Read Perelman I, §6 and §7, then the detailed treatment of L-geodesics and the reduced volume in Kleiner and Lott's notes or in Morgan and Tian's book. Huisken's monotonicity formula (6A.8 Curve Shortening and the First Geometric Flows) and Bishop–Gromov (9B.2 Volume Comparison) are the two models to have in mind.
The W-entropy of 12A.3 The 𝓦-Entropy is an integral over a whole manifold, so it controls global things. For the flow with surgery, Perelman needed a monotone quantity attached to a single point of space-time, which sees only the part of the flow that can influence that point. He built it from a new notion of length for curves in space-time, the L-length. Its minimisers give a reduced distanceℓ, and the Gaussian built from ℓ integrates to the reduced volumeV~(τ). The reduced volume is monotone along every Ricci flow, with no curvature assumption, and equals 1 on flat space. It is the Ricci flow's version of the Bishop–Gromov volume ratio, and Perelman found it by applying Bishop–Gromov to a Ricci-flat manifold of very high dimension.
By the end of this chapter you will be able to:
define the L-length, L-geodesics, the reduced distance and the reduced volume, and compute them on flat space;
state the differential inequalities for ℓ and use them to prove that V~ is nonincreasing in τ;
show that ℓ≤2n somewhere at every τ;
read the reduced volume against Bishop–Gromov, row by row, and against Huisken's monotonicity formula;
describe Perelman's heuristic derivation in N→∞ dimensions, and the uses of V~.
A particle diffusing in Rn from 0 is found near x after time τ with density (4πτ)−n/2e−∣x∣2/4τ, the heat kernel. The exponent 4τ∣x∣2 is the least value of the action 41∫0τ∣γ˙∣2ds over paths from 0 to x in time τ: diffusion is governed, to leading order, by its cheapest paths. Varadhan proved in 1967 that this persists on curved spaces for small times, with −4τlogp(τ,x,y)→d(x,y)2. Peter Li and Shing-Tung Yau used such path lengths, adapted to a linear parabolic equation, to integrate their Harnack inequality in 1986, and Perelman names their paper as the closest precedent for his construction. His reduced distance is the least action for paths in a Ricci flow, with the scalar curvature as a potential, and (4πτ)−n/2e−ℓ plays the part of the heat kernel.
Work in backward time. Fix a Ricci flow and a base time t0, set τ=t0−t, so that ∂τg=2Ric, and assume the manifold is closed, or that each g(τ) is complete with uniformly bounded curvature. Fix a base point p.
Definition 5.1L-length and reduced distance
For a curve γ:[0,τˉ]→M with γ(0)=p, the L-length is
L(γ)=∫0τˉτ(R(γ(τ),τ)+∣γ˙(τ)∣g(τ)2)dτ.
Let L(q,τˉ) be the infimum of L(γ) over curves from p at τ=0 to q at τ=τˉ. The reduced distance is
ℓ(q,τˉ)=2τˉL(q,τˉ).
The weight τ is what makes the theory scale correctly. With s=τ the curve has finite energy near τ=0, and the change of variable turns ∫τ∣γ˙∣2dτ into 21∫∣γ′(s)∣2ds. Perelman's first variation (his (7.1)) gives the L-geodesic equation, with X=γ˙:
∇XX−21∇R+2τ1X+2Ric(X,⋅)=0.
Minimisers exist and are L-geodesics, and τX(τ) has a limit v∈TpM as τ→0. The L-exponential map sends v to γv(τˉ). Where minimisers are not unique, or L is not smooth, the inequalities below hold in the barrier sense, as for the distance function (9B.1 Laplacian Comparison).
