On a complete compact Riemannian manifold, nondegenerate critical points of fixed-endpoint geodesic energy yield a CW complex model of the path space, with one cell per geodesic and dimension equal to its Morse index. Finite-dimensional broken-geodesic models prove the assertion at bounded energy, and exhaustion gives the full path space. On with distinct nonantipodal endpoints the cell dimensions are , one in each such dimension.
Morse index theorem 2026-10-06
The Morse index of a fixed-endpoint geodesic equals the number of conjugate points strictly between its endpoints, counted with multiplicity. Its nullity equals the multiplicity of the terminal conjugate point. A conjugate multiplicity is the dimension of the space of Jacobi fields vanishing at the initial point and at the point in question.
Morse theory 2026-10-06
Morse theory relates the critical points of a Morse function to changes in the homotopy type of its sublevel sets. Crossing a nondegenerate critical value attaches a cell or handle of dimension equal to the Morse index. The theory also applies to geodesic energy through broken-geodesic approximations.
Along the downward gradient flow, the gradient-flow dissipation identity, the chain rule and the defining property of the Riemannian gradient give
A smooth vector field on a compact manifold is complete, so the trajectory exists for every . In particular, its function value never increases.
If the trajectory is still in at time , its monotone function value has stayed in throughout . Consequently
Thus a uniform exit bound is
The trajectory is outside the closed band for every . Once it leaves below level , monotonicity prevents its return. The argument also covers the zero-width band .
For the total occupation-time bound for a gradient flow, let and , which exist by compactness. For every , the same gradient flow identity gives
Taking , by monotone convergence theorem, gives the total occupation-time bound
This allows arbitrarily many visits to ; it bounds their total duration. Neither of these two estimates needs the Morse function hypothesis.
For exponential convergence of a Morse gradient flow, first observe that a limiting point is a critical point. Indeed, writing for the flow and using continuous dependence on initial data,
Differentiation at gives .
We use the Morse lemma: near a nondegenerate critical point of Morse index , there are coordinates in which
Choose a Riemannian metric equal to the Euclidean metric on a smaller ball in these coordinates. Such a global Riemannian metric exists by a partition of unity: patch this metric to any background metric outside a slightly larger ball. One can do this simultaneously at every critical point, since a Morse function on a compact manifold has only finitely many critical points. The metric is chosen before forming its gradient flow; changing the metric can change trajectories.
For this metric, any trajectory converging to eventually remains in the smaller coordinate ball. From some time onward its equations are exactly
Convergence forces , and then
The straight radial segment stays in the coordinate ball, so its length bounds the Riemannian distance from above:
Increase beyond both and . Then the requested strict estimate holds for all :
This proof uses the Morse lemma, existence and uniqueness for smooth ordinary differential equations, continuous dependence on initial data, and the existence of a partition of unity. The expanding coordinates explain why convergence to a saddle occurs only along its stable manifold.
For a counterexample, use an arc coordinate around a point of the circle, its flat local metric, and a globally smooth function that equals on this arc. Such a function can be made by a smooth cutoff, agreeing with a positive constant outside a larger arc. For sufficiently small the downward gradient flow remains in the arc and is
It converges to the degenerate critical point , and its Riemannian distance from is for sufficiently large . For every , , so no exponential bound is possible. This counterexample is on a compact manifold as well.
Figure 1.
Exponential decay near a Morse minimum and algebraic decay near a degenerate quartic minimum, on a logarithmic vertical scale
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