Book 9A

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Course 9Book 9A: Metrics, Connections and CurvatureChapter 4

Curvature and What It Means

Riemann, sectional, Ricci and scalar curvature, and why tides are curvature.

31 min read · Updated Oct 3, 2026

Read with Lee, Introduction to Riemannian Manifolds (2nd edition), chapter 7 (curvature: the curvature tensor, flat manifolds, symmetries and the Bianchi identities, Ricci and scalar curvature) and the parts of chapter 8 on sectional curvature. Petersen's Riemannian Geometry, chapter 3, is the second voice.

In this chapter · 8 sections
  1. 4.1The tides
  2. 4.2The curvature tensor
  3. 4.3Sectional curvature
  4. 4.4Ricci and scalar curvature
  5. 4.5Three meanings of curvature
  6. 4.6Conventions
  7. 4.7History
  8. 4.8Exercises

The Ricci flow equation ∂tg=−2Ric⁡\partial_tg = -2\operatorname{Ric} says that a metric moves in the direction of minus its Ricci curvature. To understand the equation you need to know what the Ricci tensor is: how it is built from the full curvature tensor, and what it measures. This chapter defines the Riemann curvature tensor, the failure of covariant derivatives to commute, and the quantities built from it: sectional curvature, which generalises the Gauss curvature of 8A.9 The Curvature of Surfaces to each 2-plane; Ricci curvature, an average of sectional curvatures; and scalar curvature, the average of those.

Each has a concrete meaning. Sectional curvature measures how much shorter (or longer) small geodesic circles are than Euclidean ones. Ricci curvature measures how much smaller (or larger) the volume of a thin cone of geodesics is. In general relativity, Ricci curvature measures how quickly a ball of freely falling particles starts to shrink, which is where matter enters. The tides show the curvature that is left in empty space. That leftover curvature changes the shape of a ball but not, to first order, its volume.

By the end of this chapter you will be able to:

  • define the curvature tensor, compute it from Christoffel symbols, and use its symmetries and the Bianchi identities;
  • define sectional, Ricci and scalar curvature and relate them as averages;
  • derive the contracted Bianchi identity div⁡Ric⁡=12dR\operatorname{div}\operatorname{Ric} = \frac12dR;
  • state and check the three meanings of curvature: circumferences, volumes and gravity;
  • convert a curvature formula from another book to this guide's conventions by testing it on the sphere.

The tides

In the world Model Tides are curvature

The Moon pulls on the whole Earth, but it pulls harder on the near side and more weakly on the far side. Relative to the Earth's centre, which falls freely towards the Moon, the oceans on both sides are pulled away: a stretch along the Earth–Moon line, and a squeeze in the two directions across it. This relative acceleration of nearby freely falling bodies is the tidal acceleration. For a point mass MM at distance dd, it is 2GMd3\frac{2GM}{d^3} per unit separation along the line, and −GMd3-\frac{GM}{d^3} in each perpendicular direction (Exercise 4.7). At the Earth's surface the Moon's tidal acceleration is about 1.1×10−61.1\times10^{-6} m/s², roughly a ten-millionth of the Earth's gravity, and it raises the two daily ocean bulges.

In general relativity, freely falling bodies follow geodesics (9A.3 Geodesics and the Exponential Map), and the relative acceleration of nearby geodesics is the Riemann curvature of spacetime: the tidal acceleration is the Newtonian limit of R(⋅,u)uR(\cdot, u)u. Notice that the three numbers 22, −1-1, −1-1 (in units of GMd3\frac{GM}{d^3}) add to zero. A small ball of freely falling particles in empty space is stretched into an ellipsoid of the same volume, to first order. That trace is the Ricci curvature, and in empty space Einstein's equations make it vanish. Where there is matter, the trace is not zero, and the ball begins to shrink.

The curvature tensor

The curvature endomorphism of (M,g)(M, g) is

R(X,Y)Z=∇X∇YZ−∇Y∇XZ−∇[X,Y]Z,R(X, Y)Z = \nabla_X\nabla_YZ - \nabla_Y\nabla_XZ - \nabla_{[X, Y]}Z,

and the Riemann curvature tensor is Rm⁡(X,Y,Z,W)=⟨R(X,Y)Z,W⟩\operatorname{Rm}(X, Y, Z, W) = \langle R(X, Y)Z, W\rangle, with components Rijkl=Rm⁡(∂i,∂j,∂k,∂l)R_{ijkl} = \operatorname{Rm}(\partial_i, \partial_j, \partial_k, \partial_l). Although it is built from derivatives, R(X,Y)ZR(X, Y)Z at pp depends only on XpX_p, YpY_p and ZpZ_p: it is linear over functions in each slot (Exercise 4.2), so it is a tensor. In coordinates, R(∂i,∂j)∂k=Rijkl∂lR(\partial_i, \partial_j)\partial_k = R_{ijk}{}^l\partial_l with

Rijkl=∂iΓjkl−∂jΓikl+ΓjkmΓiml−ΓikmΓjml,Rijkl=glmRijkm.R_{ijk}{}^l = \partial_i\Gamma_{jk}^l - \partial_j\Gamma_{ik}^l + \Gamma_{jk}^m\Gamma_{im}^l - \Gamma_{ik}^m\Gamma_{jm}^l, \qquad R_{ijkl} = g_{lm}R_{ijk}{}^m.

What it measures. For coordinate fields, [∂i,∂j]=0[\partial_i, \partial_j] = 0 and R(∂i,∂j)=∇i∇j−∇j∇iR(\partial_i, \partial_j) = \nabla_i\nabla_j - \nabla_j\nabla_i: curvature is the failure of covariant derivatives to commute. Geometrically, parallel transport around the small coordinate parallelogram with sides ε∂i\varepsilon\partial_i and ε∂j\varepsilon\partial_j changes a vector vv by ±ε2R(∂i,∂j)v+O(ε3)\pm\varepsilon^2R(\partial_i, \partial_j)v + O(\varepsilon^3), the sign depending on the direction of travel: curvature is infinitesimal holonomy (9A.2 Connections). And Rm⁡≡0\operatorname{Rm} \equiv 0 exactly when (M,g)(M, g) is locally flat, locally isometric to Rn\mathbb{R}^n (Lee, chapter 7).

Symmetries. For all X,Y,Z,WX, Y, Z, W:

  1. Rm⁡(X,Y,Z,W)=−Rm⁡(Y,X,Z,W)\operatorname{Rm}(X, Y, Z, W) = -\operatorname{Rm}(Y, X, Z, W);
  2. Rm⁡(X,Y,Z,W)=−Rm⁡(X,Y,W,Z)\operatorname{Rm}(X, Y, Z, W) = -\operatorname{Rm}(X, Y, W, Z) (from metric compatibility);
  3. R(X,Y)Z+R(Y,Z)X+R(Z,X)Y=0R(X, Y)Z + R(Y, Z)X + R(Z, X)Y = 0, the first Bianchi identity (from torsion-freeness);
  4. Rm⁡(X,Y,Z,W)=Rm⁡(Z,W,X,Y)\operatorname{Rm}(X, Y, Z, W) = \operatorname{Rm}(Z, W, X, Y) (a consequence of 1–3).

In components: Rijkl=−Rjikl=−Rijlk=RklijR_{ijkl} = -R_{jikl} = -R_{ijlk} = R_{klij} and Rijkl+Rjkil+Rkijl=0R_{ijkl} + R_{jkil} + R_{kijl} = 0. These cut the n4n^4 components down to n2(n2−1)12\frac{n^2(n^2 - 1)}{12} independent ones: 11 in dimension 22, 66 in dimension 33, 2020 in dimension 44. The derivatives satisfy the second Bianchi identity

∇mRijkl+∇kRijlm+∇lRijmk=0,\nabla_mR_{ijkl} + \nabla_kR_{ijlm} + \nabla_lR_{ijmk} = 0,

cyclic in the last three indices k,l,mk, l, m (Lee, chapter 7). It is the identity behind the contracted Bianchi identity below, and behind the evolution equations of 11A.2 How Curvature Evolves.

Sectional curvature

For linearly independent X,Y∈TpMX, Y \in T_pM, the sectional curvature of the plane Π=span⁡(X,Y)\Pi = \operatorname{span}(X, Y) is

K(X,Y)=Rm⁡(X,Y,Y,X)∣X∣2∣Y∣2−⟨X,Y⟩2,K(X, Y) = \frac{\operatorname{Rm}(X, Y, Y, X)}{|X|^2|Y|^2 - \langle X, Y\rangle^2},

which depends only on the plane. It is the Gauss curvature at pp of the surface swept out by the geodesics from pp tangent to Π\Pi (Lee, chapter 8). The sectional curvatures determine Rm⁡\operatorname{Rm} completely, by a polarisation argument that uses the symmetries above.

