On Geodesic Triangles in Hyperbolic Plane
Rita Gitik

TL;DR
This paper proves that in a hyperbolic surface, any side of a triangle formed by lifts of a closed geodesic is shorter than the geodesic itself, revealing geometric constraints in hyperbolic geometry.
Contribution
It establishes a new inequality relating sides of triangles formed by lifts of a closed geodesic in hyperbolic surfaces.
Findings
Any side of a triangle formed by lifts of a closed geodesic is shorter than the geodesic.
The result applies to orientable hyperbolic surfaces without boundary.
Provides insight into the geometric structure of hyperbolic surfaces.
Abstract
Let M be an orientable hyperbolic surface without boundary and let be a closed geodesic in M. We prove that any side of any triangle formed by distinct lifts of in H2 is shorter than .
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Taxonomy
TopicsGeometric Analysis and Curvature Flows · Mathematics and Applications · Geometric and Algebraic Topology
On Geodesic Triangles in
Rita Gitik
Department of Mathematics
University of Michigan
Ann Arbor, MI, 48109
Abstract.
Let be an orientable hyperbolic surface without boundary and let be a closed geodesic in . We prove that any side of any triangle formed by distinct lifts of in is shorter then .
Key words and phrases:
Hyperbolic Surface, Poincaré Disc, Geodesic, Quasi-Isometry, Triangle, Tree, Free Group
2010 Mathematics Subject Classification:
Primary: 51M10; Secondary: 53C22, 30F45, 20E05
1. Introduction
Behaviour of closed geodesics in hyperbolic surfaces has been a fruitful subject of research for many years. Such geodesics are often studied by looking at their lifts in covering spaces of the surface, cf. [2], [3], [6], [8], [9], [11], and [4]. In this paper we consider three geodesics in which are lifts of the same closed geodesic in an orientable hyperbolic surface without boundary, cf. [7] and [4]. We prove that if these three geodesics intersect to form a triangle then each side of that triangle is shorter than . In contrast, a triangle in formed by three arbitrary geodesic lines can have sides of any length.
The main result of this paper is the following theorem.
Theorem 1**.**
Let be an orientable hyperbolic surface without boundary and let be a closed geodesic in . Any side of any triangle formed by distinct lifts of in is shorter then .
Theorem 1 is related to the results giving lower bounds on the angles of intersections of closed geodesics in hyperbolic surfaces, cf. [5].
An important tool in studying geodesics in is a tree in , defined in Section 2 of this paper, cf. [7], pp. 111-112 and [4]. It was shown in [4] that no analogue of Theorem 1 holds in .
The proof of Theorem 1 is given at in Section 5 of this paper. In order to prove Theorem 1, we need to prove the following special case first.
Lemma 1**.**
Let be an orientable non-compact hyperbolic surface without boundary which has finitely generated fundamental group and let be a closed geodesic in . Any side of any triangle formed by distinct geodesic lines in the preimage of in is shorter then .
Note that a single-punctured hyperbolic sphere has a trivial fundamental group, so it does not have closed geodesics, hence Lemma 1 is vacuously true in this case.
A twice-punctured sphere is homeomorphic to an annulus, so its fundamental group is infinite cyclic. Hence the preimage in of any closed geodesic in a two-punctured sphere consists of a single geodesic line. It follows that in this case there are no triangles in which satisfy the hypothesis of Lemma 1, so Lemma 1 is vacuously true in this case.
The proof of Lemma 1 for a hyperbolic single-punctured torus is given in [4].
The proof of Lemma 1 for all remaining cases is given in Section 4 of this paper.
2. The Tree T in
Excellent expositions of hyperbolic geometry can be found in [1], [10], [12], [13], and [14].
Let be an orientable non-compact hyperbolic surface without boundary which has finitely generated fundamental group. Let the genus of be and let be the number of punctures in . Let . There exist infinite simple disjoint geodesics in such that cut along the union of , is an open two-dimensional disk . Also there exist closed geodesics in such that point and for , which generate the fundamental group of . Note that the fundamental group of is a free group of rank . The universal cover of is the hyperbolic plane , so is the quotient of by the action of .
