K\'arm\'an Vortex Street in incompressible fluid models
Claudia Garc\'ia

TL;DR
This paper develops a robust, desingularized model for the Kármán Vortex Street phenomenon in incompressible fluids, extending classical point vortex models to more general fluid dynamics frameworks.
Contribution
It introduces a flexible, desingularized vortex patch model for Kármán Vortex Streets within Euler equations, improving upon classical point vortex approaches.
Findings
Provides a new vortex patch model for Kármán Vortex Streets
Extends classical models to more general incompressible fluid equations
Offers a flexible framework for future fluid dynamics studies
Abstract
This paper aims to provide a robust model for the well-known phenomenon of K\'arm\'an Vortex Street arising in Fluid Mechanics. The first theoretical attempt to model this pattern was given by von K\'arm\'an [22, 23]. He considered two parallel staggered rows of point vortices, with opposite strength, that translate at the same speed. Following the ideas of Saffman and Schatzman [36], we propose to study this phenomenon in the Euler equations by considering two infinite arrows of vortex patches. The key idea is to desingularize the point vortex model proposed by von K\'arm\'an. Our construction is flexible and can be extended to more general incompressible models.
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Kármán Vortex Street in incompressible fluid models
Claudia García
Departamento de Matemática Aplicada and Research Unit “Modeling Nature” (MNat), Facultad de Ciencias. Universidad de Granada
18071-Granada, Spain. & IRMAR, Université de Rennes 1
Campus de Beaulieu
35 042 Rennes cedex
France
(Date: March 19, 2024)
Abstract.
This paper aims to provide a robust model for the well–known phenomenon of Kármán Vortex Street arising in Fluid Mechanics. The first theoretical attempt to model this pattern was given by von Kármán [22, 23]. He considered two parallel staggered rows of point vortices, with opposite strength, that translate at the same speed. Following the ideas of Saffman and Schatzman [36], we propose to study this phenomenon in the Euler equations by considering two infinite arrows of vortex patches. The key idea is to desingularize the point vortex model proposed by von Kármán. Our construction is flexible and can be extended to more general incompressible models.
Key words and phrases:
Kármán Vortex Street, point vortex model, vortex shedding, Euler equations, incompressible fluids
2010 Mathematics Subject Classification:
35Q31, 35Q35, 35B32, 35B36
This work has been partially supported by the MINECO-Feder (Spain) research grant number MTM2017-91054EXP, the Junta de Andalucía (Spain) Project FQM 954 and the MECD (Spain) research grant FPU15/04094.
Contents
1. Introduction
A distinctive pattern is observed in the wake of a two–dimensional bluff body placed in a uniform stream at certain velocities: this is called the von Kármán Vortex Street. It consists of vortices of high vorticity in an irrotational fluid. This complex phenomenon occurs in a large amount of circumstances. For instance, the singing of power transmission lines or kite strings in the wind. It can also be observed in atmospheric flow about islands, in ocean flows about pipes or in aeronautical systems. See [22, 23, 34, 36, 37, 38, 39].
The phenomenon of periodic vortex shedding, which is an oscillating flow that takes place when a fluid past a bluff body, was first studied experimentally with the works [34, 39]. The more classical model for Kármán Vortex Street, and the first theoretical one, was presented by von Kármán in [22, 23]. He considered a distribution of point vortices located in two parallel staggered rows, where the strength is opposite in each row. Other works concerning this model are [2, 26, 35]. Since the exact problem seems to be complex from a theoretical point of view, there has been a large variety of approximations.
It is observed that viscosity is involved with the generation of the vortex layers by the body, which generates the shedding process. However, it seems that viscosity does not play an essential role in the formation of the vortex street once the vortex layers have been created. Moreover, it would appear also that the body is not important in the formation and the evolution of the vortex street. If we concentrate on the evolution of the street, and not in the vortex layer formation process, an inviscid incompressible fluid model can be proposed to model this situation.
Kármán Vortex Street structures arise in the context of the Euler equations in the works of Saffman and Schatzman [36, 37, 38]. Following the ideas of von Kármán [22, 23], they considered two parallel infinite array of vortices with finite area and uniform vorticity. They found numerically the existence of this kind of solutions that translate at a constant speed and studied their linear stability.
In this paper, we focus on the study of these structures in different inviscid incompressible fluid models via a desingularization of the point vortex model proposed by von Kármán [22, 23]. We obtain two infinite arrows of vortex patches, i.e. vortices with finite area and uniform vorticity, that translate. Then, we recover analytically the solutions found numerically by Saffman and Schatzman, not only in the Euler equations framework, but also in other incompressible models, that we recall in the following.
Let be a scalar magnitude of the fluid satisfying the following transport equation
[TABLE]
Note that the velocity field is given in terms of via the interaction kernel , which is assumed to be a smooth off zero function. Here, . In the case that , we arrive at the Euler equations. On the other hand, if , with and the Bessel function, the quasi–geostrophic shallow water (QGSW) equations are found. Finally, the generalized surface quasi–geostrophic (gSQG) equations appears in the case that , for and . Note that all the previous models have a common property: the kernel is radial, which will be crucial in this work.
The Euler equations deal with uniform incompressible ideal fluids and represents the vorticity of the fluid, usually denoted by . Yudovich solutions, that are bounded and integrable solutions, are known to exist globally in time, see [28, 41]. When the initial data is the characteristic function of a simply–connected bounded domain , the solution continues being a characteristic function over , that propagates along the flow. These are known as the vortex patches solutions. If the initial domain is , with , the regularity persists for any time, see [4, 11]. The only explicit simply–connected vortex patches known up to now are the Rankine vortex (the circular patch), which are stationary, and the Kirchhoff ellipses [24], that rotate. Later, Deem and Zabusky [14] gave some numerical observations of the existence of V–states, i.e. rotating vortex patches, with fold symmetry. Using the bifurcation theory, Burbea [5] proved analytically the existence of these V–states close to the Rankine vortex. There has been several works concerning the V–states following the approach of Burbea: doubly–conected V–states, corotating and counter–rotating vortex pairs, non uniform rotating vortices and global bifurcation, see [8, 13, 15, 18, 20, 21].
