Well-posedness of strong solutions to the anelastic equations of stratified viscous flows
Xin Liu, Edriss S. Titi

TL;DR
This paper proves the existence and uniqueness of strong solutions to the anelastic equations modeling stratified viscous flows, including cases with vacuum singularities, with solutions existing globally in 2D and locally in 3D.
Contribution
It establishes well-posedness results for the anelastic equations with physical vacuum singularities, extending previous work to more realistic density profiles.
Findings
Global existence of solutions in 2D for general initial data
Local (and sometimes global) solutions in 3D for small initial data
Inclusion of vacuum singularities in the density profile
Abstract
We establish the local and global well-posedness of strong solutions to the two- and three-dimensional anelastic equations of stratified viscous flows. In this model, the interaction of the density profile with the velocity field is taken into account, and the density background profile is permitted to have physical vacuum singularity. The existing time of the solutions is infinite in two dimensions, with general initial data, and in three dimensions with small initial data.
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Well-posedness of strong solutions to the anelastic equations of stratified viscous flows
Xin Liu111Department of Mathematics, Texas A&M University, College Station, TX 77843, USA. Email: [email protected] and Edriss S. Titi222Department of Mathematics, Texas A&M University, College Station, TX 77840, USA. Department of Applied Mathematics and Theoretical Physics, University of Cambridge, Cambridge CB3 0WA, UK. Department of Computer Science and Applied Mathematics, Weizmann Institute of Science, Rehovot 76100, Israel. Email: [email protected] and [email protected]
(June 26, 2019)
Abstract
We establish the local and global well-posedness of strong solutions to the two– and three-dimensional anelastic equations of stratified viscous flows. In this model, the interaction of the density profile with the velocity field is taken into account, and the density background profile is permitted to have physical vacuum singularity. The existing time of the solutions is infinite in two dimensions, with general initial data, and in three dimensions with small initial data.
Keywords: anelastic approximation; well-posedness; physical vacuum; stratified flows
MSC: 35Q30; 35Q86; 76D03; 76D05
1 Introduction
The anelastic Navier-Stokes system for stratified flows,
[TABLE]
is derived as the limiting system of the compressible Navier-Stokes system after filtering out the acoustic waves for strong stratified flows. Here the velocity field and the pressure are the unknowns while the background density is given as a time-independent, negative function. The rigorous derivation of (1) can be found in [21]. Comparing to the incompressible Navier-Stokes system (see, e.g., [26, 5]), the main difference is the incompressible condition is replaced by the anelastic relation with the background density profile , which represents the strong stratification owing to the balance of the gravity and the pressure (see, e.g., [10]). Such an approximation preserves slight compressibility while filtering out the acoustic waves, which significantly simplifies the original compressible Navier-Stokes system, and enables more efficient computation applications to relevant model flows in physical reality. In particular, the anelastic approximation is used to describe the semi-compressible ocean dynamics (see, e.g., [7, 8]), as well as the tornado-hurricane dynamics (see, e.g., [22, 24]). We refer the readers to [23, 14, 20, 2, 1, 9, 15, 16] for related topics and comparisons of various models of the atmospheric and oceanic dynamics.
We remark that the background density profile in the anelastic relation is given by the resting state , where denotes the pressure potential and is the gravity acceleration. For the sake of simplifying the presentation, we have choosed the gravity to point upwards, which can be done after performing a vertical reflection of the coordinates. In the case when the flow connects to vacuum continuously, the resting state yields a degenerate density profile. For an isentropic flow with , this implies , referred to as the physical vacuum in the study of compressible flows (see, e.g., [17, 13]). The main characteristics of the physical vacuum is the Hölder continuity of the background density profile, whose derivatives are singular at . While there are some recent developments in the global stability of background solutions to compressible Euler or Navier-Stokes equations for one-dimensional or radial-symmetric flows (see, e.g., [19, 18, 12, 11]), the corresponding multi-dimensional problem is mostly open. On the other hand, after formally filtering out the acoustic waves by sending the Mach number and the Froude number to zero at the same rate in the compressible Navier-Stokes equations with physical vacuum, the resulting equations appear to be the aforementioned anelastic system with .
