Global H\"older estimates for 2D linearized Monge-Amp\`ere equations with right-hand side in divergence form
Nam Q. Le

TL;DR
This paper proves global H"older continuity estimates for solutions to 2D linearized Monge-Amp ext`ere equations with divergence-form right-hand side, relevant in meteorology and convex functional approximation.
Contribution
It introduces affine invariant, degenerate H"older estimates for these equations under natural boundedness assumptions, extending classical second order elliptic estimates.
Findings
Estimates hold under natural domain and boundary conditions.
Results are affine invariant and applicable to degenerate cases.
Applicable in meteorology and convex functional approximation.
Abstract
We establish global H\"older estimates for solutions to inhomogeneous linearized Monge-Amp\`ere equations in two dimensions with the right hand side being the divergence of a bounded vector field. These equations arise in the semi-geostrophic equations in meteorology and in the approximation of convex functionals subject to a convexity constraint using fourth order Abreu type equations. Our estimates hold under natural assumptions on the domain, boundary data and Monge-Amp\`ere measure being bounded away from zero and infinity. They are an affine invariant and degenerate version of global H\"older estimates by Murthy-Stampacchia and Trudinger for second order elliptic equations in divergence form.
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Global Hölder estimates for 2D
linearized Monge–Ampère equations with right-hand side in divergence form
Nam Q. Le
Department of Mathematics, Indiana University, Bloomington, IN 47405, USA
Abstract.
We establish global Hölder estimates for solutions to inhomogeneous linearized Monge–Ampère equations in two dimensions with the right hand side being the divergence of a bounded vector field. These equations arise in the semi-geostrophic equations in meteorology and in the approximation of convex functionals subject to a convexity constraint using fourth order Abreu type equations. Our estimates hold under natural assumptions on the domain, boundary data and Monge-Ampère measure being bounded away from zero and infinity. They are an affine invariant and degenerate version of global Hölder estimates by Murthy-Stampacchia and Trudinger for second order elliptic equations in divergence form.
Key words and phrases:
Linearized Monge-Ampère equation, global Hölder estimates, Green’s function
2010 Mathematics Subject Classification:
35J70, 35B65, 35B45, 35J96
The research of the author was supported in part by NSF grant DMS-1764248.
1. Introduction and statement of the main result
In this paper, we establish global Hölder estimates for solutions to inhomogeneous linearized Monge–Ampère equations in two dimensions with the right hand side being the divergence of a bounded vector field; see Theorem 1.2. Theorem 1.2 is an affine invariant and degenerate version of global Hölder estimates by Murthy-Stampacchia [19] and Trudinger [24] for second order elliptic equations in divergence form with coefficient matrices together with their inverses having highly integrable eigenvalues. Our global Hölder estimates hold under natural assumptions on the domain, boundary data and Monge-Ampère measure being bounded away from zero and infinity. They are the global counterpart of the interior Hölder estimates recently established in [13] that we will recall in Theorem 1.1. A crucial tool for our global Hölder estimates is the global estimates for the Green’s function of the linearized Monge-Ampère operator in two dimensions established in Theorem 2.1. An application of Theorem 1.2 to solvability of singular, fourth order Abreu type equations will be presented in Theorem 1.3.
Let () be a bounded convex domain and let be a locally uniformly convex function on . The linearized Monge-Ampère equations corresponding to are of the form
[TABLE]
where
[TABLE]
is the cofactor matrix of the Hessian matrix . The operator appears in several contexts including affine differential geometry [25], complex geometry [7], and fluid mechanics [1, 2, 5, 16, 17]. In these contexts, one usually encounters the linearized Monge-Ampère equations with the Monge-Ampère measure satisfying the pinching condition
[TABLE]
In this paper, we focus our attention to (1.1) under (1.2). Notice that since is positive semi-definite, is a linear elliptic partial differential operator, possibly both degenerate and singular. Caffarelli and Gutiérrez initiated the study of the linearized Monge-Ampère equations in the fundamental paper [4]. There they developed an interior Harnack inequality theory for nonnegative solutions of the homogeneous equation in terms of the pinching of the Hessian determinant in (1.2). This theory is an affine invariant version of the classical Harnack inequality for linear, uniformly elliptic equations with measurable coefficients. As a consequence, they obtained interior Hölder estimates for the homogeneous linearized Monge-Ampère equation .
For the inhomogeneous equation (1.1) with right hand side where , Nguyen and the author [15] recently established an interior Harnack inequality, interior Hölder estimates, and global Hölder estimates for solutions under natural conditions when , which is the optimal range of . The interior and global Hölder estimates, respectively, in [15] rely heavily on the corresponding interior and global high integrability of Green’s function of the linearized Monge–Ampère operator established in [11, 12].
