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Unit 29: Geodesics
Thus, any result proved concerning the usual covariant differentiation, in particular also for the Notes
covariant differentiation along a curve.
Y 0.
Definition 2. A vector field Y along a curve is said to be parallel along if
Note that if Y and Z are parallel along , then g(Y,Z) is constant.
g(Y,Z) g Y,Z g Y, Z 0.
Proposition 1. Let :[a,b] U be a curve into the Riemannian surface (U, g), let u U, and let
0
Y Tu U. Then there is a unique vector field Y along which is parallel along and satisfies
0
0
Y(a) = Y .
0
Proof. The condition that Y is parallel along is a pair of linear first-order ordinary differential
equations:
i
y i jk j y . j
i
Given initial conditions i (a) y , the existence and uniqueness of a solution on [a, b] follows
0
from the theory of ordinary differential equations.
The proposition together with the comment preceding it shows that parallel translation along a
curve is an isometry between inner-product spaces P : T U T U.
a
b
Definition 3. A curve is a geodesic if its tangent is parallel along :
0.
If is a geodesic, then is constant and hence, every geodesic is parametrized proportionally
to arc length. In particular, if is a reparametrization of , then is not a geodesic unless
is a linear map.
Proposition 2. Let (U, g) be a Riemannian surface, let u U and let 0 Y T U. Then there is
0
0
u0
and > 0, and a unique geodesic :( , ) U, such that (0) u , 0 and (0) Y . 0
Proof. We have:
i i jk j k . i
Thus, the condition that is a geodesic can written as a pair of non-linear second order ordinary
differential equations:
j
i
i jk (t) k .
i
i
i
Given initial conditions i (0) u , (0) y , there is a unique solution on defined on a small
0
0
enough interval (, ).
Definition 4. Let :[a,b] U be a curve. We say that is length minimizing, or L-minimizing,
if:
L L
for all curves in U such that (a) (a) and (b) (b).
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