In this work, we aim at studying the well-posedness issue of strong solutions to (1) in , where denotes the spatial-dimension. Specifically, we will study system (1) with two kinds of density profiles:
[TABLE]
(See Remark 1, below.) After denoting the velocity field by its horizontal component and its vertical component , i.e., , where is a scaler if and a two-dimensional vector if , system (1) is complemented with the following stress-free and non-permeable boundary conditions, respectively,
[TABLE]
and initial data
[TABLE]
Compatibility conditions for are given by,
[TABLE]
where is the solution to the following elliptic problem
[TABLE]
Hereafter, for any subscript , we will alway use the letter to denote the horizontal velocity, to denote the vertical velocity, and to denote the velocity field, i.e., .
Remark 1**.**
The meaning of (2) is that the non-degenerate profile can be extended as a non-degenerate and smooth function in .
On the other hand, one can replace in (3) with any density profile which satisfies the aforementioned physical vacuum near (i.e., near ), and is smooth and non-degenerate at . The requirement of smoothness and the non-degeneracy of the density profile at is owing to technical reasons.
Remark 2**.**
We require the supports of and to be away from the boundary . This can be modified as follows:
[TABLE]
Equation (7) should be considered as a compatibility condition of .
In comparison to the Navier-Stokes system (see, e.g., [5]), the density profile interacts with the velocity field. To explain this statement, let us forget about the boundary and consider (1) in for a moment. Also we assume the density profile is non-degenerate and smooth. Let be any smooth vector field, and suppose that it can be decomposed, in analogy with the Helmholtz decomposition, as
[TABLE]
where , and is a smooth function. One can see that and are orthogonal in , i.e., the square–integrable space with respect to the measure , where is the Lebesgue measure. Then one can easily see that, the –regularity of , , depends not only on the regularity of , but also on that of . Such an interaction of in the -regularity estimates causes the main difficulty in the study of strong solutions. As one will see later, one will need to consider the interaction of the pressure term with the nonlinearity term as well as the viscosity term . We take advantage of the regular density profile in (2), and consider an associated problem in , whose solutions satisfies (1) in . Then we employ an elementary approach in the Galerkin’s approximation which takes into account the aforementioned interactions. After studying the regularity, we restrict our solutions back to the original domain and obtain a unique strong solution to (1) with (4) in the non-degenerate case, i.e., (2).
To deal with the physical vacuum profile in (3), we approximate the problem with a sequence of non-degenerate profiles in the class of (2). The existence theorem in the non-degenerate case yields a sequence of approximating solutions. Then we derive the necessary uniform weighted estimates. To handle the physical vacuum density profile, the desired strong solutions to (1) in the physical vacuum case, i.e., (3), are constructed as the limit of the approximating sequence. However, the solutions that we obtain lack regularity on the boundary , due to the weighted estimates. In particular, the solutions are not regular enough to have trace of on , which causes troubles when one try to show the uniqueness of solutions. We employ the arguments originated in [25] for the Navier-Stokes system to establish the uniqueness of strong solutions.
Next, we sum up the main theorems. The first theorem concerns the local well-posedness of strong solutions to (1):
Theorem 1**.**
Let satisfy either (2) or (3). Consider initial data satisfying (5) and (6). There exists a unique strong solution to (1) with (4) in , for some . In the case of (2), the strong solution satisfies the regularity:
[TABLE]
In the case of (3), the strong solution satisfies the regularity:
[TABLE]
See section 2 for the notations etc..
We refer the detailed description of local well-posedness to Theorem 3 and Theorem 4, below. At the same time, we also have the following theorem concerning global well-posedness of strong solutions:
Theorem 2**.**
Under either one of the following conditions, the existing time of the local strong solutions constructed in Theorem 1 becomes infinite:
;
- 2.
, provided initial velocity satisfies, for satisfying either (2) or (3),
[TABLE]
with some , small enough.
