$n$-Harmonicity, Minimality, Conformality and Cohomology
Bang-Yen Chen, Shihshu Walter Wei

TL;DR
This paper explores the relationships between cohomology classes, $n$-harmonic morphisms, and $F$-harmonic maps, extending existing theories and providing sharp results on harmonic maps and Riemannian submersions.
Contribution
It extends previous work on harmonic maps and morphisms by studying cohomology classes related to $n$-harmonic morphisms, introducing new results and revisiting earlier findings.
Findings
Results on $F$-harmonic maps are extended and augmented.
Theorem 3.2 provides sharp results using the $n$-conservation law.
Revisits and generalizes previous results on Riemannian submersions and $n$-harmonic morphisms.
Abstract
By studying cohomology classes that are related with -harmonic morphisms and -harmonic maps, we augment and extend several results on -harmonic maps, harmonic maps in [1, 3, 14], -harmonic morphisms in [17], and also revisit our previous results in [9, 10, 21] on Riemannian submersions and -harmonic morphisms which are submersions. The results, for example Theorem 3.2 obtained by utilizing the -conservation law (2.6), are sharp.
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Taxonomy
TopicsGeometric Analysis and Curvature Flows · Analytic and geometric function theory · Geometry and complex manifolds
-harmonicity, minimality, conformality and cohomology
Bang-Yen Chen
Department of Mathematics
Michigan State University
East Lansing, Michigan 48824–1027
U.S.A.
and
Shihshu Walter Wei
Department of Mathematics
University of Oklahoma
Norman, Oklahoma 73019-0315
U.S.A.
Abstract.
By studying cohomology classes that are related with -harmonic morphisms and -harmonic maps, we augment and extend several results on -harmonic maps, harmonic maps in [1, 3, 15], -harmonic morphisms in [23], and also revisit our previous results in [10, 11, 29] on Riemannian submersions and -harmonic morphisms which are submersions. The results, for example Theorem 3.2 obtained by utilizing the -conservation law (2.6), are sharp.
Key words and phrases:
-harmonic maps, -harmonic morphism, Cohomology class, minimal submanifold, submersion.
2000 Mathematics Subject Classification:
Primary 31B35; Secondary 53C40, 58E20
1. Introduction
Harmonicity and its variants are related with the topology and geometry of manifolds. It was shown in [27] that homotopy classes can be represented by -harmonic maps (see, e.g. [29], for definition and examples of -harmonic maps):
Theorem A. If is a compact Riemannian -manifold, then for any positive integer , each class in the i-th homotopy group can be represented by a -harmonic map from an -dimensional sphere into minimizing -energy in its homotopy class for any .
On the other hand, B.-Y. Chen established in [7] the following result involving Riemannian submersion, minimal immersion, and cohomology class.
Theorem B. ([7]) Let be a Riemannian submersion with minimal fibers and orientable base manifold . If is a closed manifold with cohomology class , then the horizontal distribution of the Riemannian submersion is never integrable. Thus the submersion is never non-trivial.
Whereas -harmonic maps represent homotopy classes, B.-Y. Chen and S. W. Wei connected the two seemingly unrelated areas of -harmonic morphisms and cohomology classes in the following.
Theorem C. ([10, 11]) Let be an -harmonic morphism which is a submersion. If is an orientable -manifold and is a closed -manifold with -th cohomology class , then the horizontal distribution of is never integrable. Hence the submersion is always non-trivial.
This recaptures Theorem B when is a Riemannian submersion with minimal fibers and orientable base manifold . While a horizontally weak conformal -harmonic map is a -harmonic morphism (cf. e.g., [11, Theorem 4]), -harmonic morphism is also linked to cohomology class as follows.
Theorem D. ([10, 11]) Let be an -harmonic morphism which is a submersion. Then the pull back of the volume element of the base manifold is a harmonic -form if and only if the horizontal distribution of is completely integrable.