Example 5.2Flat space
On Rn with the static flat metric, R=0. In s=τ the length is 21∫0τˉ∣γ′(s)∣2ds, minimised by the straight line at constant speed ∣x∣/τˉ, so L(x,τˉ)=2τˉ∣x∣2 and
Figure 5.1.L-geodesics from p in flat R, with τ increasing downward: γv(τ)=2τv for v=−1,−43,…,1 (computed). They leave p with infinite speed, like Brownian paths at small scales, and the L-exponential map sends v to γv(τˉ). In a curved flow they bend, following the geodesic equation above.
Perelman computes the first and second variations of L exactly as in Riemannian geometry, with one new feature: the time derivative of the metric is 2Ric, so Ricci terms appear, and along the curve they combine into Hamilton's Harnack expressions (11B.2 Ancient Solutions and the Harnack Inequality). He collects them in a quantity K=∫0τˉτ3/2H(X)dτ, where H is Hamilton's trace Harnack expression. Then (his (7.5), (7.6) and (7.10)), in terms of ℓ:
The last is the space-time Laplacian comparison, the analogue of Δr≤rn−1 when Ric≥0 (9B.1 Laplacian Comparison). It is proved with the test fields Y solving ∇XY=−Ric(Y,⋅)+2τ1Y, which play the part of the linear Jacobi fields rsE in Euclidean space. The unknown K cancels from the right combinations, and gives (Perelman's (7.13) and (7.14))
∂τˉℓ−Δℓ+∣∇ℓ∣2−R+2τˉn≥0,2Δℓ−∣∇ℓ∣2+R+τˉℓ−n≤0.
On flat space both are equalities (Exercise 5.8). No curvature hypothesis is needed anywhere: this is the decisive difference from Bishop–Gromov.
Proposition 5.3A point where ℓ≤2n (Perelman I, §7.1)
For every τˉ>0 there is a point q with ℓ(q,τˉ)≤2n.
Proof. Let Lˉ=2τˉL=4τˉℓ. Perelman's (7.5) and (7.10) give ∂τˉLˉ+ΔLˉ≤2n (Exercise 5.9). At a minimum point of Lˉ(⋅,τˉ), ΔLˉ≥0, so the minimum of Lˉ−2nτˉ is nonincreasing (in the barrier sense, on a closed manifold or with the stated bounds). As τˉ→0, Lˉ(p,τˉ)→0. So minLˉ(⋅,τˉ)≤2nτˉ, which is minℓ≤2n.
Perelman's own definition omits the factor (4π)−n/2; with it, V~≡1 on flat Rn, since the integrand is the heat kernel. This normalisation is common in the expositions.
Theorem 5.5Monotonicity of the reduced volume (Perelman I, §7.1)
Along any Ricci flow as above, V~(τˉ) is nonincreasing in τˉ. The monotonicity is strict unless the flow is a shrinking gradient soliton.
Proof. Set u=(4πτˉ)−n/2e−ℓ. Since ∂τˉu=u(−2τˉn−∂τˉℓ) and Δu=u(∣∇ℓ∣2−Δℓ),
∂τˉu−Δu+Ru=−u(∂τˉℓ−Δℓ+∣∇ℓ∣2−R+2τˉn)≤0
by the first inequality above. In backward time the conjugate heat operator is ∂τˉ−Δ+R, so u is a subsolution of the conjugate heat equation. Since ∂τˉdV=RdV,
dτˉd∫MudV=∫M(∂τˉu+Ru)dV=∫M(∂τˉu−Δu+Ru)dV≤0.
Making this rigorous where ℓ is not smooth needs the barrier sense and care at the cut locus. Perelman's main argument avoids it by working along each L-geodesic: the Jacobian J of the L-exponential map satisfies dτdlogJ≤2τn−21τ−3/2K, so τ−n/2e−ℓ(γ(τ),τ)J(τ) is nonincreasing along each geodesic, and integrating over TpM gives the theorem. Equality along all geodesics forces Ric+∇2ℓ=2τ1g, a shrinking gradient soliton.