The quasi–geostrophic shallow water equations are found in the limit of fast rotation and weak variations of the free surface in the rotating shallow water equations, see [40]. In this context, the function is called the potential vorticity. The parameter is known as the inverse “Rossby deformation length”, and when it is small, it corresponds to a free surface that is nearly rigid. In the case , we recover the Euler equations. Although vortex patches solutions are better known in the Euler equations, there are also some results in the quasi–geostrophic shallow water equations. For the analogue to the Kirchhoff ellipses in these equations, we refer to the works of Dristchhel, Flierl, Polvani and Zabusky [31, 32, 33]. In [12], Dristchel, Hmidi and Renault proved the existence of V–states bifurcating from the circular patch.
In the case of the generalized surface quasi–geostrophic, describes the potential temperature. This model has been proposed by Córdoba et al. in [10] as an interpolation between the Euler equations and the surface quasi–geostrophic (SQG) equations, corresponding to and , respectively. The mathematical analogy with the classical three–dimensional incompressible Euler equations can be found in [9]. Some works concerning V–states in the gSQG equations are [6, 7, 17, 20].
The point model for a Kármán Vortex Street consists in two infinite arrays of point vortices with opposite strength. More specifically, consider a uniformly distributed arrow of points, with same strength in every point, located in the horizontal axis, i.e., , with and . The other arrow contains an infinite number of points, with opposite strength, which will be parallel to the other one and with arbitrary stagger: with and . We refer to Figure 1 for a better understanding of the localization of the points. Hence, we consider the following distribution:
[TABLE]
where , and . If the kernel is radial, then we will show that every point translates in time, with the same constant speed. Moreover, if or , the translation is parallel to the real axis. In the typical case of the Newtonian interaction, that is , the evolution of (6) has been fully studied, see [2, 26, 22, 23, 29, 30, 35]. The problem consists in a first order Hamiltonian system and the evolution of every point is given by the following system:
[TABLE]
with initial conditions
[TABLE]
for . It can be checked that the velocity at every point is the same, providing us with a translating motion. Indeed, if or , the speed can be expressed by elementary functions, where we observe that the translation is horizontal:
[TABLE]
The works of Saffmann and Schatzman [36, 37, 38] refer to the study of these structures in the Euler equations. In fact, they consider two infinite arrows of vortices with finite area, which have uniform vorticity inside. These are two infinite arrows of vortex patches distributed as in (6). They found existence of this kind of solutions numerically and they studied their linear stability, see [36, 37, 38]. The problem can be studied not only in the Euler equations for the full space, but in the Euler equations in the periodic setting. A theory for the Euler equations in an infinite strip can be found in [3]. In [16], Gryanik, Borth and Olbers studied the quasi–geostrophic Kármán Vortex Street in two–layer fluids.
The aim of this work is to find analitically solutions to the model proposed by Saffman and Schatzman in [36, 37, 38]. We will do it not only for the Euler equations, but also for other inviscid incompressible models. Here, we follow the idea of Hmidi and Mateu in [20], where they desingularize a vortex pairs obtaining a pair of vortex patches that rotate or translate (depending on the strength of the points). The plan is the following. For and , consider
[TABLE]
where and are simply–connected bounded domains. In the case and , with or , and , we find the Kármán Vortex Street (6) in the limit . This means
[TABLE]
in the distribution sense. Then, we connect the vortex patch model (7) with the point vortex model (6). In the following, we will refer to Kármán Vortex Street or Kármán Point Vortex Street when having the point vortex model (6). Otherwise, we denote by Kármán Vortex Patch Street in the case of (7). Some relation between the two domains is needed, and the suitable one is mentioned before: . Assuming that , for some , and using a conformal map , we arrive at the following equation
[TABLE]
where
[TABLE]
Let us explain the meaning of . Assume that the conformal map is a perturbation of the identity in the following way
[TABLE]
for and . Whereas, it will be consider as
[TABLE]
for more singular kernels, such as , for . Moreover, we have that , for any . Here, is the speed of the point model (6). The nonlinear functional is well-defined from to , where
[TABLE]
for some . However, is not an isomorphism in these spaces. Defining as a function of and in the following way
[TABLE]
then, is also well-defined from to , where
[TABLE]
Indeed, is an isomorphism in these spaces. Then, we fix the velocity depending on and as in (10). In this way, the Implicit Function theorem can be applied in order to desingularize the point model (6) obtaining our main result:
Theorem 1.1**.**
Consider , , or , for and . Let , with and , and or . Then, there exists a simply–connected bounded domain such that
[TABLE]
defines a horizontal translating solution of (5), with constant speed, for any and small enough .
The proof of the theorem has to be adapted to each case. For the cases and , the kernel has a logarithm singularity at the origin, which will play an important role in the choice of the scaling of the conformal map (8). Otherwise, if , for , or for more general kernels, the scaling of the conformal map will depend on the singularity at the origin as depicted in (9).
This work is organized as follows. In Section 2, we introduce some preliminary results about the –vortex problem and, in particular, the point model for the Kármán Vortex Street (6) with general interactions. Section 3 refers to the Euler and QGSW equations, where the singularity of the kernel is logarithmic. We will deal with the general case in Section 4, following the same ideas as in the Euler equations. The gSQG equations will become a particular case of this study. Finally, Appendix A and Appendix B will be devoted to provide some definitions and properties concerning special functions and complex integrals.
