Conformal anti-invariant $\xi^\perp-$submersions
Mehmet Akif Akyol, Y{\i}lmaz G\"und\"uzalp

TL;DR
This paper introduces conformal anti-invariant 11-submersions from almost contact metric manifolds to Riemannian manifolds, analyzing their geometric properties, conditions for being totally geodesic and harmonic, and associated product structures.
Contribution
It generalizes anti-invariant 11-submersions to conformal cases and explores their geometric and structural properties.
Findings
Conditions for conformal anti-invariant 11-submersions to be totally geodesic.
Conditions for these submersions to be harmonic.
Existence of certain product structures on the total space.
Abstract
As a generalization of anti-invariant Riemannian submersions, we introduce conformal anti-invariant submersions from almost contact metric manifolds onto Riemannian manifolds. We investigate the geometry of foliations which are arisen from the definition of a conformal submersion and find necessary and sufficient conditions for a conformal anti-invariant submersion to be totally geodesic and harmonic, respectively. Moreover, we show that there are certain product structures on the total space of a conformal anti-invariant submersion.
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Taxonomy
TopicsGeometric Analysis and Curvature Flows · Point processes and geometric inequalities · Geometric and Algebraic Topology
CONFORMAL ANTI-INVARIANT SUBMERSIONS
Mehmet Akif Akyol
Bingöl University, Faculty of Arts and Sciences, Deparment of Mathematics, 12000, Bingöl, Turkey
and
Yılmaz Gündüzalp
Dicle University, Faculty of Arts and Sciences, Deparment of Mathematics, 21280, Diyarbakır, Turkey
Abstract.
As a generalization of anti-invariant Riemannian submersions, we introduce conformal anti-invariant submersions from almost contact metric manifolds onto Riemannian manifolds. We investigate the geometry of foliations which are arisen from the definition of a conformal submersion and find necessary and sufficient conditions for a conformal anti-invariant submersion to be totally geodesic and harmonic, respectively. Moreover, we show that there are certain product structures on the total space of a conformal anti-invariant submersion.
Key words and phrases:
Almost contact metric manifold, conformal submersion, conformal anti-invariant submersion.
2010 Mathematics Subject Classification:
53C15, 53C40.
1. Introduction
Riemannian submersions between Riemannian manifolds were studied by O’Neill [28] and Gray [22], for recent developments on the geometry of Riemannian submanifolds and Riemannian submersions, see:[9] and [15], respectively. In [43], the Riemannian submersions were considered between almost Hermitian manifolds by Watson under the name of almost Hermitian submersions. In this case, the Riemannian submersion is also an almost complex mapping and consequently the vertical and horizontal distribution are invariant with respect to the almost complex structure of the total manifold of the submersion. The study of anti-invariant Riemannian submersions from almost Hermitian manifolds were initiated by Şahin [38]. In this case, the fibres are anti-invariant with respect to the almost complex structure of the total manifold. Beside there are many notions related with anti-invariant Riemannian submersion (see: [2], [7], [8], [16], [19], [20], [21], [25], [30], [31], [32], [33], [35], [39], [40], [42]). In [13], Chinea defined almost contact Riemannian submersions between almost contact metric manifolds and examined the differential geometric properties of Riemannian submersions between almost contact metric manifolds. More precisely, let and be almost contact manifolds with and . A Riemannian submersion is called the almost contact metric submersion if is an almost contact mapping, i.e., . An immediate consequence of the above definition is that the vertical and horizontal distributions are -invariant. Moreover, the characteristic vector field is horizontal. We note that only -holomorphic submersions have been considered on almost contact manifolds [13].
One the other hand, as a generalization of Riemannian submersion, horizontally conformal submersions are defined as follows [6]: Suppose that and are Riemannian manifolds and is a smooth submersion, then is called a horizontally conformal submersion, if there is a positive function such that
[TABLE]
for every It is obvious that every Riemannian submersion is a particular horizontally conformal submersion with . We note that horizontally conformal submersions are special horizontally conformal maps which were introduced independently by Fuglede [14] and Ishihara [23]. We also note that a horizontally conformal submersion is said to be horizontally homothetic if the gradient of its dilation is vertical, i.e.,
[TABLE]
at , where is the projection on the horizontal space . For conformal submersion, see: [6], [17], [29].