A manifold has constant curvature κ\kappa if K≡κK \equiv \kappa for all planes at all points. Then

Rijkl=κ (gilgjk−gikgjl).R_{ijkl} = \kappa\,(g_{il}g_{jk} - g_{ik}g_{jl}).

The model spaces have constant curvature 00, 11 and −1-1 (9A.5 Computing Curvature computes this), and the sphere of radius rr has κ=1r2\kappa = \frac{1}{r^2}. In dimension 22 there is only one plane at each point, so Rm⁡\operatorname{Rm} is determined by one function, the Gauss curvature KK of 8A.9 The Curvature of Surfaces (Exercise 4.3).

Ricci and scalar curvature

The Ricci tensor is the trace Rij=gklRkijlR_{ij} = g^{kl}R_{kijl}, Ric⁡(Y,Z)=tr⁡(X↦R(X,Y)Z)\operatorname{Ric}(Y, Z) = \operatorname{tr}\big(X \mapsto R(X, Y)Z\big), a symmetric 2-tensor. The scalar curvature is R=gijRijR = g^{ij}R_{ij}. In an orthonormal basis e1,…,ene_1, \dots, e_n with e1=ve_1 = v a unit vector,

Ric⁡(v,v)=∑i=2nK(v,ei),R=∑i≠jK(ei,ej),\operatorname{Ric}(v, v) = \sum_{i = 2}^nK(v, e_i), \qquad R = \sum_{i \neq j}K(e_i, e_j),

so Ric⁡(v,v)n−1\frac{\operatorname{Ric}(v, v)}{n - 1} is the average sectional curvature of the planes containing vv, and Rn(n−1)\frac{R}{n(n - 1)} is the average over all planes (Exercise 4.4). For the unit sphere, Ric⁡=(n−1)g\operatorname{Ric} = (n - 1)g and R=n(n−1)R = n(n - 1); in dimension 22, Ric⁡=Kg\operatorname{Ric} = Kg and R=2KR = 2K.

A metric is Einstein if Ric⁡=λg\operatorname{Ric} = \lambda g for a constant λ\lambda. Spaces of constant curvature are Einstein, and in dimension 33 the converse holds (9A.5 Computing Curvature). Einstein metrics are the fixed points of the Ricci flow up to scaling: if Ric⁡(g0)=λg0\operatorname{Ric}(g_0) = \lambda g_0, then g(t)=(1−2λt)g0g(t) = (1 - 2\lambda t)g_0 (Exercise 4.8).

Proposition 4.1 The contracted Bianchi identity
∇iRij=12∇jR,that is,div⁡Ric⁡=12dR.\nabla^iR_{ij} = \tfrac12\nabla_jR, \qquad\text{that is,}\qquad \operatorname{div}\operatorname{Ric} = \tfrac12dR.

Proof. Recall Rjk=gilRijklR_{jk} = g^{il}R_{ijkl} (contract the first and last slots). Contract the second Bianchi identity ∇mRijkl+∇kRijlm+∇lRijmk=0\nabla_mR_{ijkl} + \nabla_kR_{ijlm} + \nabla_lR_{ijmk} = 0 with gilg^{il}; since ∇g=0\nabla g = 0, contraction commutes with ∇\nabla. The first term gives ∇mRjk\nabla_mR_{jk}. In the second, Rijlm=−RijmlR_{ijlm} = -R_{ijml}, so it gives −∇kRjm-\nabla_kR_{jm}. The third gives ∇iRijmk\nabla^iR_{ijmk}. So

∇mRjk−∇kRjm+∇iRijmk=0.\nabla_mR_{jk} - \nabla_kR_{jm} + \nabla^iR_{ijmk} = 0.

Now contract with gjkg^{jk}. The first term gives ∇mR\nabla_mR, the second −∇jRjm-\nabla^jR_{jm}. In the third, Rijmk=Rmkij=−RkmijR_{ijmk} = R_{mkij} = -R_{kmij}, and contracting its jj and kk gives −Rmi-R_{mi}, so it contributes −∇iRim-\nabla^iR_{im}. Hence ∇mR−2∇iRim=0\nabla_mR - 2\nabla^iR_{im} = 0.

The identity says that Ric⁡−12Rg\operatorname{Ric} - \frac12Rg, the Einstein tensor, is divergence-free. In general relativity that is the conservation of energy and momentum. In the Ricci flow it is the algebraic shadow of the diffeomorphism invariance of 8A.6 Flows and the Lie Derivative, which keeps the flow from being strictly parabolic, a degeneracy that DeTurck's trick removes (11A.3 Short-Time Existence and Uniqueness). It also gives Schur's lemma: in dimension n≥3n \geq 3, if Ric⁡=fg\operatorname{Ric} = fg for a function ff, then ff is constant (Exercise 4.5).