Let be a lift of the disc to . Note that is a -gon in .
Recall that an end of a surface without boundary and finitely generated fundamental group is homeomorphic to a product . Hyperbolic surfaces without boundary and finitely generated fundamental group have two kinds of ends: a cusp end, which has finite area, and a flare end, which has infinite area. If all the ends of are cusps then is an ideal -gon in . The action of on creates a tessellation of by the translates of the closure of .
Let be the graph in dual to that tessellation, i.e. the vertices of are located one in each translate of , and each edge of connects two vertices of in adjacent copies of , so each edge of intersects just one lift of one in one point. As is simply connected, is a tree. The tree can be considered to be the Cayley graph of the group which is a free group of rank generated by the set . Define the distance between two vertices and of to be the number of edges in a shortest path in connecting and .
Any element of acts on leaving invariant a unique geodesic line, called the axis of . The vertices of this geodesic line are characterized as those which minimize . That minimum is called the translation length of , and is equal to the length of the word in , obtained from by reduction and cyclic reduction. Denote the length of the word in by . Note that each oriented edge of is labeled by one of the generators or their inverses , so each oriented path in is labeled by a word in and .
The following result is a generalization of Lemma 1 in [4]. We include the proof for the sake of completeness of this paper.
Lemma 2**.**
Let be an element in and let be its reduced and cyclically reduced conjugate. Consider two axes in the tree stabilized by and its conjugate . If those axes intersect in an interval labeled with a word such that then they coincide.
Proof.
WLOG is an initial subword of , hence WLOG there exists a decomposition , where is either a generator or an inverse of a generator in . Let be a reduced and cyclically reduced conjugate of containing . Then the abelianization of implies that either or . In either case, the intersection of the axes of and of contains an interval of length , obtained by adding a single edge with label to an end of the interval with label . Hence the axes of and coincide. ∎
3. Quasi-Isometry of T and
In this paper we work with the Poincaré disk model of the hyperbolic plane and the Poincaré metric, given by
[TABLE]
Any pair of points and in the Poincaré disk are joined by a unique geodesic, which is a part of the circle or the straight line passing through and and orthogonal to the boundary of the Poincaré disc. The distance between and is given by
[TABLE]
The topology defined by that metric on the Poincaré disc is equivalent to the Euclidean topology, but the Poincaré disc equipped with the Poincaré metric is complete.
We consider the standard metric on the hyperbolic surface , given by the covering map from to .
Recall that a (not necessarily continuous) map from a metric space to a metric space is a quasi-isometry if there exists a constant and non-negative constants and such that the following two conditions are satisfied.
- (1)
For any pair of points and in ,
[TABLE] 2. (2)
For any point there exists a point such that
[TABLE]
Two metric spaces are called quasi-isometric if there exists a quasi-isometry between them. Note that two compact metric spaces are always quasi-isometric.
Let be an orientable non-compact hyperbolic manifold without boundary such that the fundamental group of is finitely generated and let be the tree in defined in the previous section.
Recall that a map is -equivariant if for any and .
Consider the closure of the -gon in , defined in the previous section. Its intersection with the tree , which we denote by , is a union of geodesic segments which have one end in common. That endpoint is a vertex of the tree , denote it by . Define a -equivariant continuous map as follows. Consider the -neighborhood of the boundary of for some small positive function . Denote by the intersection of that neighborhood with . For in the closure of define . For define in two steps. First, project onto the intersection of with . Second, stretch the image of the first step to fill the entire edge of the tree containing that image. Extend the map to the whole hyperbolic plane by the action of the group . By construction, the map is -equivariant and continuous.
Note that the restriction of to any compact subset of is a quasi-isometry even though might fail to be a quasi-isometry on the whole hyperbolic plane.