Notice that, by taking , Theorems 1 and 2 apply to the homogeneous Navier–Stokes equations (see, e.g., [26]). The compatibility conditions in (6) are similar to those in the study of the non-homogeneous incompressible Navier–Stokes equations (see, e.g., [6]).
The rest of this work is organized as follows. In section 2, we summarize the notations, definitions and inequalities which will be used in this paper. In section 3, we construct the local strong solutions to (1) with the non-degenerate density profile. In section 4, we consider (1) with the physical vacuum profile, when the uniform estimates and approximation arguments are presented. These two sections finish the proof of Theorem 1. In the last two sections, i.e., sections 5 and 6, we employ some global a priori estimates, which lead to the proof of Theorem 2.
2 Preliminaries
Throughout this paper, we use the following definition of strong solutions:
Definition 1** (Strong solutions).**
* is called a strong solution to (1) if system (1) holds almost everywhere in .*
We use the notation to denote the spatial derivative in the horizontal direction, i.e. derivative with respect to , when , and for , when ; the notation to denote the spatial derivative in the vertical direction; the notation to denote the temporal derivative; for is short for ; also and for are short for . are used to denote the divergence, the gradient, the Laplace, respectively, in horizontal direction, i.e.
[TABLE]
In addition, we abuse the notation:
[TABLE]
are used to denote or , depending on the context.
Also, we summarize the symmetric-periodic extensions in the following:
Definition 2** (Symmetric-periodic extensions).**
For any smooth function defined in , one can extend it to an even function in , using the even-symmetric extension , defined by
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In addition, if , one can also extend to a odd function in , using the odd-symmetric extension , defined by
[TABLE]
Also, for any smooth function defined in , one can extend it to a function in using the periodic extension , defined by
[TABLE]
Then the even-symmetric-periodic extension operator is defined by
[TABLE]
The odd-symmetric-periodic extension operator is defined by
[TABLE]
To study (1) in the case of physical vacuum, i.e., (3), we will need to apply the following Hardy-type inequalities:
Lemma 1** (Hardy-type inequalities).**
Let be a real number. Suppose that a function satisfies . Then for some positive constant , independent of , one has
for ,
[TABLE] 2. 2.
for ,
[TABLE]
In particular, after taking in (13) and (14), one will arrive at the standard Hardy’s inequalities.
Proof.
Inequality (13): . The mean value theorem guarantees that there is a such that . Then applying the Fundamental Theorem of Calculus and the Fubini’s theorem yields, since ,
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where is an arbitrary constant and . Then after choosing small enough, this finishes the proof of (13).
Inequality (14): . Without loss of generality, we assume . Then, again, the Fundamental Theorem of Calculus implies that . Thus, since ,
[TABLE]
Thus (14) follows. ∎
3 The non-degenerate case
Recall that our goal is to construct the local strong solutions to the anelastic Navier-Stokes equations, (1), i.e.,
[TABLE]
with (4) in the case of non-degenerate background density profiles, i.e., (2). In fact, we will only need and
[TABLE]
Recall that, , .
Our strategy of constructing solutions is: first, we introduce a problem in , which is associated with (15); then we construct the solutions with enough regularity to the associated problem; by restricting such solutions to the associated problem back in , we obtain the required solutions to (15).
The following theorem is the main part of this section:
Theorem 3**.**
Let be a strict positive scalar function in that satisfies (16). Consider initial data satisfying (5) and (6). Then there exists a unique strong solution to (15), with (4), in , for some . Moreover, the strong solution satisfies the following regularity:
[TABLE]
Furthermore, the following estimates hold:
[TABLE]
where depends only on the initial data and
[TABLE]
Also, one can choose to satisfy
[TABLE]
In addition, let be strong solutions with initial data , respectively. Then the following estimate holds,
[TABLE]
where is the co-existence time of the solutions, and depends on the initial data and .
Remark 3**.**
We observe that conditions (6) and (16) are essential factors in Theorem 3. See Remark 4 and Remark 5, below.