Three meanings of curvature

1. Circumferences: sectional curvature. Let Π\Pi be a plane at pp and CrC_r the curve traced by the points at distance rr along the geodesics from pp tangent to Π\Pi. Then

L(Cr)=2πr(1−K(Π)6r2+O(r3)).L(C_r) = 2\pi r\Big(1 - \frac{K(\Pi)}{6}r^2 + O(r^3)\Big).

On a surface this is the Bertrand–Diguet–Puiseux formula. Positive curvature makes small circles shorter than in the plane, and negative curvature makes them longer. On the model surfaces the circumferences are exactly 2πsin⁡r2\pi\sin r, 2πr2\pi r and 2πsinh⁡r2\pi\sinh r (Figure 4.1). The formula follows from the normal-coordinate expansion of 9A.3 Geodesics and the Exponential Map, or from Jacobi fields (9A.7 Jacobi Fields and Curvature versus Topology).

Figure 4.1. The circumference of a geodesic circle divided by the Euclidean value 2πr2\pi r, on the unit sphere (K=1K = 1), the plane and the hyperbolic plane (K=−1K = -1). Dashed: the approximations 1∓r261 \mp \frac{r^2}{6} from the formula above.

2. Volumes: Ricci curvature. In normal coordinates at pp the metric and its volume element are

gij(x)=δij−13Rikljxkxl+O(∣x∣3),det⁡gij(x)=1−16Rklxkxl+O(∣x∣3)g_{ij}(x) = \delta_{ij} - \tfrac13R_{iklj}x^kx^l + O(|x|^3), \qquad \sqrt{\det g_{ij}}(x) = 1 - \tfrac16R_{kl}x^kx^l + O(|x|^3)

(a standard computation with the Jacobi fields of 9A.7 Jacobi Fields and Curvature versus Topology). You check the first on the sphere in the last exercise of 9A.3 Geodesics and the Exponential Map and derive the second from it in Exercise 4.6. So the volume of a thin cone of geodesics leaving pp in the direction of a unit vector vv is reduced, at distance rr, by the factor 1−16Ric⁡(v,v)r21 - \frac16\operatorname{Ric}(v, v)r^2 compared with Euclidean space. Positive Ricci curvature in a direction focuses the geodesics in that direction and shrinks volume. Integrating over all directions,

Vol⁡(B(p,r))=ωnrn(1−R(p)6(n+2)r2+O(r4)),\operatorname{Vol}(B(p, r)) = \omega_nr^n\Big(1 - \frac{R(p)}{6(n + 2)}r^2 + O(r^4)\Big),

where ωn\omega_n is the volume of the Euclidean unit ball. Scalar curvature measures the volume of small balls.

This is the intuition for the Ricci flow. Where Ricci curvature is positive the metric has "too little volume", and ∂tg=−2Ric⁡\partial_tg = -2\operatorname{Ric} shrinks those directions further, as a round sphere shrinks to a point. Where it is negative the metric expands.

3. Gravity: Ricci curvature again. In a spacetime, consider a small ball of test particles, initially at rest relative to each other, falling freely with four-velocity uu. Its volume VV satisfies

V¨V∣t=0=−Ric⁡(u,u)\frac{\ddot V}{V}\Big|_{t = 0} = -\operatorname{Ric}(u, u)

(a form of Raychaudhuri's equation). Einstein's equations, for matter that is a perfect fluid at rest relative to the ball, turn this into

V¨V∣t=0=−4πG (ρ+Px+Py+Pz)\frac{\ddot V}{V}\Big|_{t = 0} = -4\pi G\,(\rho + P_x + P_y + P_z)

in units where c=1c = 1: the ball begins to shrink in proportion to the density plus the pressures. In empty space the right-hand side is zero, and the remaining curvature (the Weyl tensor, 9A.5 Computing Curvature) changes the shape of the ball without changing its volume (Figure 4.2). John Baez and Emory Bunn made this statement the starting point of an exposition of general relativity ("The meaning of Einstein's equation", American Journal of Physics, 2005).

