indicates the persistence of ocean circulation in a given region. These bounds are determined by the behavior of the vorticity function.
keywords
Geophysical flow, ocean gyre, Minty-Browder, Trudinger-Moser inequality, Moser-Harnack inequality, exponential growthpacs
[1 Introduction and Preliminaries
In this paper, we study a recently derived model describing oceanic gyres, introduced in [1]. Gyres are large-scale geophysical circulatory flows generated by ocean currents that rotate around a central region. Such flows occur only north and south of the Equator, since near the Equator the dynamics of the oceanic flow have a peculiar behavior (see [2, 3, 4, 5, 6, 7, 8]). Oceanic gyres are driven by gravitational effects combined with Coriolis forces from the Earth’s rotation, and by wind stress acting on the ocean surface.
An important feature of gyre dynamics is that the ratio between the vertical and horizontal velocities is typically of order [9], so the vertical motion can be neglected. Introducing a stream function, as in [1], to describe the horizontal component of the flow, the dynamics can be viewed as those of shallow-water flows on a rotating sphere, making a formulation in spherical coordinates natural. Using a stereographic projection, the model can subsequently be transformed from spherical coordinates into a planar partial differential equation subject to Dirichlet boundary conditions.
In the following, we briefly recall the derivation of the model presented in [1]. Let denote the polar angle (so that represents the usual latitude, with corresponding to the North Pole), and let denote the longitude (azimuthal) angle. In terms of the stream function , the horizontal gyre flow on the spherical Earth has the azimuthal and polar velocity components given by
Letting denote the stream function associated only with the oceanic vorticity (neglecting the effect of the Earth’s rotation), one has
where is the nondimensional Coriolis parameter. Then, the governing equation for the gyre flow takes the form
| (1) |
where the term represents the oceanic vorticity, while corresponds to the planetary vorticity generated by the Earth’s rotation. The total vorticity of the flow is therefore the sum of the oceanic contribution and the spin vorticity . Typically, the oceanic vorticity is one order of magnitude larger than . While the planetary vorticity is prescribed, the function depends on the type of geophysical flow under consideration; for instance, corresponds to irrotational flows.
Equation (1) can be transformed from spherical coordinates into an equivalent planar equation (see [1]) by means of the stereographic projection of the unit sphere centered at the origin, projected from the North Pole onto the equatorial plane:
where are polar coordinates. Under this transformation, equation (1) becomes
where and are the Wirtinger derivatives. Passing to Cartesian coordinates, this equation is equivalent to the semilinear elliptic equation
| (2) |
where denotes the Laplace operator. The flow at the surface of the gyre is determined by solutions of (2) in a planar region bounded by two level sets of the stream function; therefore, equation (2) is supplemented with Dirichlet boundary conditions, i.e., on .
Sufficient conditions for problem (3) to admit a unique solution are given in [10]. The existence of radial solutions for problem (3) has also been studied in the literature [11, 12, 13], using various fixed point techniques, such as the Leray–Schauder principle or Krasnosel’skii’s fixed point theorem.
The initial flow is considered in the Southern Ocean, within a region bounded away from both the South Pole and the Equator. After the transformation to Cartesian coordinates described above, the domain is mapped onto a planar domain . Since the stereographic projection maps the entire southern region of the sphere into the unit disk, and the analysis is restricted to this region, there exist constants such that
In this paper, we study the existence, uniqueness, and localization of a solution to equation (2) in a bounded domain subject to the Dirichlet boundary condition. First, in Subsection 2.1, we establish the existence and uniqueness of a weak solution by means of the Minty–Browder theorem assuming that satisfies a monotonicity property and, using the Trudinger–Moser inequality, only an exponential growth condition, which is more general than assuming polynomial type growth.
Later, in Subsection 2.2, we use the weak Moser–Harnack inequality to provide sufficient conditions for the existence of a positive solution in a conical annular region. This localization result immediately yields multiple solutions, provided that the function is oscillatory.
From a physical perspective, an upper bound for the stream function provides quantitative control on its amplitude, while a lower bound prevents it from approaching a trivial state in the region under consideration. In particular, the latter indicates the persistence of a nontrivial circulation in that region. These bounds are determined by the behaviour of the vorticity function. We emphasize, however, that bounds on the stream function do not directly yield bounds on the corresponding velocity field, which depends on its spatial derivatives.
We conclude this section by recalling some fundamental results in nonlinear analysis that will be used in the proof of our main results. See [14, 15, 16, 18, 17, 19, 20] for details and applications in other contexts.
The first one is the celebrated result of Trudinger and Moser, which essentially states that is continuously embedded into the Orlicz space with when is a bounded domain with smooth boundary. More precisely, the following result holds (see [21, Theorem 2], [22, Theorem 1]).
Theorem 1 (Trudinger–Moser).
Let be a bounded domain with smooth boundary. Then, for every , one has for all . Moreover, there exists a constant such that
This estimate is sharp in the sense that the corresponding supremum is infinite whenever .
