Solutions to the Exercises in Elementary Differential Geometry Chapter 1 1.1.1 It is a parametrization of the part of the parabola with x ≥ 0. 1.1.2 (i) γ (t) = (sec t, tan t) with −π/2 < t < π/2 and π/2 < t < 3π/2. Note that γ is defined on the union of two disjoint intervals: this corresponds to the fact that the hyperbola y 2 − x2 = 1 is in two pieces, where y ≥ 1 and where y ≤ −1. (ii) γ (t) = (2 cos t, 3 sin t). 1.1.3 (i) x + y = 1. (ii) y = (ln x)2 . 1.1.4 (i) γ̇γ (t) = sin 2t(−1, 1). (ii) γ̇γ (t) = (et , 2t). 1.1.5 γ̇γ (t) = 3 sin t cos t(− cos t, sin t) vanishes where sin t = 0 or cos t = 0, i.e. t = nπ/2 where n is any integer. These points correspond to the four cusps of the astroid (see Exercise 1.3.3). 1.1.6 (i) The squares of the distances from p to the foci are (p cos t ± ǫp)2 + q 2 sin2 t = (p2 − q 2 ) cos2 t ± 2ǫp2 cos t + p2 = p2 (1 ± ǫ cos t)2 , so the sum of the distances is 2p. (ii) γ̇γ = (−p sin t, q cos t) so if n = (q cos t, p sin t) then n.γ̇γ = 0. Hence the distances from the foci to the tangent line at γ (t) are n (p cos t ∓ ǫp, q sin t).n pq(1 ∓ ǫ cos t) = 2 2 knk (p sin t + q 2 cos2 t)1/2 1 2 and their product is p2 q 2 (1−ǫ2 cos2 t) = q2 . (p2 sin2 t+q 2 cos2 t) (p−f1 ).n (iii) It is enough to prove that both sides are equal to q. = kp−f 1 k (p−f2 ).n kp−f 2 k t 0 . Computation shows that a at 1.1.7 When the circle has rotated through an angle t, its centre has moved to (at, a), so the point on the circle initially at the origin is now at the point (a(t − sin t), a(1 − cos t)) (see the diagram above). 1.1.8 Suppose that a point (x, y, z) lies on the cylinder if x2 + y 2 = 1/4 and on the sphere if (x + 21 )2 + y 2 + z 2 = 1. From the second equation, −1 ≤ z ≤ 1 so let z = sin t. Subtracting the two equations gives x + 14 + sin2 t = 43 , so x = 12 − sin2 t = cos2 t − 21 . From either equation we then get y = sin t cos t (or y = − sin t cos t, but the two solutions are interchanged by t 7→ π − t). √ √ 1.1.9 γ̇γ = (−2 sin t + 2 sin 2t, 2 cos t − 2 cos 2t) = √ 2( 2 − 1, 1) at t = π/4. So the √ 1 √ tangent line is y − ( 2 − 1) = (x − 2)/( 2 − 1) and the normal line is √ √ 1 y − ( √ − 1) = −(x − 2)( 2 − 1). 2 1.1.10 (i) Putting x = sec t gives y = ± sec t tan t so γ (t) = (sec t, ± sec t tan t) gives parametrizations of the two pieces of this curve (x ≥ 1 and x ≤ −1). 3t 3t2 (ii) Putting y = tx gives x = 1+t 3 , y = 1+t3 . 1.1.11 (i) From x = 1 + cos t, y = sin t(1 + cos t) we get y = x sin t so y 2 = x2 (1 − (x − 1)2 ) = x3 (2 − x). (ii) y = tx so x4 = t2 x3 + t3 x3 = y 2 x + y 3 = y 2 (x + y). 1.1.12 (i) γ̇γ (t) = (− sin t, cos t + cos 2t) so γ̇γ (t) = 0 if and only if t = nπ (n ∈ Z) and (−1)n + 1 = 0, so n must be odd. 3 (ii) γ̇γ (t) = (2t+3t2 , 3t2 +4t3 ). This vanishes ⇐⇒ t(2+3t) = 0 and t2 (3+4t) = 0, i.e. ⇐⇒ t = 0. 1.1.13 (i) Let OP make an angle θ with the positive x-axis. Then R has coordinates γ (θ) = (2a cot θ, a(1 − cos 2θ)). (ii) From x = 2a cot θ, y = a(1 − cos 2θ), we get sin2 θ = y/2a, cos2 θ = cot2 θ sin2 θ = x2 y/8a3 , so the Cartesian equation is y/2a + x2 y/8a3 = 1. 1.1.14 Let the fixed circle have radius a, and the moving circle radius b (so that b < a in the case of the hypocycloid), and let the point P of the moving circle be initially in contact with the fixed circle at (a, 0). When the moving circle has rotated through an angle ϕ, the line joining the origin to the point of contact of the circles makes an angle θ with the positive x-axis, where aθ = bϕ. The point P is then at the point γ (θ) = ((a + b) cos θ − b cos(θ + ϕ), (a + b) sin θ − b sin(θ + ϕ)) a+b a+b = (a + b) cos θ − b cos θ , (a + b) sin θ b b in the case of the epicycloid, b a ' P and γ (θ) = ((a − b) cos θ + b cos(ϕ − θ), (a − b) sin θ − b sin(ϕ − θ)) a−b a−b θ , (a − b) sin θ = (a − b) cos θ − b cos b b in the case of the hypocycloid. 1.1.15 γ̇γ (t) = (et (cos t − sin t), et (sin t + cos t)) so the angle θ between γ (t) and γ̇γ (t) is given by cos θ = e2t (cos2 t − sin t cos t + sin2 t + sin t cos t) 1 γ .γ̇γ = = , 2t 2 2 k γ kk γ̇γ k e ((cos t − sin t) + (sin t + cos t) ) 2 4 so θ = π/3. 1.1.16 γ̇γ (t) = (t cos t, t sin t) so a unit tangent vector is t = (cos t, sin t). The distance of the normal line at γ (t) from the origin is |γγ (t)..t| = | cos2 t + t sin t cos t + sin2 t − t sin t cos t| = 1. 1.2.1 γ̇γ (t) = (1, sinh t) so k γ̇γ k = cosh t and the arc-length is s = Rt 0 cosh u du = sinh t. 1.2.2 (i) k γ̇γ k2 = 14 (1 + t) + 14 (1 − t) + 12 = 1. 2 2 2 9 2 2 (ii) k γ̇γ k2 = 16 25 sin t + cos t + 25 sin t = cos t + sin t = 1. 1.2.3 Denoting d/dθ by a dot, γ̇γ = (ṙ cos θ − r sin θ, ṙ sin θ + r cos θ) so k γ̇γ k2 = ṙ 2 + r 2 . Hence, γ is regular unless r = ṙ = 0 for some value of θ. It is unit-speed if and only if ṙ 2 = 1 − r 2 , which gives r = ± sin(θ + α) for some constant α. To see that this is the equation of a circle of radius 1/2, see the diagram in the proof of Theorem 3.2.2. 1.2.4 Since u is a unit vector, |γ̇γ.u| = k γ̇γ k cos θ, where θ is the angle between γ̇γ and Rb Rb q − p)..u = (γγ (b) − γ (a))..u = a γ̇γ .u dt ≤ a k γ̇γ k dt. u, so γ̇γ.u ≤k γ̇γ k. Then, (q q − p)/ k q − p k gives the result. Taking u = (q √ 1.2.5 γ̇γ (t) = (6t, 1 − 9t2 ) so k γ̇γ (t) k = 36t2 + 1 − 18t2 + 81t4 = 1 + 9t2 . So the arc-length is Z t (1 + 9u2 )du = t + 3t3 . s= 0 1.2.6 We have γ̇γ (t) = (−2 sin t + 2 sin 2t, 2 cos t − 2 cos 2t) so k γ̇γ (t) k = p 8(1 − sin t sin 2t − cos t cos 2t = So the arc-length is s= Z x 0 p t 8(1 − cos t) = 4 sin . 2 x x t = 16 sin2 . 4 sin dt = 8 1 − cos 2 2 4 1.2.7 The cycloid is parametrized by γ (t) = a(t − sin t, 1 − cos t), where t is the angle through which the circle has rotated. So t γ̇γ = a(1 − cos t, sin t), k γ̇γ k2 = a2 (2 − 2 cos t) = 4a2 sin2 , 2 and the arc-length is Z 0 2π t t 2a sin dt = −4a cos 2 2 t=2π = 8a. t=0 5 1.2.8 The curve intersects the x-axis where cosh t = 3, say at t = ±a where a > 0. We have k γ̇γ (t) k2 = 2 cosh2 t − 2 cosh t so the arc-length is Z ap Z ap 2 2 cosh t − 2 cosh t dt = 2 2 cosh2 t − 2 cosh t dt. s= −a 0 To evaluate the integral put u = cosh t. Then, √ Z 3r hp i3 √ √ √ √ 2+ 3 u √ . du = s=2 u(u + 1) − ln( u + u + 1) = 2 3− 2−ln u+1 1 1+ 2 1 ... b + t2 c, where a, b, c are constant vectors. This implies 1.2.9 γ = 0 =⇒ γ = a + tb that γ is contained in the plane passing through the point with position vector a and parallel to the vectors b and c (i.e. perpendicular to b × c). (If b and c are parallel there are infinitely-many such planes.) 1.3.1 (i) γ̇γ = sin 2t(−1, 1) vanishes when t is an integer multiple of π/2, so γ is not regular. (ii) γ is regular since γ̇γ 6= 0 for 0 < t < π/2. (iii) γ̇γ = (1, sinh t) is obviously never zero, so γ is regular. 1.3.2 x = r cos θ = sin2 θ, y = r sin θ = sin2 θ tan θ, so the parametrization in terms of θ is θ 7→ (sin2 θ, sin2 θ tan θ). Since θ 7→ sin θ is a bijective smooth map (−π/2, π/2) → (−1, 1), with smooth inverse t 7→ sin−1 t,√ t = sin θ is a reparametrization map. Since sin2 θ = t2 , sin2 θ tan θ = t3 / 1 − t2 , so the reparametrized curve is as stated. 1.3.3 (i) γ̇γ = 0 at t = 0 ⇐⇒ m and n are both ≥ 2. If m > 3 the first components of ... γ̈γ and γ are both 0 at t = 0 so γ̈γ and γ̈γ are linearly dependent at t = 0; similarly ... if n > 3. So there are four cases: if (m, n) = (2, 2) or (3, 3) then either γ̈γ or γ is zero at t = 0, so the only possibilities for an ordinary cusp are (m, n) = (2, 3) ... and (3, 2) and then γ̈γ and γ are easily seen to 3be linearly independent at t = 0. t (ii) Using the parametrization γ (t) = t2 , √1−t , we get γ̇γ = 0, γ̈γ = (2, 0), 2 ... γ = (0, 6) at t = 0 so the origin is an ordinary cusp. (iii) Let γ̃γ (t̃) be a reparametrization of γ (t), and suppose γ has an ordinary cusp at t = t0 . Then, at t = t0 , dγ̃γ /dt̃ = (dγγ /dt)(dt/dt̃) = 0, d2 γ̃γ /dt̃2 = (d2γ /dt2 )(dt/dt̃)2 , d3γ̃γ /dt̃3 = (d3γ /dt3 )(dt/dt̃)3 + 3(d2γ /dt2 )(dt/dt̃)(d2 t/dt̃2 ). Using the fact that dt/dt̃ 6= 0, it is easy to see that d2γ̃γ /dt̃2 and d3γ̃γ /dt̃3 are linearly independent when t = t0 . 1.3.4 (i) If γ̃γ (t) = γ (ϕ(t)), let ψ be the inverse of the reparametrization map ϕ. Then γ̃γ (ψ(t)) = γ (ϕ(ψ(t))) = γ (t). (ii) If γ̃γ (t) = γ (ϕ(t)) and γ̂γ (t) = γ̃γ (ψ(t)), where ϕ and ψ are reparametrization maps, then γ̂γ (t) = γ ((ϕ ◦ ψ)(t)) and ϕ ◦ ψ is a reparametrization map because it d is smooth and dt (ϕ(ψ(t)) = ϕ̇(ψ(t))ψ̇(t) 6= 0 as ϕ̇ and ψ̇ are both 6= 0. 6 1.3.5 (i) γ̇γ (t) = (2t, 3t3 ) which vanishes ⇐⇒ t = 0. So γ is not regular. (ii) γ̇γ (t) = (− sin t − sin 2t, cos t + cos 2t) so k γ̇γ (t) k = 2 cos 2t . Hence, γ̇γ (t) = 0 ⇐⇒ t is an odd multiple of π. Thus, when t is retricted to the interval −π < t < π, γ is regular. 4t cos t 1.3.6 γ̇γ (t) = 2, − (1+t is obviously never zero, so γ is regular. Let ϕ(t) = 1+sin 2 )2 t. 1 Then, dϕ dt = − 1+sin t is never zero so ϕ is a reparametrization map. Setting u = ϕ(t) we get ! 2 2 cos t 2(1 + sin t)2 2 cos t γ (u) = = γ̃γ (t), , , = cos2 t 1 + sin t 1 + (1+sin 1 + sin t 2 + 2 sin t 2 t) so γ is a reparametrization of γ̃γ . 1.3.7 γ̇γ (t) = (aω cos ωt, b cos t) = 0 ⇐⇒ cos ωt = cos t = 0 ⇐⇒ ωt = (2k +1) π2 and t = (2l + 1) π2 , where k, l ∈ Z. This means that ω = 2k+1 2l+1 is the ratio of two odd integers. R t̃ Rt 1.3.8 We have s = t0 k dγγ /du k du, s̃ = t̃0 k dγ̃γ /dũ k dũ. By the chain rule, Rt dγγ /du = (dγ̃γ /dũ)(dũ/du), so s = ± t0 k dγ̃γ /dũ k (dũ/du) du = ±s̃, the sign being that of dũ/du. 1.3.9 We can assume that the curve γ is unit-speed and that the tangent lines all pass through the origin (by applying a translation to γ ). Then, there is a scalar λ(t) such that γ̇γ (t) = λ(t)γγ (t) for all t. Then, γ̈γ = λ̇γγ + λγ̇γ = (λ̇ + λ2 )γγ . This implies that γ̈γ is parallel to γ̇γ . But these vectors are perpendicular since γ is unit-speed. b where a , b are constant vectors, i.e. γ is a straight Hence, γ̈γ = 0, so γ (t) = taa +b line. If all the normal lines are parallel, so are all the tangent lines. If γ is assumed to be unit-speed, this means that γ̇γ is constant, say equal to a. Then γ (t) = taa + b as before. 1.4.1 It is closed because γ (t + 2π) = γ (t) for all t. Suppose that γ (t) = γ (u). Then cos3 t(cos 3t, sin 3t) = cos3 u(cos 3u, sin 3u). Taking lengths gives cos3 t = ± cos3 u so cos t = ± cos u, so u = t, π − t, π + t or 2π − t (up to adding multiples of 2π). The second possibility forces t = nπ/3 for some integer n and the third possibility is true for all t. Hence, the period is π and for the self-intersections we need only consider t = π/3, 2π/3, giving u = 2π/3, π/3, respectively. Hence, there is a unique self-intersection at γ (π/3) = (−1/8, 0). 1.4.2 The curve γ̃γ (t) = (cos(t3 + t), sin(t3 + t)) is a reparametrization of the circle γ (t) = (cos t, sin t) but it is not closed. 1.4.3 If γ is T -periodic then it is kT -periodic for all k 6= 0 (this can be proved by induction on k if k > 0, or on −k if k < 0). If γ is T1 -periodic and T2 -periodic 7 then it is k1 T1 - and k2 T2 -periodic for all non-zero integers k1 , k2 , so γ (t + k1 T1 + k2 T2 ) = γ (t + k1 T1 ) as γ is k2 T2 -periodic, which = γ (t) as γ is k1 T1 -periodic. 1.4.4 If γ is T -periodic write T = kT0 + T1 where k is an integer and 0 ≤ T1 < T0 . By Exercise 1.4.3 γ is T1 -periodic; if T1 > 0 this contradicts the definition of T0 . 1.4.5 (i) Choose T1 > 0 such that γ is T1 -periodic; then T1 is not the smallest positive number with this property, so there is a T2 > 0 such that γ is T2 -periodic. Iterating this argument gives the desired sequence. (ii) The sequence {Tr }r≥1 in (i) is decreasing and bounded below, so must converge to some T∞ ≥ 0. Then γ is T∞ -periodic because (using continuity of γ ) γ (t + T∞ ) = limr→∞ γ (t + Tr ) = limr→∞ γ (t) = γ (t). By Exercise 1.4.3, γ is (Tr − T∞ )-periodic for all r ≥ 1, and this sequence of positive numbers converges to 0. (iii) If {Tr } is as in (i) and Tr → 0 as r → ∞, then by the mean value theorem 0 = (f (t + Tr ) − f (t))/Tr = f˙(t + λTr ) for some 0 < λ < 1. Letting r → ∞ gives f˙(t) = 0 for all t, so f is constant. 1.4.6 Following the hint, since T0 = (ki /k)Ti is an integer multiple of Ti , each γi is T0 periodic. Let T be the union of the finite sets of real numbers {Ti , 2Ti , . . . , ki Ti } over all i such that γi is not constant, and let P = {T ′ ∈ T | γ is T ′ -periodic}. Then P is finite (because T is) and non-empty (because T ∈ P). The smallest element of P is the smallest positive number T0′ such that γ is T0′ -periodic (since if γ is T ′ -periodic either T ′ > T or T ′ ∈ P). By Exercise 1.4.4, T0 = k ′ T0′ for some integer k ′ and then there are integers ki′ such that T0′ = ki′ Ti for all i such that γi is not constant. Then, ki Ti /k = k ′ ki Ti so kk ′ divides each ki . As k is the largest such divisor, k ′ = 1, so T0 = T0′ . 2 2 u −3 2 2 1.4.7 If γ (t) = γ (u) then tt2 −3 +1 = u2 +1 . This implies t = u . This shows that γ is not periodic and that for a self-intersection we must have t = −u. The √ 2 −3) = 0, so t = 0 or ± 3. Hence, the unique equation γ (t) = γ (−t) implies t(tt2 +1 √ √ self-intersection is at γ ( 3) = γ (− 3) = 0. 1.4.8 If γ (t) = γ (u) then sin t = sin u. Also, k γ (t) k2 = k γ (u) k2 , which gives 5 + 4 cos t = 5 + 4 cos u, hence cos t = cos u. So t = u + 2nπ for some integer n. We must have cos ω(t + 2nπ) = cos ωt so ω(t + 2nπ) = ωt + 2mπ for some integer m. Hence, ω = m/n is rational. The period T of γ is the smallest positive number such that γ (t + T ) = γ (t) for all t. From the first part we know that T = 2N π for some integer N . Then, N is the smallest positive integer N such that ω(t+2N π) = ωt+2M π for some integer M , i.e. the smallest positive integer such that mN/n is an integer. If m and n have no common factor, N = n. 8 1.5.1 x(1 − x2 ) ≥ 0 ⇐⇒ x ≤ −1 or 0 ≤ x ≤ 1 so the curve is in (at least) two pieces. The parametrization is defined for t ≤ −1 and 0 ≤ t ≤ 1 and it covers the part of the curve with y ≥ 0. 1.5.2 If γ (t) = (x(t), y(t), z(t)) is a curve in the surface f (x, y, z) = 0, differentiating f (x(t), y(t), z(t)) = 0 with respect to t gives ẋfx + ẏfy + żfz = 0, so γ̇γ is perpendicular to ∇ f = (fx , fy , fz ). Since this holds for every curve in the surface, ∇f is perpendicular to the surface. The surfaces f = 0 and g = 0 should intersect in a curve if the vectors ∇ f and ∇g are not parallel at any point of the intersection. 1.5.3 Let γ (t) = (u(t), v(t), w(t)) be a regular curve in R3 . At least one of u̇, v̇, ẇ is non-zero at each value of t. Suppose that u̇(t0 ) 6= 0 and x0 = u(t0 ). As in the ‘proof’ of Theorem 1.5.2, there is a smooth function h(x) defined for x near x0 such that t = h(x) is the unique solution of x = u(t) for each t near t0 . Then, for t near t0 , γ (t) is contained in the level curve f (x, y, z) = g(x, y, z) = 0, where f (x, y, z) = y − v(h(x)) and g(x, y, z) = z − w(h(x)). The functions f and g satisfy the conditions in the previous exercise, since ∇f = (−v̇h′ , 1, 0), ∇ g = (−ẇh′ , 0, 1), a dash denoting d/dx. 1.5.4 The equation cannot be satisfied if x = 1, so the line x = 1 separates the curve into at least two connected pieces. The curve γ is a parametrization because (x − 1)2 (x2 + y 2 ) = cos2 t((1 + cos t)2 + (sin t + tan t)2 ) = cos2 t(1 + cos t)2 (1 + tan2 t) = (1 + cos t)2 = x2 . But since tan t is undefined when t = ±π/2, ±3π/2, ..., γ must be defined on one of the intervals (−π/2, π/2), (π/2, 3π/2), etc. The restriction of γ to the first of these intervals parametrizes the part of the curve with x > 1, the second gives the part with x < 1. This shows that the two parts of the curve with x < 1 and with x > 1 are connected. 1.5.5 Letting f (x, y, z) = x2 + y 2 = 1/4, g(x, y, z) = x2 + y 2 + z 2 + x − 3/4, we find ∂f ∂f ∂f ∂g ∂g ∂g that ( ∂x , ∂y , ∂z ) = (2x, 2y, 0), ( ∂x , ∂y , ∂z ) = (2x + 1, 2y, 2z). If these vectors are parallel, z = 0; if y 6= 0 the vectors must then be equal and this is impossible; so y = 0 and then we must have x = 1/2 to satisfy both equations. Hence, the vectors are parallel only at the point (1/2, 0, 0). For the parametrization γ in Exercise 1.1.8, γ̇γ (t) = (− sin 2t, cos 2t, cos t). This is never zero as k γ̇γ (t) k2 = 1 + cos2 t, so γ is regular. 1.5.6 Define Θ(t) = tan πθ(t)/2, where θ is the function defined in Exercise 9.4.3. Then Θ is smooth, Θ(t) = 0 if t ≤ 0, and Θ : (0, ∞) → (0, ∞) is a bijection. The curve (Θ(t), Θ(t)) if t ≥ 0, γ (t) = (−Θ(−t), Θ(−t)) if t ≤ 0, is a smooth parametrization of y = |x|. 9 There is no regular parametrization of y = |x|. For if there were, there would be a unit-speed parametrization γ̃γ (t), say, and we can assume that γ̃γ (0) = (0, 0). The unit tangent vector γ̃γ˙ would have to be either √12 (1, 1) or − √12 (1, 1) when x > 0, so by continuity we would have γ̃γ˙ (0) = ± √1 (1, 1). But, by considering the 2 part x < 0 in the same way, we see that γ̃γ˙ (0) = ± √12 (1, −1). These statements are contradictory. Chapter 2 2.1.1 (i) γ is unit-speed (Exercise 1.2.2(i)) so 1 1 1 κ = k γ̈γ k = k ( (1 + t)−1/2 , (1 − t)−1/2 , 0) k = p . 4 4 8(1 − t2 ) (ii) γ is unit-speed (Exercise 1.2.2(ii)) so κ = k γ̈γ k = k (− 45 cos t, sin t, 53 cos t) k = 1. t,0)×(0,cosh t,0)k 2 cosh t (iii) κ = k(1,sinh = cosh 3 t = sech t using Proposition 2.1.2. k(1,sinh t,0)k3 (iv) (−3 cos2 t sin t, 3 sin2 t cos t, 0)×(−3 cos3 t+6 cos t sin2 t, 6 sin t cos2 t−3 sin3 t, 0) sin2 t cos2 t)k = (0, 0, −9 sin2 t cos2 t), so κ = k(−3 k(0,0,−9 = 3| sin 1t cos t| . This cos2 t sin t,3 sin2 t cos t,0)k3 becomes infinite when t is an integer multiple of π/2, i.e. at the four cusps (±1, 0) and (0, ±1) of the astroid. 2.1.2 The proof of Proposition 1.3.5 shows that, if v(t) is a smooth (vector) function of t, then k v(t) k is a smooth (scalar) function of t provided v(t) is non-zero for all t. The result now follows from the formula in Proposition 2.1.2. The curvature of the regular curve γ (t) = (t, t3 ) is κ(t) = 6|t|/(1 + 9t4 )3/2 , which is not differentiable at t = 0. 2.1.3 Working in R3 , γ̇γ (t) = (1 − cosh 2t, 2 sinh t, 0) = 2 sinh t(− sinh t, 1, 0), γ̈γ (t) = γ ×γ̈γ k kγ̇ (−2 sinh 2t, 2 cosh t, 0) which gives γ̇γ ×γ̈γ = (0, 0, 4 sinh2 t cosh t) and κ = kγ̇γ k3 = 1/2 sinh t cosh2 t. This is non-zero if t > 0, but → 0 as t → ∞. 10 2.1.4 We have γ̇γ (t) = (sec t tan t, sec t tan2 t + sec3 t, 0), γ̈γ (t) = (2 sec3 t − sec t, 6 sec3 t tan t − sec t tan t), which gives γ̇γ × γ̈γ = sec4 t(0, 0, 2 sec2 t − 3). Hence, the curvature vanishes where sec2 t = 3/2. If −π/2 < t < π/2, cos t > 0 so the curvature vanishes at the two values of t between −π/2 and π/2 at which cos t = 2/3, i.e. at the point √ (3/2, 5/2). ns = 0 and use ṫt = κsns . 2.2.1 Differentiate t.n 2.2.2 If γ is smooth, t = γ̇γ is smooth and hence so are ṫt and ns (since ns is obtained ns is smooth. by applying a rotation to t). So κs = ṫt.n 2.2.3 For the first part, from the results in Appendix 1 it suffices to show that κ̃s = −κs if M is the reflection in a straight line l. But this is clear: if we take the fixed angle ϕ0 in Proposition 2.2.1 to be the angle between l and the positive x-axis, then (in the obvious notation) ϕ̃ = −ϕ. Conversely, if γ and γ̃γ have the same non-zero curvature, their signed curvatures are either the same or differ in sign. In the first case the curves differ by a direct isometry by Theorem 2.2.5; in the latter case, applying a reflection to one curve gives two curves with the same signed curvature, and these curves then differ by a direct isometry, so the original curves differ by an opposite isometry. 2.2.4 The first part is obvious as the effect of the dilation is to multiply s by a and leave ϕ unchanged. For the second part, consider the small piece of the chain between the points with arc-length s and s + δs. The net horizontal force on this piece is (in the obvious notation) δ(T cos ϕ), and as this must vanish T cos ϕ must be a constant, say λ. The net vertical force is δ(T sin ϕ), and this must balance the weight of the piece of chain, which is a constant multiple of δs. This shows that T sin ϕ = µs + ν for some constants µ, ν, and ν must be zero because ϕ = s = 0 at the lowest point of C. From T cos ϕ = λ, T sin ϕ = µs, we get tan ϕ = s/a where a = λ/µ. = 1/a, so the signed curvature is Hence, sec2 ϕ dϕ ds κs = dϕ/ds = 1/a sec2 ϕ = 1/a(1 + tan2 ϕ) = s2 a . + a2 Using the first part and Example 2.2.4 gives the result. ns /dt = (1 − λκs )ds/dt t, so the arc-length sλ 2.2.5 We have dγγ λ /dt = dγγ /dt + λdn of γ λ satisfies dsλ /dt = |1 − λκs |ds/dt. The unit tangent vector of γ λ is tλ = ns . Then, (dγγ λ /dt)/(dsλ/dt) = ǫtt, hence the signed unit normal of γ λ is nλs = ǫn 11 the signed curvature κλs of γ λ is given by dttλ /dt ǫ dtt dttλ = = λ ds |1 − λκs |(ds/dt) |1 − λκs | ds κs ǫκs κs = ns = nλs = nλ . 1 − λκs 1 − λκs |1 − λκs | s κλsnλs = 2.2.6 ǫ(s0 ) lies on the perpendicular bisector of the line joining γ (s0 ) and γ (s0 + δs). This gives (ǫǫ(s0 ) − 21 (γγ (s0 ) +γγ (s0 + δs)))..(γγ (s0 + δs) −γγ (s0 )) = 0. Using Taylor’s theorem, and discarding terms involving powers of δs higher than the second, this gives (with all quantities evaluated at s0 ) (ǫǫ − γ )..γ̇γ δs + 21 (ǫǫ.γ̈γ − 1 − γ .γ̈γ )(δs)2 = 0. This must also hold when δs is replaced by −δs; adding and subtracting the two equations gives (ǫǫ − γ )..γ̇γ = 0 and (ǫǫ − γ )..γ̈γ = 1. The first equation gives ns for some scalar λ, and since γ̈γ = κsns the second gives λ = 1/κs . ǫ = γ + λn 2.2.7 The tangent vector of ǫ is t + κ1s (−κs t) − κκ̇2s ns = − κ̇κs2 ns so its arc-length is s s R R u = k ǫ̇ǫ k ds = κκ̇s2 ds = u0 − κ1s , where u0 is a constant. Hence, the unit s ns and its signed unit normal is t. Since −dn ns /du = tangent vector of ǫ is −n κ3s 3 κst/(du/ds) = κ̇s t, the signed curvature of ǫ is κs /κ̇s . ns (s) for some λ. Hence, Any point on the normal line to γ at γ (s) is γ (s) + λn the normal line intersects ǫ at the point ǫ(s), where λ = 1/κs (s), and since the tangent vector of ǫ there is parallel to ns (s) by the first part, the normal line is tangent to ǫ at ǫ(s). Denoting d/dt by a dash, γ ′ = a(1 − cos t, sin t) so the arc-length s of γ is given by ds/dt = 2a sin(t/2) and t = dγγ /ds = (sin(t/2), cos(t/2)). So ns = 1 (− cos(t/2), sin(t/2)) and ṫt = (dtt/dt)/(ds/dt) = 4a sin(t/2) (cos(t/2), − sin(t/2)) = ns , so the signed curvature of γ is −1/4a sin(t/2) and its evolute −1/4a sin(t/2)n ǫ(t) = a(t − sin t, 1 − cos t) − 4a sin(t/2)(− cos(t/2), sin(t/2)) = a(t + sin t, −1 + cos t). Reparametrizing ǫ by t̃ = π + t, we get a(t̃ − sin t̃, 1 − cos t̃) + a(−π, −2), so ǫ is obtained from a reparametrization of γ by translating by the vector a(−π, −2). 2.2.8 The free part of the string is tangent to γ at γ (s) and has length ℓ − s, hence the ns stated formula for ι(s). The tangent vector of ι is γ̇γ − γ̇γ + (ℓ − s)γ̈γ = κs (ℓ − s)n ι (a dot denotes d/ds). The arc-length v of is given by dv/ds = κs (ℓ − s) so ns /dv = its unit tangent vector is ns and its signed unit normal is −tt. Now dn 1 −1 n κs (ℓ−s) ṅ s = ℓ−s t , so the signed curvature of ι is 1/(ℓ − s). √ 2.2.9 The arc-length parametrization of the catenary is γ̃γ (s) = (sinh−1 s, 1 + s2 ). The involute 1 s −1 ˙ ,√ = (u − tanhu, sechu) ι(s) = γ̃γ (s) − sγ̃γ (s) = sinh s − √ 1 + s2 1 + s2 12 if u = sinh−1 s. Thus, if (x, y) is a point on the involute ι, u = cosh−1 (1/y) and p x = cosh−1 (1/y) − 1 − y 2 . 2.2.10 The rotation ρ−θ(s) takes the tangent line of γ at γ (s) to l and the line joining q and γ (s) to a line parallel to that joining Γ(s) to p + saa. Hence, p + saa) = ρ−θ(s) (q q − γ (s)), Γ(s) − (p which gives the stated equation. Now, d q − γ (s)) − ρ−θ(s)γ̇γ (s). Γ(s) = a + ρ−θ(s) (q Γ̇ ds The last term is clearly parallel to a and as they are both unit vectors they are equal. So we want to prove that d q − γ (s))..ρ−θ(s) (q q − γ (s)) = 0. ρ−θ(s) (q ds v)t dA If A = ρ−θ(s) , v = q − γ (s), we have to show (in matrix notation) (Av ds v = 0, t t dA i.e. v A ds v = 0. Since A is orthogonal, this follows from parts (i) and (ii) of the hint. P P P To prove (i), use components: vt Svv = i,j vi vj Sij = i,j vj vi Sji = − i,j vi vj Sij . For (ii), differentiate At A = I. 2.2.11 If two unit-speed curves have the same non-zero curvature, their signed curvatures are either the same or differ in sign. In the first case the curves differ by a direct isometry by Theorem 2.2.6; in the latter case, applying a reflection to one curve gives two curves with the same signed curvature by Exercise 2.2.3, and these curves then differ by a direct isometry. 2.2.12 By applying a translation we can assume that all the normal lines pass through ns (t) for all t. the origin. Then, there is a scalar λ(t) such that γ (t) = λ(t)n ns − λκs t using Exercise 2.2.1. It follows that λ̇ = 0, Differentiating gives t = λ̇n so λ is constant, and that λκs = −1, so κs = −1/λ is constant. Hence, γ is a circle by Example 2.2.7. 2.2.13 The arc-length Z Z s= k γ̇γ k dt = k ekt (k cos t − sin t, k sin t + cos t) k dt √ Z p k 2 + 1 kt kt k 2 + 1e dt = e + c, = k where c is a constant. Taking c = 0 makes s → 0 as t → ∓∞ if ±k > 0. 13 Since t = γ̇γ / k γ̇γ k = √k12 +1 (k cos t − sin t, k sin t + cos t), the signed unit normal is ns = √k12 +1 (−k sin t − cos t, k cos t − sin t). So dtt/dt e−kt e−kt dtt = = 2 (−k sin t − cos t, k cos t − sin t) = √ ns , ds ds/dt k +1 k2 + 1 hence κs = 1/ks. By Theorem 2.2.6, any other curve with the same signed curvature is obtained from the logarithmic spiral by applying a direct isometry. 2.2.14 Let δ (t) be the foot of the perpendicular from p to the tangent line of γ at γ (t). ns for some scalar λ = (δδ − p)..ns . But γ − δ is parallel to the Then δ = p + λn tangent line, so is perpendicular to ns : (γγ − δ )..ns = 0. Hence, δ .ns = γ .ns and we get λ = (γγ − p)..ns . p)..t )n ns +((γγ −p p)..ns )tt). So δ̇δ = 0 Using Exercise 2.1.1, we find that δ̇δ = −κs (((γγ −p ns + ((γγ − p)..ns )tt) = 0. Since ns and t if and only if either κs = 0 or (((γγ − p)..t)n are perpendicular, the last equation can hold only if (γγ − p)..t = (γγ − p)..ns = 0, which implies that γ = p. Hence, δ is regular if and only if γ has nowhere vanishing curvature and does not pass through p. For the circle γ (t) = (cos t, sin t), ns = −γγ and so δ (t) = (−2, 0) + (2 + cos t, sin t)..(cos t, sin t)(cos t, sin t) = ((1 + 2 cos t) cos t − 2, (1 + 2 cos t) sin t), which is obtained by translating the limaçon in Example 1.1.7 by (−2, 0). ns . Since t and ns are perpendicular 2.2.15 (i) Differentiating γ = rtt gives t = ṙtt + κs rn vectors, it follows that κs = 0 and γ is part of a straight line. ns gives t = ṙn ns + rṅ ns = ṙn ns − κs rtt (Exercise 2.1.1). (ii) Differentiating γ = rn Hence, ṙ = 0, so r is constant, and κs = −1/r, hence κs is constant. So γ is part of a circle. (iii) Write γ = r(tt cos θ + ns sin θ). Differentiating and equating coefficients of t and ns gives ṙ cos θ − κs r sin θ = 1, ṙ sin θ + κs r cos θ = 0, from which ṙ = cos θ and κs r = − sin θ. From the first equation, r = s cos θ (we can assume the arbitrary constant is zero by adding a suitable constant to s) so κs = −1/s cot θ. By Exercise 2.2.13, γ is obtained by applying a direct isometry to the logarithmic spiral defined there with k = − cot θ. 1 1 (1, 2t), ns = √1+4t 2.2.16 For the parabola γ (t) = (t, t2 ), t = √1+4t (−2t, 1), so 2 2 λ 2λ 2λ 2 √ λ γ (1, 2t). , t + . This gives γ̇ = 1 − γ λ (t) = t − √1+4t 2 (1+4t2 )3/2 1+4t2 Hence, γ̇γ λ (t) = 0 ⇐⇒ 2λ = (1 + 4t2 )3/2 . If λ < 1/2 this has no solution for t, so γ λ is regular. If λ = 1/2, the only solution is t = 0 so (0, 1/2) is the unique singular point of γ . If λ > 1/2 there are two solutions for t, hence γ λ has two singular points. 14 2.2.17 Ḟ = 2γ̇γ.(γγ − c). So F (t0 ) = Ḟ (t0 ) = 0 ⇐⇒ k γ (t0 ) − c k = R and γ̇γ (t0 ) is perpendicular to γ (t0 ) − c. This means that γ (t0 ) is on the circle C and that γ̇γ (t0 ) = t(t0 ) is parallel to the tangent to C at that point (since this tangent is perpendicular to the radius γ (t0 ) − c). Now F̈ = 2ṫt. (γγ −cc)+2 (since γ is unit-speed), so F̈ (t0 ) = 0 ⇐⇒ ṫt(t0 ).(γγ (t0 )−cc) = ns (t0 ) is perpendicular to t(t0 ) (since γ is unit-speed), −1. Now ṫt(t0 ) = κs (t0 )n hence parallel to γ (t0 )−cc from the condition Ḟ (t0 ) = 0. So the condition F̈ (t0 ) = ns (t0 ) for some scalar λ and we have κs (t0 )n ns (t0 )..λn ns (t0 ) = 0 gives γ (t0 ) − c = λn −1 which gives λ = −1/κs (t0 ). So the conditions F (t0 ) = Ḟ (t0 ) = F̈ (t0 ) = 0 are 1 satisfied if and only if the centre of C is c = γ (t0 ) + κs (t ns (t0 ) and its radius is 0) k γ (t0 ) − c k = |λ| = 1/|κs (t0 )|. Comparing with Exercise 2.2.6 shows that C is the osculating circle of γ at γ (t0 ). 2.2.18 From the solution of Exercise 2.2.16, t = 1 √ 1 (1, 2t), ns = √1+4t (−2t, 1), 2 1+4t √2 k = 1 + 4t2 (a dot denoting d/dt). and if s is the arc-length of γ , ds/dt = k γ̇γ Hence, 1 2 4t dtt , =√ , ṫt = − ds (1 + 4t2 )2 (1 + 4t2 )2 1 + 4t2 hence κs = 2(1 + 4t2 )−3/2 . The evolute is therefore 1 1 ǫ = γ + ns = (t, t2 ) + (1 + 4t2 )(−2t, 1) = κs 2 1 −4t , 3t + 2 3 2 . p a2 sin2 t + b2 cos2 t = 1/λ, say. Then, 2.2.19 If s is the arc-length of γ , ds/dt = denoting d/ds by a dot, t = γ̇γ = λ(−a sin t, b cos t), ns = λ(−b cos t, −a sin t), ns ṫt = λ[λ(−a cos t, −b sin t) − λ3 (a2 − b2 ) sin t cos t(−a sin t, b cos t)] = λ3 abn after some simplification. Hence, κs = λ3 ab = λ ǫ = (a cos t, b sin t) + 3 (−b cos t, −a sin t) = λ ab ab (a2 sin2 t+b2 cos2 t)3/2 and so a2 − b2 b2 − a2 3 3 cos t, sin t . a b ns . Then, γ̇γ λ = γ̇γ +λṅ ns = (1−λκs )n ns . Assuming that λκs 6= 1 (so 2.2.20 Let γ λ = γ +λn λ λ t that γ λ is regular), we have (in an obvious notation) ds ds = |1 − λκs |, t = ±t , nλs = ±n ns , where ± is the sign of 1 − λκs . Hence, ±ṫt κsns κsnλs dttλ = = ± = . dsλ |1 − λκs | |1 − λκs | |1 − λκs | 15 So κλs = κs |1−λκs | and ns + ǫλ = γ + λn |1 − λκs | 1 − λκs ns ) = γ + λn ns + (±n ns = ǫ. κs κs 2.2.21 (i) With the notation in Exercise 2.2.7, the involute of ǫ is ι(u) = ǫ + (ℓ − u) 1 dǫǫ ns = γ − (ℓ − u0 )n ns , = γ + ns − (ℓ − u)n du κs since u = u0 − κ1s , so ι is the parallel curve γ −(ℓ−u0 ) . (ii) Using the results of Exercise 2.2.8, the evolute of ι is ι + (ℓ − s)(−tt) = γ + (ℓ − s)tt − (ℓ − s)tt = γ . 2.2.22 (i) If γ (θ) = (x(θ), y(θ)), we have x cos θ + y sin θ = p. Denoting d/dθ by a dot, we also have ẏ dy cos θ = =− . ẋ dx sin θ Differentiating the first equation and using the second gives −x sin θ + y cos θ = ṗ. Solving the first and third equations for x and y gives the stated formula for γ . (ii) From (i), γ̇γ = (p + p̈)(− sin θ, cos θ), so k γ̇γ k = |p + p̈|. Hence, γ is regular if and only if p + p̈ is never zero. In that case p + p̈ must be either always > 0 or always < 0. But the latter R 2π case is impossible since it implies that p̈ < 0, contradicting the fact that 0 p̈ dθ = 0 since p is smooth and 2π-periodic. 1 d θ + π2 = dθ (iii) If s is the arc-length of γ , the signed curvature is ds ds = ds/dθ = 1 1 γ k = p+p̈ . kγ̇ (iv) Since ds dθ = p + p̈, the length of γ is Z 0 2π (p + p̈)dθ = Z 2π p dθ. 0 (v) The first part is obvious. The foot of the perpendicular from the origin to the tangent line at γ (θ) is p(θ)(cos θ, sin θ), so w(θ) is the distance between this 16 point and p(θ + π)(cos(θ + π), sin(θ + π)) = p(θ + π)(− cos θ, − sin θ) which is p(θ) + p(θ + π). (vi) The function q(θ) = w(θ) − w(θ + π) is smooth and q(0) = −q(π/2) because w(0) = w(π). Hence, for some angle θ0 with 0 ≤ θ0 ≤ π/2, we have q(θ0 ) = 0, i.e. w(θ0 ) = w(θ0 +π/2). This means that the tangent lines at θ0 , θ0 +π/2, θ0 +π and θ0 + 3π/2 form a square. (vii) From (iv) and (v), the length is Z π (p(θ) + p(θ + π))dθ = 0 Z π w(θ) dθ, 0 which is equal to πD if w(θ) is equal to the constant D. kπ 2 kθ (viii) If p(θ) is as stated, w(θ) = a cos2 kθ + 2b = a + 2b. 2 + cos 2 + 2 (ix) If |k| = 1 we find that γ (θ) = 1 1 a, 0 + a + b (cos θ, sin θ), 2 2 which is the circle with centre ( 21 a, 0) and radius − 21 ka sin kθ, p̈ = − 12 k 2 a cos kθ, so κs = 1 a cos2 kθ 2 − 1 2 k a cos kθ 2 +b = 1 2a +b+ 1 2a + b. In general, ṗ = 1 , − k 2 )a cos kθ 1 2 (1 which is constant ⇐⇒ k = 0 or ± 1 (and k = 0 does not give a regular curve). 2.2.23 Parametrize the parabola by x = sinh t, y = at the origin) is s= Z t 1 2 sinh2 t. The arc-length (starting (cosh2 u + cosh2 u sinh2 u)1/2 du = 0 1 (t + sinh t cosh t). 2 In the notation of Exercise 2.2.10, θ is the angle between (cosh t, cosh t sinh t) and the x-axis, so cos θ = secht, sin θ = tanht, p = (0, 0), a = (1, 0) and we get Γ = (s, 0) + cos θ − sin θ sin θ cos θ − sinh t 1 − 12 sinh2 t . Using the formulas for s and θ from above gives the stated formula for Γ after simplification. 2.2.24 Differentiating γ (t+a) = γ (t) gives t (t+a) = t(a); rotating anti-clockwise by π/2 ns (t + a) = κs (t)n ns (t), gives ns (t + a) = ns (t); differentiating again gives κs (t + a)n so κs (t + a) = κs (t). 17 2.3.1 (i) t = ( 21 (1 + t)1/2 , − 12 (1 − t)1/2 , √12 ) is a unit vector so γ is unit-speed; p ṫt = ( 14 (1 + t)−1/2 , 14 (1 − t)−1/2 , 0), so κ = k ṫt k = 1/ 8(1 − t2 ); n = κ1 ṫt = √12 ((1 − t)1/2 , (1 + t)1/2 , 0); b = t × n = (− 12 (1 + t)1/2 , 21 (1 − t)1/2 , √12 ); p b = (− 14 (1 + t)−1/2 , − 14 (1 − t)−1/2 , 0) so the torsion τ = 1/ 8(1 − t2 ). The ḃ n = −κtt + τn n is easily checked. equation ṅ (ii) t = (− 54 sin t, − cos t, 53 sin t) is a unit vector so γ is unit-speed; ṫt = (− 54 cos t, sin t, 35 cos t), so κ = k ṫt k = 1; n = κ1 ṫt = (− 54 cos t, sin t, 53 cos t); b = 0 and τ = 0. By the proof of Proposition 2.3.5, b = t × n = (− 35 , 0, − 54 ), so ḃ γ is a circle of radius 1/κ = 1 with centre γ + κ1 n = (0, 1, 0) in the plane passing through (0, 1, 0) perpendicular to b = (− 35 , 0, − 54 ), i.e. the plane 3x + 4z = 0. 2.3.2 Let a = κ/(κ2 + τ 2 ), b = τ /(κ2 + τ 2 ). By Examples 2.1.3 and 2.3.2, the circular b a helix with parameters a and b has curvature a2 +b 2 = κ and torsion a2 +b2 = τ . By Theorem 2.3.6, every curve with curvature κ and torsion τ is obtained by applying a direct isometry to this helix. 2.3.3 Differentiating t .aa (= constant) gives n.aa = 0; since t, n, b are an orthonormal b for some scalar µ; since a is a unit vector, µ = ± sin θ; basis of R3 , a = t cos θ+µb differentiating a = t cos θ ± b sin θ gives τ = κ cot θ. Conversely, if τ = λκ, there b sin θ is a constant exists θ with λ = cot θ; differentiating shows that a = t cos θ+b t a t a vector and .a = cos θ so θ is the angle between and . For the circular helix in Example 2.1.3, the angle between the tangent vector dγγ /dθ = (−a sin θ, a cos θ, b) √ −1 2 and the z-axis is the constant cos (b/ a + b2 ). n.(γγ −aa) = 2.3.4 Differentiating (γγ −aa).(γγ −aa) = r 2 repeatedly gives t.(γγ −aa) = 0; t.tt +κn b).(γγ −aa) = κ̇/κ2 , and so b.(γγ −aa) = κ̇/τ κ2 ; 0, so n.(γγ −aa) = −1/κ; n.tt +(−κtt +τb n.(γγ − a ) = (κ̇/τ κ2 )˙, and so τ /κ = (κ̇/τ κ2 )˙. Conversely, if Eq. and finally b.tt − τn (2.22) holds, then ρ = −σ(ρ̇σ)˙, so (ρ2 + (ρ̇σ)2 )˙ = 2ρρ̇ + 2(ρ̇σ)(ρ̇σ)˙ = 0, hence n + ρ̇σb b; then ρ2 + (ρ̇σ)2 is a constant, say r 2 (where r > 0). Let a = γ + ρn a t n t b b n ȧ = + ρ̇n + ρ(−κt + τb) + (ρ̇σ)˙b + (ρ̇σ)(−τn) = 0 using Eq. (2.22); so a is a constant vector and k γ − a k2 = ρ2 + (ρ̇σ)2 = r 2 , hence γ is contained in the sphere with centre a and radius r. Γ = P γ̇γ so T = P t and k Γ̇ Γ k2 = (P γ̇γ )..(P γ̇γ ) = γ̇γ.γ̇γ since P is orthogonal. Then, 2.3.5 Γ̇ Γ = P γ̈γ , taking lengths shows that γ and Γ have the same curvature κ, and then Γ̈ dividing by κ gives N = P n. Then B = P t × P n. If P corresponds to a direct isometry (i.e. a rotation), this is equal to P (tt × n) = P b, but if P corresponds to an opposite isometry, P t × P n = −P b (Proposition A.1.6). vj . The vectors v1 , v2 , v3 are orthonormal if and only if λij = δij 2.3.6 Let λij = vi .v (= 1 if i = j and = 0 if i 6= j). So it is enough to prove that λij = δij vj gives for all values of s given that it holds for s = s0 . Differentiating vi .v P3 λ̇ij = k=1 (aik λkj + ajk λik ). Now λij = δij is a solution of this system of differential equations because aij +aji = 0. But the theory of ordinary differential 18 equations tells us that there is a unique solution with given values when s = s0 . √ √ √ √ 2.3.7 (i) t = γ̇γ = ( √12 sin t 2 cos t 2, √12 ), ṫt = (cos t 2, − sin t 2, 0) so κ = k ṫt k = 1, √ √ b = n so τ = 1. n = ṫt, b = t × n = ( √12 sin t 2, √12 cos t 2, − √12 ). Then, ḃ (ii) t = γ̇γ = (− √13 sin t + √12 cos t, − √13 sin t, − √13 sin t − √12 cos t), so κ = k ṫt k = 1 and n = ṫt. Then b = t × n = (− √1 , √2 , − √1 ) is constant so τ = 0. 6 6 6 1 √ (sinh t, cosh t, 1) 2 2.3.8 Denoting d/dt by a dot, γ̇γ = so k γ̇γ k = cosh t. Hence, the arc-length is s = sinh t, up to adding a constant. The unit tangent vector is 1 t = ds/dt γ̇γ = √12 (tanht, 1, secht) so dtt/dt secht dtt = = √ (sech2 t, 0, −secht tanht) ds ds/dt 2 and κ = k dtt/ds k = √12 sech2 t. Then, n = t × n = √12 (−tanht, 1, −secht). Finally, 1 dt κ ds = (secht, 0, −tanht) and b = b secht db sech2 t 2 √ = (−sech t, 0, secht tanht) = − √ n, ds 2 2 √1 sech2 t. 2 ... 1 γ̇γ = (− t2 + 1, 1, − t12 ),...γ̈γ = ( t23 , 0, t23 ), γ = (− t64 , 0, − t64 ). Hence γ̈γ ... γ ×γ̈γ ). γ 1+t2 γ , and so τ = (γ̇ γ = 0. Alternatively, note that − (1−t) t t γk kγ̇ ×γ̈ so τ = 2.3.9 is parallel to = t + 1 so γ is contained in the plane x − z = y. 2.3.10 We have γ̇γ = (cos(ln t) − sin(ln t), sin(ln t) + cos(ln t), 1), 1 γ̈γ = (− sin(ln t) − cos(ln t), cos(ln t) − sin(ln t), 0), t 1 ∴ γ̇γ × γ̈γ = (sin(ln t) − cos(ln t), − sin(ln t) − cos(ln t), 2), t q γ ×γ̈γ k kγ̇ so κ = kγ̇γ k3 = 1t 29 . 2.3.11 The torsion is defined whenever the curvature is non-zero. In that case k γ̇γ × γ̈γ k > 0 for all t and so is a smooth function of t (compare the proof of Proposition ... γ ×γ̈γ ). γ (γ̇ 1.3.5). Hence, τ = kγ̇γ ×γ̈γ k is smooth. n, so the unit tangent vector of δ 2.3.12 Let a dot denote d/dt. Then, δ̇δ = γ̈γ = κn T/ds = ṅ n/(ds/dt) = is T = n and its arc-length s satisfies ds/dt = κ. Now dT 2 τ τ −1 b) = −tt + κ b. Hence, the curvature of δ is k −tt + κ b k = (1+ κτ 2 )1/2 = κ (−κtt +τb 19 µ, say. The principal normal of δ is N = µ−1 (−tt + κτ b) and its binormal is b + κτ t). The torsion T of δ is given by dB B/ds = −T N , i.e. B = T × N == µ−1 (b −1 B κ Ḃ = −T N . Computing the derivatives and equating coefficients of b gives T = (κτ̇ − τ κ̇)/κ(κ2 + τ 2 ). 2.3.13 The curve is γ (t) = (eλt cos t, eλt sin t, eλt ). The angle between the tangent vectorγ̇γ = eλt (λ cos t − sin t, λ sin t + cos t, λ) and the vector k = (0, 0, 1) is γ̇γ.k cos−1 kγ̇γ k = cos−1 √2λλ2 +1 , which is constant. 2.3.14 We find that 2(9b2 c2 t4 + 9a2 c2 t2 + a2 b2 )1/2 3abc κ= . , τ = 9b2 c2 t4 + 9a2 c2 t2 + a2 b2 (a2 + 4b2 t2 + 9c2 t4 )3/2 Now γ is a generalized helix if and only if there is a constant λ such that τ = λκ, i.e. 3abc(a2 + 4b2 t2 + 9c2 t4 )3/2 = 2λ(9b2 c2 t4 + 9a2 c2 t2 + a2 b2 )3/2 , which is equivalent to (*) 9b2 c2 t4 + 9a2 c2 t2 + a2 b2 = µ(a2 + 4b2 t2 + 9c2 t4 ) where µ = (3abc/2λ)2/3. The last equation holds if and only if 9b2 c2 = 9µc2 , 9a2 c2 = 4µb2 , a2 b2 = µa2 . The first and third equations give µ = b2 and the second gives µ = 9a2 c2 /4b2 . Hence, if γ is a generalized helix 9a2 c2 /4b2 = b2 , which is equivalent to the stated condition. Conversely, if this condition holds, taking µ = b2 (and hence λ = 3ac/2b2 ) satisfies (*) so τ = 3ac 2b2 κ and γ is a generalized helix. n(s), where a is a scalar possibly 2.3.15 (i) From the definition, γ̃γ (s̃) = γ (s) + a(s)n depending on s. Then, n da dn da dγγ ds̃ b. + n+a = (1 − κa)tt + n + τ ab t̃t = ds ds ds ds ds n = ±n n, so t̃t is perpendicular to n. This implies that But we are given that ñ da/ds = 0 and hence a is constant. (ii) We have d ds̃ n = 0, n.t̃t + κ̃tt.ñ (tt.t̃t) = κn ds ds n and hence to n, and similarly t is perpendicular to ñ n. since t̃t is perpendicular to ñ Hence, t.t̃t is a constant, say cos α (it must lie between −1 and 1 as t and t̃t are unit 20 b, vectors). Then, since t is perpendicular to n, we must have t̃t = cos αtt ± sin αb and we can assume the sign is − by changing α to −α if necessary. Then, b = t̃t × ñ n = ±(cos αtt − sin αb b) × n = ±(sin αtt + cos αb b). b̃ (iii) From (i) and (ii), ds̃ b) = (1 − κa)tt + τ ab b. (cos αtt − sin αb ds Equating coefficients of t and b gives the first pair of equations. The second pair follows by interchanging the roles of γ and γ̃γ , which changes α to −α and a to −a. (iv) This follows from the first pair of equations in (iii). (v) The first equation follows from the two equations in (iii) involving the torsion, ds̃ ds = 1. The first equation follows similarly from the other two noting that ds ds̃ equations in (iii). n for any constant a 6= 0. If 2.3.16 Let γ (s) be a unit-speed plane curve, and let γ̃γ = γ +an t̃t = (1 − κa)tt. s̃ is the arc-length of γ̃γ , the unit tangent vector t̃t of γ̃γ is given by ds̃ ds n = ±n n. Hence t̃t = ±tt and so (since γ is planar) ñ 2.3.17 The ‘only if’ part was proved in Exercise 2.3.15(iv). Conversely, if aκ + bτ = 1, n. Then, let γ̃γ = γ + an ds̃ b = τ (btt + ab b). t̃t = (1 − κa)tt + τ ab ds b). Differentiating, Hence, t̃t = ± √a21+b2 (btt + ab n = ±√ κ̃ñ b db κb − τ a ds 1 ds dtt (b + a ) = ± √ n. 2 ds + b ds̃ ds a2 + b2 ds̃ a2 n = ±n n. It follows that ñ n is a Bertrand 2.3.18 The solutions of Exercises 2.3.15 and 2.3.17 show that γ̃γ = γ + an mate of γ (a being a constant) if and only if aκ + bτ = 1 for some constant b, and that such curves γ̃γ are all the Bertrand mates of γ . Thus, γ has more than one Bertrand mate if and only if the equation aκ + bτ = 1 is satisfied by more than one value of a (and some corresponding values of b). In that case κ and τ must be constant, so γ is a circular helix (Exercise 2.3.2). To see that γ̃γ is then a circular helix with the same axis and pitch as γ , take γ to have axis the z-axis (this can be achieved by applying an isometry of R3 ). Then, γ (t) = (c cos λt, c sin λt, dλt), where c is the radius of γ , 2πd is its pitch and λ = (c2 + d2 )−1/2 . Hence, n = (− cos λt, − sin λt, 0) so the most general Bertrand mate of γ is γ̃γ = γ a + n = ((c − a) cos λt, (c − a) sin λt, dλt) , 21 which is a circular helix with axis the z-axis, pitch 2πd and radius |c − a|. 2.3.19 If κ is constant, Eq. (2.22) in Exercise 2.3.4 gives τ = 0, so the curve is a circle (constant curvature and zero torsion). 2.3.20 Let γ (t) be a unit-speed parametrization of C. If all the normal planes of C pass through a point p, there are scalars λ, µ (possibly depending on t) such that n + µb b=p γ + λn for all t. Differentiating and using the Frenet-Serret equations, n + λ(−κtt + τb b) + µ̇b b − µτn n = 0. t + λ̇n Hence, 1 − λκ = 0, λ̇ − µτ = 0, λτ + µ̇ = 0. Using the first and third equations, d 2 (λ + µ2 ) = 2λλ̇ + 2µµ̇ = 2λ(µτ ) + 2µ(−λτ ) = 0, ds p so k γ − p k = λ2 + µ2 is constant. Hence, γ lies on a sphere with centre p. (An alternative is to make use of Exercise 2.3.4.) 2.3.21 (i) is obvious. (ii) Ḟ = γ̇γ .N so Ḟ (t0 ) = 0 if and only if the tangent vector of γ at γ (t0 ) is parallel to Π. Using (i) this gives (ii). n.N, so F̈ (t0 ) = 0 if and only if n(t0 ) is parallel to Π. Thus, (iii) F̈ = γ̈γ.N = κn the unique plane Π such that F (t0 ) = Ḟ (t0 ) = F̈ (t0 ) = 0 is that passing through γ (t0 ) and parallel to t(t0 ) and n(t0 ), i.e. perpendicular to b(t0 ). (iv) If γ is contained in the plane v.N′ = d′ , then γ̇γ .N ′ = γ̈γ .N′ = 0 so by (iii) the osculating plane Π of γ at any point γ (t0 ) is perpendicular to N′ , and so is parallel to Π′ . But both Π and Π′ pass through γ (t0 ), so they must coincide. (v) The (signed) distance from γ (t) to Π is d(t) = (γγ (t) − γ (t0 ))..b(t0 ). Then, d(t0 ) = 0 and ˙ 0 ) = t(t0 )..b(t0 ) = 0, d(t ¨ 0 ) = κ(t0 )n n(t0 )..b(t0 ) = 0, d(t ... n + κ(−κtt + τb b))(t0 )..b(t0 ) = κ(t0 )τ (t0 ). d (t0 ) = (κ̇n If τ (t0 ) 6= 0, Taylor’s theorem gives d(t) = 1 κ(t0 )τ (t0 )(t − t0 )3 + higher order terms. 6 22 As t passes from values < t0 to values > t0 , the leading term changes sign, so γ crosses Π. 2.3.22 For the circular helix γ (t) = (a cos t, a sin t, bt), b = √a21+b2 (b sin t, −b cos t, a), so by Exercise 2.3.21 the osculating plane at γ (t0 ) is (γγ (t) − γ (t0 ))..b(t0 ) = 0, i.e. xb sin t0 − yb cos t0 + az = abt0 . 2.3.23 Proceeding as in the preceding exercise, the osculating plane at γ (t) is found to be 3t2 x − 3ty + z = t3 . If P1 , P2 , P3 correspond to t = t1 , t2 , t3 , the three osculating planes intersect at a single point if and only if the determinant 3t21 3t22 3t23 −3t1 −3t2 −3t3 1 1 6= 0. 1 But the determinant equals 9(t1 −t2 )(t2 −t3 )(t3 −t1 ), and this is indeed non-zero as t1 , t2 , t3 are distinct. If Q is the point (X, Y, Z), then t1 , t2 , t3 are the roots of t3 − 3t2 X + 3tY − Z = 0. On the other hand, if the plane Π passing through the points γ (t1 ), γ (t2 ) and γ (t3 ) has equation ax + by + cz + d = 0, then t1 , t2 , t3 are also the roots of at + bt2 + ct3 + d = 0. The two cubic equations must be the same, so Π must be the plane 3Y x − 3Xy + z = Z, and the point (X, Y, Z) obviously lies on this plane. 2.3.24 We can assume that γ is unit-speed. If all the osculating planes pass through a point p, there are scalars λ, µ such that n = p. γ + λtt + µn Proceeding as in Exercise 2.3.20 we find that µτ = 0, λ̇ − µκ = −1, λκ + µ̇ = 0. 23 If µ = 0 the third equation gives λ = 0, which contradicts the second equation. So µ 6= 0 and the first equation gives τ = 0, i.e. γ is planar. 2.3.25 Let γ be a unit-speed curve. Its orthogonal projection onto the normal plane at γ (t0 ) is Γ = γ − (γγ .t(t0 ))tt(t0 ). Then, Γ = t − (tt.t (t0 ))tt(t0 ) = 0 Γ̇ if t = t0 . Hence, Γ has a singular point at t = t0 . Similarly, we find that ... Γ(t0 ) = κ(t0 )n n(t0 ), Γ (t0 ) = κ̇(t0 )n n(t0 ) + κ(t0 )τ (t0 )tt(t0 ). Γ̈ These vectors are linearly independent if κ(t0 ) and τ (t0 ) are non-zero, so in that case Γ has an ordinary cusp at t = t0 . The orthogonal projection of γ onto its osculating plane at γ (t0 ) is Γ = γ − (γγ.b(t0 ))b b(t0 ), Γ̃ so ˙ Γ(t0 ) = t(t0 ) − (tt(t0 )..b(t0 ))b b(t0 ) = t(t0 ) 6= 0, Γ̃ Γ. so γ (t0 ) is a regular point of Γ̃ 2.3.26 (i) is obvious. (ii) Ḟ = 4tt.(γγ − c) so Ḟ (t0 ) = 0 if and only if t(t0 ) is perpendicular to γ (t0 ) − c, i.e. γ is tangent to S at γ (t0 ). Next, ... n.(γγ − c) + 2, F = 2κ̇n n.(γγ − c) + 2κ(−κtt + τb b)..(γγ − c). F̈ = 2κn ... Hence, F (t0 ) = Ḟ (t0 ) = F̈ (t0 ) = F (t0 ) = 0 if and only if γ is tangent to S at γ (t0 ) and κ̇ n. (γγ − c) = −1, κτb b.(γγ − c) = κn κ (all quantities evaluated at t = t0 ). These equations and the fact that γ (t0 ) − c is perpendicular to t(t0 ) are equivalent to 1 κ̇ γ − c = − n + 2 b, κ κ τ so the centre c of S is uniquely determined and its radius is R =k γ −c k= r 1 κ̇2 + κ2 κ4 τ 2 24 (again, all quantities evaluated at t = t0 ). The centre c is independent of t0 if and only if d 1 κ̇ γ+ n− 2 b =0 dt κ κ τ when t = t0 . Using Frenet-Serret, the derivative is found to be κ̇ d τ b. − κ dt κ2 τ By Exercise 2.3.4, c is independent of t0 if and only if γ is spherical, in which case the solution of Exercise 2.3.4 shows that γ lies on the sphere with centre c and radius R, i.e. the osculating sphere. 