Following the proofs given in [10, 11], and by applying a characterization theorem of a -harmonic morphism from [4, 6], and [29, Theorem 2.5], we seek a dual version of Theorem D. In particular, -harmonic maps and cohomology classes are interrelated in [29] as follows.
Theorem E. Let be a closed -manifold and be an -harmonic map which is a submersion. If is a closed -manifold and the horizontal distribution of is integrable and is an -harmonic morphism, then we have .
Theorem F. ([29]) Let be an -harmonic map which is a submersion such that the horizontal distribution of is integrable. If is a closed manifold with cohomology class . Then is not an -harmonic morphism. Thus the submersion is always nontrivial.
The purpose of this paper is to point out the underlying essence of the foregoing Theorems C, D, E, and F is an application of stress-energy tensor and a conservation law. The results, for example Theorem 3.2 obtained by utilizing the -conservation law (2.6), are sharp.
2. Preliminaries
2.1. Submersions
A differential map between two Riemannian manifolds is called a submersion at a point if its differential is a surjective linear map. A differentiable map that is a submersion at each point is called a submersion. For each point , is called a fiber. For a submersion , let denote the orthogonal complement of Kernel\,\big{(}du_{x}:T_{x}(M^{m})\to T_{u(x)}(N^{n})\big{)}. Let denote the horizontal distribution of .
A submersion is called horizontally weakly conformal if the restriction of to is conformal, i.e., there exists a smooth function on such that
[TABLE]
for all and . If the function in (2.1) is positive, then is called horizontally conformal and is called the dilation of . For a horizontally conformal submersion with dilation , the energy density of is (cf. (2.2)).
A horizontally conformal submersion with dilation is called a Riemannian submersion. Recall that a -form on a compact Riemannian manifold is called harmonic if is both closed and co-closed, i.e., .
In [29, 4], generalizing the work of P. Baird and J. Eells for the case , and the necessary condition for the fibers being minimal, S. W. Wei linked -harmonicity for every , and P. Baird and S. Gudmundsson linked -harmonicity, with minimal fibers as follows.
Theorem 2.1** ([29], Theorem 2.5 ).**
Let be a Riemannian submersion. Then is a -harmonic map, for every , if and only if all fibers are minimal submanifolds in
Proposition 2.1** ([29], Proposition 2.4 ).**
Let be a Riemannian submersion. Then is a -harmonic morphism, for every , if and only if all fibers are minimal submanifolds in
The case in Theorem 2.1 and Proposition 2.1 are due to Eells-Sampson [16].
Theorem 2.2** (P. Baird and S. Gudmundsson [4], Corollary 2.6 ).**
If is a horizontally conformal submersion from a Riemannian manifold onto a Riemannian manifold , then is -harmonic if and only if the fibers of are minimal in .
Remark 2.1*.*
(i). The results of linking -harmonicity for every , with minimal fibers in Theorem 2.1 can be extended to with minimal fibers. We refer to the celebrated work of E. Bombieri - E. De Gorgi - E. Jiusti on minimal cones and the Bernstein problem ([5]), S.W. Wei on -harmonic functions ([28]), P. Baird - S. Gudmundsson on -harmonic maps and minimal submanifods ([4]), Y.I. Lee - S.W. Wei - A.N. Wang on a generalized -harmonic equation and the inverse mean curvature flow ([21]), etc. (ii). We also note that utilizing symmetry, Wu-Yi Hsiang pioneered the study of the inverse image of minimal submanifolds being minimal under appropriate conditions ([18]), which marked the birth of equivariant differential geometry (cf. e.g. W.Y. Hsiang - H.B. Lawson [19], S.W. Wei [26], etc.).
2.2. - and -harmonic morphisms
Let be a differential map between two Riemannian manifolds and . Denote the energy density of , which is given by
[TABLE]
where is a local orthonormal frame field on and is the Hilbert-Schmidt norm of , determined by the metric of and the metric of . The energy of , denoted by , is defined to be
[TABLE]
A smooth map is called harmonic if is a critical point of the energy functional with respect to any compactly supported variation.
