Opentopia Directory Encyclopedia Tools

Poincaré half-plane model

Encyclopedia : P : PO : POI : Poincaré half-plane model


In non-Euclidean geometry, the Poincaré model, named after Henri Poincaré, is a model of two-dimensional hyperbolic geometry as a homogeneous space for the group of Möbius transformations. The model is commonly expressed in terms of the complex upper half-plane or the unit disc, both of which are related through a conformal mapping. Along with the Klein model and the Poincaré disk model, it was proposed by Eugenio Beltrami who used these models to show hyperbolic geometry was equiconsistent with Euclidean geometry.

The Poincaré metric is a metric tensor on the disk or plane, expressing its hyperbolic nature.

Symmetry groups

A variety of different groups appear in the discussion of the upper half-plane. One is the linear group GL(2,C), called the Möbius group. The projective linear group PGL(2,C) is isomorphic to the group of all orientation-preserving conformal maps of the upper half-plane. Important subgroups of PGL(2,C) are called Kleinian groups. However, conformal maps do not in general preserve the Poincaré metric and thus are not an isometry of the Poincaré model.

There are four groups that do preserve the metric tensor. These are:

The relationship of these groups to the Poincaré model is as follows: Important subgroups of the isometry group are the Fuchsian groups.

One also frequently sees the modular group SL(2,Z). This group is important in two ways. First, it is a symmetry group of the square 2x2 lattice of points. Thus, functions that are periodic on a square grid, such as modular forms and elliptic functions, will thus inherit an SL(2,Z) symmetry from the grid. Second, SL(2,Z) is of course a subgroup of SL(2,R), and thus has a hyperbolic behavior embedded in it. In particular, SL(2,Z) can be used to tessellate the hyperbolic plane into cells of equal (Poincaré) area.

Isometric symmetry

The group action of the special linear group PSL(2,R) on H is defined by

[\left(\begina&b\\ c&d\\ \end\right) \cdot z = \frac = .]
Note that the action is transitive, in that for any [z_1,z_2\in\mathbb], there exists a [g\in (2,\mathbb)] such that [gz_1=z_2]. It is also faithful, in that if [gz=z] for all z in H, then g=e.

The stabilizer or isotropy subroup of an element z in H is the set of [g\in(2,\mathbb)] leave z unchanged: gz=z. The stabilizer of i is the rotation group

[(2) = \left\\cos\theta&\sin\theta\\ -\sin\theta&\cos\theta\\ \end\right)\,:\,\theta\in\right\}.]
Since any element z in H is mapped to i by an element of PSL(2,R), this means that the isotropy subgroup of any z is isomorphic to SO(2). Thus, H = PSL(2,R)/SO(2). Alternately, the vector bundle of unit-length tangent vectors on the upper half-plane is isomorphic to PSL(2,R).

The upper half-plane is tessellated into free regular sets by the modular group SL(2,Z).

Geodesics

The geodesics for this metric tensor are circular arcs perpendicular to the real axis (half-circles whose origin is on the real axis) and straight vertical lines ending on the real axis.

The unit-speed geodesic going up vertically, through the point i is given by

[\gamma(t) = \left(\begine^&0\\ 0&e^\\ \end\right) \cdot i = ie^t.]
Because PSL(2,R) is an isometry of the upper half-plane, this geodesic is mapped into the other geodesics through the action of PSL(2,R). Thus, the general unit-speed geodesic is given by

[\gamma(t) = \left(\begina&b\\ c&d\\ \end\right) \left(\begine^&0\\ 0&e^\\ \end\right) \cdot i = \frac ]
This provides the complete description of the geodesic flow on the unit-length tangent bundle (complex line bundle) on the upper half-plane.

See also

References

 


From Wikipedia, the Free Encyclopedia. Original article here. Support Wikipedia by contributing or donating.
All text is available under the terms of the GNU Free Documentation License See Wikipedia Copyrights for details.

Search Titles
0123456789
ABCDEFGHIJ
KLMNOPQRST
UVWXYZ?

E-mail this article to:

Personal Message: