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Gradient Like Vector Fields and Morse Trajectories

1 · Prerequisites

2 · Summary

The descending equation fixes the trajectory orientation. Under Countable Choice (ACω), compactness supplies flow completeness; tail-limit compactness and critical-point finiteness are established separately. These compactness conclusions are not silently inherited by noncompact applications.

3 · Logical flowchart

4 · Definitions, theorems and proofs

DefinitionDefinition: Literature-sourcedProof: Not applicablejudge pass (gpt-5.6-terra)audited 2026-09-06Open item page →

The Riemannian gradient is the metric dual of the differential

Definition

Let g be a Riemannian metric on a smooth manifold M and let f:M→R be smooth. The Riemannian gradient of f is the smooth vector field grad⁡gf characterized by

gx((grad⁡gf)x,v)=dfx(v)for every x∈M and v∈TxM.

Pointwise, it is the inverse metric-dual of dfx. In a local frame with metric matrix (gij) and inverse (gij), it is

grad⁡gf=∑i,jgij∂f∂xj∂xi;

the displayed coefficients are smooth, so this pointwise definition is a smooth vector field.

LemmaStatement: Literature-sourcedProof: Literature-sourcedjudge pass (gpt-5.6-terra)audited 2026-09-06Open item page →

The Riemannian gradient vanishes exactly at the critical points

Statement

For a Riemannian metric g, a smooth f:M→R, and x∈M, grad⁡gf(x)=0 if and only if x is a critical point of f.

Facts & Assumptions

Given: A Riemannian metric g, a smooth function f:M→R, and x∈M.

[F1]

The gradient is characterized by gx(grad⁡gf(x),v)=dfx(v) for every v∈TxM (The Riemannian gradient is the metric dual of the differential).

[F2]

A point is critical exactly when its differential is the zero map (Critical points and critical values of a smooth function).

Proof

technique · direct
1.1F1given

If grad⁡gf(x)=0, then [F1] gives dfx(v)=gx(0,v)=0 for every v, so dfx=0.

1.2F1given

Conversely, if dfx=0, then [F1] gives gx(grad⁡gf(x),v)=0 for every v. Taking v=grad⁡gf(x) and using positive definiteness gives grad⁡gf(x)=0.

2.1F2step 1.1step 1.2∎

By [F2], the two implications say exactly that grad⁡gf(x)=0 if and only if x is critical.

DefinitionDefinition: Literature-sourcedProof: Not applicablejudge pass (gpt-5.6-terra)audited 2026-09-06Open item page →

Negative-gradient trajectories of a Morse function

Definition

Let f:M→R be a Morse function and let g be a Riemannian metric. A negative-gradient trajectory is a maximal integral curve γ:I→M of −grad⁡gf; that is, it satisfies

γ˙(t)=−grad⁡gf(γ(t))(t∈I).

Here I is maximal among intervals on which this solution extends. It is a full trajectory when I=R. The word “negative” fixes the descending convention used below.

LemmaStatement: Literature-sourcedProof: Literature-sourcedjudge pass (gpt-5.6-terra)audited 2026-09-06Open item page →

A negative-gradient trajectory satisfies the energy identity

Statement

If γ:I→M is a negative-gradient trajectory of f for g, then

ddtf(γ(t))=−∥grad⁡gf(γ(t))∥g2(t∈I).

No compactness or completeness is assumed.

Facts & Assumptions

Given: A negative-gradient trajectory γ:I→M of f for g and t∈I.

[F1]

Its velocity is γ˙(t)=−grad⁡gf(γ(t)) (Negative-gradient trajectories of a Morse function).

[F2]

The gradient satisfies dfx(v)=gx(grad⁡gf(x),v) (The Riemannian gradient is the metric dual of the differential).

[F3]

The differential chain rule applies to the smooth maps γ and f (The chain rule for differentials of smooth maps).

Proof

technique · direct
1.1F3given

By [F3], (f∘γ)′(t)=dfγ(t)(γ˙(t)).

2.1F1F2step 1.1

Substituting [F1] into step 1.1 and applying [F2] gives (f∘γ)′(t)=−gγ(t)(grad⁡gf,grad⁡gf).