Let be a strictly increasing function with and let be a smooth map between two compact Riemannian manifolds. Then the map is called -harmonic if it is a critical point of the -energy functional:
[TABLE]
In particular, if , then the -energy becomes -energy, and its critical point is called -harmonic map. A map is a -harmonic morphism if for any -harmonic function defined on an open set of , the composition is -harmonic on .
2.3. Stress-Energy tensor
Let be a smooth Riemannian -manifold. Let be a smooth Riemannian vector bundle over i.e. a vector bundle such that at each fiber is equipped with a positive inner product Set the space of smooth -forms on with values in the vector bundle .
For , set defined as in ([13, (2.3)],). The authors of [20] defined the following -energy functional given by
[TABLE]
where is as before.
The stress-energy associated with the -energy functional is defined as follows:
[TABLE]
where is the interior multiplication by the vector field given by
[TABLE]
for and any vector fields on , .
When and for a map , is just the stress-energy tensor introduced in [3]. And when and for a map , is the -stress energy tensor given by
[TABLE]
Definition 2.1**.**
* is said to satisfy an -conservation law if is divergence free, i.e., the -type tensor field vanishes identically (i.e., ).*
The -conservation law is given by
[TABLE]
(cf. [13, 22] for details), in which coarea formula was first employed by Y. X. Dong and S. W. Wei to derive monotonicity formulas, vanishing theorems, and Liouville theorems on complete noncompact manifolds from conservation laws.
3. Main Theorems and Their Proofs
Assume that and .
Theorem 3.1**.**
Let be a non-constant map. Then the -stress tensor if and only if and is conformal.
Proof.
If , then
[TABLE]
in the region , where is the dilation and thus
[TABLE]
where is the -energy density of given by . Hence, we get .
Conversely, if and , then we find
[TABLE]
Therefore, we obtain
[TABLE]
which shows that the -stress tensor vanishes identically. ∎
Theorem 3.2**.**
If and is an -harmonic and conformal map, then is homothetic.
Proof.
If is -harmonic, then it follows from [13, Corollary 2.2] that satisfies -conservation law, i.e., div.
In virtue of Theorem 3.1 and (3.3), with these hypotheses, we find
[TABLE]
Thus, it follows from the assumption that is a constant. Therefore, is homothetic. ∎
Theorems 3.2 is sharp in dimensions . That is, if , then the results no longer hold. Counterexamples can be provided and based on the fact that a conformal map between equal dimensional -manifolds, such as stereographic projections is -harmonic, but is not homothetic (cf. [30, 23]). In fact, Y. L. Ou and S. W. Wei proved the following:
Theorem G. ([23]) Let be a non-constant map between Riemannian manifolds with . Then is an -harmonic morphism if and only if is weakly conformal.
While Theorems 3.2 on the one hand, augments Theorem G, on the other hand, Theorems 3.1 and 3.2 generalize the work of J. Eells and L. Lemaire ([15]) in which . Furthermore, Theorems 3.1 and 3.2 augment a theorem of M. Ara in [1] for the case the zeros of are being isolated for horizontally conformal -harmonic maps. Hence we obtain:
Theorem 3.3**.**
Let , , be an -harmonic map, which is horizontally conformal with dilation .
Case 1. Assume that the zeros of are isolated. Then the following three properties are equivalent:
- (1)
The fibers of are minimal submanifolds.
- (2)
* is vertical.*
- (3)
The horizontally distribution of has mean curvature vector .
Case 2. Assume that the zeros of are not isolated. Then
- (1)
The fibers of are minimal submanifolds.
- (2)
* is homothetic, i.e. a positive constant.*
- (3)
, hence it is vertical.
Proof.
Case 1 is exactly [1, Theorem 5.1] proved by M. Ara.