Our second tool is the Minty–Browder theorem for strongly monotone operators (see, for example, [23, 24]).
Theorem 2 (Minty–Browder).
Let be a separable and reflexive Banach space, and let be a hemicontinuous and strongly monotone operator, i.e., there exists such that
where denotes the duality pairing between and . Then is bijective.
Another useful result in our analysis is the local Moser-Harnack inequality [25]; see also [26, Theorem 8.26] and [27, 28].
Theorem 3.
Let be a bounded domain, and let be a subdomain such that . For any , there exists a constant , depending only on , , and , such that for every nonnegative superharmonic function in (that is, in ), the following estimate holds:
2 Main results
In this section we present the main results concerning the existence, uniqueness, localization, and multiplicity of solutions to the boundary value problem
| (3) |
where is a domain from , , and the functions are defined by
Let us denote
Then problem (3) can be written as
| (4) |
By a weak solution of (4) we mean a function satisfying in the equation
that is
where is the Nemytskii superposition operator defined by
Equivalently, is a weak solution of (4) if it solves in the equatin
| (5) |
that is the fixed point equation
where is the composed operator
Here denotes the solution operator of the Dirichlet problem, which associates to each the unique weak solution of
Obviously, the above operator approach requires us to specify the functional spaces with respect to which the operators are well defined and possess the properties assumed by the abstract existence results that will be applied.
2.1 Existence and uniqueness via Minty-Browder theorem
Assume that is a bounded domain with a smooth boundary, i.e., of class . We seek a weak solution to problem (3) in the Sobolev space , that is, a function such that
| (6) |
Endow with the inner product
and the corresponding norm
In our study, we make use of the Poincaré inequality
| (7) |
where denotes the first eigenvalue of the Dirichlet problem
We also denote by the duality pairing between and its dual space .
The assumptions imposed in this section on the function consist of an exponential growth condition, related to the Trudinger–Moser inequality, and a strong monotonicity property, in connection with the Minty–Browder theorem:
- (h1)
-
There exist and constants such that
(8) - (h2)
-
There exists satisfying
(9) such that
(10)
By definition of , it follows that it also satisfies the growth condition (8), possibly with different constants ().
Our first result concerns the well-definedness and continuity of the Nemytskii operator , under the exponential growth of given by (h1). The result complements the classical result on the Nemytskii operator corresponding to functions with power growth.
Lemma 1.
Let assumption (h1) hold. Then the operator is well defined and continuous from into .
Proof.
Well-definedness. Since we are in dimension two, the Sobolev embedding theorem (see, e.g., [26]) ensures that embeds continuously into for every . Combining this with Theorem 1 and the growth condition (8), we deduce that for all and all . Thus is well defined.
Continuity. Let in . Then there exists a subsequence (still denoted by ) such that for a.e. . Since the embedding is continuous (recall that embeds continuously into and that is identified with its dual), it suffices to prove that in in order to conclude that in .
We first claim that in , i.e.,
| (11) |
Inspired by [16, Lemma 2.1] (see also [29, Proposition 17.3]), denoting , we estimate
Since
and
one has
Using the generalized Hölder inequality with such that , we obtain
| (12) | ||||
| (13) |
Clearly,
and the sequence
is uniformly bounded.
Denoting , we have
| (14) |
Since as , there exists such that
Given that , the Trudinger–Moser inequality implies that the sequence from (14) is uniformly bounded for , whence is uniformly bounded for all . Consequently, the right hand side of (12) converges to zero, which shows that our claim (11) holds.
We now prove that in . To this end, we apply Vitali’s theorem (see, e.g., [30, Lemma 9.1]). The continuity of , and hence of , implies that
| (15) |
Let . Since in for every , the necessity part of Vitali’s theorem ensures that there exists such that
whenever satisfies . Similarly, from (11), there exists such that
for all with .
We return to the existence of a solution of (5), and thus of a weak solution of problem (4). More exactly, based on the Minty–Browder theorem, we have the following existence and uniqueness result.
Theorem 4.
Assume that the function satisfies conditions (h1) and (h2). Then problem (3) admits a unique weak solution in .
Proof.
Let be defined by
where is the embedding operator from into By Lemma 1, the operator is continuous and thus hemicontinuous. In view of Theorem 2, it remains to prove that is strongly monotone.
For any , using (10), we obtain
Applying the Poincaré inequality (7), we deduce
where, by condition (9),
Thus, is strongly monotone, so the Minty–Browder theorem ensures that is a bijection from onto . Consequently, there exists a unique such that , which is the unique weak solution to our problem (3). ∎
Remark 1.
Given that the domain is smooth, the unique solution to our problem (3) has a higher regularity.
Remark 2.
If we additionally require that is a -smooth domain and that the function is infinitely many times differentiable, then the following result holds.
Corollary 1.