As a generalization of holomorphic submersions, conformal holomorphic submersions were studied by Gudmundsson and Wood [18]. They obtained necessary and sufficient conditions for con- formal holomorphic submersions to be a harmonic morphism, see also [10], [11] and [12] for the harmonicity of conformal holomorphic submersions.
Recently, in [3] we have introduced conformal anti-invariant submersions from almost Hermitian manifolds onto Riemannian manifolds and investigated the geometry of such submersions. (See also:[1]) We showed that the geometry of such submersions are different from anti-invariant Riemannian submersions. In this paper, we consider conformal anti-invariant submersions from an almost contact metric manifold under the assumption that the fibers are anti-invariant with respect to the tensor field of type of the almost contact manifold.
The paper is organized as follows. In the second section, we gather main notions and formulas for other sections. In section 3, we introduce conformal anti-invariant submersions from almost contact metric manifolds onto Riemannian manifolds, investigates the geometry of leaves of the horizontal distribution and the vertical distribution and find necessary and sufficient conditions for a conformal anti-invariant submersion to be totally geodesic and harmonic, respectively. In section 4, we show that there are certain product structures on the total space of a conformal anti-invariant submersion.
2. Preliminaries
In this section, we define almost contact metric manifolds, recall the notion of (horizontally) conformal submersions between Riemannian manifolds and give a brief review of basic facts of (horizontally) conformal submersions.
Let be an almost contact metric manifold with structure tensors where is a tensor field of type (1,1), is a vector field, is a 1-form and is the Riemannian metric on Then these tensors satisfy [5]
[TABLE]
[TABLE]
where denotes the identity endomorphism of and are any vector fields on . Moreover, if is Sasakian [37], then we have
[TABLE]
where is the connection of Levi-Civita covariant differentiation.
Conformal submersions belong to a wide class of conformal maps that we are going to recall their definition, but we will not study such maps in this paper.
Definition 2.1**.**
([6]) Let be a smooth map between Riemannian manifolds, and let . Then is called horizontally weakly conformal or semi conformal at if either
- (i)
, or 2. (ii)
* maps horizontal space conformally onto , i.e., is surjective and there exists a number such that*
[TABLE]
A point is of type (i) in Definition if and only if it is a critical point of ; we shall call a point of type (ii) a regular point. At a critical point, has rank [math]; at a regular point, has rank and is submersion. The number is called the square dilation (of at ); it is necessarily non-negative; its square root is called the dilation (of at ). The map is called horizontally weakly conformal or semi conformal (on ) if it is horizontally weakly conformal at every point of . It is clear that if has no critical points, then we call it a (horizontally) conformal submersion.
Next, we recall the following definition from [17]. Let be a submersion. A vector field on is said to be projectable if there exists a vector field on , such that for all . In this case and are called related. A horizontal vector field on is called basic, if it is projectable. It is well known fact, that is is a vector field on , then there exists a unique basic vector field on , such that and are related. The vector field is called the horizontal lift of .
The fundamental tensors of a submersion were introduced in [28]. They play a similar role to that of the second fundamental form of an immersion. More precisely, O’Neill’s tensors and defined for vector fields on by
[TABLE]
[TABLE]
where and are the vertical and horizontal projections (see [15]). On the other hand, from (2.5) and (2.6), we have
[TABLE]
[TABLE]
[TABLE]
[TABLE]
for and , where . If is basic, then . It is easily seen that for , and the linear operators , are skew-symmetric, that is
[TABLE]
for all . We also see that the restriction of to the vertical distribution is exactly the second fundamental form of the fibres of . Since skew-symmetric we get: has totally geodesic fibres if and only if . For the special case when is horizontally conformal we have the following:
Proposition 2.1**.**
([17]) Let be a horizontally conformal submersion with dilation and be horizontal vectors, then
[TABLE]
We see that the skew-symmetric part of measures the obstruction integrability of the horizontal distribution .