2.3.27 Since b(t0 ) is perpendicular to the osculating plane at γ (t0 ), the centre of the b(t0 ) for some scalar λ. As this osculating circle will be of the form c′ = c(t0 ) + λb n(t0 ) point lies on the osculating plane, it must be of the form γ (t0 ) + µtt(t0 ) + νn for some µ, ν. Hence, γ+ κ̇ 1 b = γ + µtt + νn n, n − 2 b + λb κ κ τ all quantities being evaluated at t = t0 . So λ = osculating circle is b(t0 ) = γ (t0 ) + c(t0 ) + λb κ̇ κ2 τ and the centre of the 1 n(t0 ). κ(t0 ) If R is the radius of the osculating sphere, the radius r of the osculating circle is given by κ̇2 1 1 2 2 ′ 2 c c r = R − k − k = 2 + 4 2 − λ2 = 2 , κ κ τ κ so r = 1/κ(t0 ). Chapter 3 3.1.1 γ̇γ = (− sin t − a sin 2t, cos t + a cos 2t), k γ̇γ k2 = 1 + a2 + 2a cos t ≥ 1 + a2 − 2|a| = (1 − |a|)2 so γ is regular if |a| = 6 1. If |a| = 1 then k γ̇γ k = 2(1 + a cos t) so the origin is a singular point of γ . If a = 0 then γ is a circle. If 0 < |a| < 1, then γ (t1 ) = γ (t2 ) =⇒ 1 + a cos t1 = 1 + a cos t2 =⇒ cos t1 = cos t2 =⇒ t2 = t1 or 2π − t1 . In the latter case, γ (t2 ) = ((1 + a cos t1 ) cos t1 , −(1 + a cos t1 ) sin t1 ) so γ (t1 ) = γ (t2 ) =⇒ sin t1 = 0 =⇒ t1 = 0 or π. In all cases, t2 − t1 is a multiple of 2π, so γ is a closed curve with period 2π without self-intersections. If |a| > 1, γ passes through the origin when cos t = −1/a, which has two roots 25 with 0 ≤ t < 2π, say t1 < t2 , so the origin is a self-intersection. The picture is qualitatively similar to that in Example 1.1.7 (which is the case a = 2), so the complement of the image of γ is the union of two bounded regions enclosed by the part of the curve with t1 ≤ t ≤ t2 , and an unbounded region. 3.1.2 γ̇γ = (− sin t − 2a sin t cos t, cos t + a(cos2 t − sin2 t)) so cos t + a cos 2t , sin t + a sin 2t dϕ 1 + 3a cos t + 2a2 ∴ sec2 t = , dt (sin t + a sin 2t)2 dϕ 1 + 3a cos t + 2a2 a(cos t + a) = =1+ . 2 dt 1 + 2a cos t + a 1 + 2a cos t + a2 tan ϕ = − ∴ If |a| < 1, γ is a simple closed curve of period 2π (Exercise 3.1.1), so by the Umlaufsatz, Z 2π dϕ dt = 2π, dt 0 giving Z 2π 0 a(cos t + a) dt = 0. 1 + 2a cos t + a2 If |a| > 1, it is clear geometrically that the tangent vector of γ rotates by 4π on going once around γ (see the diagram in Example 1.1.7 for the case a = 2), so Z giving Z 0 2π 2π 0 dϕ dt = 4π, dt a(cos t + a) dt = 2π. 1 + 2a cos t + a2 v) = P v +b b, where P is a 3.2.1 By Appendix 1, any isometry M of R2 is of the form M (v 3×3 orthogonal matrix and b is a constant vector. If γ̃γ = M (γγ ), then γ̃γ˙ = P γ̇γ , so k γ̃γ˙ k = k γ̇γ k, which implies that γ and γ̃γ have the same length. If we think of γ RT as a curve in the xy-plane in R3 , Eq. (3.2) can be written A(γγ ) = 0 (γ̇γ × γ̈γ )..k dt, where k = (0, 0, 1). It now follows from Proposition A.1.6 that γ and γ̃γ have the same area (note that if M is opposite, the area appears to change sign, but it does not because in that case γ̃γ is negatively-oriented when γ is positively-oriented). 3.2.2 Parametrizing the ellipse by γ (t) = (p cos t, q sin t), with 0 ≤ t ≤ 2π, its area is R 2π p √ 2 pq sin t + pq cos2 t dt = 2π pq. By the isoperimetric inequality, the length 0 √ √ ℓ of the ellipse satisfies ℓ ≥ 4π × πpq = 2π pq, with equality if and only 26 if the ellipse is a circle, i.e. R 2π p p2 sin2 t + q 2 cos2 t dt. 0 p = q. But its length is R 2π 0 k γ̇γ k dt = 3.2.3 γ (t′ ) = γ (t) ⇐⇒ cos t′ = cos t and sin t′ = sin t ⇐⇒ t′ − t is a multiple of 2π, so γ is simple closed with period 2π. Taking x = p cos t, y = q sin t in Eq. 3.2 gives R 1 2π the area as 2 0 pq dt = πpq. 3.3.1 Let (x1 , y1 ) and (x2 , y2 ) be points in the interior of the ellipse, so that for i = 1, 2. A point of the line segment joining the two points is x2i p2 y2 + qi2 < 1 (tx1 + (1 − t)x2 , ty1 + (1 − t)y2 ) for some 0 ≤ t ≤ 1. This is in the interior of the ellipse because (ty1 + (1 − t)y2 )2 (tx1 + (1 − t)x2 )2 + p2 q2 2 x1 x22 y12 y22 y1 y2 x1 x2 2 2 =t + 2 + (1 − t) + 2 + 2t(1 − t) + 2 p2 q p2 q p2 q 2 2 2 2 y x y x1 + 12 + 22 + 22 ≤ t2 + (1 − t)2 + 2t(1 − t) = 1. < t2 + (1 − t)2 + t(1 − t) 2 p q p q √ 3.3.2 γ̇γ = (− sin t − 2 sin 2t, cos t + 2 cos 2t) and k γ̇γ k = 5 + 4 cos t, so the angle ϕ sin t−2 sin 2t √ t+2 cos 2t . between γ̇γ and the x-axis is given by cos ϕ = − √ , sin ϕ = cos 5+4 cos t 5+4 cos t Differentiating the second equation gives ϕ̇ cos ϕ = ϕ̇ = 2 sin t(24 cos t+42 cos t+9) (5+4 cos t)(sin t+2 sin 2t) = 9+6 cos t . 5+4 cos t − sin t(24 cos2 t+42 cos t+9) , (5+4 cos t)3/2 so Hence, if s is the arc-length of γ , κs = dϕ/ds = (dϕ/dt)/(ds/dt) = (9 + 6 cos t)/(5 + 4 cos t)3/2 , so κ̇s = 12 sin t(2 + cos t) . (5 + 4 cos t)5/2 This vanishes at only two points of the curve, where t = 0 and t = π. 3.3.3 From ǫ(s) = γ (s) + κ1s ns we get ǫ̇ǫ = −κ̇s ns /κ2s , so ǫ has a singular point where κ̇s = 0, i.e. where γ has a vertex. 3.3.4 Parametrize by q γ (x) = (x, f (x)) and denote d/dx by a dot. The arc-length s is ds given by dx = 1 + f˙2 , so the unit tangent vector is t = √ 1 ˙2 (1, f˙) and we 1+f find that 1 1 dtt (−f˙f¨, f¨). = ṫt = ds ds/dx (1 + f˙2 )2 27 The signed unit normal ns = √ f¨ . (1+f˙2 )3/2 Then, 1 (−f˙, 1), 1+f˙2 so the signed curvature is κs = ... f (1 + f˙2 ) − 3f˙f¨2 . κ̇s = (1 + f˙2 )5/2 ... = 0 ⇐⇒ f (1 + f˙2 ) = 3f˙f¨2 . dκs s Hence, dκ ds = 0 ⇐⇒ dx 3.3.5 γ̇γ = (a − b cos t, b sin t), so if ϕ is a turning angle for γ , b sin t , a − b cos t b(a cos t − b) ∴ ϕ̇ sec2 ϕ = , (a − b cos t)2 (a − b cos t)2 b(a cos t − b) b(a cos t − b) . ϕ̇ = = 2 2 2 (a − b cos t) (a − b cos t)2 + b2 sin t a − 2ab cos t + b2 tan ϕ = ∴ If s is the arc-length of γ , the signed curvature is κs = Hence, dϕ dϕ/dt ϕ̇ b(a cos t − b) = = = 2 . ds ds/dt k γ̇γ k (a − 2ab cos t + b2 )3/2 ab sin t(2b2 − a2 − ab sin t cos t) dκs . = dt (a2 − 2ab cos t + b2 )5/2 Thus, γ (t) is a vertex if and only if sin t = 0 or cos t = 2b2 −a2 ab . Hence, there are vertices when t is an integer multiple of π, and no other vertices if On the other hand, if 2b2 −a2 ab ≤ 1, i.e. if many values of t such that cos t = points on the curve. 2 2 2b −a ab a−b b ≤ 2b a ≤ a+b , b 2b2 −a2 ab > 1. there are infinitely- , and these all correspond to different Chapter 4 4.1.1 Let U be an open disc in R2 and S = {(x, y, z) ∈ R3 | (x, y) ∈ U, z = 0}. If W = {(x, y, z) ∈ R3 | (x, y) ∈ U }, then W is an open subset of R3 , and S ∩ W is homeomorphic to U by (x, y, 0) 7→ (x, y). So S is a surface. 4.1.2 The image of σ x± is the intersection of the sphere with the open set ±x > 0 in R3 , and its inverse is the projection (x, y, z) 7→ (y, z). Similarly for σ y± and σ z± . A point of the sphere not in the image of any of the six patches would have to have x, y and z all zero, which is impossible. 28 4.1.3 Multiplying the two equations gives (x2 − z 2 ) sin θ cos θ = (1 − y 2 ) sin θ cos θ, so x2 + y 2 − z 2 = 1 unless cos θ = 0 or sin θ = 0; if cos θ = 0, then x = −z and y = 1 and if sin θ = 0 then x = z and y = −1, and both of these lines are also contained in the surface. The given line Lθ passes through (sin 2θ, − cos 2θ, 0) and is parallel to the vector (cos 2θ, sin 2θ, 1); it follows that we get all of the lines by taking 0 ≤ θ < π. Let (x, y, z) be a point of the surface; if x 6= z, let θ be such that cot θ = (1 − y)/(x − z); then (x, y, z) is on Lθ ; similarly if x 6= −z. The only remaining cases are the points (0, 0, ±1), which lie on the lines Lπ/2 and L0 . To get a surface patch covering S, define σ : U → R3 by σ (u, v) = (sin 2θ, − cos 2θ, 0) + t(cos 2θ, sin 2θ, 1). By the preceding paragraph, this patch covers the whole surface. Let Mϕ be the line (x−z) cos ϕ = (1+y) sin ϕ, (x+z) sin ϕ = (1−y) cos ϕ. By the same argument as above, Mϕ is contained in the surface and every point of the surface lies on some Mϕ with 0 ≤ ϕ < π. If θ + ϕ is not a multiple of π, the lines sin(θ−ϕ) cos(θ+ϕ) Lθ and Mϕ intersect in the point ( cos(θ−ϕ) sin(θ+ϕ) , sin(θ+ϕ) , sin(θ+ϕ) ); for each θ with 0 ≤ θ < π, there is exactly one ϕ with 0 ≤ ϕ < π such that θ + ϕ is a multiple of π, and the lines Lθ and Mϕ do not intersect. If (x, y, z) lies on both Lθ and Lϕ , with θ 6= ϕ, then (1 − y) tan θ = (1 − y) tan ϕ and (1 + y) cot θ = (1 − y) cot ϕ, which gives both y = 1 and y = −1 (the case in which θ = 0 and ϕ = π/2, or vice versa, has to be treated separately, but the conclusion is the same). This shows that Lθ and Lϕ do not intersect; similarly, Mθ and Mϕ do not intersect. √ 4.1.4 For the first part, let U = {(u, v) ∈ R2 | 0 < u2 + v 2 < π 2 }, let r = u2 + v 2 , and define σ : U → R3 by σ (u, v) = ( ur , vr , tan(r − π2 )). If S 2 could be covered by a single surface patch σ : U → R3 , then S 2 would be homeomorphic to the open subset U of R2 . As S 2 is a closed and bounded subset of R3 , it is compact. Hence, U would be compact, and hence closed. But, since R2 is connected, the only non-empty subset of R2 that is both open and closed is R2 itself, and this is not compact as it is not bounded. σ α : Uα → R3 } is an atlas for a surface S, and if W is an open subset of R3 , 4.1.5 If {σ σ |Uα ∩σ −1 } form an atlas of S ∩ W (one should discard then the restrictions {σ α (W ) −1 the restrictions for which Uα ∩ σ α (W ) is empty). 4.1.6 Parametrize the curve by γ (t) = (cos θ, sin θ, z) where θ and z are smooth functions of t, and assume that γ is unit-speed. Then, γ̇γ = (−θ̇ sin θ, θ̇ cos θ, ż) so γ interescts the rulings of the cylinder at a constant angle if and only if ż is constant, i.e. z = at + b for some constant a, b. Since γ is unit-speed, θ̇ 2 + ż 2 = 1 so θ̇ is a constant c such that a2 + c2 = 1 and θ = ct + d where d is a constant. Then, γ (t) = (cos(ct + d), sin(ct + d), at + b). This is a circle if a = 0, a straight line if c = 0 and a circular helix in all other cases. 29 4.1.7 Noting that (x, y, z) lies on the ellipsoid if and only if ( xp , yq , zq ) ∈ S 2 , we can use the latitude-longitude parametrization of S 2 to get the parametrization σ (θ, ϕ) = (p cos θ cos ϕ, q cos θ sin ϕ, r sin θ) of the ellipsoid. σ is continuous and is a homeomorphism onto its image if (θ, ϕ) is restricted in the same way as for S 2 (Example 4.1.4). 4.1.8 If x = sin u, y = sin v and z = sin(u + v), then x2 − y 2 + z 2 = sin2 u − sin2 v + sin2 (u + v) = sin2 u − sin2 v + sin2 u cos2 v + cos2 u sin2 v + 2 sin u sin v cos u cos v = sin2 u + sin2 u cos2 v − sin2 v(1 − cos2 u) + 2 sin u sin v cos u cos v = (1 − sin2 v) sin2 u + sin2 u cos2 v + 2 sin u sin v cos u cos v = 2 sin2 u cos2 v + 2 sin u sin v cos u cos v = 2 sin u cos v(sin u cos v + cos u sin v) = 2 sin u cos v sin(u + v). Hence, (x2 − y 2 + z 2 )2 = 4 sin2 u(1 − sin2 v) sin2 (u + v) = 4x2 (1 − y 2 )z 2 . Now, σ is clearly continuous, as is its inverse map (x, y, z) 7→ (sin−1 x, sin−1 y), so σ is a homeomorphism. 4.2.1 σ is obviously smooth and σ u × σ v = (−fu , −fv , 1) is nowhere zero, so σ is regular. √ √ 4.2.2 σ z± is a special case of Exercise 4.2.1, with f = ± 1 − u2 − v 2 ( 1 − u2 − v 2 is smooth because 1 − u2 − v 2 > 0 if (u, v) ∈ U ); similarly for the other patches. The transition map from σ x+ to σ y+ , for example, is Φ(ũ, ṽ) = (u, v), where √ σ y+ (ũ, ṽ) = σ x+ (u, v); so u = 1 − ũ2 − ṽ 2 , v = ṽ, and this is smooth since 1 − ũ2 − ṽ 2 > 0 if (ũ, ṽ) ∈ U . σ v = (−v, −u, 1) 4.2.3 (i) is clearly injective and is regular because σ is smooth and σ u ×σ is never zero. (ii) is injective but is not regular since σ u × σ v = (0, −3v 2 , 2v) vanishes when v = 0. σ (−u − 1, v) and is also not regular since (iii) is not injective because σ (u, v) = (σ σ u × σ v = (0, 2v(1 + 2u), 1 + 2u) vanishes when u = −1/2. 