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Complex Analysis and Differential Geometry
Notes Setting s = 0, (14) follows.
Proof of Proposition 5. We compute:
1 b b b
E 2 a Yg (X,X)dt a Yg Y X,X dt a Yg X Y,X dt
Y
b
a g X Y,X g X Y, Y X dt
Y
b
a g Y Y,X g Y , X Y,X g X Y, X Y dt
X
b d
dt,
g Y,X g Y, X R(X,Y,Y,X) g Y, Y
a dt Y Y X X X
,
where as above X and Y = . Now, the first term integrates to g Y Y,X a b 0, and when
we set s = 0, the second term also vanishes since X X 0. Furthermore, the last term
Y . Hence, we conclude:
becomes g Y,
b 2
E (0) a Y R(X,Y,X,Y) dt. ...(15)
The proposition now follows from (12).
Thus, E (0) can be viewed as a quadratic form in the generator Y . The corresponding symmetric
bilinear form is called the index form of :
b
I(Y,Z) a g Y, Z K g Y,Z g ,Y g ,Z dt.
It is the Hessian of the functional E, and if E has a local minimum, I is positive semi-definite. We
will also write I(Y) = I(Y, Y).
Definition 6. Let be a geodesic parametrized by arc length on the Riemannian surface (U, g). A
vector field Y along is called a Jacobi field, if it satisfies the following differential equation:
Y K Y g ,Y
0.
Two points (a) and (b) along a geodesic are called conjugate along if there is a non-zero
Jacobi field along which vanishes at those two points.
The Jacobi field equation is a linear system of second-order differential equations. Hence given
initial data specifying the initial value and initial derivative of Y, a unique solution exists along
the entire geodesic .
Proposition 6. Let be a geodesic on the Riemannian surface (U, g). Then given two vectors
Z , Z T (a) U, there is a unique Jacobi field Y along such that Y(a) = Z , and Y(a) Z .
2
2
1
1
In particular, any Jacobi field which is tangent to is a linear combination of and t . The
significance of Jacobi fields is seen in the following two propositions. We say that is a variation
of through geodesics if the curves t (t;s) are geodesics for all s.
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