Let and be Riemannian manifolds and suppose that is a smooth map between them. The differential of can be viewed a section of the bundle , where is the pullback bundle which has fibres , . has a connection induced from the Levi-Civita connection and the pullback connection. Then the second fundamental form of is given by
[TABLE]
defined by
[TABLE]
for , where is the pullback connection. It is known that the second fundamental form is symmetric.
Lemma 2.1**.**
[44]** Let and be Riemannian manifolds and suppose that is a smooth map between them. Then we have
[TABLE]
for .
A smooth map is said to be harmonic if . On the other hand, the tension field of is the section of defined by
[TABLE]
where is the orthonormal frame on . Then it follows that is harmonic if and only if (for details, see [6]). Finally, we recall the following lemma from [6].
Lemma 2.2**.**
Suppose that is a horizontally conformal submersion. Then, for any horizontal vector fields and vertical fields we have
- (i)
; 2. (ii)
; 3. (iii)
.
3. Conformal Anti-invariant submersions
In this section, we define conformal anti-invariant submersions from an almost contact metric manifold onto a Riemannian manifold and investigate the integrability of distributions and obtain a necessary and sufficient condition for such submersions to be totally geodesic map. We also investigate the harmonicity of such submersions.
Definition 3.1**.**
Let be an almost contact metric manifold and and be a Riemannian manifold. We suppose that there exist a horizontally conformal submersion such that is normal to and is anti-invariant with respect to , i.e., Then we say that is a conformal anti-invariant submersion.
Here, we assume that if is a conformal anti-invariant submersion from a Sasakian manifold to a Riemannian manifold . Then from Definition 3.1, we have We denote the complementary orthogonal distribution to in by Then we have
[TABLE]
We can easily to see that is an invariant distribution of with respect to Hence contains Thus, for , we have
[TABLE]
where and On the other hand, since and is a conformal submersion, using (3.2) we derive for any and which implies that
[TABLE]
Remark 3.1**.**
We note that every anti-invariant submersion from an almost contact manifold onto a Riemannian manifold is a conformal anti-invariant submersion with , where denotes the identity function [24].
Lemma 3.1**.**
Let be a conformal anti-invariant -submersion from a Sasakian manifold onto a Riemannian manifold . Then we have
[TABLE]
[TABLE]
[TABLE]
[TABLE]
for and .
Proof.
By virtue of (2.3), (2.10) and (3.2) we have (3.4). Using (2.3) and (2.8) we get (3.5). By using (2.2), for and , we have
[TABLE]
since and Differentiating (3.6) with respect to we get
[TABLE]
due to Our assertion is complete. ∎
Since the distribution is integrable, we only study the integrability of the distribution and then we investigate the geometry of leaves of and .
Theorem 3.1**.**
Let be a conformal anti-invariant submersion from a Sasakian manifold onto a Riemannian manifold . Then the following assertions are equivalent to each other;
- (a)
* is integrable,* 2. (b)
**
for and .
Proof.
From (2.2) and (2.3), we obtain
[TABLE]
for and . Then, from (3.2) and (3.8), we have
[TABLE]
Using (2.9) and if we take into account that is a conformal submersion, we obtain
[TABLE]
Thus, from (2.12) and Lemma 2.2 we derive
[TABLE]
Moreover, using (3.6), we obtain
[TABLE]
This show that . ∎
From Theorem we deduce the following which shows that a conformal anti-invariant submersion with integrable turns out to be a horizontally homothetic submersion.
Theorem 3.2**.**
Let be a conformal anti-invariant submersion from a Sasakian manifold onto a Riemannian manifold . Then any two conditions below imply the third;
- (i)
* is integrable.* 2. (ii)
* is horizontally homothetic submersion.* 3. (iii)
**
for and .
Proof.
From Theorem 3.1, we have
[TABLE]
for and . Now, if we have (i) and (iii), then we arrive at
[TABLE]
Now, taking in (3.9) for , using (2.2) and (3.6), we get
[TABLE]
Hence is a constant on . On the other hand, taking in (3.9) for and using (3.6) we derive
[TABLE]
thus, we arrive at
[TABLE]
From above equation, is a constant on Similarly, one can obtain the other assertions. ∎
Remark 3.2**.**
We assume that Using (3.2) one can prove that
Hence we have the following corollary.