Regarding Hölder estimates, less is know about (1.1) when the right hand side is the divergence of a bounded vector field. This type of inhomogeneous linearized Monge-Ampère equations arises in the semi-geostrophic equations in meteorology [1, 2, 5, 13, 16, 17]. They also appear in second boundary value problems of fourth order equations of Abreu type arising from approximation of convex functionals whose Lagrangians depend on the gradient variable, subject to a convexity constraint; see [14]. These functionals arise in different scientific disciplines such as Newton’s problem of minimal resistance in physics and monopolist’s problem in economics [3, 20].
In the case of the semi-geostrophic equations in meteorology, when the Monge-Ampère measures are continuous, interior Hölder estimates for solutions to (1.1) were obtained by Loeper [16]. However, when the measures are only bounded away from zero and infinity, up to now, interior Hölder estimates have only been obtained in two dimensions [13] which we recall here:
Theorem 1.1** (Interior Hölder estimates, [13]).**
Assume . Let be a convex function satisfying in . Let is a bounded vector field. Given a section . Let . There exist a universal constant depending only on and and a constant , depending only on , , and with the following property. For every solution to
[TABLE]
in , and for all , we have the Hölder estimate:
[TABLE]
In Theorem 1.1, the section of a convex function at with height is defined by
[TABLE]
When , Theorem 1.1 was established, in all dimensions, by Caffarelli and Gutiérrez in [4]. Because is divergence-free, that is, for all , we can also write as a divergence form operator:
[TABLE]
Thus, Theorem 1.1 can be viewed as an affine invariant version of related results by Murthy-Stampacchia [19] and Trudinger [24] for second order elliptic equations in divergence form. These authors studied the maximum principle, local and global estimates, local and global regularity for degenerate elliptic equations in the divergence form
[TABLE]
where is nonnegative symmetric matrix, and is a bounded vector field in . To obtain the Hölder regularity for solutions to (1.4), Murthy-Stampacchia and Trudinger required the high integrability of the eigenvalues of and their inverses. By Wang’s counterexamples [27] to estimates for the Monge-Ampère equations, this condition fails for the matrix in Theorem 1.1 (even in two dimensions) when the ratio is large.
A natural question regarding Theorem 1.1 is whether one can obtain the global Hölder estimates for solutions to (1.3) under suitable boundary conditions. In this paper, we answer this question in the affirmative in two dimensions. Precisely, we obtain:
Theorem 1.2** (Global Hölder estimates).**
Let be a bounded convex domain. Assume that . Assume that there exists a small constant such that
[TABLE]
Let be a convex function satisfying
[TABLE]
Assume further that on , separates quadratically from its tangent planes, namely
[TABLE]
Let be a continuous function that solves the linearized Monge-Ampère equation
[TABLE]
where is a function defined on and . Then, there are positive constants and depending only on such that the following global Hölder estimates hold:
[TABLE]
The global Hölder estimates in Theorem 1.2 are an affine invariant and degenerate version of global Hölder estimates by Murthy-Stampacchia [19] and Trudinger [24] for second order elliptic equations in divergence form. Our proof of Theorem 1.2 relies heavily on the new global high integrability of the gradient of Green’s function of the linearized Monge-Ampère operator in two dimensions. It is an open question whether our interior and global Hölder estimates for (1.8) can be obtained in higher dimensions.
We note from [21, Proposition 3.2] that the quadratic separation (1.7) holds for solutions to the Monge-Ampère equations with the right hand side bounded away from [math] and on uniformly convex domains and boundary data.
In the next theorem, we give an application of Theorem 1.2 to solvability of the second boundary value problem of singular, fourth order, fully nonlinear equations of Abreu type; see [14] for a different approach using global Hölder estimates for linearized Monge-Ampère equation with right hand side having low integrability.
Theorem 1.3**.**
Let be an open, smooth, bounded and uniformly convex domain. Let and with . Then there exists a unique smooth, uniformly convex solution to the following second boundary value problem:
[TABLE]
Here is the cofactor matrix of , that is, .
The rest of the paper is devoted to proving Theorems 1.2 and 1.3. We use a priori estimates and degree theory to prove Theorem 1.3. Note that the right hand side of the first equation in (1.9) is the p-Laplacian with :
[TABLE]
We can assume that all functions , in this paper are smooth. However, our estimates do not depend on the assumed smoothness but only on the given structural constants.
The analysis in this paper will be involved with and satisfying either the global conditions (1.5)-(1.7) or the following local conditions (1.10)-(1.13).
Let be a bounded convex set with
[TABLE]
for some small where we denote . Assume that
[TABLE]
Let be a convex function satisfying
[TABLE]
We assume that on , separates quadratically from its tangent planes on , that is, if then
[TABLE]
We will use the letters , etc, to denote *universal * constants that depend only on the structural constants and/or . They may change from line to line.