Let us end this part by summarizing some notation to be used along the paper. We will denote the unit disc by and its boundary by . The integral
[TABLE]
denotes the usual complex integral, for some complex function . Moreover, we will use the symmetry sums defined by
[TABLE]
except being specified.
2. The N–vortex problem
The –vortex problem consists in the study of the evolution of a set of points that interact according to some laws. Originally, the Newtonian interaction for the –vortex problem is considered. But here, we start by assuming that the interaction between the points is due to a general function , which is smooth off zero. The problem is a first order Hamiltonian system of the form
[TABLE]
with some initial conditions at and where . Moreover, if , are –points located in the plane . The constants mean the strength of each point and the interaction between them is due to . In the case that , we arrive at the typical –vortex problem:
[TABLE]
First, we deal with the evolution of two points. We can check that they rotate or translate depending on their strengh: and . Later, we will move on the configuration that we concern: an infinite number of points with a periodic pattern in space. For more details about the –vortex problem in the case of the Newtonian interaction see [29].
2.1. Finite configurations
There are some stable situations yielding to steady configurations. Here, we illustrate the evolution of –points since the same idea is used later in the case of periodic configurations.
Proposition 2.1**.**
Let us consider two initial points and , with , located in the real axis, with strengths and respectively. We have:
- (1)
If and , then the solution behaves as for , with . 2. (2)
If , then , for , with .
Proof.
According to (12), the evolution of the two points is given by the following system:
[TABLE]
(1) By the above system, it is clear that , which implies that
[TABLE]
Assuming that , and using the above equation, one arrives at . Then, the system (13) yields
[TABLE]
Since and are located in the real axis, one has that , and then subtracting the above two equations amounts to
[TABLE]
(2) In this case, we have that , and thus
[TABLE]
As a consequence, (13) agrees with
[TABLE]
which can be solved as
[TABLE]
∎
The above result gives us that two vortex points with , have a rotating evolution. Otherwise, they translate. From now on, we refer that a structure translates when the evolution of every point (or every patch, in the case of (5)) is a translation, with the same constant speed.
In the usual –vortex problem, meaning , the above result is well–known. Here, we have seen that if the interaction of the points is due to a kernel that is radial, we get the same evolution.
2.2. Periodic setting
This section deals with the evolution of two infinite arrays of points with opposite strength, which are periodic in space. More specifically, the points of the first arrow, which have the same strength, will be located in the horizontal axis. Let us assume that we have one point at the origin, and the next one differs of it a distance . This means that we have the points , for and . The second arrow, with opposite strength to the previous arrow, will be parallel to the horizontal axis but with a height , having the following distribution of points: , for and . For the moment, let us consider that is any real number.
Then, we focus on
[TABLE]
with , and . In the following results, we check that the above initial configuration translate when , , for , or for satisfying some general conditions. Moreover, if or , the translation is horizontal.
We are going to differentiate two cases depending on the behavior of the interaction at infinity. This is important in order to give a meaning to the infinite sum coming from (14), whose equations are given by
[TABLE]
with initial conditions
[TABLE]
for . Then, we refer to the critical case in the case of the Newtonian interaction
[TABLE]
Here, we must use the structure of the logarithm in order to have a convergence sum. Note that here we need to use strongly the symmetry sum. Otherwise, the subcritical cases will use the faster decay of at infinity as it is the case of the QGSW or gSQG interactions.
Critical case: Let us first show the result for the Newtonian interaction, that is, . Here, we denote to to emphasize that we are working with the vorticity.
Proposition 2.2**.**
Given the point vortex street (14) with , for , and , then the street is moving with the following constant velocity speed
[TABLE]
In the case that or , the translation is parallel to the horizontal axis with velocity
[TABLE]
Remark 2.3**.**
If with and given by (14), then the velocity of the street is .
Proof.
Define
[TABLE]
The idea is to consider , getting in the distribution sense. The associated stream function to is given by
[TABLE]
where we are using complex notation. In order to pass to the limit, we need to use the structure of the logarithm. Let us work with the sum in the following way
[TABLE]
Then, we have
[TABLE]
Using the product expression for the sine, that is
[TABLE]
we get that
[TABLE]
In this way, we achieve that the sum in (16) converges. In the same way, the corresponding velocity agrees with
[TABLE]
where is none of the points vortex. In each of the points, the velocity is given by
[TABLE]
for any . We define as the limit of the above function.
First, let us show that the velocity at every point is the same. We begin with the first arrow
[TABLE]
Note that
[TABLE]
since we are using the symmetry sum (11). For the second arrow, we obtain
[TABLE]
Then, the velocity speed of the street is given by
[TABLE]
In order to find a better expression for , let us come back to the stream function. Using
[TABLE]
we achieve
[TABLE]
Let us now work with . Using the definition of the complex cotangent, we obtain
[TABLE]
which is the announced expression for the velocity. The same idea can be applied to get the expression when . ∎
For the cases and we notice that the velocity increases as goes to 0. Moreover, considering and in the above proposition, one obtains the following corollary.
Corollary 2.4**.**
The vortex arrow given by
[TABLE]
is stationary, for any .
Similar ideas can be applied to find that a horizontal arrow of points with the same strength is stationary.
Proposition 2.5**.**
The vortex arrow given by
[TABLE]
is stationary, for any and .
Subcritical case: We finish this section by showing the result for faster decays interactions. This case will cover the QGSW and gSQG interactions: or for . The result reads as follows.
Proposition 2.6**.**
Let be a smooth off zero function satisfying
- (H1)
* is radial such that ,* 2. (H2)
there exists and such that , for .
