Geodesic normal coordinates are local coordinates on a manifold with an affine connection afforded by the exponential map and an isomorphism given by any basis of the tangent space at the fixed basepoint p ∈ M. If the additional structure of a Riemannian metric is imposed, then the basis defined by E may be required in addition to be orthonormal, and the resulting coordinate system is then known as a Riemannian normal coordinate system. Normal coordinates exist on a normal neighborhood of a point p in M. A normal neighborhoodU is a subset of M such that there is a proper neighborhood V of the origin in the tangent space TpM, and expp acts as a diffeomorphism between U and V. On the normal neighborhood U of p in M, the chart is given by: The isomorphism E can be any isomorphism between the two vector spaces, so there are as many charts as there are different orthonormal bases in the domain of E.
Properties
The properties of normal coordinates often simplify computations. In the following, assume that is a normal neighborhood centered at a point in and are normal coordinates on.
Let be some vector from with components in local coordinates, and be the geodesic at pass through the point with velocity vector, then is represented in normal coordinates by as long as it is in.
The coordinates of a point are
In Riemannian normal coordinates at a point the components of the Riemannian metric simplify to, i.e.,.
The Christoffel symbols vanish at, i.e.,. In the Riemannian case, so do the first partial derivatives of, i.e.,.
Explicit formulae
In the neighbourhood of any point equipped with a locally orthonormal coordinate system in which and the Riemann tensor at takes the value we can adjust the coordinates so that the components of the metric tensor away from become The corresponding Levi-Civita connection Christoffel symbols are Similarly we can construct local coframes in which and the spin-connection coefficients take the values
On a Riemannian manifold, a normal coordinate system at p facilitates the introduction of a system of spherical coordinates, known as polar coordinates. These are the coordinates on M obtained by introducing the standard spherical coordinate system on the Euclidean spaceTpM. That is, one introduces on TpM the standard spherical coordinate system where r ≥ 0 is the radial parameter and φ = is a parameterization of the -sphere. Composition of with the inverse of the exponential map at p is a polar coordinate system. Polar coordinates provide a number of fundamental tools in Riemannian geometry. The radial coordinate is the most significant: geometrically it represents the geodesic distance to p of nearby points. Gauss's lemma asserts that the gradient of r is simply the partial derivative. That is, for any smooth functionƒ. As a result, the metric in polar coordinates assumes a block diagonal form