Figure 4.2. A ball of freely falling test particles after a short time (a cross-section, deformations exaggerated). Middle: in empty space near a mass, tidal stretching along one axis and squeezing across it. In three dimensions the semi-axes become 1+kt21 + kt^2, 1−12kt21 - \frac12kt^2, 1−12kt21 - \frac12kt^2, and the volume is unchanged to order t2t^2. Right: inside matter, the Ricci term shrinks every direction.
In the world Data Measuring the Earth's gravity by geodesic deviation

The twin satellites of NASA and the German Aerospace Center's GRACE mission (2002–2017), and of its successor GRACE Follow-On (launched 2018), fly one behind the other in the same orbit, about 220220 km apart, and continuously measure the changes in their separation, GRACE by microwave ranging and GRACE-FO also with a laser ranging interferometer. As the pair passes over a mass concentration, the leading satellite is pulled ahead first, and the separation changes. That is the relative acceleration of two nearby free-fall paths, the Newtonian form of geodesic deviation. Month by month, these data map changes in the Earth's gravity field, and hence the movement of water: the loss of ice from Greenland and Antarctica, the depletion of groundwater, and seasonal flooding.

Conventions

Books differ in two ways: the overall sign of R(X,Y)ZR(X, Y)Z, and the order of the indices in RijklR_{ijkl}. This guide follows Lee (8A.7 Tensors and Index Notation):

quantity this guide on the round unit SnS^n
curvature endomorphism R(X,Y)Z=∇X∇YZ−∇Y∇XZ−∇[X,Y]ZR(X, Y)Z = \nabla_X\nabla_YZ - \nabla_Y\nabla_XZ - \nabla_{[X, Y]}Z
curvature tensor Rijkl=⟨R(∂i,∂j)∂k,∂l⟩R_{ijkl} = \langle R(\partial_i, \partial_j)\partial_k, \partial_l\rangle Rijkl=gilgjk−gikgjlR_{ijkl} = g_{il}g_{jk} - g_{ik}g_{jl}
sectional curvature K(X,Y)=Rm⁡(X,Y,Y,X)/∣X∧Y∣2K(X, Y) = \operatorname{Rm}(X, Y, Y, X)/\lvert X\wedge Y\rvert^2 K≡1K \equiv 1
Ricci tensor Rij=gklRkijlR_{ij} = g^{kl}R_{kijl} Rij=(n−1)gijR_{ij} = (n - 1)g_{ij}
scalar curvature R=gijRijR = g^{ij}R_{ij} R=n(n−1)R = n(n - 1)

The last column is the key to converting. Sectional, Ricci and scalar curvature are almost always normalised so that the round sphere has K=1K = 1, Ric⁡=(n−1)g\operatorname{Ric} = (n - 1)g and R=n(n−1)R = n(n - 1) (some physics texts flip the sign of the Ricci tensor); the four-index tensor is where books differ most. To translate a formula involving RijklR_{ijkl} from another book, substitute that book's expression for the unit sphere and compare with the column. One substitution fixes both the sign and the index order. When you read a Ricci flow paper, check its formula for RijklR_{ijkl} on the sphere before using any identity in it.

Where this goes What the flow does to curvature

Under ∂tg=−2Ric⁡\partial_tg = -2\operatorname{Ric}, the volume form evolves by ∂t dV=−R dV\partial_t\,dV = -R\,dV (8A.7 Tensors and Index Notation): volume decreases where scalar curvature is positive, as meaning 2 suggests. The curvature itself evolves by a heat equation, ∂tR=ΔR+2∣Ric⁡∣2\partial_tR = \Delta R + 2|\operatorname{Ric}|^2, derived in 11A.2 How Curvature Evolves with the commuting identities of 9A.6 The Laplacian and the Bochner Formula and the variation formula from the last exercise of 9A.2 Connections. The maximum principle of 6A.4 Maximum Principles applied to that equation gives the first pinching estimates.

History

Riemann introduced the curvature of a manifold of any dimension in his 1854 lecture, defining it through the curvature of surfaces swept out by geodesics, what is now sectional curvature, and wrote it as a tensor expression in an 1861 essay for the Paris Academy. Christoffel (1869) and Lipschitz derived the four-index tensor from the metric. Gregorio Ricci-Curbastro introduced the contracted tensor that bears his name around 1903–04, and Einstein made it the left-hand side of his field equations in 1915. The second Bianchi identity is named after Luigi Bianchi (1902), though it was found earlier. Amal Kumar Raychaudhuri published his equation for the focusing of geodesics in 1955. The circumference formula is due to Joseph Bertrand, Charles Diguet and Victor Puiseux (1848).