3.1step 2.1algebra∎

The right-hand side in step 2.1 is −∥grad⁡gf(γ(t))∥g2, proving the identity on I.

CorollaryStatement: Literature-sourcedProof: Literature-sourcedjudge pass (gpt-5.6-terra)audited 2026-09-06Open item page →

Nonconstant negative-gradient trajectories strictly decrease the function

Statement

If γ:I→M is a nonconstant negative-gradient trajectory, then (f∘γ)′(t)<0 for every t∈I.

Facts & Assumptions

Given: A nonconstant negative-gradient trajectory γ:I→M.

[F1]

(f∘γ)′=−∥grad⁡gf∥g2 along γ (A negative-gradient trajectory satisfies the energy identity).

[F2]

The gradient vanishes exactly at a critical point (The Riemannian gradient vanishes exactly at the critical points).

[F3]

An integral curve through a prescribed point is unique on its maximal interval (Through each point there is a unique maximal integral curve).

Proof

technique · direct
1.1F2given

If γ(t0) were critical, [F2] would make the vector field −grad⁡gf vanish there, so the constant curve at γ(t0) is an integral curve through that point.

2.1F3step 1.1

By [F3], that constant integral curve and γ agree on I, contradicting the hypothesis that γ is nonconstant. Hence γ(t) is never critical.

3.1F1F2step 2.1∎

By [F2] the gradient is nonzero at every γ(t), and [F1] now gives (f∘γ)′(t)<0 for every t∈I.

DefinitionDefinition: Literature-sourcedProof: Not applicablejudge pass (gpt-5.6-terra)audited 2026-09-06Open item page →

Downward gradient-like vector fields for a Morse function

Definition

Let f:M→R be Morse. A smooth vector field X is downward gradient-like for f if both conditions hold:

  1. dfx(Xx)<0 at every x∉Crit⁡(f); and
  2. for every p∈Crit⁡(f) there are Morse coordinates (u,v) centred at p, with f=f(p)−∣u∣2+∣v∣2, in which X=2∑iui∂ui−2∑jvj∂vj.

Thus the field is the negative Euclidean gradient in the required local Morse model, not merely a strictly descending field off the critical set.

PropositionStatement: Literature-sourcedProof: Literature-sourcedverified 2026-09-23 (gpt-6-sol)Open item page →

Every Morse function admits a complete downward gradient-like field on a closed manifold

Statement

Assume ACω (The Axiom of Countable Choice (ACω)). If M is a closed smooth manifold and f:M→R is Morse, then f admits a complete downward gradient-like vector field.

Facts & Assumptions

Given: ACω, a closed smooth manifold M and a Morse function f:M→R.

[F2]

Under the stated ACω premise, every smooth vector field on a compact manifold is complete (Every smooth vector field on a compact manifold is complete). Step 3.1 is the exact use of this choice assumption.

[F3]

A downward gradient-like field must have strict descent off the critical set and the stated Morse-coordinate model at every critical point (Downward gradient-like vector fields for a Morse function).

Proof

technique · direct
1.1F1F3choose

By [F1], choose pairwise disjoint Morse-coordinate neighbourhoods of the finitely many critical points, and smaller neighbourhoods inside them. On each smaller neighbourhood prescribe the local field in [F3].

2.1F3step 1.1construct

On the complement of the smaller neighbourhoods, df is nowhere zero. In each coordinate patch choose a vector Y with df(Y)<0; a partition of unity and cutoffs that equal one on the smaller neighbourhoods patch these choices with the prescribed local fields to a smooth X satisfying both clauses of [F3].

3.1F2step 2.1∎

The resulting X is smooth on the compact manifold M, so [F2] makes it complete. Therefore it is the required complete downward gradient-like field.

LemmaStatement: Literature-sourcedProof: Literature-sourcedverified 2026-09-26 (gpt-6-sol)Open item page →

Precompact trajectory tails have nonempty compact connected flow-invariant limit sets

Statement

Let γ:R→M be a full negative-gradient trajectory and let Φ be its flow. If γ([0,∞))‾ is compact, then

ω(γ):=⋂T≥0γ([T,∞))‾

is nonempty, compact, connected, and invariant under every Φs. The analogous conclusion holds for α(γ):=⋂T≥0γ((−∞,−T])‾ when its negative tail has compact closure.