Then,
[TABLE]
with , and , translates with constant velocity speed
[TABLE]
In the case or , the translation is parallel to the horizontal axis.
Remark 2.7**.**
From now on, we will assume that is radial via (H1), we will write for when there is no confusion in order to simplify notation.
Remark 2.8**.**
The second hypothesis is required to give a meaning to the infinite sum, which converges absolutely. This condition could be weakened by assuming
[TABLE]
Proof.
As in the previous models, the velocity at the points is given by
[TABLE]
for . The above sums are converging due to the second assumption. We can check that the velocity is the same at every point of the street:
[TABLE]
Then,
[TABLE]
If or , one has that
[TABLE]
and the translation is in the horizontal direction. ∎
In the general case, we also have that an array is stationary.
Proposition 2.9**.**
Let be a smooth off zero function satisfying (H1)-(H2), then
[TABLE]
is stationary for any and .
It is clear that , for , satisfies the hypothesis of the above results. In the case of the QGSW interaction, we obtain similar results. In this case, the stream function associated to (14) is given by
[TABLE]
The definition and some properties of the Bessel functions can be found in Appendix A. The above sum is convergent due to the behavior of at infinity, which is exponential:
[TABLE]
There is another representation of the stream function given in [16], where the periodicity structure is emphasized:
[TABLE]
Then, we state the result concerning the QGSW interaction.
Proposition 2.10**.**
Given the point vortex street (14), with , and , then the street translates with the following constant velocity speed
[TABLE]
In the case that or , the translation is parallel to the horizontal axis.
3. Periodic patterns in the Euler and QGSW equations
This section is devoted to show the full construction of the Kármán Vortex Street structures in the Euler equations. Instead of considering two arrows of points as in Section 2, we consider two infinite arrows of patches distributed in the same way than the arrows of points (14). We will refer to this configuration in the Euler equations as Kármán Vortex Patch Street.
In the case of arrows of points, we showed in the last section that they translate. Here, we want to find a similar evolution in the Euler equations. Since these structures are periodic is space, first we will have to look for the green function associated to the operator in , which will come as an infinite sum of functions. This infinite sum can be expressed in terms of elementary functions, which helps us in the computations. Once we have the equation that will characterize the Kármán Vortex Patch Street, we will have to deal with the Implicit Function theorem. Hence, a desingularization of the Kármán Point Vortex Street will show the existence of these structures in terms of finite area domains that translate.
At the end of this section, we will analyze the case of the QGSW equations, which will follow similarly. Let us focus now in the Euler equations:
[TABLE]
The second equation links the velocity to the vorticity through the Biot–Savart law, where and . We denote by the stream function, which verifies .
From now on we will use complex notation in order to simplify the computations. Then, we identify with . In the same way, . Moreover, the gradient operator in can be identified with the Wirtinger derivative, i.e.,
[TABLE]
for a complex function .
3.1. Velocity of the Kármán Vortex Patch Street
Consider the initial condition given by
[TABLE]
where and are simply–connected bounded domains such that , and .
The velocity field can be computed through the Biot–Savart law in . For that, one must find the Green function associated to the operator in order to have an expression for the stream function . Later, we just use that , or with the complex notation, . This will be developed in the next result, obtaining different expressions for the velocity, which will be useful later.
Proposition 3.1**.**
The velocity field of the Euler equations associated to (3.1) is given by the following expressions:
- (1)
[TABLE] 2. (2)
[TABLE] 3. (3)
[TABLE]
with
[TABLE]
Proof.
(1) Let us begin finding the stream function associated to
[TABLE]
by superposing the stream function of each one of the elements of the sum, i.e.,
[TABLE]
Using the same idea than in Proposition 2.2, we find that
[TABLE]
and hence
[TABLE]
Using that and have same area, it follows that
[TABLE]
where the sine formula (17) yields
[TABLE]
Then,
[TABLE]
The Stokes theorem, see Appendix B, has been applied in the last line.
(2) This expression comes from (3.1) and
[TABLE]
used in Proposition 2.2.
(3) From (1), we can use the series expansion of the complex sine,
[TABLE]
in order to obtain
[TABLE]
Then, we have
[TABLE]
Moreover, the Stokes formula (85) yields
[TABLE]
Finally, let us now use the Cauchy–Pompeiu’s formula (86) for the first and third terms, to find
[TABLE]
∎
3.2. Functional setting of the problem
The first step is to scale the vorticity (3.1) in order to introduce the point vortices in our formulation and be able to desingularize them. Let us define
[TABLE]
for and . The domains and are simply–connected and bounded. In the case that and , with and , we find the point vortex street (14) passing to the limit :
[TABLE]
Proposition 2.2 deals with (30) from the dynamical system point of view, showing that it translates. Moreover, if or , the translation is horizontal.
Now, we try to find the equation that characterize a translating evolution in the Euler equations. Assume that we have , with . Inserting this ansatz in the Euler equations, we arrived at
[TABLE]
where “” indicates the scalar product in . As in the previous section, we want to work always in the complex sense identifying as . The gradient operator can be identify to the derivative as in (24). Then, we above equation can be written as:
[TABLE]
When working with the scaled vorticity , this equation must be understood in the weak sense, yielding
[TABLE]
or similarly,
[TABLE]
for any . Here, is the exterior normal vector and is the velocity associated to (29). The expression of coming from Proposition 3.1–(2) gives us
[TABLE]
We can check that , for any . Moreover, we have that , for any simply–connected bounded domain . Then, the equation (31) reduces to
[TABLE]
Consider , for or , and . By using the relation between and , the above system reduces to just one equation:
[TABLE]
where
[TABLE]
Other representations of the velocity field can be obtained using Proposition 3.1:
[TABLE]
At this stage, we are going to introduce an exterior conformal map from into given by
[TABLE]
For others values of , one must readjust the conformal map, but here we will consider and having a horizontal translation in the point vortex system.