In fact, we will only show the proof of Theorem 3 when . The case when is similar and we omit it for the sake of clarity of our presentation. The proof is done in the following steps: introducing the associated problem via the symmetric-periodic extension; introducing the Galerkin approximating problem; establishing existence of strong solutions; improving the regularity; establishing uniqueness and continuous dependency on the initial data.
Step 0: the associated problem. We observe that system (15) is invariant with respect to the following symmetry:
[TABLE]
Recalling , that is to say, by extending any solution to system (15) to
[TABLE]
satisfies the same equations as in system (15) in domain .
Then the new system for the extended functions is invariant with respect to translation . Thus, we further extend periodically in the -variable by applying to . Combining these two extensions together, we obtain,
[TABLE]
and satisfies the same equations as in system (15) in domain .
Therefore, we end up with the same set of equations as in system (15) in periodic domain , and for simplicity, the same notations are used to denote . Such a convention will be adopted in the following. Then we have got the following system,
[TABLE]
with symmetry (SYM). We adopt initial data for (15’), which we will denote by the same notation as the original initial data, i.e., . Notice, the boundary conditions in (4) are automatically implied by symmetry (SYM). In the next step, a Galerkin approximating procedure will be used to construct solutions to (15’).
Step 1: the Galerkin approximating problem. Given any non-negative integer , we consider the finite dimensional space, denoted by and defined as follows:
[TABLE]
Notice that, the dimension of over is . Also, we define the lower--frequency projection operator , , as follows.
[TABLE]
Then projects with symmetry (SYM) into via , where we have taken .
Consider any non-negative integer and with given as in (20). To solve the problem (15’), we consider the following system of ODE:
[TABLE]
To find a solution , with , for some to (22), we will need to reformulate (22) into a system of dimension . In fact, we claim that can be represented as functions of by inverting a linear algebraic system of dimension , and one can derive a first-order ODE system for of dimension .
Taking and to and , respectively, and summing the results together yield, using ,
[TABLE]
which is, due to the even symmetry and the strict positivity of , a non-singular linear system with the unknowns of dimension . Thus after solving for , (22) can be written as the following dimensional system,
[TABLE]
In particular, and form the dimensional ODE system of . We remark that, is preserved by the solutions to (23) with compatible initial data, since (23) implies that \partial_{t}\bigl{[}\partial_{x}\mathbb{P}_{m}(\rho v_{m})+\partial_{z}\mathbb{P}_{m}(\rho w_{m})\bigr{]}=0. Also, it is easy to verify, after solving for with given via and substituting the solutions to and , we will have an ODE system of the form
[TABLE]
with being locally Lipschitz continuous, in fact quadratic functions, with respect to the arguments. Here we need again that is strictly positive. Then the existence theorem of ODE systems yields that given initial data
[TABLE]
where , with , is determined by solving, as above, the non-singular linear algebraic system
[TABLE]
there exists a solution to system (23), or equivalently system (22), for some positive constant .
We remark that, as , in . In fact, owing to the fact , the elliptic estimate yields, as ,
[TABLE]
Hence (v_{m},w_{m})\big{|}_{t=0} is an approximation of .
Remark 4**.**
We remind the reader that the smoothness of in (i.e., (16)) is essential in showing (24).
Step 2: existence of strong solutions. In order to pass the limit in (22) to obtain a solution to (15’), we need to establish that the existence time , obtained above, is independent of . This is done via some uniform-in- estimates. Let be the maximal existing time of the solutions . All the estimates below in this step are done in the time interval .