Recall Where we stand

The curvature tensor R(X,Y)Z=∇X∇YZ−∇Y∇XZ−∇[X,Y]ZR(X, Y)Z = \nabla_X\nabla_YZ - \nabla_Y\nabla_XZ - \nabla_{[X, Y]}Z measures the failure of second derivatives to commute and the holonomy of small loops; it vanishes exactly for locally flat metrics. RijklR_{ijkl} is antisymmetric in each pair, symmetric under exchanging the pairs, and satisfies both Bianchi identities. Sectional curvatures generalise Gauss curvature to planes and determine Rm⁡\operatorname{Rm}; Ricci curvature averages them over the planes containing a direction, and scalar curvature over all planes. Contracting Bianchi gives div⁡Ric⁡=12dR\operatorname{div}\operatorname{Ric} = \frac12dR. Sectional curvature shortens small circles, Ricci curvature shrinks thin cones and makes freely falling balls of matter contract, and scalar curvature shrinks small balls. To convert another book's formulas, test them on the unit sphere. 9A.5 Computing Curvature computes curvature for the model spaces, warped products, products and Lie groups.

Exercises

Exercise 4.2 Curvature is a tensor

Show that R(fX,Y)Z=fR(X,Y)ZR(fX, Y)Z = fR(X, Y)Z and R(X,Y)(fZ)=fR(X,Y)ZR(X, Y)(fZ) = fR(X, Y)Z for every smooth function ff. (Use [fX,Y]=f[X,Y]−(Yf)X[fX, Y] = f[X, Y] - (Yf)X for the first.)

Solution

First: ∇fX∇YZ−∇Y∇fXZ−∇[fX,Y]Z=f∇X∇YZ−(Yf)∇XZ−f∇Y∇XZ−f∇[X,Y]Z+(Yf)∇XZ=fR(X,Y)Z\nabla_{fX}\nabla_YZ - \nabla_Y\nabla_{fX}Z - \nabla_{[fX, Y]}Z = f\nabla_X\nabla_YZ - (Yf)\nabla_XZ - f\nabla_Y\nabla_XZ - f\nabla_{[X, Y]}Z + (Yf)\nabla_XZ = fR(X, Y)Z. Third slot: ∇X∇Y(fZ)=∇X((Yf)Z+f∇YZ)=(XYf)Z+(Yf)∇XZ+(Xf)∇YZ+f∇X∇YZ\nabla_X\nabla_Y(fZ) = \nabla_X((Yf)Z + f\nabla_YZ) = (XYf)Z + (Yf)\nabla_XZ + (Xf)\nabla_YZ + f\nabla_X\nabla_YZ; subtracting the same with X,YX, Y exchanged and ∇[X,Y](fZ)=([X,Y]f)Z+f∇[X,Y]Z\nabla_{[X, Y]}(fZ) = ([X, Y]f)Z + f\nabla_{[X, Y]}Z, everything cancels except fR(X,Y)ZfR(X, Y)Z, because XYf−YXf=[X,Y]fXYf - YXf = [X, Y]f.

Exercise 4.3 Dimension two

On a surface, show that the symmetries force Rijkl=K(gilgjk−gikgjl)R_{ijkl} = K(g_{il}g_{jk} - g_{ik}g_{jl}), where KK is the sectional (Gauss) curvature, and deduce Ric⁡=Kg\operatorname{Ric} = Kg and R=2KR = 2K.

Solution

In an orthonormal basis, antisymmetry in ijij and in klkl leaves only components with {i,j}={k,l}={1,2}\{i, j\} = \{k, l\} = \{1, 2\}: R1221=KR_{1221} = K, R1212=R2121=−KR_{1212} = R_{2121} = -K, R2112=KR_{2112} = K. The tensor K(gilgjk−gikgjl)K(g_{il}g_{jk} - g_{ik}g_{jl}) has the same components, so they are equal in every frame. Contracting, Rjk=gilRijkl=K(2gjk−gjk)=KgjkR_{jk} = g^{il}R_{ijkl} = K(2g_{jk} - g_{jk}) = Kg_{jk}, and R=2KR = 2K.

Exercise 4.4 Ricci as an average

Using the definition Rij=gklRkijlR_{ij} = g^{kl}R_{kijl} in an orthonormal basis with e1=ve_1 = v, show Ric⁡(v,v)=∑i≥2K(v,ei)\operatorname{Ric}(v, v) = \sum_{i \geq 2}K(v, e_i) and R=∑i≠jK(ei,ej)R = \sum_{i \neq j}K(e_i, e_j). For the unit sphere, recover Ric⁡=(n−1)g\operatorname{Ric} = (n - 1)g and R=n(n−1)R = n(n - 1).