Corollary 3.1**.**
Let be a conformal anti-invariant submersion from a Sasakian manifold onto a Riemannian manifold with . Then the following assertions are equivalent to each other;
- (i)
* is integrable* 2. (ii)
** 3. (iii)
**
for .
For the geometry of leaves of the horizontal distribution, we have the following theorem.
Theorem 3.3**.**
Let be a conformal anti-invariant -submersion from a Sasakian manifold onto a Riemannian manifold . Then the following assertions are equivalent to each other;
- (i)
* defines a totally geodesic foliation on .* 2. (ii)
**
for and .
Proof.
By using (2.2), (2.9), (2.10), (3.1), (3.2) and (3.8), have
[TABLE]
for and . Since is a conformal submersion, using (2.12) and Lemma (2.2) we arrive at
[TABLE]
Moreover, using Definiton 3.1 and (3.6) we obtain
[TABLE]
which tells that . ∎
From Theorem 3.3, we also deduce the following characterization.
Theorem 3.4**.**
Let be a conformal anti-invariant submersion from a Sasakian manifold onto a Riemannian manifold . Then any two conditions below imply the third;
- (i)
* defines a totally geodesic foliation on .* 2. (ii)
* is a horizontally homothetic submersion.* 3. (iii)
**
for and .
Proof.
For and , from Theorem 3.3, we have
[TABLE]
Now, if we have (i) and (iii), then we obtain
[TABLE]
Now, taking in (3.10) and using (3.6), we get Hence, is a constant on . On the other hand, taking in (3.10) and using (3.6) we derive
[TABLE]
From above equation, is a constant on . Similarly, one can obtain the other assertions. ∎
In particular, as an analogue of a conformal Lagrangian submersion in [3], we have the following corollary.
Corollary 3.2**.**
Let be a conformal anti-invariant submersion from a Sasakian manifold onto a Riemannian manifold with . Then the following assertions are equivalent to each other;
- (i)
* defines a totally geodesic foliation on .* 2. (ii)
** 3. (iii)
**
for and .
In the sequel we are going to investigate the geometry of leaves of the distribution .
Theorem 3.5**.**
Let be a conformal anti-invariant submersion from a Sasakian manifold onto a Riemannian manifold . Then the following assertions are equivalent to each other;
- (i)
* defines a totally geodesic foliation on .* 2. (ii)
**
for and .
Proof.
Since using (2.3) we have for and Thus we have
[TABLE]
Using (2.3), (2.7) and (3.2) we have
[TABLE]
Since is torsion free and we obtain
[TABLE]
Using (2.3) and (2.10) we have
[TABLE]
here we have used that is invariant. Using (2.12) and Lemma 2.2 (i) and if we take into account that is a conformal submersion, we obtain
[TABLE]
Moreover, using Definition 3.1 and (3.6), we obtain
[TABLE]
which tells that . ∎
From Theorem 3.5, we deduce the following result.
Theorem 3.6**.**
Let be a conformal anti-invariant submersion from a Sasakian manifold onto a Riemannian manifold . Then any two conditions below imply the third;
- (i)
* defines a totally geodesic foliation on .* 2. (ii)
* is a constant on .* 3. (iii)
**
for and .
Proof.
From Theorem (3.5) we have
[TABLE]
for and Now, if we have (i) and (iii), then we obtain
[TABLE]
From above equation, is a constant on . Similarly, one can obtain the other assertions. ∎
As an analogue of a conformal Lagrangian submersion in [3], (3.3) implies that . Hence we have the following.
Corollary 3.3**.**
Let be a conformal anti-invariant submersion from a Sasakian manifold onto a Riemannian manifold with . Then the following assertions are equivalent to each other;
- (i)
* defines a totally geodesic foliation on .* 2. (ii)
**
for and .