After taking the -inner product of and with and , respectively, summing up the resulting equations and applying integration by parts yield,
[TABLE]
where we have used . Next, we take the -inner product of and with and , respectively. Similarly, after summing up the resulting equations and applying integration by parts, one will have, since has uniform upper bound and strictly positive lower bound,
[TABLE]
where we have applied the two-dimensional Sobolev embedding inequality. Thus, we have, after applying Young’s inequality and (25),
[TABLE]
In order to estimate , we rewrite and in the following pressure-viscosity form:
[TABLE]
which yield
[TABLE]
Meanwhile, direct calculations show that
[TABLE]
Since
[TABLE]
we have, after applying integration by parts,
[TABLE]
where we need . Therefore, (28) and (29) imply,
[TABLE]
On the other hand, taking the -inner product of with yields
[TABLE]
Therefore, after applying the two-dimensional Sobolev embedding inequality, together with the fact that is strictly positive, we arrive at
[TABLE]
[TABLE]
Consequently, (26) and (32) yield
[TABLE]
Thus, (33) implies that, there exists , independent of , such that
[TABLE]
where depends only on the initial data and , and is independent of . Then, after passing with a suitable subsequence according to the weak compactness theorem of Sobolev spaces and Aubin’s compactness theorem (see, e.g., [26]), we have obtianed
[TABLE]
such that
[TABLE]
Thus it is easy to verify that is a strong solution to (15’) with (35), which satisfies, according to (34),
[TABLE]
Step 3: improving the regularity. In this step, we establish the regularity of solution to (15’) via some a priori estimates. In the following, we use to denote a generic constant depending only on the initial data and on
[TABLE]
Here we focus with our estimates over . We emphasize that all the estimates in this step are formal and can be proved rigorously via the Galerkin method.
First, we obtain the time-derivative estimate. After applying a time derivative to , the resulting equation is
[TABLE]
Then after taking the -inner product of (37) with , one has
[TABLE]
The right-hand side of (38) can be estimated as follows:
[TABLE]
Together with Young’s inequality, (38) and (39) imply
[TABLE]
Thus applying Grönwall’s inequality to the above yields, together with (36),
[TABLE]
where is given in step 2. Then, following similar arguments as in (32), one can obtain,
[TABLE]
Next, we will sketch the estimate of . First, applying to yields,
[TABLE]
After taking the -inner product of (42) with and applying integration by parts, we obtain
[TABLE]
where we have applied (40), (41), Hölder’s and the Sobolev embedding inequalities. Then, after noticing and using (42), (43) implies
[TABLE]
Moreover, since
[TABLE]
one can also derive
[TABLE]
What is left is to obtain the estimate of , or equivalently, the estimate of . We rewrite , after multiplying it with and applying to the resulting, as,
[TABLE]
where we have used and the identity
[TABLE]
Thus we have
[TABLE]
which yields, together with (40) and (41),
[TABLE]
Then (40), (45) and (47) yield
[TABLE]
Now we can restrict the solution in . It is easy to verify is the strong solution to (15) with the boundary condition (4), and it satisfies (17) owing to (40), (41), and (48). In particular, the regularity of allows us to take the trace of on the boundary, and it follows from the construction that satisfies (18).
Step 4: uniqueness and continuous dependency on the initial data. Let , be two strong solutions to (15) with initial data , respectively, and satisfy the estimates in (17) for , respectively. That is
[TABLE]
where depend only on the initial data and
[TABLE]
In the following, we denote and . Also, let . Then satisfies
[TABLE]
Then taking the -inner product of with yields
[TABLE]
Then applying Grönwall’s inequality yields (19).
In particular, for , we have and .
This finishes the proof of Theorem 3 in the case when . The case when follows by similar arguments, employing the three-dimensional Sobolev embedding inequalities.
Remark 5**.**
It is worth stressing that thanks to the uniqueness of solutions in Step 4, all strong solutions to (15) with (4) with the same initial data as described in Theorem 3 should be equal to the one constructed by our extension-restriction techniques through Step 0 to Step 3.
4 The physical vacuum profile
This section will discuss the anelastic equations (1) with (4) in the case of physical vacuum density profile, i.e., (2). We remind the reader that
[TABLE]
Thus in this section, we will study the following system,
[TABLE]
and we will show the following theorem:
Theorem 4**.**
Consider , and initial data as in (5), satisfying the compatibility condition (6), with replaced by . There exists a positive constant and a unique strong solution to the anelastic equations (51) with the boundary condition (4) in , which satisfies the following regularity:
[TABLE]
In addition, we have the estimates
[TABLE]
where depends only on the initial data. Suppose that there are two solutions with initial data in time interval . Then
[TABLE]
for some constant depending on initial data and .
