Elliptic, hyperbolic and parabolic geometry

The three models of surfaces can be seen within a common framework.
Let's consider the space M4, that is, the manifold R4 with coordinates (x,y,z,t) but with the pseudo-Riemannian metric given in each tangent space by

ds2=dx2+dy2+dz2dt2.

This space with this pseudo-metric is called Minkowski space, and can be also denoted by R3,1.
This metric is left invariant by the group O(3,1) when acting on M4. It also leaves invariant the cone

t2x2y2z2=0

so is logical that we pay attention to it, because it is very "physical": the group O(3,1) represents all the change of point of view of a physical observer, that is, rotations and Lorentz boost.
Now, following [TRTR] from Penrose page 423, we can consider the family of hyperplanes inside M4 given by

z+t+λ(tz)=2

intersecting our cone in different 2-dimensional submanifolds Pλ of M4.
Here we have a picture from that book, where we consider only (x,z,t) for purposes of drawability.
conicgeometry.png

If we analyse the case λ=0, we observe that we obtain the submanifold P0, E in the picture with a shape of a parabola, given by the embedding

ϕ:R2M4(u1,u2)(u1,u2,1u12+u224,1+u12+u224)

We can look for the (possibly pseudo) Riemannian metric inherited by P0. Since

dϕ=(1001u12u22u12u22)

we conclude that P0 consists of R2 with the euclidean metric:

g=(1001)

That is, although we see it like a parabola, intrinsically is only the Euclidean plane, and that is the reason the latter is sometimes called parabolic geometry.
But, what happens for others λ? Let's see. We have a far more complicated parametrization of our embedded manifold:

ϕ(u1,u2)=(u1,u2,1+λ+(1+λ)2(1+λ(u12+u22))2λ,2+λ+(1+λ)2(1+λ(u12+u22))+1(1+λ)2(1+λ(u12+u22))λ2(1+λ))

(computations made with Mathematica).
If we compute the (possibly pseudo) Riemannian metric in this chart we obtain the inherited metric in R2

gλ=(1λu221λ(u12+u22)λu1u21λ(u12+u22)λu1u21λ(u12+u22)1λu121λ(u12+u22))

Next step is to show that for λ>0 we have an isometry into the usual sphere (a model for spherical geoemtry), and that for λ<0 we have an isometry into a model for hyperbolic geometry. This would justify the terms elliptic and hyperbolic for those geometries, as you can see at the picture above (S and H respectively). In order to keep it simple we can work with λ=1 and λ=1.
For λ=1, we have

g=(1u221(u12+u22)u1u21(u12+u22)u1u21(u12+u22)1u121(u12+u22))

But if we look at a typical chart of the usual sphere in E3

ψ:(x,y)(x,y,1x2y2)

and compute the metric we obtain just

g=(1y21(x2+y2)xy1(x2+y2)xy1(x2+y2)1x21(x2+y2))

so they are the same.
And for λ=1 we have

g=(1+u221+u12+u22u1u21+u12+u22u1u21+u12+u221+u121+u12+u22)

But if we look at the typical model for hyperbolic plane that consists of the pseudosphere embedded in M3:

x2+y2z2=1

with a chart given by

ψ:(x,y)(x,y,1+x2+y2)

we obtain the inherited metric in R2 (keep an eye: inherited from the Minkowski metric, not the Euclidean one):

g=(1+y21+x2+y2xy1+x2+y2xy1+x2+y21+x21+x2+y2)

so we are done.