Facts & Assumptions

Given: A full trajectory γ and a compact closure K of its positive tail.

[F2]

The maximal flow has open domain in R×M, is continuous, and obeys Φs(γ(t))=γ(t+s) whenever defined (The fundamental theorem on flows).

Proof

technique · direct
1.1given

Each KT:=γ([T,∞))‾ is a nonempty closed subset of K, the family is decreasing, and each KT is connected because it is the closure of the connected image of [T,∞).

1.2F1F2given

The flow domain is open and contains {0}×K by [F2]. For each q∈K there are δq>0 and a neighbourhood Vq with (−δq,δq)×Vq in that domain. A finite subcover of K gives one δ>0 such that Φs(p) is defined for every p∈K and ∣s∣<δ.

2.1F1step 1.1

If ⋂T≥0KT were empty, the open sets K∖KT would cover K; [F1] would give finitely many of them that cover. Since the KT decrease, one already covers, contradicting KT≠∅. Thus ω(γ) is nonempty; it is closed in K, hence compact, and the nested connected-set argument makes it connected.

3.1F2step 2.1step 1.2

Let p∈ω(γ) and ∣s∣<δ. Fix T≥0 and a neighbourhood W of Φs(p). Continuity gives a neighbourhood V of p with Φs(V)⊆W. Since p∈KT+∣s∣, some t≥T+∣s∣ has γ(t)∈V; then γ(t+s)=Φs(γ(t))∈W and t+s≥T. Thus Φs(p)∈KT for every T, so Φs(ω(γ))⊆ω(γ). Divide any real s into finitely many increments of size less than δ and apply this inclusion repeatedly; all intermediate points remain in ω(γ)⊆K, where the next increment is defined. The flow law then defines Φs on all of ω(γ) and maps it into itself. Applying the argument to −s gives equality.

4.1step 1.1step 2.1step 1.2step 3.1∎

Replacing t by −t and using the reverse-time flow gives the asserted nonempty compact connected invariant set α(γ) for a precompact negative tail.

LemmaStatement: Literature-sourcedProof: Literature-sourcedjudge pass (gpt-5.6-terra)audited 2026-09-06Open item page →

Every precompact end-limit point of a negative-gradient trajectory is critical

Statement

Every point of a nonempty precompact α- or ω-limit set of a full negative-gradient trajectory is a critical point of f.

Facts & Assumptions

Given: A full negative-gradient trajectory γ with a precompact positive or negative tail.

[F1]
[F2]

Along γ, (f∘γ)′=−∥grad⁡gf∥g2 (A negative-gradient trajectory satisfies the energy identity).

[F3]

A noncritical point has nonzero gradient (The Riemannian gradient vanishes exactly at the critical points).

Proof

technique · direct
1.1F2F1given

On a precompact positive tail, f∘γ is decreasing by [F2] and bounded below because f is continuous on its compact closure. It therefore has a finite limit ℓ; every point of ω(γ) is a limit of tail values and has f=ℓ. The same argument, with increasing time reversed, applies to α(γ).

1.2F2F3assume-contra

Let z lie in either limit set. If z were noncritical, [F3] and [F2] would give a sufficiently short positive orbit segment from z on which f strictly decreases.

2.1F1step 1.1step 1.2discharge-contradiction∎

By [F1] the entire short segment in step 1.2 remains in the same limit set, whereas step 1.1 makes f constant there. This contradiction proves that z is critical.

LemmaStatement: Literature-sourcedProof: Literature-sourcedverified 2026-09-23 (gpt-6-sol)Open item page →

A negative-gradient trajectory on a compact Morse manifold has single critical alpha and omega limits

Statement

Assume ACω (The Axiom of Countable Choice (ACω)). Let M be compact, let f:M→R be Morse, and let γ be a negative-gradient trajectory. Then γ is full and there are critical points α(γ) and ω(γ) such that

lim⁡t→−∞γ(t)=α(γ),lim⁡t→∞γ(t)=ω(γ).

Facts & Assumptions

Given: ACω, a compact smooth manifold M, a Morse function f, and a negative-gradient trajectory γ.

[F1]

Under the stated ACω premise, a smooth vector field on a compact manifold is complete (Every smooth vector field on a compact manifold is complete). Proof 1.1 is the exact use of this choice assumption.

[F2]

Precompact full tails have nonempty compact connected invariant limit sets (Precompact trajectory tails have nonempty compact connected flow-invariant limit sets).

[F3]

Such limit sets for a negative-gradient trajectory consist of critical points (Every precompact end-limit point of a negative-gradient trajectory is critical).

[F4]

A Morse function on a compact manifold has finitely many critical points (A Morse function on a compact manifold has finitely many critical points).

Proof

technique · direct
1.1F1given

By [F1], the negative-gradient field is complete, so γ has domain R. Both tails have compact closure because they lie in M.

2.1F2F3step 1.1

By [F2] each of α(γ) and ω(γ) is nonempty and connected, and [F3] places it in Crit⁡(f).

3.1F4step 2.1

By [F4], Crit⁡(f) is finite and hence discrete. A connected subset of a discrete finite set is one point, so both limit sets are single critical points.

4.1F2step 1.1step 3.1∎

Let p be the single point of ω(γ) and let U be any open neighbourhood of p. If no positive tail lies in U, then every compact set KT=γ([T,∞))‾ meets the closed set M∖U. The nested nonempty compact sets KT∩(M∖U) have nonempty intersection by compactness, giving a point of ω(γ)∖U, a contradiction. Thus γ(t)→p as t→∞; the same argument on negative tails proves convergence to the single point of α(γ).

DefinitionDefinition: Literature-sourcedProof: Not applicableverified 2026-09-23 (gpt-6-sol)Open item page →

A Morse trajectory from one critical point to another

Definition

Fix a Riemannian metric g on M. For critical points p,q of a Morse function f:M→R, a Morse trajectory from p to q is a nonconstant full trajectory of −grad⁡gf with

lim⁡t→−∞γ(t)=pandlim⁡t→∞γ(t)=q.

On a compact manifold, under ACω (The Axiom of Countable Choice (ACω)) as assumed in the preceding endpoint lemma, that lemma supplies these limits. On a noncompact manifold, their existence is part of this definition's hypothesis.

LemmaStatement: Literature-sourcedProof: Literature-sourcedjudge pass (gpt-5.6-terra)audited 2026-09-06Open item page →

Morse trajectories have a positive energy drop

Statement

If γ is a Morse trajectory from p to q, then

f(p)−f(q)=∫−∞∞∥grad⁡gf(γ(t))∥g2 dt>0.

Facts & Assumptions

Given: A Morse trajectory γ:R→M from p to q.

[F1]

Its endpoint limits are p and q and it is nonconstant (A Morse trajectory from one critical point to another).

[F2]

Its energy identity is (f∘γ)′=−∥grad⁡gf∥g2 (A negative-gradient trajectory satisfies the energy identity).

[F3]

A nonconstant negative-gradient trajectory strictly decreases f (Nonconstant negative-gradient trajectories strictly decrease the function).

Proof

technique · direct
1.1F2given

Integrating [F2] on [−T,T] gives f(γ(−T))−f(γ(T))=∫−TT∥grad⁡gf(γ(t))∥g2 dt.

2.1F1step 1.1

Letting T→∞ and using [F1] and continuity of f yields the stated improper-integral equality.

3.1F3step 2.1∎

By [F3], f∘γ is strictly decreasing, so f(p)>f(q). The equality in step 2.1 therefore has strictly positive value.

DefinitionDefinition: Literature-sourcedProof: Not applicablejudge pass (gpt-5.6-terra)audited 2026-09-06Open item page →

Stable and unstable sets of a critical point

Definition

Let X be a complete downward gradient-like field for f, let Φ be its global descending flow, and let p∈Crit⁡(f). Define

Ws(p):={x∈M:Φt(x)→p as t→∞},Wu(p):={x∈M:Φt(x)→p as t→−∞}.

These definitions use the descending flow of X. Thus “unstable” means the backward-limit set, as required by the Morse-index convention.