Solution

Ric⁡(v,v)=∑kRm⁡(ek,v,v,ek)=∑k≥2K(ek,v)\operatorname{Ric}(v, v) = \sum_k\operatorname{Rm}(e_k, v, v, e_k) = \sum_{k \geq 2}K(e_k, v), the k=1k = 1 term vanishing by antisymmetry. Summing over v=ejv = e_j: R=∑j∑k≠jK(ek,ej)R = \sum_j\sum_{k \neq j}K(e_k, e_j). On the unit sphere each K=1K = 1, giving n−1n - 1 and n(n−1)n(n - 1).

Exercise 4.5 Schur's lemma

Suppose n≥3n \geq 3 and Ric⁡=fg\operatorname{Ric} = fg for a smooth function ff. Using div⁡Ric⁡=12dR\operatorname{div}\operatorname{Ric} = \frac12dR, show that df=0df = 0. Why does this fail in dimension 22?

Solution

R=nfR = nf and ∇iRij=∇i(fgij)=∇jf\nabla^iR_{ij} = \nabla^i(fg_{ij}) = \nabla_jf. The contracted Bianchi identity gives ∇jf=n2∇jf\nabla_jf = \frac n2\nabla_jf, so (1−n2)df=0(1 - \frac n2)df = 0 and df=0df = 0 when n≠2n \neq 2. In dimension 22, Ric⁡=Kg\operatorname{Ric} = Kg always (Exercise 4.3), with KK any function.

Exercise 4.6 Volumes of small balls

(a) From gij=δij+hijg_{ij} = \delta_{ij} + h_{ij} with hij=−13Rikljxkxl+O(∣x∣3)h_{ij} = -\frac13R_{iklj}x^kx^l + O(|x|^3), use det⁡(I+h)=1+12tr⁡h+O(∣h∣2)\sqrt{\det(I + h)} = 1 + \frac12\operatorname{tr}h + O(|h|^2) to derive det⁡g=1−16Rklxkxl+O(∣x∣3)\sqrt{\det g} = 1 - \frac16R_{kl}x^kx^l + O(|x|^3). (b) Using ∫Brxkxl dx=ωnrn+2n+2δkl\int_{B_r}x^kx^l\,dx = \frac{\omega_nr^{n + 2}}{n + 2}\delta^{kl}, derive the expansion of Vol⁡B(p,r)\operatorname{Vol}B(p, r). (c) Check it on S3S^3, where Vol⁡B(p,r)=π(2r−sin⁡2r)\operatorname{Vol}B(p, r) = \pi(2r - \sin2r).

Solution

(a) tr⁡h=δijhij=−13δijRikljxkxl=−13Rklxkxl\operatorname{tr}h = \delta^{ij}h_{ij} = -\frac13\delta^{ij}R_{iklj}x^kx^l = -\frac13R_{kl}x^kx^l (at pp, gij=δijg^{ij} = \delta^{ij}, and Rkl=gijRikljR_{kl} = g^{ij}R_{iklj} contracts the first and last slots). (b) Vol⁡=∫Br(1−16Rklxkxl) dx+O(rn+3)=ωnrn−16Rklδklωnrn+2n+2+⋯=ωnrn(1−R6(n+2)r2+… )\operatorname{Vol} = \int_{B_r}(1 - \frac16R_{kl}x^kx^l)\,dx + O(r^{n + 3}) = \omega_nr^n - \frac16R_{kl}\delta^{kl}\frac{\omega_nr^{n + 2}}{n + 2} + \dots = \omega_nr^n(1 - \frac{R}{6(n + 2)}r^2 + \dots); the O(∣x∣3)O(|x|^3) term in the volume element is odd and integrates to O(rn+4)O(r^{n + 4}), hence the O(r4)O(r^4). (c) π(2r−sin⁡2r)=π(8r36−32r5120+… )=43πr3(1−r25+… )\pi(2r - \sin2r) = \pi(\frac{8r^3}{6} - \frac{32r^5}{120} + \dots) = \frac43\pi r^3(1 - \frac{r^2}{5} + \dots), and with R=6R = 6, n=3n = 3: 66⋅5=15\frac{6}{6\cdot5} = \frac15.