4. Proof of Lemma 1
Assume to the contrary that there exists a triangle in formed by geodesic lines , and , which are distinct lifts of the geodesic , such that the length of the side of lying in is longer than . Note that is stabilized by some element in which acts as a hyperbolic isometry of .
Let be the tree in defined in Section 2 and let be a reduced and cyclically reduced word conjugate to in . Note that the geodesic lines , and are transversal to the lifts of the geodesics in .
Let be the map defined in the previous section. Consider a very large disk in which contains . As was explained in the previous section, the map restricted to is a quasi-isometry. It can be arranged that the restriction of to the intersection of each of the lines , and with is monotone, so maps those intersections onto geodesics in .
Lemma 2 implies that the length of any side of is strictly less then .
As is a quasi-isometry, the length of any side of should be less than (length of for some constant and a non-negative constant . The careful analysis of the geometry of given below, shows that and , proving Lemma 1.
Indeed, let be the intersection of and , and let be the intersection of and . The length of is equal to the length of the segment from to . As is an isometry, the length of that segment is equal to the length of the segment from to . By assumption, the segment from to is longer than , so the segment from to is shorter than the segment from to . As is an isometry, the geodesics , and make the same angle with . Then as the segment from to is shorter than the segment from to , the angle between and is equal to the angle between and , and the opposite angles between and are equal, it follows that and intersect.
Consider the intersections of the lifts of the geodesics with lines , and . Let lifts of intersect both and to the left of the point and let lifts of intersect both and to the right of the point . Then there are lifts of crossing and , hence the length of the intersection is . Lemma 2 implies that . By a similar argument, the number of the lifts of intersecting both and is also less than . As is an isometry, there are lifts of crossing and to the left of . Then the total number of the lifts of crossing between the points and is at most , which is strictly less than . However by construction, the number of the lifts of crossing between the points and should be equal to . This contradiction completes the proof of Lemma 1.
5. Proof of Theorem 1
Let be any orientable hyperbolic surface without boundary (possibly with infinitely generated fundamental group) and let be a closed geodesic in . Let , and be distinct lifts of to the hyperbolic plane which form a triangle. Let generate the stabilizer of in . Let and be elements of such that and . Let be the cover of corresponding to the subgroup of generated by and . As has generators, it follows that is an orientable not-compact hyperbolic surface without boundary which has finitely generated fundamental group. As contains , it follows that lifts to a closed geodesic in , and the geodesics and are lifts of to the hyperbolic plane. So applying Lemma 1, we obtain that each side of the geodesic triangle formed by and is shorter that which by construction has the same length as .
6. Acknowledgment
The author would like to thank Peter Scott for helpful conversations.
The reference list from the paper itself. Each links out to its DOI / PubMed record.
- 1[1] A. F. Beardon, The Geometry of Discrete Groups , Graduate Texts in Mathematics 91 (1983), Springer, New York.
- 2[2] M.Freedman, J. Hass, and P. Scott, Closed Geodesics on Surfaces , Bull. LMS, 14 (1982), 385-391.
- 3[3] M. Gage, Curve Shortening Makes Convex Curves Circular , Invent. Math., 76 (1984), 357-364.
- 4[4] R. Gitik, Conjugate Words and Intersections of Geodesics in ℍ 2 superscript ℍ 2 \mathbb{H}^{2} , J. Topology and Analysis, DOI:10.1142/S 1793525320500107.
- 5[5] J. Gilman, A Geometric Approach to The Hyperbolic Jorgensen Inequality , Bull. AMS, 16 (1987), 91-92.
- 6[6] M. Grayson, Shortening Embedded Curves , Ann. of Math. (2), 129 (1989), 71-111.
- 7[7] J. Hass and P. Scott, Intersections of Curves on Surfaces , Israel J. Math, 51 (1985), 90-120.
- 8[8] J. Hass and P. Scott, Curve Flows on Surfaces and Intersections of Curves , Proc. Symp. Pure Math., 54 (1993) Part 3, 415-421.