As τˉ→0, the flow near (p,t0) looks Euclidean at the relevant scale τˉ, and V~(τˉ)→1; the expositions prove this limit carefully. So V~≤1, with 1 the value of flat space. Figure 5.2 computes it for the round shrinking 3-sphere.
Figure 5.2.V~(τˉ) for the round shrinking S3 of radius 1 at the base time, so that r(τ)2=1+4τ (computed). By symmetry the L-shortest curves run along great circles, which gives ℓ in closed form (Exercise 5.10). V~ decreases from 1 towards 2πe−3/2≈0.79 as τˉ→∞: looking further into the past, the flow is seen as the shrinking soliton it is.
5.6Perelman's heuristic: Bishop–Gromov in N dimensions
Perelman explains in §6 where the reduced volume comes from. Take a large integer N and the manifold M~=M×SN×R+ with metric
g~=g(τ)+τgSN+(2τN+R)dτ2,
where g(τ) is the backward Ricci flow and gSN is the round metric of constant curvature 2N1. He reports that g~ is Ricci-flat up to errors of order N−1, and that its curvature components reproduce Hamilton's Harnack expressions. For a curve from a point p at τ=0, orthogonal to the sphere factor, the g~-length is
2Nτ(q)+2N1L(γ)+O(N−3/2),
so shortest geodesics in M~ minimise L. The volume of the geodesic sphere of radius 2Nτ about p, divided by the Euclidean value, is a constant times N−n/2 times ∫τ−n/2e−ℓ, up to O(N−1). Bishop–Gromov for the nearly Ricci-flat M~ then suggests that this quantity increases as τ decreases. Perelman presents this as a heuristic, and gives the rigorous proof separately in §7. The heuristic explains why no curvature hypothesis is needed: the extra dimensions make the space-time Ricci-flat.
5.7Huisken's formula and the direction of monotonicity
nonincreasing in t, and constant exactly on self-shrinkers. The reduced volume has the same shape, with the Euclidean distance replaced by ℓ. Perelman points out that the monotonicity runs the other way. In τ=t0−t, Huisken's Θ is nondecreasing, while V~ is nonincreasing. Both are nevertheless constant exactly on the self-similar shrinking solutions, and both are used in the same way: they are evaluated at very small and very large scales and compared, to show that a blow-up looks like a soliton.
Where this goesUses of the reduced volume
Perelman's §7.3 reproves noncollapsing with V~: if a ball is collapsed, V~ based near it is small at small τ, while at τ comparable to the whole time interval it is bounded below, by using the point where ℓ≤2n; monotonicity forbids this. Because the argument needs only local control, it survives surgery (No local collapsing theorem II, §8; 12B.5 Ricci Flow with Surgery for All Time). On κ-solutions, letting τ→∞ and rescaling by τ produces the asymptotic soliton (12B.1 κ-Solutions). 12A.6 Pseudolocality turns to the other side of §§8–10: the Harnack inequality for the conjugate heat kernel and pseudolocality.
Perelman introduced L-length, reduced distance and reduced volume in §§6–7 of his first preprint (2002). He described the computations as natural modifications of the classical variational theory of geodesics, with Li and Yau's 1986 paper as the closest reference, and noted that Chow and Chu had found the first geometric interpretation of Hamilton's Harnack expressions, using a degenerate metric on M×R, to which his construction is in a sense dual. Huisken's formula dates from 1990.
RecallWhere we stand
In backward time τ, the L-length ∫τ(R+∣γ˙∣2)dτ defines a reduced distance ℓ=L/(2τ) from a base point; on flat space ℓ=4τ∣x∣2 and (4πτ)−n/2e−ℓ is the heat kernel. Perelman's variational formulas give ∂τℓ−Δℓ+∣∇ℓ∣2−R+2τn≥0, so (4πτ)−n/2e−ℓ is a subsolution of the conjugate heat equation and the reduced volume V~(τ) is nonincreasing, for every Ricci flow, strictly unless on a shrinking soliton. Also minℓ≤2n, and V~→1 as τ→0. It is Bishop–Gromov in space-time, found by applying Bishop–Gromov to a nearly Ricci-flat manifold in N→∞ dimensions. 12A.6 Pseudolocality completes Book 12A with Perelman's Harnack inequality and pseudolocality.