2.2 Existence and localization via Moser-Harnack inequality
In this subsection, we assume that the domain is of class for some , and that the function satisfies
| (17) |
which guarantees the positivity of the right-hand side of equation (3) for every nonnegative function .
Recall that [26, Theorem 8.34] (see also [32]) if is a bounded domain of class , with , and , then the boundary value problem
| (18) |
admits a unique weak solution . Thus, we may define the solution operator
which assigns to each the unique solution of problem (18). The mapping is a bounded linear operator. Since the embedding is compact (see, e.g., [26, Lemma 6.36]), it follows that is completely continuous as an operator from into . Moreover, is order preserving (monotone) with respect to the usual pointwise ordering of functions.
Letting
be endowed with the supremum norm , our problem (3) is equivalent to the fixed point equation in ,
where
Observe that the operator can be written as
where the embedding mappings
are bounded linear operators. Since is continuous from to and bounded (maps bounded sets into bounded sets), and is completely continuous from into , it follows that is completely continuous from to itself, as the composition of a completely continuous operator with bounded continuous operators.
For any fixed subdomain such that , and any , we consider the continuous seminorm on
By means of , we further define the cone
where is the constant given by Theorem 3.
Given arbitrary numbers , we denote by the conical set
and define the quantities
where is the characteristic function of , i.e.,
The following existence and localization result holds.
Theorem 5.
Let be such that the set is nonempty and
| (19) |
and
| (20) |
Then problem (3) admits a solution satisfying
Proof.
First, since , condition (17) implies that for all and , so the order-preserving property of yields for all . Moreover, the Moser–Harnack inequality ensures that for every . Therefore, the cone is invariant under the operator , that is, .
We claim that
| (21) |
Since the set is closed, by the continuity of it suffices to guaranty that
We prove this in two steps.
Step 1: We show that for all satisfying .
Let with , so that for all . From (17), since and are decreasing, one clearly has
which, by condition (19), yields
| (22) |
Also,
and therefore, using (22) together with the monotonicity of the norm , we obtain
as desired. Obviously, the same inequality holds for every
Step 2: We show that for all and .
Let for , and let . By the definition of the cone , we have
and therefore
| (23) |
Since for all , it follows from (17) and (23) that
which implies
| (24) |
Applying to both sides of (24) (recall that is monotone), we obtain
| (25) |
Now, taking the seminorm in the above relation (25) (note that it is also monotone), and using condition (20), we obtain
Consequently, our claim (21) follows. Since is completely continuous and is a bounded, closed, and convex set, Schauder’s fixed point theorem applied to the operator
ensures the existence of a fixed point for , that is, . Since , it follows that . This completes our proof, as any fixed point of is a solution of problem (3); so, solves (3), and by the definition of it satisfies and .
∎
Remark 3.
In the case , the proof simplifies since the set is convex. Indeed, when the considered seminorm is linear on , and therefore the set
is convex. Since
and both sets in the intersection are convex, it follows that is convex as well.
We emphasize that, in the case , the functional is linear on the cone , although it is not linear on the whole space
Remark 4.
In the case that is a monotone function, the two conditions in Theorem 5 reduce simply to the behavior of at only two points:
The localization Theorem 5 immediately ensures multiple solutions in the case where the nonlinearity is oscillatory.
Theorem 6.
Let and , , be positive real numbers such that the sets are nonempty and pairwise disjoint. If
then problem (3) admits at least distinct solutions satisfying
Proof.
The application of Theorem 5 to each set yields a solution in that set. The sets being pairwise disjoint, these solutions are distinct. ∎
Remark 5.
(a) A necessary condition for a set be nonempty is Indeed, if then on and These inequalities immediately yields
(b) A sufficient condition for the set to be nonempty is where is the first eigenfunction of the Dirichlet problem for the Laplacian, normalized by Indeed, under this condition there exists a positive constant such that In fact, must satisfy and Such a number exists provided that
(c) If the numbers in Theorem 6 satisfy for then the sets are pairwise disjoint. To see this, from the above condition, we have for If now then
whence Hence for every Similarly, the conditions on and imply for Then which shows that for every Therefore, the sets are pairwise disjoint.
AcknowledgementsThe second author A. Stan acknowledges the support provided by the project
”Nonlinear Studies of Stratified Oceanic and Atmospheric Flows”, funded by
the European Union through the Next Generation EU initiative and the
Romanian Government under the National Recovery and Resilience Plan for
Romania. The project is contracted under number 760040/23.05.2023, cod
PNRR-C9-I8-CF 185/22.11.2022, through the Romanian Ministry of Research,
Innovation, and Digitalization, within Component 9, Investment I8. He is also grateful to Professor Călin I. Martin for
valuable discussions and helpful suggestions throughout the course of this project.
Both authors thank the anonymous reviewer for the careful reading of the manuscript and for the suggested modifications.
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Funding
The authors declare that no funds, grants, or other support were received during the preparation of this manuscript.
Conflict of interest
The author have no relevant financial or non-financial interests to disclose.
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Acknowledgements
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