TheoremStatement: Literature-sourcedProof: Literature-sourcedjudge pass (gpt-5.6-terra)audited 2026-09-06Open item page →

Local stable and unstable manifolds at a Morse critical point

Statement

Let p be a critical point of index λ of a Morse function on an n-manifold, and let X be downward gradient-like. In the Morse coordinates of its definition, the local unstable and stable manifolds are respectively

{v=0}≅Rλ,{u=0}≅Rn−λ.

After restricting to sufficiently small balls, they are embedded disks tangent at p to the negative and positive Hessian eigenspaces, respectively.

Facts & Assumptions

Given: A Morse critical point p of index λ and a downward gradient-like field X.

[F1]

In Morse coordinates f=f(p)−∣u∣2+∣v∣2 and X=2u∂u−2v∂v (Downward gradient-like vector fields for a Morse function).

[F2]

The index and coindex are the dimensions of the negative and positive Hessian directions (Nondegenerate critical points, nullity, index, and coindex).

Proof

technique · direct
1.1F1givenalgebra

By [F1], the coordinate flow solves u˙=2u and v˙=−2v, hence u(t)=e2tu(0) and v(t)=e−2tv(0).

2.1step 1.1

A point remains near p and converges to it in forward time exactly when u(0)=0; in backward time exactly when v(0)=0. Thus the local stable disk is {u=0} and the local unstable disk is {v=0}.

3.1F2step 2.1∎

By [F2], the u-space has dimension λ and is the negative Hessian space, while the v-space has dimension n−λ and is the positive one. This gives the claimed disk dimensions and tangent spaces.

TheoremStatement: Literature-sourcedProof: Literature-sourcedjudge pass (gpt-5.6-terra)audited 2026-09-06Open item page →

Global stable and unstable manifolds are immersed Euclidean spaces

Statement

For a complete downward gradient-like flow on an n-manifold and a critical point p of index λ, Wu(p) and Ws(p) are immersed submanifolds diffeomorphic to Rλ and Rn−λ, respectively. This does not assert that either global submanifold is embedded.

Facts & Assumptions

Given: A complete downward gradient-like flow Φ and a critical point p of index λ.

[F1]

The local unstable and stable sets are embedded disks of dimensions λ and n−λ (Local stable and unstable manifolds at a Morse critical point).

[F2]

Ws(p) and Wu(p) are defined by forward and backward convergence under the global flow (Stable and unstable sets of a critical point).

[F3]

Every global flow map Φt is a diffeomorphism with inverse Φ−t (The fundamental theorem on flows).

Proof

technique · direct
1.1F1F2given

Let Du and Ds be the local disks from [F1]. From the defining limits in [F2], every x∈Wu(p) has Φ−T(x)∈Du for some T≥0, and every x∈Ws(p) has ΦT(x)∈Ds for some T≥0.

2.1F3step 1.1

Hence Wu(p)=⋃T≥0ΦT(Du) and Ws(p)=⋃T≥0Φ−T(Ds). By [F3], these are increasing compatible immersed-manifold charts transported from the disks.

3.1F1step 2.1∎

The standard flow-exhaustion parametrization of these compatible disks identifies the unions with the corresponding Euclidean spaces; their dimensions are those in [F1]. Thus they are immersed submanifolds diffeomorphic to Rλ and Rn−λ, with no embeddedness conclusion.

LemmaStatement: Literature-sourcedProof: Literature-sourcedaudited 2026-09-06Open item page →

Stable and unstable manifolds are flow invariant

Statement

For every s∈R and critical point p of a complete descending flow Φ,

Φs(Ws(p))=Ws(p),Φs(Wu(p))=Wu(p).

Facts & Assumptions

Given: A complete descending flow Φ, a critical point p, and s∈R.

[F1]

Stable and unstable sets are the forward and backward convergence sets (Stable and unstable sets of a critical point).

[F2]

The flow satisfies Φt(Φs(x))=Φt+s(x) and has inverse Φ−s (The fundamental theorem on flows).

Proof

technique · direct
1.1F1F2given

If x∈Ws(p), then [F2] gives Φt(Φs(x))=Φt+s(x)→p as t→∞, so Φs(x)∈Ws(p) by [F1]. The same calculation with t→−∞ proves inclusion for Wu(p).

2.1F2step 1.1

Applying step 1.1 with −s and using the inverse in [F2] proves the reverse inclusions.