4.2.4 This is similar to Example 4.1.4, but using the ‘latitude-longitude’ patch σ (θ, ϕ) = (p cos θ cos ϕ, q cos θ sin ϕ, r sin θ). 4.2.5 A typical point on the circle C has coordinates (a+b cos θ, 0, b sin θ); rotating this about the z-axis through an angle ϕ gives the point σ (θ, ϕ); the torus is covered 30 by the four patches obtained by taking (θ, ϕ) to lie in one of the following open sets: (i) 0 < θ < 2π, 0 < ϕ < 2π; (ii) 0 < θ < 2π, −π < ϕ < π; (iii) −π < θ < π, 0 < ϕ < 2π; (iv) −π < θ < π, −π < ϕ < π. Each patch is regular because σ θ × σ ϕ = −b(a + b cos θ)(cos θ cos ϕ, cos θ sin ϕ, sin θ) is never zero (since k σ u × σ v k = b(a + b cos θ) ≥ b(a − b) > 0). 4.2.6 Suppose the centre of the propeller is initially at the origin. At time t, the centre is at (0, 0, αt) where α is the speed of the aeroplane. If the propeller is initially along the x-axis, the point initially at (v, 0, 0) is therefore at the point (v cos ωt, v sin ωt, αt) at time t, where ω is the angular velocity of the propeller. Let u = ωt, λ = α/ω. Next, σ u = (−v sin u, v cos u, λ), σ v = (cos u, sin u, 0), so the standard unit normal is N = (λ2 + v 2 )−1/2 (−λ sin u, λ cos u, −v). If θ is the angle between N and the z-axis, cos θ = −v/(λ2 +v 2 )1/2 and hence cot θ = ±v/λ, while the distance from the z-axis is v. 4.2.7 σ is the tube swept out by a circle of radius a in a plane perpendicular to n + τ a cos θb b, γ as its centre moves along γ . σ s = (1 − κa cos θ)tt − τ a sin θn n + a cos θb b, giving σ s × σ θ = −a(1 − κa cos θ)(cos θn n + sin θb b); σ θ = −a sin θn this is never zero since κa < 1 implies that 1 − κa cos θ > 0 for all θ. The first fundamental form is ((1 − κa cos θ)2 + τ 2 a2 ) ds2 + 2τ a2 dsdθ + a2 dθ 2 , so the area R s R 2π is s01 0 a(1 − κa cos θ)dsdθ = 2πa(s1 − s0 ). σ = σ + a , where a is a constant vector, then σ̃ σ is smooth if σ is smooth, and 4.2.8 If σ̃ σ u = σ u , σ̃ σ v = σ v , so σ̃ σ is regular if σ is regular. If A is an invertible 3 × 3 σ̃ σ σ σ is smooth if σ is smooth and σ̃ σ u = Aσ σ u , σ̃ σ v = Aσ σv , matrix and σ̃ = Aσ , then σ̃ σ u and σ̃ σ v are linearly independent if σ u and σ v are so since A is invertible σ̃ linearly independent. 4.2.9 See Exercise 4.1.5. The restriction of a smooth map U → R2 , where U is an open subset of R2 , to an open subset of U is smooth. 4.2.10 The map σ is a diffeomorphism, since it is smooth, obviously bijective, and has smooth inverse (x, y, z) 7→ (x, y). 4.2.11 We find that σ u × σ v = (− cos v cos(u + v), − cos u cos(u + v), cos u cos v). This is non-zero when −π/2 < u, v < π/2 since cos u and cos v are non-zero in this range. 4.2.12 The torus is covered by the patches σ : Un → R3 , n = 1, 2, 3, where σ is as in 31 the question and U1 = {(θ, ϕ) | 0 < θ < 2π, 0 < ϕ < 2π}, 2π 4π 4π U2 = (θ, ϕ) | − <θ< ,− <ϕ< 3 3 3 2π 2π 4π <θ< ,− <ϕ< U3 = (θ, ϕ) | − 3 3 3 2π , 3 4π . 3 Suppose for a contradiction that the torus is covered by two patches σ : V → R3 and σ : V ′ → R3 , where σ is as before and V, V ′ are open subsets of R2 . We might as well assume that V = {(θ, ϕ) | α < θ < α + 2π, β < ϕ < β + 2π}, V ′ = {(θ, ϕ) | α′ < θ < α′ + 2π, β ′ < ϕ < β ′ + 2π}, for some α, α′ , β, β ′ ∈ R. But neither of the patches σ : V → R3 or σ : V ′ → R3 contains the point σ (α′ , β) (for example). 4.2.13 Taking f = 3xy − z(z + 4) + c, we have ∇ f = (3y, 3x, −2z − 4) which is zero only at the point (0, 0, −2). But f (0, 0, −2) = 0 only if c = −4. So if c 6= −4, f = 0 is a smooth surface. 4.2.14 Taking f = x3 + 3(y 2 + z 2 )2 − 2, we have ∇f = (3x2 , 12y(y 2 + z 2 ), 12z(y 2 + z 2 )) which is zero only at the origin. But f (0, 0, 0) 6= 0, so f = 0 is a smooth surface. 4.2.15 Take f = x2/3 + y 2/3 + z 2/3 = 1. Not that f is smooth provided x, y and z are never zero, i.e. if we exclude the points on the coordinate planes. Then ∇ f = ( 23 x−1/3 , 32 y −1/3 , 23 z −1/3 ) which is non-zero. 4.2.16 If xyz = 1 then x, y and z are all non-zero. By the intermediate value theorem, a smooth (or even just continuous) curve on the surface cannot connect a point with x > 0 (for example) to a point with x < 0 (as it would have to pass through a point with x = 0). Thus, two points in the same connected piece of the surface must have x-coordinates of the same sign (and similarly for their yand z-coordinates). Note that the sign of any two of the coordinates determines that of the third, since xyz = 1. Consider the piece with x, y and z all > 0. This can be parametrized using the single patch σ (u, v) = (u, v, 1/uv), defined on the open set {(u, v) | u > 0, v > 0}. It is clear that σ is smooth and injective. 4.2.17 Consider the circular helix γ (θ) = (a cos θ, a sin θ, bθ). The mid-point of the chord joining γ (θ) and γ (ϕ) is the point 1 1 1 a(cos θ + cos ϕ), a(sin θ + sin ϕ), b(θ + ϕ) = (v cos u, v sin u, bu), 2 2 2 32 where u = 12 (θ + ϕ), v = a cos 12 (θ − ϕ). Hence, the set of mid-points of the chords of the helix is the subset of the helicoid in Exercise 4.2.6 with λ = b given by |v| ≤ |a|. 4.3.1 If S is covered by a single surface patch σ : U → R3 , then f : S → R is smooth σ : Ũ → R3 is if and only if f ◦ σ : U → R is smooth. We must check that, if σ̃ σ is smooth if and only if f ◦ σ is smooth. another patch covering S, then f ◦ σ̃ σ = (f ◦ σ ) ◦ Φ, where Φ is the transition map from σ to This is true because f ◦ σ̃ σ , and both Φ and Φ−1 are smooth. The last part is true because if σ : U → R3 σ̃ is a smooth map, where U is an open subset of R2 , then each component of σ (which is a map U → R) is smooth (this is because a vector function such as σ is differentiated ‘componentwise’). 4.3.2 f is not a diffeomorphism as it is not injective: f (0, y, z) = f (0, y, z + 2π). Take an atlas for the cone consisting of the patches σ (u, v) = (u cos v, u sin v, u), defined on the open sets U1 = {(u, v)|u > 0, 0 < v < 2π} and U2 = {(u, v)|u > 0, −π < v < π} (call these σ 1 and σ 2 ), and parametrize the half-plane by π (u, v) = (0, u, v) with u > 0. If (0, a, b) is any point in the plane, assume first that b is not an even multiple of π, say 2nπ < b < 2(n + 1)π for some integer n. Then, π(u, v)) = σ 1 (u, v − 2nπ) if 2nπ < v < 2(n + 1)π. So f is a diffeomorphism f (π from the open subset {(0, y, z)|2nπ < z < 2(n + 1)π} of the half-plane to the cone with the half-line y = 0, x = z > 0 removed. Similarly if b is not an odd multiple of π. This proves that f is a local diffeomorphism. 4.4.1 (i) At (1, 1, 0), σ u = (1, 0, 2), σ v = (0, 1, −2) so σ u × σ v = (−2, 2, 1) and the tangent plane is −2x + 2y + z = 0. (ii) At (1, 0, 1), where r = 1, θ = 0, σ r = (1, 0, 2), σ θ = (0, 1, 2) so σ r × σ θ = (−2, −2, 1) and the equation of the tangent plane is −2x − 2y + z = 0. σ (ũ, ṽ) be a reparametrization of σ . Then, 4.4.2 Let σ̃ σu = ∂ṽ ∂ṽ ∂ ũ ∂ ũ σ ũ + σ ṽ , σ v = σ ũ + σ ṽ , σ̃ σ̃ σ̃ σ̃ ∂u ∂u ∂v ∂v σ ũ and σ̃ σ ṽ . Hence, any linear combination so σ u and σ v are linear combinations of σ̃ σ ũ and σ̃ σ ṽ . The converse is also true of σ u and σ v is a linear combination of σ̃ σ σ since is a reparametrization of σ̃ . d F (γγ (t)) = Fx ẋ + Fy ẏ + Fz ż = ∇F .γ̇γ . Since 4.4.3 If γ (t) = (x(t), y(t), z(t)) then dt ∇ S F − ∇F is perpendicular to Tp S, it is perpendicular to γ̇γ (t0 ) for every curve γ on S passing through p when t = t0 . It follows that ∇S F .γ̇γ = ∇F .γ̇γ at p. If the restriction of F to S has a local maximum or a local minimum at p, so does 33 d F (γγ (t)) = 0 at p, which F (γγ (t)) for all curves γ on S passing through p, hence dt implies that ∇F is perpendicular to γ̇γ , and hence perpendicular to the tangent plane of S at p. This means that ∇S F = 0. 4.4.4 d(f ◦ γ )/dt) = Dγ (t) f (γ̇γ (t)) is non-zero because γ̇γ is non-zero (γγ is regular) and Dγ (t) f is invertible (Proposition 4.4.6). √ √ 4.4.5 We find that, at θ = ϕ = π/4, σ θ = 21 b(−1, −1, 2), σ ϕ = 21 (a 2 + b)(−1, 1, 0), so the unit normal of the torus at this point is parallel to √ √ √ (−1, −1, 2) × (−1, 1, 0) = − 2(1, 1, 2). Hence, the tangent plane is x + y + √ 2z = 0. 4.5.1 The transition map Φ(t, θ) = (t̃, θ̃) is defined on the union of the rectangles given by 0 < θ < π and π < θ < 2π (and −1/2 < t < 1/2). Obviously Φ(t, θ) = (t, θ) if 0 < θ < π. If π < θ < 2π, we must have θ̃ = θ − 2π. Since sin θ̃2 = − sin θ2 , σ (t̃, θ̃) forces t̃ = −t. So Φ(t, θ) = (t, θ) if 0 < θ < π, cos 2θ̃ = − cos θ2 , σ (t, θ) = σ̃ and = (−t, θ − 2π) if π < θ < 2π. The Jacobian determinant is +1 on the first rectangle, −1 on the second. σ α : Uα → R3 } be an atlas for S such that the transition map Φαβ between 4.5.2 Let {σ σ α and σ β satisfies det(J(Φαβ )) > 0 for all α, β (Definition 4.5.1). By Proposition 4.3.1, {f ◦ σ α } is an atlas for S̃, and the transition maps for this atlas are the same as those for the atlas of S, because (f ◦ σ β )−1 ◦ (f ◦ σ α ) = σ −1 β ◦ σα (where this composite is defined). So the atlas {f ◦ σ α } gives S̃ the structure of an oriented surface. σ (θ, ϕ). 4.5.3 If σ (θ, ϕ) = (cos θ cos ϕ, cos θ sin ϕ, sin θ), we find that σ θ × σ ϕ = − cos θσ Hence, the standard unit normal points inwards if cos θ > 0 (if −π/2 < θ < π/2, for example) and outwards of cos θ < 0. Note that the points at which cos θ = 0 (i.e. the north and south pole) must be excluded for σ to be regular. σ x± )u ×(σ σ x± )v = ± √1−u12 −v 2 σ x± , so For the patches σ x± , for example, we find that (σ the standard unit normal of σ x+ points outwards and that of σ x− points inwards. v. 4.5.4 Apply the proof of Proposition 2.2.1 with f = γ̇γ .v, g = γ̇γ.ṽ 4.5.5 From σ ∗ = σσ.σ , we get σ ∗u = σ.σ )σ σ u − 2(σ σ u.σ )σ σ (σ , 4 kσ k 34 with a similar formula for σ ∗v . This gives 1 2 σ σ σ σ σ σ k σ k (σ × σ ) − 2σ × ((σ . σ )σ − (σ . σ )σ ) u v u v v u k σ k6 1 2 σ σ σ σ k σ k (σ × σ ) + 2σ × (σ × (σ × σ )) = u v u v k σ k6 1 σ.(σ σ u × σ v ))σ σ − k σ k2 (σ σu × σ v ) 2(σ = 6 kσ k σ .N)σ σ k σ u × σ v k 2(σ −N . = k σ k4 k σ k2 σ ∗u × σ ∗v = .N )σ − N is a unit vector. But its squared Hence, it suffices to show that 2(σ kσ k2 length is σ. N ) 2 σ.N )2 4(σ 4(σ − + k N k2 = 1. k σ k2 k σ k2 Chapter 5 5.1.1 (i) fx = 2x, fy = 2y and fz = 4z 3 vanish simultaneously only when x = y = z = 0, but this does not satisfy x2 + y 2 + z 4 = 1. So by Theorem 5.1.1 this is a smooth surface. (ii) Let f (x, y, z) be the left-hand side minus the right-hand side; then, fx = 4x(x2 + y 2 + z 2 − a2 − b2 ), fy = 4y(x2 + y 2 + z 2 − a2 − b2 ), fz = 4z(x2 + y 2 + z 2 + a2 − b2 ); if fz = 0 then z = 0 since x2 + y 2 + z 2 + a2 − b2 > 0 everywhere on the torus; if fx = fy = 0 too, then since the origin is not on the torus, we must have x2 + y 2 = a2 + b2 , but then substituting into the equation of the torus gives (2a2 )2 = 4a2 (a2 + b2 ), a contradiction. For the last part, let σ (θ, ϕ) = (x, y, z) be the parametrization in Exercise 4.2.5. Then, x2 + y 2 + z 2 + a2 − b2 = 2a(a + b cos θ), so (x2 + y 2 + z 2 + a2 − b2 )2 = 4a2 (a + b cos θ)2 = 4a2 (x2 + y 2 ). p Conversely, if (x, y, z) satisfies the given equation, let r = x2 + y 2 . A little algebra gives (r 2 + z 2 − a2 − b2 )2 = 4a2 (b2 − z 2 ). Hence, |z| ≤ b so z = b sin θ for some θ ∈ R. Then we find r 2 = a2 + b2 cos2 θ ± 2ab cos θ, so (since r ≥ 0) r = a ± b cos θ. With the plus sign (x, y, z) = σ (θ, ϕ) for some ϕ ∈ R; with the 35 minus sign, (x, y, z) = σ (π − θ, ϕ) for some ϕ. Thus, the image of σ : R2 → R3 coincides with the set of solutions to the given equation. 