On static flat Rn with p=0: (a) show that the substitution s=τ turns ∫0τˉτ∣γ˙∣2dτ into 21∫0τˉ∣γ′(s)∣2ds; (b) deduce L(x,τˉ)=2τˉ∣x∣2 and ℓ=4τˉ∣x∣2; (c) show V~≡1.
Solution
(a) dτ=2sds and γ˙=2sγ′(s), so τ∣γ˙∣2dτ=s4s2∣γ′∣22sds=21∣γ′∣2ds. (b) Energy is minimised by the constant-speed line, γ(s)=τˉsx, giving 21τˉ∣x∣2τˉ. Then ℓ=2τˉL. (c) ∫(4πτˉ)−n/2e−∣x∣2/4τˉdx=1.
Exercise 5.7The geodesic equation on flat space
On static flat space the L-geodesic equation reads γ¨+2τ1γ˙=0. Solve it with γ(0)=0, and show that the solutions are γ(τ)=2τv with v=limτ→0τγ˙(τ).
Solution
dτd(τγ˙)=τ(γ¨+2τ1γ˙)=0, so τγ˙=v is constant, γ˙=vτ−1/2, and γ=2τv.
Exercise 5.8The inequalities on flat space
With ℓ=4τ∣x∣2 on flat Rn (so R=0, K=0), check that ∂τℓ−Δℓ+∣∇ℓ∣2+2τn=0 and 2Δℓ−∣∇ℓ∣2+τℓ−n=0.
Using ∂τˉL=2τˉR−2τˉ1L+τˉ1K and ΔL≤−2τˉR+τˉn−τˉ1K (Perelman's (7.5) and (7.10)), show that Lˉ=2τˉL satisfies ∂τˉLˉ+ΔLˉ≤2n.
Solution
∂τˉLˉ=τˉL+2τˉ∂τˉL=τˉL+4τˉR−τˉL+τˉ2K=4τˉR+τˉ2K. And ΔLˉ=2τˉΔL≤−4τˉR+2n−τˉ2K. Adding gives 2n.
Exercise 5.10Rehearsal: the shrinking sphere
On the round shrinking S3 with g(τ)=(1+4τ)gS3 and R=1+4τ6, let θ be the angle from p. (a) Explain why L(q,τˉ)=∫0τˉτRdτ+min∫0τˉτ(1+4τ)θ˙2dτ over θ(0)=0, θ(τˉ)=θ(q). (b) Show that the minimum is θ(q)2/I(τˉ) with I(τˉ)=∫0τˉτ(1+4τ)dτ=arctan(2τˉ), and that ∫0τˉτRdτ=3τˉ−23arctan(2τˉ). (c) Show that as τˉ→∞, ℓ→23 uniformly, and deduce V~→(4π)−3/2⋅2π2⋅43/2e−3/2=2πe−3/2.
Solution
(a) R depends only on τ, so its integral is the same for every curve; and ∣γ˙∣2≥(1+4τ)θ˙2, with equality along great circles. (b) By Cauchy–Schwarz, θ(q)2=(∫θ˙)2≤∫aθ˙2∫a1 with a=τ(1+4τ), with equality when θ˙∝a1. With s=τ, I=∫0τˉ1+4s22ds=arctan(2τˉ) and ∫τR=12∫0τˉ1+4s2s2ds=3s−23arctan2s. (c) ℓ=2τˉ1(arctan2τˉθ2+3τˉ−23arctan2τˉ)→23, since θ≤π. Then V~≈(4πτˉ)−3/2(4τˉ)3/2∣S3∣e−3/2, and ∣S3∣=2π2.