For Case 2, statement (1) follows from that fact that general solutions of
[TABLE]
are given by with constants . Hence, is an -harmonic map, and so we may apply Theorem 2.2 to conclude that fibers of are minimal in . Statements (2) and (3) of Case 2 follow from Theorem 3.2 and the fact that is -harmonic. ∎
In examining the converse of Theorem 3.3, Case 2, (1), we characterize the minimal fibers of a horizontally conformal map from the previously untreated case in -harmonic maps:
Theorem 3.4**.**
Let , , be a horizontally conformal map. Assume that the zeros of are not isolated. Then the fibers of are minimal submanifolds if and only if is an -harmonic map; if and only if is an -harmonic map.
Proof.
This follows from the fact that when the zeros of are not isolated, -harmonic map is an -harmonic map, and Theorem 2.2. ∎
When the target manifold of is a Riemann surface, i.e. , then we associate with a harmonic map in the following way:
Theorem 3.5**.**
Let be a Riemann surface, and , , be a horizontally conformal map. Assume that the zeros of are not isolated. Then the fibers of are minimal submanifolds if and only if is an -harmonic map; if and only if is a harmonic map.
Proof.
This follows from the fact that when the zeros of are not isolated, -harmonic map is a harmonic map, and Theorem 3.4. ∎
4. Applications
As an application of Theorems 3.1 and 3.2, we revisit
Theorem 4.1** (Theorem C. ([10, 11]).**
Let be an -harmonic morphism which is a submersion. If is an orientable manifold and is a closed manifold with the -th cohomology class , then the horizontal distribution of is never integrable.
Proof.
Under the hypothesis, in view of Theorem 2.2, has minimal fibers and, according to Theorem 3.2, is constant. Let be an oriented local orthonormal frame of the base manifold and let denote the dual 1-forms of on . Then is the volume form of , which is a closed -form on .
Consider the pull back of the volume form of via , which is denoted by . Then is a simple -form on satisfying
[TABLE]
due to the fact that the exterior differentiation and the pullback commute.
Assume that and let be a local orthonormal frame field with being its dual coframe fields on such that
(i) are basic horizontal vector fields satisfying , , and give a positive orientation of ; and
(ii) are vertical vector fields.
Then we have
[TABLE]
Also, it follows from (i) that
[TABLE]
If we put
[TABLE]
then
[TABLE]
It follows from (4.2) and (4.5) that holds identically if and only if the following two conditions are satisfied:
[TABLE]
and
[TABLE]
for any horizontal vector fields and for vertical vector fields .
Since the fibers of are minimal submanifolds of , we find for each that
[TABLE]
where “” denotes the missing term and denotes the second fundamental form of fibers in , which prove that condition (4.2) holds.
Now, suppose that the horizontal distribution is integrable. If are horizontal vector fields, then is also horizontal by Frobenius theorem. So, for vertical vector fields we find (cf. [7, formula (6.7)] or [29, formula (3.5)])
[TABLE]
Consequently, from (4.8) and (4.9) we get
[TABLE]
Next, we show that if is integrable, then we have d\big{(}(u^{\ast}\bar{\omega}\,)^{\bot}\big{)}=0\,. Since is a horizontally conformal submersion with constant dilation , it preserves orthogonality, which is crucial to horizontal and vertical distributions, and the pullback expands the length of -form constantly by in every direction. This, via (4.3) and (4.10) leads to
[TABLE]
Since d\big{(}(u^{\ast}\omega)^{\bot}\big{)}=0 is equivalent to being co-closed, it follows that, under the condition that is integrable, the pullback of the volume form, is a harmonic -form on . Thus, gives rise to a non-trivial cohomology class in by Hodge Theorem ([17]). Therefore, if , then the horizontal distribution of is never integrable. ∎
From the proof of Theorem 4.1, we have the following.
Theorem 4.2**.**
Let be an -harmonic morphism with which is a submersion. Then the pull back of the volume element of is a harmonic -form if and only if the horizontal distribution of is completely integrable.
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