"Don't panic!" said:
I think what has confused me earlier is that we discussed how points on a manifold could be locally described by n-tuples in \mathbb{R}^{n} and we can do this because the manifold is locally homeomorphic to Euclidean space, but to me this implies that the manifold is locally flat and so Cartesian coordinates are applicable. However, if we do consider larger patches that are curved (in the sense that the geometry over them is non-Euclidean) how can we still describe the points in terms of n-tuples of coordinates in \mathbb{R}^{n}?
Well, take the example of the surface of the Earth. The "patch" that is the entire Earth except for the north and south poles can be described by the pair of coordinates:
(latitude, longitude).
So it's a 2-D manifold described by two coordinates. It's certainly non-Euclidean, though.
Here is perhaps a way to think about it: You have a two-dimensional space. That means that the points on that space can be described by two real numbers: (x,y). For simplicity, let me assume that it is Riemannian, which just means that the relevant notion of "length" of a curve through space is always positive. Let \mathcal{P}_0 and \mathcal{P}_1 be two points that are close enough together that there is a unique minimal-distance path connecting the two. Let the coordinate of the two point be written as:
\mathcal{P}_0 = (x, y)
\mathcal{P}_1 = (x+\delta x, y + \delta y)
Let \delta s be the distance between the points (as measured along the unique minimal-distance path).
\delta s^2 can be expressed as a double power series in \delta x and \delta y as follows:
\delta s^2 = A_{xx} \delta x^2 + A_{xy} \delta x \delta y + A_{yx} \delta y \delta x + A_{yy} \delta y^2
+ B_{xxx} \delta x^3 + B_{xxy} \delta x^2 \delta y + ...
+ C_{xxxx} \delta x^4 + C_{xxxy} \delta x^3 \delta y + ...
+ ...
The first line groups together the terms that are second-order in the differences \delta x, \delta y. The second line are the terms of 3rd order, the third line are the terms of 4th order, etc.
So far, that's true for any 2D patch, and for any coordinate system on that patch. We can define the coordinate system to be "locally cartesian at point \mathcal{P}_0" if
- A_{xx} = A_{yy} = 1
- A_{xy} = A_{yx} = 0
- For all i, j, k, B_{ijk} = 0
For every 2-D patch, and for every point on that patch, there is a coordinate system that is locally cartesian at that point.
For the coordinate system to be
globally cartesian within the patch, it would have to be the case that all the terms are zero except for the first line (only 2nd order terms).