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Lesson 25 of 30

Jacobi fields and geodesic separation

Derive the linearized equation for neighboring geodesics.

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Try

Shoot nearby unit-speed geodesics from one point. On a plane their separation initially grows linearly. On a sphere they eventually meet again at the antipode. In a hyperbolic plane their separation grows faster than linearly. Jacobi fields turn this comparison into a differential equation.

A Jacobi field is the variation field produced by a smooth family of geodesics, or equivalently a solution of the resulting linearized geodesic equation along a fixed geodesic. The linearization describes infinitesimal separation, not the exact distance between two widely separated curves.

Predict

Predict why curvature should enter the derivative-commutation step. Covariant derivatives in different directions need not commute; their discrepancy is the curvature tensor.

Predict whether every point where global shortest paths stop being unique is caused by a Jacobi field vanishing. A flat cylinder has competing routes from topology without positive-curvature focusing, so cut points and conjugate points are different concepts.

Experiment

For a unit-speed geodesic and perpendicular initial variation with j(0)=0,j′(0)=1, compare constant-curvature solutions.

KScalar separation j(s)First positive zero
0sNone
a², a>0sin(as)/aπ/a
−a²sinh(as)/aNone

Differentiate each expression twice and check both initial conditions. The normalization j′(0)=1 fixes the scale of the infinitesimal opening angle. It does not claim that arbitrary finite geodesic spacing equals j exactly.

Understand

Let F(s,ε) be a variation by geodesics, T=F_s and J=F_ε. Each radial curve satisfies D_sT=0. Differentiate this identity in ε and commute derivatives using our convention R(X,Y)Z=∇_X∇_YZ−∇_Y∇_XZ−∇_[X,Y]Z. Since the parameter fields commute and the connection is torsion-free, D_εT=D_sJ. The result is D_s²J+R(J,T)T=0.

Along a unit-speed surface geodesic choose a parallel unit field E perpendicular to T. For a normal variation J=jE, the second covariant derivative is j″E. The surface curvature identity gives R(E,T)T=KE. Therefore the Jacobi equation reduces to j″+Kj=0, with K evaluated along the geodesic.

The table solves this scalar ODE when K is constant. Positive curvature can force a second zero; in the round sphere this corresponds to the failure of the exponential map’s differential at the antipode. Nonpositive constant curvature produces no such zero in these radial examples.

Apply

A conjugate point is detected by a nonzero Jacobi field vanishing at both endpoints, equivalently a singularity of the exponential differential along the appropriate initial vector. This is a local variational phenomenon. A cut point concerns where a geodesic ceases to be globally minimizing, and can occur because another distinct minimizing route arrives first.

On a flat cylinder, points half a circumference apart have two equal shortest routes around the cylinder. Yet K=0 and the normal Jacobi solution s has no positive zero. This separates topological competition from curvature focusing.

Repair “Negative curvature makes all distances increase exponentially.” The table concerns an infinitesimal normal variation in constant curvature. A general statement about arbitrary pairs, variable curvature or nonunit parameters needs additional hypotheses and comparison theorems.

Continue

State the reference geodesic, initial variation and curvature convention before interpreting a Jacobi calculation. Continue to completeness and minimizing geodesics to examine global existence and shortest-path questions that local ODE theory alone does not settle.

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Practice and reasoning

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For curvature K=−4 and normal Jacobi data j(0)=0,j′(0)=1, use j(s)=sinh(2s)/2 to find j′((log 2)/2), where log is the natural logarithm.

Integers, fractions and finite decimals are accepted. Expressions such as sqrt(2) are not parsed by this checker.

On a sphere of radius R, the first zero after zero of the radial normal Jacobi solution occurs at

Your response

For a variation by unit-speed geodesics with tangent T and variation field J, derive D_s²J+R(J,T)T=0.

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On an oriented surface along a unit-speed geodesic, use a parallel unit normal E in the tangent plane to reduce J=jE to j″+Kj=0.

Structure your argument and preserve revisions

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Each field allows 2,000 characters. Keep a specific claim, state where it applies, cite the facts you use, and explain what still needs checking. Blank fields are allowed and are not evidence of mastery.

Solve j″+Kj=0 with j(0)=0,j′(0)=1 for K=0, K=a² and K=−a², a>0.

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Each field allows 2,000 characters. Keep a specific claim, state where it applies, cite the facts you use, and explain what still needs checking. Blank fields are allowed and are not evidence of mastery.

Why can global minimizing behavior fail before a conjugate point? Give a flat example.

Structure your argument and preserve revisions

These optional planning fields save locally. Recording your response saves an immutable copy of the argument and these fields. Older records may contain only first/latest responses; missing intermediate revisions are not reconstructed.

Each field allows 2,000 characters. Keep a specific claim, state where it applies, cite the facts you use, and explain what still needs checking. Blank fields are allowed and are not evidence of mastery.

Reflect and continue

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