Note that . Then, we can rewrite the equation with the use of the above conformal map in the following way:
[TABLE]
where
[TABLE]
Note that
[TABLE]
As it is mentioned in the introduction, [20] deals with the desingularization of a vortex pairs in both the Euler equations and the generalized quasi-geostrophic equation. In order to relate with the functional in [20], we can write as
[TABLE]
using the expression of the velocity written in Proposition 3.1-(3). The Residue Theorem amounts to
[TABLE]
Hence, the function comes from the study of the vortex pairs in [20]. We will take advantage of the study done in that work about . In this model, indicates the contribution of just two vortex patches.
The first step is to check that we recover the point vortex street with this model. Remind that or .
Proposition 3.2**.**
For any , , the following equation is verified
[TABLE]
where is given by (15).
Proof.
The equation that we must check is
[TABLE]
Using the Stokes Theorem, it agrees with
[TABLE]
We study the equation in two parts. First, note that
[TABLE]
In the above limit, we may use the Dominated Convergence Theorem in order to introduce the limit inside the integral. Second, we use the expansion of the complex cotangent as
[TABLE]
where is a smooth function for . Then, the only contribution in is given by the first part:
[TABLE]
for , where we have used the Residue Theorem to compute the integral. ∎
We fix the Banach spaces that we will use when we apply the Implicit Function Theorem. For , we define
[TABLE]
Remark 3.3**.**
Let us explain why we need that the first frequency in the domain is vanishing. In the case that or , it can be checked that is well–defined and from to
[TABLE]
But, when we linerarize and obtain , this is not an isomorphism from to . However, it does from to . We are using instead of in order to implement later the Implicit Function Theorem.
Remark 3.4**.**
Note that if , with , then is bilipschitz.
Proposition 3.5**.**
The function , given by
[TABLE]
fulfills , where is defined in (15). The parameters satisfy: , , , and is defined in (36).
Proof.
In the expression (38), let us work with the denominator. The Residue Theorem amounts to
[TABLE]
From (3.2) and the ideas in Proposition 3.2, we get
[TABLE]
Note also that
[TABLE]
via again the Residue Theorem. Then, the first term in (3.2) does not provide any contribution. It implies that
[TABLE]
∎
Proposition 3.6**.**
If sets (38), then
[TABLE]
with , is well–defined and . The parameters satisfy that , and .
Remark 3.7**.**
Let us clarify why we need the condition . In some point of the proof we need to use Taylor formula in the following way
[TABLE]
for and . Here, the use of this formula is not explicit since we are refering to the work [20], and this condition is needed in order to check . Although we are not using it explicitly in this proof, we will use it for the general equation in the following section.
Proof.
We will divide the proof in three steps.
* First step: Symmetry of .* Note that given by (32) verifies
[TABLE]
where we are taking in order to work with or . We are going to check that , with . To do that, it is enough to prove that
[TABLE]
Recall the following property of the complex integrals over :
[TABLE]
for a complex function .
Let us start with the expression of and note that
[TABLE]
Then,
[TABLE]
for and . Notice that , which implies
[TABLE]
Next, if is given by (38), then we are going to check that . Let us analyze the denominator and the numerator of the expression of :
[TABLE]
and
[TABLE]
Then, . Hence,
[TABLE]
In order to check that , we need . For that, we ask the condition
[TABLE]
which agrees with
[TABLE]
Using that verifies (38), the last equation is clearly set.
* Second step: Regularity of . * Let us begin with the denominator, noting that
[TABLE]
by using the Residue Theorem. Then, if and , the denominator is not vanishing. Moreover, the denominator is clearly in and .
We continue with the numerator denoting
[TABLE]
using the decomposition of done in (3.2). Note that is the part of coming from the vortex pairs analyzed in [20]. In that work is analyzed showing that it is in and . Note that the spaces used in [20] are also (36)–(37) and the condition is needed in their computations, see Remark 3.7.
Then, it remains to study the regularity of . We should analyze , i.e.,
[TABLE]
Note that and are smooth in both variables, due to that , see (26). Then they are in and . Let us analyze the others terms. Using (26) and the expansion of the logarithm,
[TABLE]
one has
[TABLE]
with smooth in both variables. This implies that is in and . On the other way,
[TABLE]
with and smooth. Then, we find
[TABLE]
which is smooth in and .
Hence, we achieve that is in both variables.
* Third step: Regularity of . * Decomposing again as in (3.2), we get that
[TABLE]
Again, the part coming from is analyzed in [20], where it is shown that is in both variables. From the second step, we got that and are also smooth completing the proof. ∎
3.3. Desingularization of the Kármán Point Vortex Street
In this section, we provide the proof of the existence of Kármán Vortex Patch Street via a desingularization of the point vortex model given by the Kármán Point Vortex Street. The idea is to implement the Implicit Function Theorem to the functional defined in Proposition 3.6.
Theorem 3.8**.**
Let , with and , and or . Then, there exist such that
[TABLE]
defines a horizontal translating solution of the Euler equations, with constant speed, for any and small enough . Moreover, is at least .
Proof.
In order to look for solutions in the form (42), we need to study the functional defined in (33), where is given by (32). Moreover, is a function of described by (38).
In Proposition 3.6, we have that , with , is well–defined and , for and . Then, we wish to apply the Implicit Function Theorem to . By Proposition 3.2 and Proposition 3.5, we have that , for any .