Now we obtain necessary and sufficient condition for conformal anti-invariant submersion to be totally geodesic. We note that a differentiable map between two Riemannian manifolds is called totally geodesic if A geometric interpretation of a totally geodesic map is that it maps every geodesic in the total manifold into a geodesic in the base manifold in proportion to arc lengths.
Theorem 3.7**.**
Let be a conformal anti-invariant submersion, where is a Sasakian manifold and is a Riemannian manifold. Then is a totally geodesic map if
[TABLE]
for any , where and .
Proof.
By virtue of (2.2) and (2.12) we have
[TABLE]
for any . Then from (2.9), (2.10) and (3.2) we get
[TABLE]
for any , where and . Thus taking into account the vertical parts, we find
[TABLE]
Thus if and only if the equation (3.11) is satisfied.
∎
We now present the following definition.
Definition 3.2**.**
Let be a conformal anti-invariant submersion from a Sasakian manifold onto a Riemannian manifold with . Then is called a -totally geodesic map if
[TABLE]
In the sequel we show that this notion has an important effect on the character of the conformal submersion.
Theorem 3.8**.**
Let be a conformal anti-invariant submersion from a Sasakian manifold onto a Riemannian manifold with . Then is a -totally geodesic map if and only if is a horizontally homothetic map.
Proof.
For and , from Lemma 2.2, we have
[TABLE]
From above equation, if is a horizontally homothetic map then Conversely, if we obtain
[TABLE]
Taking inner product in (3.12) with and if we take into account is a conformal submersion, we write
[TABLE]
Above equation implies that is a constant on On the other hand, taking inner product in (3.12) with , we have
[TABLE]
From above equation, it follows that is a constant on Thus is a constant on Hence proof is complete. ∎
Here we present another result on conformal anti-invariant submersion to be totally geodesic.
Theorem 3.9**.**
Let be a conformal anti-invariant submersion from a Sasakian manifold to a Riemannian manifold . is a totally geodesic map if and only if
- (a)
* and ,* 2. (b)
* is a horizontally homotetic map,* 3. (c)
* and *
for and .
Proof.
For any , using (2.3) and (2.12) we have
[TABLE]
Then from (2.7) and (2.8) we arrive at
[TABLE]
From above equation, if and only if
[TABLE]
Since is non-singular, and On the other hand, from Lemma 2.2 we derive
[TABLE]
for any It is obvious that if is a horizontally homotetic map, it follows that Conversely, if taking in above equation, we get
[TABLE]
Taking inner product in (3.13) with we obtain
[TABLE]
From (3.14), is a constant on On the other hand, for , from Lemma 2.2 we have
[TABLE]
Again if is a horizontally homothetic map, then Conversely, if , putting instead of in above equation, we derive
[TABLE]
Taking inner product in (3.15) with and since is a conformal submersion, we have
[TABLE]
From above equation, is a constant on Thus is a constant on Now, for and from (2.3) and (2.12) we get
[TABLE]
Using (2.9) and (2.10) we have
[TABLE]
Thus if and only if
[TABLE]
Since is non-singular, and Thus proof is complete. ∎
Finally, in this section, We investigate the necessary and sufficient conditions for such submersions to be harmonic.
Theorem 3.10**.**
Let be a conformal anti-invariant submersion, where is a Sasakian manifold and is a Riemannian manifold. Then the tension field of is
[TABLE]
where is the mean curvature vector field of the distribution of .
Proof.
Let be orthonormal basis of such that be orthonormal basis of , be orthonormal basis of and be orthonormal basis of . Then the trace of second fundamental form (restriction to ) is given by
[TABLE]
Then using (2.12) we obtain
[TABLE]
In a similar way, we have
[TABLE]
Using Lemma 2.2 we arrive at
[TABLE]
Since is an orthonormal basis of and is a conformal anti-invariant -submersion, we derive
[TABLE]
Then proof follows from (3.17) and (3.18).
∎
From Theorem 3.10 we deduce that:
Theorem 3.11**.**
Let be a conformal anti-invariant submersion, where is a Sasakian manifold and is a Riemannian manifold. Then any two conditions below imply the third:
- (i)
* is harmonic* 2. (ii)
The fibres are minimal 3. (iii)
* is a horizontally homothetic map.*
We also have the following result.