In Section 2, we establish global estimates for the Green’s function of the linearized Monge-Ampère operator under (1.2). In Section 3, we establish bounds and Hölder estimates at the boundary for solutions to (1.8). The proofs of Theorems 1.2 and 1.3 will be given in Section 4.
2. Global estimates for the Green’s function
Let be the Green’s function of in with pole where ; that is is a positive solution of
[TABLE]
with denoting the Dirac measure giving unit mass to the point .
Let be a small universal constant appearing in the global high integrability estimate [15, inequality (5.12)] for the Green’s function of .
Our main tools in this paper are following global estimates for the gradient of the Green’s function of the linearized Monge-Ampère operator when the Monge-Ampère measure is only bounded away from zero and infinity. These estimates are the global version of those in [11] in two dimensions; see also [18] for related interior results in higher dimensions.
Theorem 2.1** (Global estimates for the Green’s function).**
*There exists a universal constant with the following property.
(i) Assume that and satisfy (1.5)-(1.7). Then,*
[TABLE]
(ii) Assume and satisfy (1.10)–(1.13). If where , then
[TABLE]
(iii) Let be either as in (i) or as in (ii). Let . Then there is a positive number such that if
[TABLE]
then
[TABLE]
Remark 2.2**.**
- (i) In two dimensions, Theorem 2.1 establishes the global estimates (*) for the Green’s function of the linearized Monge-Ampère operator when the Monge-Ampère measure is only bounded away from zero and infinity. *
(ii) On the other hand, in any dimension , Theorem 2.1 establishes the global estimates for any close to for the Green’s function of the linearized Monge-Ampère operator when the Monge-Ampère measure is close to a constant. In other words, if the Monge-Ampère measure is continuous then the Green’s function of the linearized Monge-Ampère operator has the same global integrability, up to the first order derivatives, as the Green’s function of the Laplace operator.
Proof of Theorem 2.1.
We first prove (i) and (ii). Let be either as in (i) or as in (ii) of the theorem. We need to show that
[TABLE]
Step 1: We first assert that for some ,
[TABLE]
Indeed, by De Philippis-Figalli-Savin’s and Schmidt’s estimates for the Monge-Ampère equation [6, 23] (see also [8, Theorem 4.36]), there exists such that . Using Savin’s technique in his proof of the global estimates [22] for the Monge-Ampère equation, we can show that (see also [8, Theorem 5.3]): If and satisfy (1.5)-(1.7), then
[TABLE]
and if and satisfy (1.10)–(1.13), then
[TABLE]
In all cases, we have (2.16) as asserted.
Let be any positive number depending on and and let
[TABLE]
Fix . Let . Let . We use to denote the partial derivative .
Step 2: We have the following integral estimate
[TABLE]
To prove (2.18), we use the truncation function to avoid the singularity of at . By the assumption on the smoothness of , is smooth away . Thus for all . Note that on while on . Thus, for all . Moreover, from the definition of , we find that
[TABLE]
Using that on while on , we obtain (2.18).
Step 3: We next claim that
[TABLE]
To prove (2.19), we use (2.18) together with the arguments in [11, 13]. For completeness, we include its short proof here. Let
[TABLE]
We will use the following inequality whose simple proof can be found in [4, Lemma 2.1]. It follows from (2.18) and that
[TABLE]
Now, since , using the Hölder inequality to with exponents and , we have
[TABLE]
Applying (2.20) to defined in (2.17), noting that and recalling (2.16), we obtain
[TABLE]
The proof of (2.19) is complete.
Step 4: For any we have
[TABLE]
Indeed, let . If and satisfy (1.10)–(1.13) and if where then estimate (5.12) in [15] gives
[TABLE]
On the other hand, if and satisfy (1.5)-(1.7), then by Corollary 2.6 in [12], we have
[TABLE]
From the preceding estimates, we obtain (2.21).
As a consequence of (2.21) and Chebyshev’s inequality, we have
[TABLE]
Step 5: Now, we pass from the truncation of level to global estimates. For any , we have
[TABLE]
By using (2.22) and (2.19), we obtain
[TABLE]
We choose such that or . Then
[TABLE]
It follows from the layer cake representation that for any with The proof of (2.15) will be complete if we can choose a suitable to make so as to choose in the above inequality. This is possible, since
[TABLE]
where the last inequality follows from . In conclusion, we can find such that
[TABLE]
The proof of (2.15) is complete.
Finally, we prove (iii). Let . From Step 5 above, we find that, in order to have (2.14), it suffices to choose and such that
[TABLE]
for some
[TABLE]
where with as in Step 1.
A direct calculation shows that (2.23) holds as long as where
[TABLE]
The last inequality is due to the fact that . Thus, we need to choose and such that
[TABLE]
This is always possible if for some small positive number ; see [8, Theorem 5.3]. ∎
3. bounds and Hölder estimates at the boundary
In this section we establish bounds in Lemma 3.1 and Hölder estimates at the boundary in Proposition 3.2 for solutions to (1.8). Let be as in Section 2.