Exercise 4.7 The tidal tensor

The Newtonian potential of a mass MM at the origin is Φ=−GM∣x∣\Phi = -\frac{GM}{|x|}, and two nearby freely falling particles separated by ξ\xi have relative acceleration ξ¨i=−∂i∂jΦ ξj\ddot\xi^i = -\partial_i\partial_j\Phi\,\xi^j. At the point (d,0,0)(d, 0, 0), compute ∂i∂jΦ\partial_i\partial_j\Phi and show the relative acceleration is GMd3(2ξ1,−ξ2,−ξ3)\frac{GM}{d^3}(2\xi^1, -\xi^2, -\xi^3). Show the trace is zero (this is ΔΦ=0\Delta\Phi = 0 in empty space). With GMMoon≈4.90×1012GM_{\text{Moon}} \approx 4.90\times10^{12} m³/s², d≈3.84×108d \approx 3.84\times10^8 m and ∣ξ∣=6.37×106|\xi| = 6.37\times10^6 m, estimate the stretching acceleration.

Solution

∂i∂j1∣x∣=3xixj−∣x∣2δij∣x∣5\partial_i\partial_j\frac{1}{|x|} = \frac{3x_ix_j - |x|^2\delta_{ij}}{|x|^5}, so at (d,0,0)(d, 0, 0), ∂i∂jΦ=−GMdiag⁡(2,−1,−1)/d3\partial_i\partial_j\Phi = -GM\operatorname{diag}(2, -1, -1)/d^3 and ξ¨=GMd3(2ξ1,−ξ2,−ξ3)\ddot\xi = \frac{GM}{d^3}(2\xi^1, -\xi^2, -\xi^3). The trace 2−1−1=02 - 1 - 1 = 0. Numerically, 2⋅4.90×1012⋅6.37×106(3.84×108)3≈1.1×10−6\frac{2\cdot4.90\times10^{12}\cdot6.37\times10^6}{(3.84\times10^8)^3} \approx 1.1\times10^{-6} m/s².

Exercise 4.8 Rehearsal: the shrinking sphere, rigorously

(a) Show that if g~=λg\tilde g = \lambda g for a constant λ>0\lambda > 0, then Γ~=Γ\tilde\Gamma = \Gamma, Ric⁡~=Ric⁡\widetilde{\operatorname{Ric}} = \operatorname{Ric} and R~=λ−1R\tilde R = \lambda^{-1}R. (b) Deduce that the round sphere of radius rr has Ric⁡=(n−1)gSn=n−1r2g\operatorname{Ric} = (n - 1)g_{S^n} = \frac{n - 1}{r^2}g and R=n(n−1)r2R = \frac{n(n - 1)}{r^2}. (c) Look for a Ricci flow of the form g(t)=ρ(t)2gSng(t) = \rho(t)^2g_{S^n} and show that ρ(t)2=r02−2(n−1)t\rho(t)^2 = r_0^2 - 2(n - 1)t, which reaches zero at T=r022(n−1)T = \frac{r_0^2}{2(n - 1)}. (d) More generally, if Ric⁡(g0)=λg0\operatorname{Ric}(g_0) = \lambda g_0, show g(t)=(1−2λt)g0g(t) = (1 - 2\lambda t)g_0 is a Ricci flow. This is the computation behind the first picture of the Path, now with every step justified.

Solution

(a) The Christoffel formula is homogeneous of degree zero in gg (gklg^{kl} scales by λ−1\lambda^{-1}, the derivatives by λ\lambda), so Γ\Gamma, R(X,Y)ZR(X, Y)Z and its trace Ric⁡\operatorname{Ric} are unchanged, and R=gijRijR = g^{ij}R_{ij} scales by λ−1\lambda^{-1}. (b) g=r2gSng = r^2g_{S^n} and Ric⁡(gSn)=(n−1)gSn=n−1r2g\operatorname{Ric}(g_{S^n}) = (n - 1)g_{S^n} = \frac{n - 1}{r^2}g; R=r−2n(n−1)R = r^{-2}n(n - 1). (c) ∂tg=(ρ2)′gSn\partial_tg = (\rho^2)'g_{S^n} and −2Ric⁡(g(t))=−2(n−1)gSn-2\operatorname{Ric}(g(t)) = -2(n - 1)g_{S^n}, so (ρ2)′=−2(n−1)(\rho^2)' = -2(n - 1). (d) Ric⁡((1−2λt)g0)=Ric⁡(g0)=λg0\operatorname{Ric}((1 - 2\lambda t)g_0) = \operatorname{Ric}(g_0) = \lambda g_0, and ∂t((1−2λt)g0)=−2λg0\partial_t((1 - 2\lambda t)g_0) = -2\lambda g_0.

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