Corollary 3.4**.**
Let be a conformal anti-invariant submersion, where is a Sasakian manifold and is a Riemannian manifold. is harmonic if and only if the fibres are minimal.
4. Decomposition theorems
In this section, we obtain decomposition theorems by using the existence of conformal anti-invariant submersions. First, we recall the following results from [34]. Let be a Riemannian metric tensor on the manifold and assume that the canonical foliations and intersect perpendiculary everywhere. Then is the metric tensor of
(i) a twisted product if and only if is a totally geodesic foliation and is a totally umbilic foliation,
(ii) a warped product if and only if is a totally geodesic foliation and is a spheric foliation, i.e., it is umbilic and its mean curvature vector field is parallel. We note that in this case, from [34] we have
[TABLE]
for and where is the Levi-Civita connection on
(iii) a usual product of Riemannian manifolds if and only if and are totally geodesic foliations.
Our first decomposition theorem for a conformal anti-invariant submersion comes from Theorem 3.3 and Theorem 3.5 in terms of the second fundamental forms of such submersions.
Theorem 4.1**.**
Let is a conformal anti-invariant submersion, where is a Sasakian manifold and is a Riemannian manifold. Then is a locally product manifold if
[TABLE]
and
[TABLE]
for and , where and are integral manifolds of the distributions and . Conversely, if is a locally product manifold of the form then we have
[TABLE]
and
[TABLE]
From Corollary 3.2 and Corollary 3.3, we have the following theorem.
Theorem 4.2**.**
Let be a conformal anti-invariant submersion from a Sasakian manifold onto a Riemannian manifold with . Then is a locally product manifold if and for and .
Next we obtain a decomposition theorem which is related to the notion of twisted product mani-fold. But we first recall the adjoint map of a map. Let be a map between Riemannian manifolds and Then the adjoint map of is characterized by for and Considering at each as a linear transformation
[TABLE]
we will denote the adjoint of by Let be adjoint of Then the linear transformation
[TABLE]
defined by where is an isomorphism and
Theorem 4.3**.**
Let is a conformal anti-invariant submersion, where is a Sasakian manifold and is a Riemannian manifold. Then is a twisted product manifold of the from if and only if
[TABLE]
and
[TABLE]
for and where and are integral manifolds of the distributions and and is the mean curvature vector field of
Proof.
Since using (2.3) we have for and Thus we have
[TABLE]
Using (2.3), (2.7) and (3.2) we have
[TABLE]
Since is torsion free and we obtain
[TABLE]
Using (2.3) and (2.10) we have
[TABLE]
here we have used that is invariant. Using (2.12) and Lemma 2.2 (i) and if we take into account that is a conformal submersion, we obtain
[TABLE]
Moreover, using Definition 3.1 and (3.6), we obtain
[TABLE]
Thus it follows that is totally geodesic if and only if the equation (4.2) is satisfied. On the other hand, for and , by using (2.2), (2.9), (2.10), (3.1), (3.2) and (3.8), have
[TABLE]
Since is a conformal submersion, using (2.12) and Lemma (2.2) we arrive at
[TABLE]
Moreover, using Definiton 3.1 and (3.6) we obtain
[TABLE]
From above equation, is totally umbilical if and only if the equation (4.3) is satisfied. ∎
However, in the sequel, we show that the notion of conformal anti-invariant submersion puts some restrictions on the total space for locally warped product manifold.
Theorem 4.4**.**
Let is a conformal anti-invariant submersion from a Sasakian manifold to a Riemannian manifold . If is a locally warped product manifold of the from , then either is a horizontally homothetic submersion or the fibres are one dimensional.
Proof.
For and , implies that from (2.3), Thus we have
[TABLE]
[TABLE]
For we derive
[TABLE]
From above equation, we conclude that is a constant on For we obtain
[TABLE]
Interchanging the roles of and in (4.4) we arrive at
[TABLE]
[TABLE]
From (4.6), either is a constant on or is 1-dimensional. Thus proof is complete. ∎
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