Apparently, is well-defined for and it is smooth at , and is smooth except . We refer to Remark 1 about .
Our strategy is to apply Theorem 3 to obtain a sequence of approximating solutions. To do this, we first have to construct an approximating sequence of . We start with a lemma.
Lemma 2**.**
For any fixed , there exists a function , which satisfies the following properties:
, and the convergence is uniform; 2. 2.
; 3. 3.
* is non-decreasing for ;* 4. 4.
* for ;* 5. 5.
, for all , for some constant , which is independent of .
Proof.
Let be a nondecreasing function satisfying,
[TABLE]
Then , and
[TABLE]
and . Then one can choose the values of for such that satisfies Properties 1–5. ∎
Remark 6**.**
Property 4 in Lemma 2 implies that Hardy’s inequalities in Lemma 1 can be applied with replaced by .
We take . Then is an approximating sequence of . In addition, for any fixed , satisfies (16) and . We also choose initial data such that in , , and the compatibility conditions in (6) hold with replaced by .
We recall that satisfies the compact support condition in (5). Thus for small enough and as constructed in Lemma 2, one can simply take .
Then applying Theorem 3, we obtain a sequence of solutions to (15) with , which is denoted as . That is, for some ,
[TABLE]
where ,
[TABLE]
The boundary condition (4) is satisfied with replaced by , and is chosen such that
[TABLE]
After passing the limit , we will obtain a solution to (51). We establish the required uniform estimates in the following two lemmas.
Lemma 3**.**
For any fixed , assume that and is the solution to (53) as mentioned above. There exists a constant independent of , such that the following estimates hold:
[TABLE]
where is a constant depending only on initial data.
Proof.
Taking the -inner product of with implies, after substituting and (4),
[TABLE]
In the meantime, the -inner product of with implies, similarly,
[TABLE]
The right-hand side of (57) can be estimated as follows,
[TABLE]
where we have used Property 4 in Lemma 2. Notice, after applying the Sobolev embedding inequality and the Hardy-type inequality in Lemma 1, one can derive
[TABLE]
provided , or equivalently, , where we have used Property 4 in Lemma 2.
On the other hand, after applying a time derivative to , the resulting equation is
[TABLE]
Then after taking the -inner product of (60) with , the result is
[TABLE]
Similarly, the right-hand side of (60) can be estimated as follows,
[TABLE]
Therefore, combining (56), (57), (58), (59), (61) and (62) gives us
[TABLE]
where we have used Property 4 in Lemma 2 and applied Young’s inequality. In particular, the above yields (55) for a short time. ∎
Next, to obtain the estimates of the spatial derivatives of requires a little work. In fact, we shall proceed with the following steps:
- obtain estimate for the horizontal derivative; 2. obtain estimate for the pressure; 3. obtain estimate for the -norm of . In conclusion, we will obtain the following:
Lemma 4**.**
In addition to the assumptions in Lemma 3, assume that . Then
[TABLE]
In particular, (63) together with (55) yields,
[TABLE]
where is the same as in (55), and is some constant depending only on initial data and is independent of .
Proof.
As mentioned above, we establish the proof in three steps.
Step 1: Obtain estimate for the horizontal derivative. Taking the -inner product of with implies
[TABLE]
Then, applying Hölder’s and the Sobolev embedding inequalities to the right-hand side of (65) yields that, together with Property 4 in Lemma 2,
[TABLE]
Therefore (65) implies
[TABLE]
Step 2: Obtain estimate for the pressure. Notice
[TABLE]
Therefore, after multiplying with and applying to the resulting equation, we end up with
[TABLE]
Recall that satisfies (54), and the integration by parts in the following is allowed.