Let us show that is an isomorphism:
[TABLE]
By Proposition 3.5, we obtain . Note also that
[TABLE]
Moreover, by expression (3.2), we have
[TABLE]
Then, we obtain
[TABLE]
By the Residue Theorem, we have
[TABLE]
Finally, we find
[TABLE]
which is an isomorpshim from to . ∎
Remark 3.9**.**
Analyzing [20], we realize that the above linearized operator (43) agrees with the linearized operator in [20] for the vortex pairs. This tells us that the only real contribution in the linearized operator is due to two vortex patches: and .
3.4. Quasi–geostrophic shallow water equation
In this section, we investigate the case of the quasi-geostrophic shallow water (QGSW) equations. Let be the potential vorticity, then the QGSW equations are given by
[TABLE]
with . The same results to the Euler equations are obtained in this case. That is due to the similarity of the kernel in both cases, in particular, they have the same behavior close to 0. In Section 2 we analyzed the case of the -vortex problem, see Proposition 2.10. Here, we want to desingularize (14) in order to obtain periodic in space solutions that translate in the QGSW equation.
The stream function can be recovered in terms of in the following way
[TABLE]
The function is the Modified Bessel function of order zero, whose definition and some of their properties can be found in Appendix A. It is of great interest the expansion of given in (83) as
[TABLE]
where
[TABLE]
The constant is the Euler’s constant and the function is defined in Appendix A, but we recall it as
[TABLE]
Via this expansion, one notice that
[TABLE]
where
[TABLE]
Note that is smooth and close to [math].
Consider a Kármán Vortex Patch Street in the QGSW equations in the sense
[TABLE]
where and are simply–connected bounded domains such that , and . Motivated by Euler equations, assume , having the following distribution
[TABLE]
where we are rewriting by . The velocity field is given by
[TABLE]
We scale the expression (46) in the following way
[TABLE]
As in the Euler equations, if , with and , we obtain the point model:
[TABLE]
which has been studied in Proposition 2.10. Considering now a translating motion in the form , with , then we arrive at
[TABLE]
In the case of , we need to solve the above equation understood in the weak sense, i.e.,
[TABLE]
which, as for the Euler equations, reduces to
[TABLE]
written in the complex sense. With the use of the conformal map (32):
[TABLE]
it agrees with
[TABLE]
where
[TABLE]
Then,
[TABLE]
Via the expansion of , given in (45), one has
[TABLE]
where is the corresponding function associated to Euler equations, see (3.2).
The analogue to Propositions 3.2, 3.5 and 3.6, and Theorem 3.8 are obtained, whose proofs are very similar and so here we omit many details. Remark that or .
Proposition 3.10**.**
For any and , the following equation is verified
[TABLE]
where is given by (22):
[TABLE]
Proof.
Using definition (50), we need to check that
[TABLE]
Via the Stokes Theorem, the expansion of given in (45) and noting that
[TABLE]
for and some function , it reduces to
[TABLE]
Note that
[TABLE]
and
[TABLE]
making use of the Dominated Convergence Theorem. Secondly, via the definition of in (22), one has that
[TABLE]
The left term is also zero using the computations in Proposition 3.2. ∎
We avoid the proof of the following result, due to the similarity with Proposition 3.5.
Proposition 3.11**.**
The function , given by
[TABLE]
fulfills , where is defined in (22). The parameters satisfy: , , , and is defined in (36).
The next result concerns the well-definition of in the spaces defined in (36)–(37).
Proposition 3.12**.**
If sets (54), then
[TABLE]
with , is well–defined and . The parameters satisfy , and .
Proof.
Note the similarity of this proposition to Proposition 3.6. Following its ideas, in order to check the symmetry of , it is enough to prove that
[TABLE]
We take advantage of (41). Via its definition, note that
[TABLE]
Note that using the decomposition of given in (3.4), the regularity problem reduces to the same one for the Euler equations, done in Proposition 3.6. ∎
Finally, we state the result concerning the desingularization of the Kármán Vortex Street.
Theorem 3.13**.**
Let , with and , and or . Then, there exist such that
[TABLE]
defines a horizontal translating solution of the quasi–geostrophic shallow water equations, with constant velocity speed, for any and small enough . Moreover, is at least .
Proof.
By Proposition 3.12, we have that , with , is well–defined and , for and . Moreover, Proposition 3.10 and Proposition 3.11 give us that , for any . In order to apply the Implicit Function Theorem, let us check that is an isomorphism.
First, using (3.4), one achieves
[TABLE]
where is a smooth function such that for small , see (45). Note that
[TABLE]
and
[TABLE]
Thus, we have
[TABLE]
which is an isomorphism from to . ∎
4. Kármán Vortex Street in general models
Kármán Vortex Patch Street structures are found both in the Euler equations and in the QGSW equations. The important fact in both models is that the Green functions associated to the elliptic problem of the stream function have the same behavior close to 0, having then the same linearized operator. We can extend it to other models, where the generalized surface quasi–geostrophic equations are a particular case, see Theorem 4.7 for more details. Here, let us work with the general model:
[TABLE]
4.1. Scaling the equation
The aim of this section is to look for solutions of the type
[TABLE]
The domains and are simply–connected bounded domains such that , and . Consider , having the following distribution
[TABLE]
where we are rewriting by . The velocity field is given by
[TABLE]
where is defined in (24) and the Stokes Theorem (85) is used. In order to introduce the point model configuration, let us scale the equation in the following way. For any , define
[TABLE]
for , and . If , then we arrive at the point vortex street (18) in the limit when , i.e.,
[TABLE]
This configuration of points is studied in Proposition 2.6, from the dynamical system point of view, showing that (64) translates. From now on, take or having a horizontal translation in the point model. The associated velocity field to (63) is given by
[TABLE]
We introduce now the conformal map. Consider such that
[TABLE]
Hence
[TABLE]
Remark 4.1**.**
The constant in the definition of the conformal map (32) comes from the singularity of the kernel in the general case. For the logarithmic singularities, we do not need to add this constant because there we use the structure of the logarithm. When having more singular kernels, as in this case, we need to introduce .