As a consequence of Theorem 2.1, we first have the following global estimates for solutions to inhomogeneous linearized Monge–Ampère equations (1.8) in two dimensions.
Lemma 3.1**.**
Assume that . Consider the following settings:
- (i) Assume that and satisfy (1.5)-(1.7).
(ii) Assume and satisfy (1.10)–(1.13). Let where .
Let be either as in (i) or A as in (ii). Assume that and satisfies
[TABLE]
Then there exist positive constants and such that
[TABLE]
Proof.
Let be as in Theorem 2.1. Set
[TABLE]
Using Hölder inequality to the estimates in Theorem 2.1, we find such that
[TABLE]
Let be the Green’s function of in with pole . Define
[TABLE]
Then is a solution of
[TABLE]
Since in , we obtain from the Aleksandrov-Bakelman-Pucci (ABP) maximum principle (see [9, Theorem 9.1]) that
[TABLE]
As the operator can be written in the divergence form with symmetric coefficient, we infer from [10, Theorem 1.3] that for all . Thus, using (3.24), we can estimate for all
[TABLE]
The desired estimate follows from (3.25) and (3.26). ∎
Next, we obtain the following Hölder estimates at the boundary for solutions to inhomogeneous linearized Monge–Ampère equations (1.8) in two dimensions.
Proposition 3.2**.**
Assume and satisfy (1.10)–(1.13). Assume that . Let be as in Lemma 3.1. Let u\in C\big{(}B_{\rho}(0)\cap\overline{\Omega}\big{)}\cap W^{2,n}_{loc}(B_{\rho}(0)\cap\Omega) be a solution to
[TABLE]
where for some and . Let
[TABLE]
Then, there exist positive constants and depending only such that, for any and for all , we have
[TABLE]
Proof.
Our proof relies on Lemma 3.1 and a construction of suitable barriers as in the proof of Proposition 5.1 in [15]. We omit the details. ∎
4. Global Hölder Estimates and Singular Abreu equations
In this section, we prove Theorems 1.2 and 1.3. Theorem 1.2 follows from Theorem 1.1, Lemma 3.1 and Theorem 4.1 below.
Theorem 4.1**.**
Assume and satisfy (1.10)–(1.13). Assume that . Let u\in C\big{(}B_{\rho}(0)\cap\overline{\Omega}\big{)}\cap W^{2,n}_{loc}(B_{\rho}(0)\cap\Omega) be a solution to
[TABLE]
where for some and . Then, there exist positive constants and depending only on such that
[TABLE]
Proof of Theorem 4.1.
The proof of the global Hölder estimates in this theorem is similar to the proof of [15, Theorem 1.7]. It combines the boundary Hölder estimates in Proposition 3.2 and the interior Hölder continuity estimates in Theorem 1.1 using Savin’s Localization Theorem [21]. Thus we omit the details. ∎
We are now in a position to complete the proof of Theorem 1.2.
Proof of Theorem 1.2.
From Lemma 3.1, we find that
[TABLE]
The desired global Hölder estimates in Theorem 1.2 follow from combining Theorems 1.1 and 4.1. ∎
Finally, we give a proof of Theorem 1.3.
Proof of Theorem 1.3.
The proof of the uniqueness of solutions is similar to that of Lemma 4.5 in [14] so we omit it. The existence proof uses a priori estimates and degree theory as in Theorem 2.1 in [14]. Here, we only focus on proving the a priori estimates for in for any . Step 1: positive bound from below and above for .
First, by the convexity of , we have
[TABLE]
By the maximum principle, the function attains its minimum value on . It follows that
[TABLE]
Therefore,
[TABLE]
Now, we can construct an explicit barrier using the uniform convexity of and the upper bound for to show that
[TABLE]
for a constant depending only on , and .
Noting that we are in two dimensions so . We compute in
[TABLE]
By the maximum principle, attains it maximum value on the boundary . Recall that on . Thus, for all , we have
[TABLE]
It follows from (4.27) and (4.29) that
[TABLE]
where depends only on , and .
Step 2: higher order derivative estimates for . From (4.30) and (4.28), we apply the global Hölder estimates for the linearized Monge-Ampère equation in Theorem 1.2 to
[TABLE]
with boundary value on to conclude that with
[TABLE]
for universal constants and . Now, we note that solves the Monge-Ampère equation
[TABLE]
with right hand side being in and boundary value on . Therefore, by the global estimates for the Monge-Ampère equation [26], we have with universal estimates
[TABLE]
As a consequence, the second order operator is uniformly elliptic with Hölder continuous coefficients. A bootstrap argument for the equation
[TABLE]
concludes the proof of the a priori estimates for in for any . ∎
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