I will keep on talking about Cartan geometry in a quite leisurely way, always using our example of a sphere rolling around on a surface, since this is easy to visualize.
I'll gradually fumble my way to the definition of "Cartan connection" in this special case. But then, at the end, we'll be able to instantly generalize everything we did, simply by replacing the sphere and surface by more general spaces, the rotation group by a more general group, and so on. So, while Garrett will be bored silly and bristling with impatience for quite a while, eager for me to bring on the fancy formulas, at the end everything will be clear (I hope).
john baez said:
Anyway, imagine we have a little piece of surface sitting in Euclidean 3-space. Call it M. Let P be the space of all ways we can place a sphere on top of M.
I should not have called this P, since it doesn't match the thing called "P" in the general definition of "Cartan connection" that I gave quite a while back on this thread. So, let's call it Q. Let me restate some stuff I said, with this new notation:
Let Q be the space of all ways we can place a sphere on top of M.
Since we can make the sphere touch any point of M, and we can also rotate the sphere arbitrarily, we have
Q = M \times SO(3)
This gadget Q is an example of a "principal bundle", but I think I'll call it the space of placements, where a placement is a way of placing a sphere on top of M.
(If our surface M is topologically tricky, we may need a "nontrivial" principal bundle, which only looks locally like what I've written down.)
Now, sitting inside the 3d rotation group SO(3) is the 2d rotation group SO(2). Think of this as consisting of all rotations of our sphere that leave the south pole fixed - imagine the Earth spinning around on its axis.
The sphere, the group SO(3), and the group SO(2) have a special relationship - if you don't understand this you can't possibly understand Cartan geometry. This relation is:
S^2 = SO(3)/SO(2)
Here S^2 is our name for the sphere, since its surface is 2-dimensional.
What does this mean? The group SO(3) acts as rotations of the sphere, and it acts
transitively: we can carry any point on the sphere to any other point using some rotation. So, we can get to any point on the sphere by taking the south pole and applying some rotation. But, lots of different rotations carry the south pole to the same point! Indeed lots of different rotations carry the south pole to itself, and these form the group SO(2).
So, we can get all points on the sphere by rotations in SO(3) but this description of points on the sphere is redundant due to SO(2). This is what we mean by saying
S^2 = SO(3)/SO(2)
One can explain this more precisely, and I think somr people on this thread already did that when discussing a fancier example, namely
deSitter spacetime = SO(4,1)/SO(3,1)
But, right now I'm having fun trying to keep everything as jargon-free as possible. So, I'll just emphasize that this business is very general. If we have any space X, we can look for a group G that acts transitively on it. If we find one, this means we can describe any point of X by taking our favorite point (the "south pole") and applying some transformation in G. But, this description of points in X will usually be redundant: there will some transformations in G that carry the south pole to itself, and these will form a group H sitting inside G. So, we will have
X = G/H
So, we're developing Cartan geometry in the special case
X = S^2, G = SO(3), H = SO(2)
but everything will generalize painlessly. Note that in our special case the surface M has the same dimension as X. We always want that in Cartan geometry!
Okay, let's see where's a good place to wrap up before everyone's eyes glaze over. (Well, not everyone - Garrett will be very frustrated at my slow pace, but he's not paying me enough to write an exposition crafted personally for him!)
I guess I should point out this. We had a "space of placements"
Q = M \times SO(3)
whose points were all ways we could place a sphere on top of the
surface M. But, we also have a smaller space
P = M \times SO(2)
and this is really the star of the show in Cartan geometry.
What is this smaller space? It's the space whose points are
ways we can place a sphere on top of M, such that
the south pole of the sphere touches M!
Do you see why? A point in M \times SO(2) is a point in M, which says where your sphere touches the surface M, and a rotation in SO(2), which says how the sphere is rotated - but making sure the south pole touches the surface.
Now, it's sort of surprising that this P guy is the star of the show in Cartan geometry, because we want to talk about a
rolling ball, and P is about a ball whose south pole touches the surface M - it can't really roll!
That's actually why I screwed up and brought in that other guy, Q. But, introducing P is part of Cartan's cleverness.
Just so you have something to do, in case you're sitting there bored browing the web, here's a little puzzle. What are the dimensions of these various space (in our example):
M, SO(3), SO(2), S^2, P, Q
and how are these dimensions related? There are a bunch of simple relationships that are not coincidences - relationships that hold in any Cartan geometry.