Assuming that we look for translating solutions, i.e., , we arrive at the equation
[TABLE]
where
[TABLE]
The next step is to check that if , and (referring to the Kármán Point Vortex Street), equation (66) is verified.
Proposition 4.2**.**
Let satisfies
- (H1)
* is radial such that ,* 2. (H2)
there exists and such that , for , 3. (H3)
there exists such that and as .
For any and , the following equation is verified
[TABLE]
where is given by (19):
[TABLE]
Remark 4.3**.**
From Hypothesis (H3) we are assuming that the kernel is more singular than the logarithmic kernel analyzed in the previous sections, but less singular than the kernel of the surface quasi–geostrophic equation. A typical kernel satisfying (H3) is the one coming from the generalized surface quasi–geostrophic equation: , for .
Proof.
By definition,
[TABLE]
Concerning the first term, we can compute it using
[TABLE]
since the integral is a pure complex number. For the second term, note that
[TABLE]
via the Stokes Theorem (85) and taking into account (53). We have computed the above limit by using the Convergence Dominated Theorem and (H3). Moreover, the sum is vanishing because we are using the symmetry sum. Using again the Stokes Theorem for the third term, one arrives at
[TABLE]
by definition of , which is given in (19). Again, the above limit is justified with the Convergence Dominated Theorem and (H3). ∎
In what follows, we will have to deal with the singularity in . But, there is a way to simplify the equation in order to control this singularity. We decompose as
[TABLE]
We can use Taylor formula (40):
[TABLE]
for and . In the case of , take and implying
[TABLE]
Let us check that :
[TABLE]
In virtue of (67), we get
[TABLE]
and then the nonlinear function can be simplified as follows
[TABLE]
We use the descomposition of in (4.1), and we are rewriting as
[TABLE]
since there is any contribution of .
In the next result, we provide how must depend on and .
Proposition 4.4**.**
Let satisfies the hypothesis (H1)–(H3) of Proposition 2.6 and Proposition 4.2, and
- (H4)
* uniformly in .*
The function , given by
[TABLE]
fulfills , where is defined in (19). The parameters satisfy: , , and is defined in (36).
Proof.
Note that
[TABLE]
via the Residue Theorem. We use the decomposition of given in (4.1). Let us begin with :
[TABLE]
Using (H4) and the Dominated Convergence Theorem, we get
[TABLE]
Note that the Dominated Convergence Theorem can be applied since the limit in (H4) is uniform. We can compute the above integrals in the following way
[TABLE]
where Note also that
[TABLE]
In this way,
[TABLE]
by the Residue Theorem. Let us move on . Here, we use also Taylor formula (40) for and , finding
[TABLE]
Let us check that , which is necessary to use Taylor formula:
[TABLE]
Note that
[TABLE]
For the other term, we achieve using (H4) that
[TABLE]
by the Residue Theorem and the definition of given in (19). Using the same ideas for , we find that
[TABLE]
and then,
[TABLE]
This implies that
[TABLE]
Finally, we find
[TABLE]
getting the announced result, i.e., ∎
Proposition 4.5**.**
Let satisfies the hypothesis (H1)–(H4) of Proposition 2.6, Proposition 4.2 and Proposition 4.4, and
- (H5)
* uniformly in .*
If sets (72), then
[TABLE]
with , is well–defined and . The spaces and are defined in (36)-(37) taking , and the parameters satisfy and .
Proof.
The proof has three steps: the symmetry of , regularity of , and regularity of .
* First step: Symmetry of .* Let us prove that with , i.e., checking that verifies . First, we work with showing that
[TABLE]
Second, we prove that analyzing the denominator and the numerator of its expression:
[TABLE]
and
[TABLE]
Thirdly, from the above computations we arrive at
[TABLE]
Now, we have that . Moreover, the condition (72) agrees with the fact that , we refer to the first step in the proof of Proposition 3.6 for more details.
* Second step: Regularity of .* In similarity with the Euler equations, we need to study first the denominator:
[TABLE]
where we have used the Residue Theorem. Then, if and , the denominator is not vanishing. Moreover, it is in and . By the expression of , it remains to study the regularity of :
[TABLE]
We use the decomposition of given in (4.1). First, we began with the continuity is both variables. Fixing , note from Proposition 4.4 that
[TABLE]
and then is continuous in . Now, fixing , by Lemma B.1 and (H3), we get easily that , for .
Secondly, we study the differentiability properties. Fix again , and we differentiate with respect to :
[TABLE]
The last expression is continuous when and now we aim to pass to the limit . By (H3) and (H4), we have that
[TABLE]
By using Proposition 4.4, we find
[TABLE]
which implies that
[TABLE]
Let us analyze the first term of (4.1). Using the decomposition (4.1), we begin with
[TABLE]
We use also the decomposition for given in (71). For the last term, one has that
[TABLE]
which is continuous in and . Moreover, (H5) implies that
[TABLE]
for any . Note that we can use the Dominated Convergence Theorem since the limit in (H5) is uniform. We can differentiate for and using once again (H5), we have that
[TABLE]
Let us now show the idea of , and will read similarly. Here, we use Taylor formula (40) as it was done in (4.1):
[TABLE]
These two expressions are smooth in . In fact, we can check that is continuous in and .
Now, fix and we focus on the regularity with respect to . The integral is the more delicate one since the kernel is singular. Remark the expression of this term:
[TABLE]
Then,
[TABLE]
For any , the above expression is continuous in by using Lemma B.1. Moreover, using (H4) we can obtain the limit when as
[TABLE]
Note that it agrees when differentiating with respect to in (73).