3.1step 1.1step 2.1∎

Therefore both stable and unstable sets are invariant under every fixed flow time.

CorollaryStatement: Literature-sourcedProof: Literature-sourcedjudge pass (gpt-5.6-terra)audited 2026-09-06Open item page →

A downward gradient flow has no nonconstant periodic or recurrent orbit

Statement

A nonconstant orbit of a negative-gradient flow is neither periodic nor recurrent. Here recurrent means that for some point x on the orbit there are tk→∞ with Φtk(x)→x.

Facts & Assumptions

Given: A nonconstant negative-gradient orbit γ(t)=Φt(x).

[F1]

The function f∘γ is strictly decreasing (Nonconstant negative-gradient trajectories strictly decrease the function).

Proof

technique · direct
1.1F1given

If the orbit had period T>0, then f(γ(T))=f(γ(0)), contradicting [F1].

1.2F1given

If Φtk(x)→x with tk→∞, fix s>0. For all sufficiently large k, tk≥s, so [F1] gives f(Φtk(x))≤f(Φs(x))<f(x).

2.1step 1.2∎

Continuity of f makes the left side of step 1.2 tend to f(x), a contradiction. Thus the orbit is not recurrent either.

DefinitionDefinition: Literature-sourcedProof: Not applicablejudge pass (gpt-5.6-terra)audited 2026-09-06Open item page →

Proper smooth functions and compact Morse slabs

Definition

A continuous map f:M→R is proper when f−1(C) is compact for every compact C⊆R. For a≤b, call

f−1([a,b])

a compact Morse slab when it is compact. In particular, a proper f has a compact Morse slab for every compact interval [a,b].

PropositionStatement: Literature-sourcedProof: Literature-sourcedjudge pass (gpt-5.6-terra)audited 2026-09-06Open item page →

Proper Morse slabs prevent finite-time escape of connecting trajectories

Statement

Let γ:I→M be a maximal negative-gradient trajectory. If its image is contained in a compact Morse slab f−1([a,b]), then I=R. Consequently, this applies to any trajectory already known to have endpoint levels in [a,b] and to remain in that slab; it is not a blanket noncompact-completeness assertion.

Facts & Assumptions

Given: A maximal negative-gradient trajectory γ:I→M with image in the compact slab K=f−1([a,b]).

[F1]

A compact Morse slab is a compact inverse image f−1([a,b]) (Proper smooth functions and compact Morse slabs).

[F2]

The energy identity makes f∘γ nonincreasing (A negative-gradient trajectory satisfies the energy identity).

[F3]

Near every point of M, the vector field has unique integral curves on a uniform local time interval (Local existence, uniqueness, and smooth dependence for manifold integral curves).

[F4]

A maximal integral curve cannot have a genuine extension (Through each point there is a unique maximal integral curve).

Proof

technique · direct
1.1F1F3assume-contra

Suppose the right endpoint T of I were finite. The local flow neighbourhoods supplied by [F3] cover the compact set K in [F1], so finitely many suffice; their time radii have a positive minimum ε.

2.1F3F4step 1.1choosedischarge-contradiction

Choose t∈I with T−t<ε. Since γ(t)∈K, the corresponding local solution from [F3] extends γ beyond T; uniqueness identifies it with γ on the overlap, contradicting [F4].

3.1F2step 2.1∎

The same argument at the left endpoint proves I=R. If endpoint levels lie in [a,b], [F2] verifies the usual monotone trapping in that slab once the trajectory is known to remain between those levels.

RemarkRemark: Literature-sourcedProof: Not applicablejudge pass (gpt-5.6-terra)audited 2026-09-06Open item page →

Completeness of a gradient flow is an extra hypothesis on a noncompact manifold

On a noncompact manifold, a gradient or gradient-like field need not be complete. A compact slab gives only the conditional nonescape conclusion of Proper Morse slabs prevent finite-time escape of connecting trajectories; it does not make all trajectories global. The explicit escape calculation is already visible on R: for f(x)=−x3/3, the negative-gradient equation is x˙=x2, and the solution from x0>0 is x(t)=x0/(1−x0t), which escapes to +∞ as t↑1/x0.

5 · Examples, counterexamples and false statements

None yet.

Sources