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Gradient Like Vector Fields and Morse Trajectories — Examples
1 · Prerequisites
None. This page is self-contained.
2 · Summary
These calculations test the descending sign, endpoint geometry, and the noncompact completeness qualification without imposing Morse--Smale transversality.
3 · Logical flowchart
4 · Definitions, theorems and proofs
None yet.
5 · Examples, counterexamples and false statements
Negative-gradient lines for a quadratic Morse function
Example
On with its Euclidean metric, let . Its negative-gradient equation is
Verification
Given: The quadratic function on Euclidean space.
Solving the separated equations gives and . Thus the forward-stable coordinate disk is and the backward-unstable disk is .
Directly, , which is strictly negative away from the origin.
Meridian trajectories for height on the sphere
Example
On the round , let . The intrinsic gradient is , so the negative gradient is . Its nonconstant orbits are the meridians from the north pole to the south pole.
Verification
Given: The round unit sphere and the height function .
The tangential projection of is , so the displayed vector field is the negative gradient. Along it, whenever .
The longitude is constant along the flow, while decreases from to . Therefore every nonpolar longitude gives a meridian from north to south, a one-parameter family before quotienting by time translation.
Gradient flow for a Morse function on the flat torus
Example
On the flat torus with angular coordinates , take . Its critical points are (maximum, index ), and (saddles, index ), and (minimum, index ). The negative-gradient equations are
Verification
Given: The flat two-torus and .
Differentiating gives , hence the displayed negative-gradient equations. Their zeros give exactly the four listed critical points, and the diagonal Hessian gives the stated indices.
The circles and are invariant and supply the coordinate-circle separatrices. On either component of , each nonconstant coordinate trajectory has backward limit and forward limit (it increases on and decreases on in the displayed coordinate). Thus the trajectories off those circles run from the maximum to the minimum in four arc-choice components. In each component, quotienting the two integration constants by common time translation leaves a one-parameter family.
Using the positive gradient reverses the stable and unstable dimensions
Statement refuted
For , one may use the positive gradient while retaining the descending convention that the unstable dimension equals the Morse index.
Counterexample
Given: The Euclidean quadratic evolved by .
The positive-gradient equations are and , so and .
Thus the forward-stable space is of index dimension and the backward-unstable space is of coindex dimension. The labels are reversed from the descending convention, refuting the assertion.
A gradient flow on a noncompact manifold can be incomplete
Statement refuted
Every negative-gradient vector field on a noncompact manifold is complete.
Counterexample
Given: The Euclidean line and .
Since , the negative-gradient field is and its equation is .
For , the solution is , which tends to as . Hence its maximal interval has a finite positive endpoint and the field is incomplete.
This witnesses incompleteness only: is not offered as a Morse-function example.