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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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