For the other two integrals, notice that and are not singular integrals due to it not vanishing for and neither , for any . This gives us that and are . Let us show the idea of :
[TABLE]
By Lemma B.1, the last expression is continuous in . Moreover, it does when and it is easy to check, with the help of the Convergence Dominated Theorem, that
[TABLE]
In the same way, one can check that is continuous in both variables and
[TABLE]
* Third step: Regularity of .* Since is in both variables and using the computations above concerning , one can easily check that is . ∎
4.2. Main result
Finally, we can announce the result concerning the desingularization of the point model (18) in the general system. We need to impose an extra condition to in order to obtain that the linearized operator is an isomorphism.
Theorem 4.6**.**
Consider satisfying (H1)–(H5) of Proposition (2.6), Proposition (4.2) and Proposition (4.4), and
- (H6)
**
Let , with and , and or . Then, there exist such that
[TABLE]
defines a horizontal translating solution of (60), with constant speed, for any and small enough . Moreover, is at least .
Proof.
Let us consider , with , and , defined in Proposition 4.5. By that proposition, it is in both variables. Moreover, Proposition 4.2 and Proposition and 4.4, give us that . In order to implement the Implicit Function Theorem, let us compute the linearized operator:
[TABLE]
By Proposition 4.4, then . In virtue of (4.1), we have
[TABLE]
which implies
[TABLE]
Then, we have
[TABLE]
On the other hand, using (78)-(79)-(80) we obtain
[TABLE]
which amounts to
[TABLE]
Note that defined by
[TABLE]
is a compact operator since it is smoothing. Since is a Fredholm operator of zero index, then so is. As a consequence, checking that is an isomorphism, it is enough to check that the kernel is trivial. We can compute the integrals involving in the linearized operator using (4.1), and finding
[TABLE]
where Note also that
[TABLE]
Finally, we achieve
[TABLE]
By (H6), we get that the kernel is trivial and then the linerized operator is an isomorphism. ∎
As a consequence, we get the result for the generalized surface quasi–geostrophic equation, meaning , for and . We just have to check that (H6) is verified and these computations are done in [20] for the vortex pairs.
Theorem 4.7**.**
Let , with and , and or . Then, there exists such that
[TABLE]
defines a horizontal translating solution of the generalized surface quasi-geostrophic equations for , with constant velocity speed, for any and small enough . Moreover, is at least .
Appendix A Special functions
This section recalls some definitions and properties about the Bessel functions. Let us define the Bessel function of the first kind and order by the expansion
[TABLE]
In addition, it is known that Bessel functions admit the following integral representation
[TABLE]
for . On the other hand, the Bessel functions of imaginary argument, denoted by and are defined by
[TABLE]
and
[TABLE]
An useful expansion for can be found in [42]:
[TABLE]
for . In the case that we concern, , it reads as
[TABLE]
where
[TABLE]
The constant is the Euler’s constant. Moreover, the following asymtotic behaviour at infinity for is given in [1]:
[TABLE]
Finally, the derivative of can be expressed by terms of Bessel functions. In particular, .
Appendix B Complex integrals and potential theory
This section concerns some complex integrals, in particular, the Stokes Theorem, the Cauchy–Pompeiu’s formula and some results on singular integrals.
The complex version of the Stokes Theorem reads as follows. Let be a simply connected domain and a scalar function, then
[TABLE]
where can be identify to the gradient operator in the same way
[TABLE]
Let us introduce now the Cauchy–Pompeiu’s formula. Consider be a complex function, then
[TABLE]
Finally, we deal with singular integrals of the type
[TABLE]
where being smooth off the diagonal. The next result focuses on the smoothness of the last operator, whose proof can be found in [17]. See also [19, 25, 27].
Lemma B.1**.**
Let and consider with the following properties. There exists such that
- (i)
* is measurable on and*
[TABLE]
- (ii)
For each , is differentiable in and
[TABLE]
Then,
- (1)
The operator defined by (87) is continuous from to . More precisely, there exists a constant depending only on such that
[TABLE] 2. (2)
For , the operator is continuous from to , for any . That is, there exists a constant depending only on such that
[TABLE]
The reference list from the paper itself. Each links out to its DOI / PubMed record.
- 1[1] M. Abramowitz, I. A. Stegun, Handbook of Mathematical Functions: With Formulas, Graphs, and Mathematical Tables. Courier Corporation, 1965.
- 2[2] H. Aref, On the equilibrium and stability of a row of point vortices. J. Fluid Mech. 290 (1995), 167–181.
- 3[3] J. Beichman, S. Denisov, 2D Euler equation on the strip: Stability of a rectangular patch. Comm. Part. Differ. Equat., 42 (2017), 100–120.
- 4[4] A. L. Bertozzi, P. Constantin, Global regularity for vortex patches. Comm. Math. Phys. 152 (1) (1993), 19–28.
- 5[5] J. Burbea, Motions of vortex patches. Lett. Math. Phys. 6 (1982), 1–16.
- 6[6] A. Castro, D. Córdoba, J. Gómez-Serrano, Existence and regularity of rotating global solutions for the generalized surface quasi-geostrophic equations. Duke Math. J. 165 (5) (2016), 935–984.
- 7[7] A. Castro, D. Córdoba, J. Gómez-Serrano, Uniformly rotating analytic global patch solutions for active scalars . J. Ann. PDE 2 (1) (2016), Art. 1, 34.
- 8[8] A. Castro, D. Córdoba, J. Gómez-Serrano, Uniformly rotating smooth solutions for the incompressible 2D Euler equations, ar Xiv:1612.08964, 2016.