5.1.2 See the solution of Exercise 4.4.3 for the first part. Since S has a (smooth) choice of unit normal ∇ f k ∇f k at each point, it is orientable. The solution of Exercise 4.4.3 also shows that if the restriction of F to S has a local maximum or a local minimum at p, then ∇ F is perpendicular to the tangent plane of S at p. But ∇ f is also perpendicular to the tangent plane. Hence, if the restriction of F to S has a local maximum or a local minimum at p, then ∇F is parallel to ∇f for some scalar λ. ∇ f at p, i.e. ∇ F = λ∇ 5.1.3 Let f (x, y, z) = xyz − 1, F (x, y, z) = x2 + y 2 + z 2 . Then, f = 0 is a smooth surface S by Theorem 5.1.1 and F defines a smooth function on S. To see that F has a smallest value on S, let B be the closed ball given by x2 + y 2 + z 2 ≤ 3. Then, B ∩ S is compact as it is closed and bounded and it is non-empty because it contains the point (1, 1, 1). Hence, the continuous positive function F must attain its lower bound, say ℓ, on B ∩ S, and ℓ ≤ 3 since F (1, 1, 1) = 3. Obviously F (x, y, z) > 3 if (x, y, z) ∈ / B, so ℓ is the smallest value of F on S. By Exercise 5.1.2, the local maxima or minima of F on S occur where (2x, 2y, 2z) = λ(yz, xz, xy) for some λ. Since xyz = 1 on S this gives x2 = y 2 = z 2 = λ/2, so x, y, z are equal up to sign. Since their product is 1, there are four possibilities: (x, y, z) = (1, 1, 1), (1, −1, −1), (−1, 1, −1) or (−1, −1, 1). The value of F is 3 at each of these points, which is the smallest value of F on S√from above. The distance between any two of these points of R3 is the same (2 2), so they form the vertices of a regular tetrahedron. 5.2.1 (i) (p cos u cos q v, q cos u sin v, r sin u) (cf. Exercise 4.2.4); (ii) see Exercise 4.1.3; (iii) (u, v, ± 1 + u2 p2 + v2 ); q2 (iv), (v), (vi) see Exercise 4.2.1; (vii) (p cos u, q cos u, v); (viii) (±p cosh u, q sinh u, v); (ix) (u, u2 /p2 , v); (x) (0, u, v); (xi) (±p, u, v). 1 −1/3 0 5.2.2 In the notation of Theorem 5.2.2, A = −1/3 1 0 . The eigenvalues 0 0 −2 are 2/3, 4/3, −2 and the corresponding unit eigenvectors are the columns of P = √ ′ √ x x 1/√2 −1/√ 2 0 1/ 2 1/ 2 0 . If y ′ = P y , then z ′ = z and the quadric z′ z 0 0 1 2 2 4 ′2 2 ′2 ′2 ′ becomes 3 x + 3 y − 2z + 4z = c, i.e. 32 x′ + 43 y ′ − 2(z ′ − 1)2 = c − 2. Comparing with the standard forms in Theorem 5.2.2 gives the stated results when c > 2 and c < 2. If c = 2 we have a cone with axis the z-axis (which is the same as the z ′ -axis), vertex at x′ = y ′ = 0, z ′ = 1, i.e. x = y = 0, z = 1, and 2 2 cross-section perpendicular to the z-axis an ellipse 23 x′ + 43 y ′ = constant. 36 b into the equation of the 5.2.3 Substituting the components (x, y, z) of γ (t) = a + tb quadric gives a quadratic equation for t; if the quadric contains three points on the line, this quadratic equation has three roots, hence is identically zero, so the quadric contains the whole line. For the second part, take three points on each of the given lines; substituting the coordinates of these nine points into the equation of the quadric gives a system of nine homogeneous linear equations for the ten coefficients a1 , . . . , c of the quadric; such a system always has a non-trivial solution. By the first part, the resulting quadric contains all three lines. 5.2.4 Let L1 , L2 , L3 be three lines from the first family; by the preceding exercise, there is a quadric Q containing all three lines; all but finitely-many lines of the second family intersect each of the three lines; if L′ is such a line, Q contains three points of L′ , and hence the whole of L′ by the preceding exercise; so Q contains all but finitely-many lines of the second family; since any quadric is a closed subset of R3 , Q must contain all the lines of the second family, and hence must contain S. 5.2.5 z = x p − y y 1 x q p + q = uv, x = 2 p(u+v), σv ( 21 p(u+v), 12 q(v −u), uv); σ u ×σ y = 12 q(v−u), so a parametrisation is σ (u, v) = = (− 21 q(u+v), 12 p(v −u), pq) is never zero so σ is regular. For a fixed value of u, σ (u, v) = ( 21 pu, − 12 qu, 0)+v( 21 p, 12 q, u) is a straight line; similarly for a fixed value of v; hence the hyperbolic paraboloid is the union of each of two families of straight lines. a c 5.2.6 Let A = . Since A is a real symmetric matrix, there is an orthogonal c b ′ a 0 t ′ ′ matrix P such that P AP = A is a diagonal matrix, say A = (see 0 b′ Appendix 0). We can assume that det(P ) = 1 by changing the sign of one of the rows of P if necessary. Then the equation of the conic becomes 2 2 a′ x′ + b′ y ′ + d′ x′ + e′ y ′ + f = 0, ′ d x d x′ = P . In other words, we might as well = P , where e y e′ y′ assume that c = 0 from the beginning. Assume then that c = 0. If a 6= 0, we can assume that d = 0 by replacing x by x + ad (a translation). Similarly, if b 6= 0 we can assume that e = 0. If a and b are both 6= 0, we can therefore assume that d = e = 0 and we are in case (i) or (iii). If a = 0 and b 6= 0, the equation takes the form by 2 + dx + f = 0. If d 6= 0 replacing x by x + fd we can assume that f = 0 and then we are in case (ii). If d = 0 we are in case (v). The case a 6= 0, b = 0 is similar. 37 If a = b = 0 we have a straight line. 5.2.7 (i) From the classification in Theorem 5.2.2, the connected quadric surfaces are those of types (i), (ii), (iv), (v), (vii), (ix) and (x) (remember that for type (vi) to be a smooth surface, we have to remove the vertex which results in a disconnected surface). Type (i) is diffeomorphic to S 2 by (x, y, z) 7→ ( xp , yq , zr ); type (ii) to the unit cylinder by (x, y, z) 7→ q x p x2 p2 ,q 2 + y2 q y q x2 p2 2 + y2 q , z ; types (iv) and (v) to a plane by (x, y, z) 7→ (x, y, 0); type (vii) to the unit cylinder by (x, y, z) 7→ ( xp , yq , z); type (ix) to a plane by (x, y, z) 7→ (x, 0, z); and type (x) is a plane. (ii) For types (iii) and (vi) the connected pieces are the parts of the quadric with z > 0 and with z < 0. Each part of type (iii) is diffeomorphic to the plane by (x, y, z) 7→ (x, y, 0). Each part of type (vi)is diffeomorphic to the unit cylinder by (x, y, z) 7→ q x p x2 p2 ,q 2 + y2 q y q x2 p2 2 + y2 q , ln |z|. The two connected pieces of type (viii) are given by x > 0 and x < 0; each piece is diffeomorphic to the plane by (x, y, z) 7→ (0, y, z). 5.3.1 From Example 5.3.2, the surface can be parametrized by σ (u, v) = (cosh u cos v, cosh u sin v, u), with u ∈ R and −π < v < π or 0 < v < 2π. 5.3.2 k σ (u, v) k2 = sech2 u(cos2 v + sin2 v) + tanh2 u = sech2 u + tanh2 u = 1, so σ parametrizes an open subset of S 2 ; σ is clearly smooth; and σ u × σ v = −sech2 u σ (u, v) is never zero, so σ is regular. Meridians correspond to the parameter curves v = constant, and parallels to the curves u = constant. 5.3.3 (i) γ̃γ .aa = 0 so γ̃γ is contained in the plane perpendicular to a and passing through the origin; (ii) simple algebra; (iii) ṽ is clearly a smooth function of (u, v) and the Jacobian matrix of the map 1 0 , where a dot denotes d/du; this matrix is invertible (u, v) 7→ (u, ṽ) is γ γ̇ .aa 1 so γ̃γ is a reparametrization of γ . 5.3.4 σ u = γ̇γ +vδ̇δ , σ v = δ (a dot denotes d/du) so δ̇δ (u) is perpendicular to the surface at σ (u, v) ⇐⇒ δ̇δ. (γ̇γ + vδ̇δ ) = 0, δ̇δ.δ = 0. The second equation follows from k δ k = 1 so the two conditions are satisfied ⇐⇒ v = −(γ̇γ.δ̇δ )/ k δ̇δ k2 . Hence, Γ(u) = Γ.δ̇δ = γ̇γ.δ̇δ − (γ̇γ .δ̇δ )δ̇δ.δ̇δ / k δ̇δ k2 = 0. γ − (γ̇γ .δ̇δ )δδ / k δ̇δ k2 . Using δ̇δ.δ = 0 again, Γ̇ 38 5.3.5 The vector σ u is tangent to the meridians, so a unit-speed curve γ is a loxodrome σ u / k σ u k = cos α, which gives u̇ = cosh u cos α; since γ is unit-speed, γ̇γ = if γ̇γ .σ (−u̇ sech u tanh u cos v−v̇ sech u sin v, −u̇ sech u tanh u sin v+v̇ sech u cos v, u̇ sech2 u) is a unit vector; this gives u̇2 + v̇ 2 = cosh2 u, so v̇ = ± cosh u sin α. The correponding curve in the uv-plane is given by dv/du = v̇/u̇ = ± tan α, and so is a straight line v = ±u tan α + c, where c is a constant. 5.3.6 The ruling that makes an angle θ with the positive x-axis is given by y = x tan θ, z = f (θ), so a point at a distance u from the z-axis has coordinates df df sin θ, − dθ cos θ, u) and this is x = u cos θ, y = u sin θ, z = f (θ). σ u × σ θ = ( dθ non-zero if u 6= 0 (i.e. if we exclude the line L itself from the surface). 5.3.7 (i) The assumption means that N is constant. Hence, σ .N is constant, since σ.N)u = σ u.N = 0, etc. So σ is contained in a plane v.N = constant. (σ N for some scalar λ. (ii) If all the normal lines pass through a point p, σ = p + λN Nu so 0 = σ u.N = λu since N u.N = 0 as N is a unit vector. Then, σ u = λuN + λN Similarly λv = 0. So λ is a constant and σ is part of the sphere k v − p k = |λ|. (iii) By applying an isometry we can assume that the given straight line is the z-axis. Reparametrize the surface using polar coordinates in the xy-plane: N is the poσ (r, θ) = (r cos θ, r sin θ, f (r, θ)), say. For some scalar µ, σ + µN sition vector of a point on the z-axis. If N = (a, b, c), setting the x- and N equal to zero gives µa = −r cos θ, µb = −r sin θ, y-components of σ + µN and hence either µ = 0 (i.e., r = 0) or a sin θ = b cos θ. But σ r × σ θ = (fθ sin θ − rfr cos θ, −fθ cos θ − rfr sin θ, r), so if µ 6= 0 then sin θ(rfr cos θ − fθ sin θ) = cos θ(rfr sin θ + fθ cos θ), i.e. fθ = 0. We have now proved that fθ = 0 except possibly when r = 0; but then fθ = 0 for all (r, θ) as f is smooth (and hence continuous). Thus, f depends only on r, and hence σ is the surface of revolution obtained by rotating the curve r 7→ (r, 0, f (r)) in the xz-plane around the z-axis. 5.3.8 Use the parametrization γ (u) = (cos u, sin u, 0) of the ‘waist’ of the hyperboloid. From Exercise 4.1.3, there is a straight line on the hyperboloid passing through γ (u), and it takes the form (x − z) cos θ = (1 − y) sin θ, (x + z) sin θ = (1 + y) cos θ. Substituting x = cos u, y = sin u, z = 0 gives θ = u2 + π4 . The vector δ (u) = (cos 2θ, sin 2θ, 1) = (− sin u, cos u, 1) is parallel to this line, so a parametrization of the hyperboloid as a ruled surface is σ (u, v) = (cos u, sin u, 0) + v(− sin u, cos u, 1) = (cos u − v sin u, sin u + v cos u, v). Since γ̇γ.δ̇δ = 0, the line of striction is γ (see the solution to Exercise 5.3.4). 39 5.3.9 We use the notation in Theorem 5.2.2. (a) Types (vii) through (xi). (b) Types (vi) and (x). (c) Types (ii), (v) and (vi) through (xi). (d) Type (i) if p2 , q 2 , r 2 are not distinct; types (ii), (iii), (iv), (vi) and (vii) if p2 = q 2 ; and types (x) and (xi). 5.3.10 Take the ruled surface to be σ (u, v) = γ (u) + vδδ (u), where γ is unit-speed and δ is a unit vector. Consider the ruling corresponding to u = u0 , say. Since σ u × σ v = (γ̇γ + vδ̇δ ) × δ (a dot denoting d/du, evaluated at u = u0 ), the union of the normal lines along the ruling u = u0 is the surface b + wcc + vwd d, Σ (v, w) = σ (u0 , v) + w(γ̇γ + vδ̇δ ) × δ = a + vb where a = γ (u0 ), b = δ (u0 ), c = γ̇γ × δ and d = δ̇δ × δ are constant vectors. By applying a translation we can assume that a = 0. Then, by applying a rotation we can assume that b = (1, 0, 0) and that δ̇δ is parallel to (0, 1, 0) (note that δ̇δ is perpendicular to δ ). Then, c is parallel to the yz-plane and d is parallel to the z-axis. If d = 0, i.e. if δ̇δ (u0 ) = 0, Σ is a plane. If d = (0, 0, λ) 6= 0 and c = (0, µ, ν), then Σ(v, w) = (v, µw, νw + λvw). If µ = 0 we have the xz-plane. Otherwise, the translation x 7→ x − λν followed by a rotation by π/2 around the z-axis takes Σ to a parametrization of the hyperbolic paraboloid z = µλ (x2 − y 2 ). 