Thus, after taking the -inner product of (68) with and applying integration by parts in the resultant using the boundary conditions (4) and (54), we arrive at
[TABLE]
where
[TABLE]
Now we need to evaluate the right-hand side of (69). Indeed, applying the Hölder and the Sobolev embedding inequalities in yields
[TABLE]
To estimate , notice that from and (4), we have
[TABLE]
Then after substituting (70) in and applying integration by parts, it follows,
[TABLE]
Then applying Properties 4 and 5 in Lemma 2 and the Hölder inequality yields,
[TABLE]
where in the last inequality, we have applied Hardy-type inequality in the vertical direction (see Lemma 1), with , i.e., .
Therefore, (69) implies, for ,
[TABLE]
Step 3: Obtain estimate for . We rewrite as,
[TABLE]
Then directly, we have
[TABLE]
where the last term on the right-hand side can be estimated as
[TABLE]
Notice,
[TABLE]
Consequently, (66), (72) and (74) yield (63).
Now we collect (55) and (63) to finish the proof. Indeed, after applying the Hardy-type inequality in Lemma 1, we have the following inequalities
[TABLE]
Therefore, together with Property 4 in Lemma 2, (55), (63) and (76) imply the estimates in (64). ∎
With (64), we claim that, as , converges to a strong solution to (51). Indeed, consider , where is a scalar function, when , a two-dimensional vector field, when . Here is the space of functions which are periodic in the horizontal variables and are of compact support in the vertical variable. Then we have,
[TABLE]
(64) implies that there exist with
[TABLE]
satisfying the estimate in (52), , and
[TABLE]
where we have used Property 1 in Lemma 2. Thus we have , and after passing the limit with , in (77), we have
[TABLE]
which verifies that is a solution to (51) in . We recall that is chosen such that its support is away from . Moreover, it is easy to verify
[TABLE]
On the other hand, the trace theorem implies that \rho_{\mathrm{pv}}\partial_{z}v\big{|}_{z=0},\partial_{z}v\big{|}_{z=1},w\big{|}_{z=0,1}\in L^{2}(0,T;L^{2}(2\mathbb{T}^{n-1})), thanks to the regularity in (78). Thus
[TABLE]
To verify the boundary condition \partial_{z}v\big{|}_{z=0}=0 in (4), consider \psi_{h,\varepsilon}(x,z,t):=\bigl{(}1-c_{\varepsilon}q_{\varepsilon}(z)\bigr{)}\psi_{1}(x,t) with for some constant satisfying
[TABLE]
Consider with given as above and
[TABLE]
Then satisfies \mathrm{div}\bigl{(}q_{\varepsilon}^{\alpha}\vec{\psi}_{\varepsilon}\bigr{)}=0, \psi_{v,\varepsilon}\big{|}_{z=0,1}=0, and as , uniformly, where
[TABLE]
Now we choose in (77). After applying integration by parts, we arrive at
[TABLE]
which, together with (64) and the trace theorem, implies that
[TABLE]
Notice that, Property 4 in Lemma 2 implies for small enough. Thus, (82) yields that \{\partial_{z}v_{\varepsilon}\big{|}_{z=0}\} is uniformly bounded in and thus as ,
[TABLE]
In particular, \partial_{z}v\big{|}_{z=0}=0~{}\text{in}~{}L^{2}(0,T;L^{2}(2\mathbb{T}^{n-1})) and so we have verified the boundary conditions in (4).
In addition, consider and . Then, is a functional which acts on by the duality
[TABLE]
Moreover, from (81), one can infer that is a functional acting on . In particular, if , we have
[TABLE]
Consequently, the regularity of , as in (78), allows us to consider the action of on . That is, the following equation holds in ,
[TABLE]
Thus we have the energy identity, for any ,
[TABLE]
With such properties, we are able to show the uniqueness of solutions. Consider being solutions to (51) as above with initial data . Also, denote as the existence time for both solutions. Then consider the actions of for with and for with . Summing up the results leads to, for any ,
[TABLE]
Notice, after applying and integration by parts, we have
[TABLE]
where the last inequality follows by applying Hardy’s inequality in Lemma 1 and the fact that for .
