A rigid motion is a linear transformation from a
vector space to itself such that the inner product structure is
preserved; that is, lengths, angles and areas are unchanged by the
mapping. There are three classes of rigid motions (isometries) of
the hyperbolic plane: inversions through a semicircle geodesic,
translations parallel to the
-axis,
and reflections about vertical geodesics. This is slightly different
from the group of isometries of
,
where we have any translation, any reflection about a line, a
rotation about a point, and a translation composed with a reflection
(a so-called "glide reflection").
We can write the explicit function of each isometry
using the complex half plane. An inversion through a semicircle of
radius
is

with
.
Note that an inversion of a polar function
centered at the center of the inversion semicircle
yields another polar function
,
and that inversions always reverse the orientation of the set upon
which it acts (just like a Euclidean reflection). Also, note
that two consecutive inversions through different semicircles
correspond to a hyperbolic rotation, in that a single point (the
intersection of the semicircles) is fixed and orientation is
preserved.
The formula for a reflection about a vertical ray
with
-coordinate
is
,
and the expression for a translation parallel to the real axis is
with
.

The figure
to the right shows that just as two
inversions can form a rotation, so can three non-collinear
translations. The segment
is parallel transported around the
triangle is such a way that the angle it makes with the initial
segment is non-zero in general (unless the triangle is ideal).
Hence, the segment
has been rotated by the angle defect of the
triangle. Remember, though, that translations not parallel to
the real axis are not isometries, and hence are not members of the
group of orthogonal transformations of
.

Let's examine the group structure of the
orientation-preserving isometries of
(the complete group of isometries, including orientation-reversing
ones, is denoted
, where the
star indicates that the determinant of the elements of that group
may be 1 or -1. For the most case, we only need to deal
with orientation-preserving transforms).
We denote this group by
,
known as the projective special linear group of dimension 2 over the
real numbers (which is the special linear group modulo the parity
group). This group acts on
as
via the complex
mapping
, with
. These
transformations are known as Möbius Transformations, which
we discuss in the next section. These transformations only preserve
the upper half-plane, though: to map all of
,
we need
,
not just the reals. Hence we have that
is the group of conformal automorphisms of the upper half plane
.
The action
is
transitive, so that
such that
. It is also
faithful, so that if
, then
, the identity
element of
, which is
just the constant 1. We can make an association between the Möbius
transformation
and the 2x2 matrix
.
Here we can see the relation to the special linear group: it is
required that
. The
stabilizer of an element
is the set
. This does not
automatically mean that
is 1; for example, the stabilizer
of the complex number
is

which is just the special orthogonal group of dimension
2. Since the action of
on
is transitive, any
can be mapped to
by some
in the group, and we
have the isomorphism
, so
that
is actually isomorphic
to the quotient group
.
Pretty amazing!
Let us now examine more closely the elements of
as they relate to the metric and as transforms of
.
We already know that
,
but let's prove that these are actually isometries, that is, they
leave the hyperbolic metric invariant. The Möbius transform
can be differentiated and simplified to yield
,
where
is the transformed complex number. Now,

so that we may make a relation between the primed and unprimed coordinates:

or, when we use
,

so that we can see that Möbius transformations
preserve the metric of
, and
hence are isometries. Since they preserve distance, we may take the
unit-speed geodesic through
as

In general, this geodesic can then be mapped to
other geodesics by elements of
as

We already know that there is a biholomorphic (bijective
holomorphic) function that maps the upper half-plane which we now
call
to the
unit disk
as a
consequence of the Riemann Mapping Theorem. In this model (the
Poincaré Disk Model), the hyperbolic plane is the set of points
lying inside of the unit circle, with the circle itself representing
the boundary at infinity. The complex function
takes the real axis to the unit circle, and the upper half-plane to
its interior, while the function
is its inverse. Note that these are both Möbius Transformations,
hence it will take geodesics to geodesics and is a conformal
mapping. If
is a
rigid motion in
,
then
is a
rigid motion in
,
so that rigid motions in the disk model take the form

with
.
Let's examine the metric on
and get a sense of what geodesics look like in the disk model. Let
and
so that
.
Then we have that
.
By equating the real and imaginary parts, we have
that
and
. The
total differential can be found via
and a similar
expression for
, with partial derivatives of

and

by the Cauchy-Riemann conditions. Hence

Now let us consider a curve
in
and a curve
in
.
Because the spaces are isometric,


so that the metric can be seen to be

for the Poincaré disk model. As an aside, let us look at a different parameterization.
The unit disk model, when the boundary is included, is homeomorphic to
the unit disk in ordinary two dimensional space. This suggests that
a polar form of hyperbolic coordinates could be used to describe
this space. Let the polar coordinates in normal 2D space be
and the hyperbolic coordinates be
(clearly the angular dependence is unchanged by symmetry). Then a
re-parameterization of the radial distance is given by

so that
.
From ordinary polar theory, we can now write
and
and
rewrite the metric using
and
:


We are now ready to examine the shape of geodesics
in
. Again due to the isometric nature of the Möbius map between
the models, we can apply our transformation to the geodesics of the
half-plane to obtain geodesics on the disk. We can see that the
geodesics on the disk are arcs of circles perpendicular to the
boundary of the disk, as well as diameters. The diameters correspond
to the vertical ray geodesics of the half-plane model, while the
arcs orthogonal to the boundary are the transforms of the
semicircles centered on the
-axis. It is important to note that the
boundary of the disk itself is not part of the hyperbolic space, but
can be included in a compactified region just as the point at
infinity can be included in the stereographic projection of the
complex plane. Hypercycles in the disk model are then arcs of
circles that cross the boundary (not necessarily at 90 degrees).
Let us look at how we might obtain a formula for
the distance between two points in
.
We start by noting that for any curve in the disk, we can
parameterize it by
,
so that

hence the hyperbolic distance along a diameter of
the disk is
.
Now let's look at the map
,
which maps the disk to itself and hence is a member of the group of
automorphisms on the disk. Because it is a Möbius transformation,
it is an isometry, and we see that it maps
,
so that

where we have used the relation
.
It would now be instructive to discuss Gaussian
curvature and it's relation to hyperbolic space. While the complete
definition of Gaussian curvature is rather technical, we can say
that it is an intrinsic measure of how a surface is curving,
independent of the space in which it is embedded. To find the
Gaussian curvature of hyperbolic space in these various models, we
first consider the notion of a conformal metric. This is a
metric which can be written as
,
so that the arc length is directly proportional to the Euclidean
metric through some function of z. For the disk model, we
have
,
while for the half plane we have
.
If the metric is conformal, we can immediately compute the Gaussian
curvature of the space using
,
where we use
. It
is easy to compute
for the two Poincaré models
discussed thus far, and we see that the Gaussian curvature is a
constant -1. The fact that it is constant means that the curvature
is the same at every point in space, and the fact that it is
negative means that the surface curves inward (like a saddle) at
every point. It is a remarkable fact that no matter how you model or
parameterize the space, the Gaussian curvature does not change, and
can be computed solely from the metric.
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