Therefore, (84), together with the energy identity (83) for , implies
[TABLE]
Then applying Grönwall’s inequality yields,
[TABLE]
for some constant depending on and the initial data . In particular, this implies the uniqueness of solutions.
We remark that the above uniqueness argument is similar to the one used by J. Serrin for weak-strong uniqueness of three-dimensional Navier–Stokes equations in [25].
5 Global-in-time a priori estimates when
In this and the following sections, we present some global-in-time a priori estimates of solutions to (51). These arguments can be rigorously justified following the arguments in sections 3 and 4. The estimates of solutions to (15) are similar, and will be omitted.
Notice that, the regularity of in (78) allows us to take the following actions. Taking the -inner product of with implies, as in (56),
[TABLE]
As in (57), we also have,
[TABLE]
The right-hand side of (87) can be estimated as follows, due to the fact that ,
[TABLE]
where we have applied Young’s inequality and the two-dimensional Brezis-Gallouate-Wainger inequality (see, e.g., [3, 4]).
Meanwhile, the same arguments as (60) through (61) imply the similar estimate to (61), i.e.,
[TABLE]
where
[TABLE]
In addition, due to the fact that for , applying Hardy’s inequality in Lemma 1 yields, with ,
[TABLE]
On the other hand, similar to (63),
[TABLE]
Then together with (87), (88) , we arrive at
[TABLE]
where
[TABLE]
Also, (86) implies, for any ,
[TABLE]
for some positive constant independent of . Therefore, (91) implies that
[TABLE]
Thus applying Grönwall’s inequality yields, together with (92),
[TABLE]
for some constant depending only on the initial data. (92) and (93) imply the global well-posedness.
6 Small data global-in-time a priori estimates when
Similarly, the estimates in (86), (87) and (88) hold. That is,
[TABLE]
We estimate the nonlinearities on the right-hand side of (87) and (88) as follows,
[TABLE]
Then, after denoting
[TABLE]
(86), (87), (88), (89) and (90) imply
[TABLE]
which implies, for small enough,
[TABLE]
Thus we have shown the global well-posedness with small initial data.
Acknowledgements
This work was supported in part by the Einstein Stiftung/Foundation - Berlin, through the Einstein Visiting Fellow Program, and by the John Simon Guggenheim Memorial Foundation.
The reference list from the paper itself. Each links out to its DOI / PubMed record.
- 1[1] Pierre-Antoine Bois. A unified asymptotic theory of the anelastic approximation in geophysical gases and liquids. Mech. Res. Commun. , 33(5):628–635, 2006.
- 2[2] Stanislav I. Braginsky and Paul H. Roberts. Anelastic and Boussinesq approximations. In Encycl. Geomagn. Paleomagn. , pages 11–19. Springer Netherlands, Dordrecht.
- 3[3] Haim Brezis and Thierry Gallouet. Nonlinear Schrödinger evolution equations. Nonlinear Analysis: Theory, Methods and Applications , 4(4):677–681, 1980.
- 4[4] Haim Brezis and Stephen Wainger. A note on limiting cases of Sobolev embeddings and convolution inequalities Communications in Partial Differential Equations , 5(7):773–789, 1980.
- 5[5] Peter Constantin and Ciprian Foias. Navier-Stokes Equations . Chicago Lectures in Mathematics. 1988.
- 6[6] Hi Jun Choe and Hyunseok Kim Strong solutions to the Navier–Stokes equations for nonhomogeneous incompressible fluids. Communications in Partial Differential Equations , 28(5–6):1183–1201, 2003.
- 7[7] W. K. Dewar, J. Schoonover, T. J. Mc Dougall, and W. R. Young. Semicompressible ocean dynamics. J. Phys. Oceanogr. , 45(1):149–156, 2015.
- 8[8] William Dewar, Joseph Schoonover, Trevor Mc Dougall, and Rupert Klein. Semicompressible ocean thermodynamics and Boussinesq energy conservation. Fluids , 1(2):9, apr 2016.