5.4.1 Both surfaces are closed subsets of R3 , as they are of the form f (x, y, z) = 0, where f : R3 → R is a continuous function (equal to x2 − y 2 + z 4 − 1 and x2 + y 2 + z 4 − 1 in the two cases). The surface in (i) is not bounded, and hence not compact, since it contains the point (1, a2 , a) for all real numbers a; that in (ii) is bounded, and hence compact, since x2 + y 2 + z 4 = 1 =⇒ −1 ≤ x, y, z ≤ 1. The surface in (ii) is obtained by rotating the curve x2 + z 4 = 1 in the xz-plane around the z-axis: 5.4.2 A closed curve γ with period T can be identified with the unit circle by γ (t) 7→ 40 (cos(2πt/T ), sin(2πt/T )). This gives rise to a diffeomorphism from the tube around γ to a tube around the circle, i.e. a torus. We have to make the tube have a sufficiently small radius as otherwise it might intersect itself and then it would not be a surface. 5.5.1 Both parts are geometrically obvious. 5.5.2 Let (a, b, c) ∈ R3 with a and b non-zero. Then Ft (a, b, c) → ∞ as t → ∞ and as t approaches p2 and q 2 from the left; and Ft (a, b, c) → −∞ as t → −∞ and as t approaches p2 and q 2 from the right. From this and the fact that Ft (a, b, c) = 0 is equivalent to a cubic equation for t, it follows that there exist unique numbers u, v, w with u < p2 , p2 < v < q 2 and q 2 < w such that Ft (a, b, c) = 0 when t = u, v or w. The surfaces Fu (x, y, z) = 0 and Fw (x, y, z) = 0 are elliptic paraboloids and Fv (x, y, z) = 0 is a hyperbolic paraboloid, and we have shown that there is one surface of each type passing through each point (a, b, c). To show that the system is orthogonal, note that ∇ Ft = p22x−t , q 22y−t , −2 so if (a, b, c) is a point at the intersection of the surfaces Fu (x, y, z) = 1 and Fv (x, y, z) =, we have 4a2 4b2 + +4 (p2 − u)(p2 − v) (q 2 − u)(q 2 − v) 4(Fu (a, b, c) − Fv (a, b, c)) 4−4 = = = 0. u−v u−v ∇Fu.∇Fv = Thus, the first two families intersect orthogonally. Similarly for the other two pairs of families. To parametrize these surfaces, write Ft (x, y, z) = 0 as the cubic equation x2 (q 2 − t) + y 2 (p2 − t) − 2z(p2 − t)(q 2 − t) + t(p2 − t)(q 2 − t) = 0, and note that the left-hand side must be equal to (t−u)(t−v)(t−w); putting t = q p2 , q 2 and then equating coefficients of t2 (say) gives x = ± q 2 2 −v)(q 2 −w) y = ± (q −u)(qp2 −q , z = 21 (u + v + w − p2 − q 2 ). 2 (p2 −u)(p2 −v)(p2 −w) , q 2 −p2 5.5.3 (i) Let U = xy − uz 2 , V = x2 + y 2 + z 2 − v, W = x2 + y 2 + z 2 − w(x2 − y 2 ). Then, ∇ U = (y, x, −2uz), ∇V = (2x, 2y, 2z), ∇ W = (2(1 − w)x, 2(1 + w)y, 2z). Hence, at a point of intersection of the surfaces U = 0, V = 0, W = 0, we have ∇ U..∇V = 4xy − 4uz 2 = 0 by the equation U = 0; ∇V .∇ W = 4((1 − w)x2 + (1 + w)y 2 + z 2 ) = 4(x2 + y 2 + z 2 − w(x2 + y 2 )) = 0 by the equation V = 0; and ∇W .∇ U = 2(1 − w)xy + 2(1 + w)xy − 4uz 2 = 4(xy − uz 2 ) = 0 41 by the equation U = 0. (ii) Let p p p p U = yz − ux, V = x2 + y 2 + x2 + z 2 − v, W = x2 + y 2 − x2 + z 2 − w. y x x z √ √ √ √ Then, ∇U = (−u, z, y), ∇V = + x2 +z2 , , x2 +z2 , ∇ W = x2 +y 2 x2 +y 2 √ 2x 2 − √ 2x 2 , √ 2y 2 , − √ 2z 2 . Hence, at a point of intersection of the x +z x +z x +y x +y surfaces U = 0, V = 0 and W = 0, ∇ U..∇V = (yz − ux) √ 21 2 + √x21+z2 = x +y 2 2 2 2 0 by the equation U = 0; ∇V .∇W = x2x+y2 − x2x+z2 + x2y+y2 − x2z+z2 = 0; 1 1 ∇ W .∇U = (yz − ux) √ 2 2 − √x2 +z2 = 0 by the equation U = 0. x +y 5.5.4 Two families of plane curves U (x, y) = u and V (x, y) = v form an orthogonal system if ∇ U..∇ V = 0 at each point of intersection of the first family of a curve ∂U ∂U with a curve of the second family. Here, ∇U = ∂x , ∂y , etc. (i) U (x, y) = x, V (x, y) = y, i.e. the two families of straight lines parallel to the y- and x-axis, respectively. The orthogonality is obvious. (ii) U (x, y) = y cos u − x sin u, V (x, y) = x2 + y 2 − v 2 , i.e. the family of straight lines passing through the origin and the family of circles with centre the origin. The orthogonality is obvious. 5.5.5 The function Ft (a, b) is a continuous function of t (for fixed non-zero real numbers a, b) in each of the open intervals (−∞, p2 ), (p2 , q 2 ) and (q 2 , ∞). Also, Ft (a, b) → 0 as t → ±∞, and Ft (a, b) → ±∞ as t approaches p2 or q 2 from the left (+ sign) or right (− sign). It follows that there is at least one value of t in each of the open intervals (−∞, p2 ) and (p2 , q 2 ) such that Ft (a, b) = 1. On the other hand, Ft (a, b) = 1 is equivalent to a quadratic equation for t which has at most two real roots. It follows that there are unique numbers u ∈ (−∞, p2 ) and v ∈ (p2 , q 2 ) such that Fu (a, b) = Fv (a, b) = 1. The conics Fu (x, y) = 1 and Fv (x, y) = 1 are ellipses and hyperbolas, respectively, and we have shown that there is one of each passing through each point on the plane that does not lie on one of the coordinate axes. To show that this is an orthogonal system of curves, we calculate ∇Fu .∇Fv at b) that lies on the conics Fu = 1 and Fv = 1. Since ∇ Fu = a point (a, 2y 2x p2 −u , q 2 −u , we get 4a2 4b2 + (p2 − u)(p2 − v) (q 2 − u)(q 2 − v) 4(Fu (a, b) − Fv (a, b) 4−4 = = = 0. u−v u−v ∇Fu.∇Fv = 42 2 For the last part, let Ft (x, y) = p2x−t − 2y + t. Arguing as in Exercise 5.5.2, for any point (a, b) ∈ R2 not on one of the coordinate axes, there are unique numbers u ∈ (−∞, p2 ) and v ∈ (p2 , ∞) such that Fu (a, b) = Fv (a, b) = 1. Both systems of curves Fu (x, y) = 1 and Fv (x, y) = 1 are parabolas. At (a, b) we find that ∇Fu.∇ Fv = 4(Fu (a, b) − Fv (a, b)) 4−4 4a2 +4= = = 0, 2 2 (p − u)(p − v) u−v u−v showing that the parabolas form an orthogonal system. 5.5.6 Let U (x, y) = u and V (x, y) = v be an orthogonal system of plane curves (see Exercise 5.5.4). We will show that the system of surfaces U (x, y) = u, V (x, y) = v, z = w is orthogonal. The first two families of surfaces consist of generalized cylinders, the third consists of parallel planes. Suppose that (a, b, c) is a point of intersection of a surface from each family. We have to prove that the vectors ∂U ∂U ∂V ∂V and (0, 0, 1) are mutually perpendicular at (a, b, c). ∂x , ∂y , 0 , ∂x , ∂y , 0 But it is obvious that the third vector is perpendicular to the other two, and the first two are perpendicular because the curves U (x, y) = u and V (x, y) = v intersect orthogonally at (a, b). 5.6.1 Let F : W → V be the smooth bijective map with smooth inverse F −1 : V → W constructed in the proof of Proposition 4.2.6. Then, (u(t), v(t)) = F −1 (γγ (t)) is smooth. 5.6.2 Suppose, for example, that fy 6= 0 at (x0 , y0). Let F (x, y) = (x, f (x, y)); then F 1 fx is smooth and its Jacobian matrix is invertible at (x0 , y0 ). By the in0 fy verse function theorem, F has a smooth inverse G defined on an open subset of R2 containing F (x0 , y0 ) = (x0 , 0), and G must be of the form G(x, z) = (x, g(x, z)) for some smooth function g. Then γ (t) = (t, g(t, 0)) is a parametrization of the level curve f (x, y) = 0 containing (x0 , y0 ). fx fy fz The matrix has rank 2 everywhere; suppose that, at some point gx gy gz fy fz (x0 , y0 , z0 ) on the level curve, the 2 × 2 submatrix is invertible. gy gz Then, the function F (x, y, z)= (x, f (x, y, z), g(x, y, z)) is smooth and its Ja1 0 0 fx fy fz is invertible at (x0 , y0 , z0 ). Let G(x, u, v) = cobian matrix gx gy gz (x, ϕ(x, u, v), ψ(x, u, v)) be the smooth inverse of F defined near (x0 , 0, 0). Then γ (t) = (t, ϕ(t, 0, 0), ψ(t, 0, 0)) is a parametrization of the level curve f (x, y, z) = g(x, y, z) = 0 containing (x0 , y0 , z0 ). 43 5.6.3 Let σ (u, v) = (f (u, v), g(u, v), h(u, v)). The condition σ u × σ v 6= 0 at (u0 , v0 ) fu fv means that the matrix gu gv has rank 2 at (u0 , v0 ), so at least one 2 × 2 hu hv fu fv submatrix is invertible, say . If F (u, v) = (f (u, v), g(u, v)), then as gu gv in the proof of Proposition 4.2.6 there is an open subset V of R2 containing F (u0 , v0 ) and an open subset W of U containing (u0 , v0 ) such that F : W → V is bijective, in particular injective. Then the restriction of σ to W is injective. 5.6.4 Let σ (u, v) = (f (u, v), g(u, v), h(u, v)). The condition that N (u0 , v0 ) is not par fu fv allel to the xy-plane means that the matrix is invertible at (u0 , v0 ). gu gv If F (u, v) = (f (u, v), g(u, v)), then as in the proof of Proposition 4.2.6 there is an open subset V of R2 containing F (u0 , v0 ) and an open subset W of U containing (u0 , v0 ) such that F : W → V is bijective with smooth inverse. If F −1 (u, v) = (α(u, v), β(u, v)), then near (x0 , y0 , z0 ) the surface coincides with the graph z = h(α(x, y), β(x, y)). If N (u0 , v0 ) is parallel to the xy-plane, then at least one of the other two 2 × 2 submatrices of the Jacobian matrix of σ (u, v) is invertible, and then the surface coincides near (x0 , y0 , z0 ) with a graph of the form x = ϕ(y, z) or y = ϕ(x, z). 5.6.5 Let γ (t) = (γ1 (t), . . . , γn (t)). As γ is regular, γ̇γ (t0 ) 6= 0, so at least one component of γ̇γ (t0 ) is non-zero, say γ̇1 (t0 ) (the proof is the same in the other cases). By the inverse function theorem for real-valued function of one variable, there is a smooth function α, say, defined on an open interval containing γ1 (t0 ), and some ǫ > 0 such that α(γ1 (t)) = t for all t ∈ (t0 − ǫ, t0 + ǫ). This implies that the restriction of γ1 to the interval (t0 − ǫ, t0 + ǫ) is injective. Hence, the restriction of γ to the same interval is injective. Chapter 6 6.1.1 (i) Quadric cone x2 + z 2 = y 2 ; we have σ u = (cosh u sinh v, cosh u cosh v, cosh u), σ v = (sinh u cosh v, sinh u sinh v, 0), k σ u k2 = 2 cosh2 u cosh2 v, σ v = 2 sinh u cosh u sinh v cosh v, σ u .σ k σ v k2 = sinh2 u cosh 2v, and the first fundamental form is 2 cosh2 u cosh2 v du2 + sinh 2u sinh 2v dudv + sinh2 u cosh 2v dv 2 . 44 (ii) Paraboloid of revolution; (2 + 4u2 ) du2 + 8uv dudv + (2 + 4v 2 ) dv 2 . (iii) Hyperbolic cylinder; (cosh2 u + sinh2 u) du2 + dv 2 . (iv) Paraboloid of revolution; (1 + 4u2 ) du2 + 8uv dudv + (1 + 4v 2 ) dv 2 . 6.1.2 Applying a translation to a surface patch σ does not change σ u or σ v . If P is σ u ), (P σ )v = P (σ σ v ), and P preserves a 3 × 3 orthogonal matrix, (P σ )u = P (σ p).P (q q) = p.q q for all vectors p, q ∈ R3 ). Applying the dilation dot products (P (p (x, y, z) 7→ a(x, y, z), where a is a non-zero constant, multiplies σ by a and hence the first fundamental form by a2 . 6.1.3 Since both sides define bilinear forms on the tangent plane, it suffices to prove σ u , σ v }. This is easily that the two sides agree when v, w belong to the basis {σ σ u ) = dv(σ σ v ) = 1, du(σ σ v ) = dv(σ σ u ) = 0. checked using du(σ ∂v σ ũ = σ u ∂∂uũ + σ v ∂∂vũ , σ̃ σ ṽ = σ u ∂u 6.1.4 By the chain rule, σ̃ ∂ ṽ + σ v ∂ ṽ , which gives Ẽ = 2 2 σ ũ .σ̃ σ ũ = E ∂u + 2F ∂∂uũ ∂∂vũ + G ∂∂vũ . Similar expressions for F̃ and G̃ can be σ̃ ∂ ũ found; multiplying out the matrices shows that these formulas are equivalent to the matrix equation in the question. Following the procedure given, Edu2 + 2F dudv + Gdv 2 = 2 ∂v 2 ∂u ∂v ∂v ∂v ∂u dṽ dũ + dṽ dũ + dṽ +G dũ + dṽ +2F . The E ∂∂uũ dũ + ∂u ∂ ṽ ∂ ũ ∂ ṽ ∂ ũ ∂ ũ ∂ ṽ ∂ ṽ ∂u 2 ∂u ∂v ∂v 2 2 coefficient of dũ is E ∂ ũ + 2F ∂ ũ ∂ ũ + G ∂ ũ , which agrees with the expression for Ẽ found above. Similarly for F̃ and G̃. 6.1.5 (i) ⇐⇒ (ii): Ev = Gu = 0 ⇐⇒ σ u.σ uv = σ v .σ uv = 0 ⇐⇒ σ uv is parallel to N. Consider the quadrilateral bounded by the parameter curves R v u = u0 , u = u1 , v = σ v (u0 , v) k dv = v0 , v = v1 . The length of the side given by u = u0 is v01 k (σ R v1 p G(u0 , v)dv. v0 (i) =⇒ (iii): If Gu = 0, G depends only on v so the last integral is unchanged when u0 is replaced by u1 . So the two sides u = u0 and u = u1 have the same length; and similarly for the other two sides. Rv p (iii) =⇒ (i): If the lengths are equal then v01 G(u, v)dv is independent of u; Rv √u dv = 0 for all v0 , v1 , so Gu = 0; differentiating with respect to u gives v01 2G G and similarly Ev = 0. Rp Rp E(u) du, ṽ = G(v) dv. Assuming conditions (i) - (iii) are satisfied, set ũ = Then, (u, v) → 7 (ũ, ṽ) is a reparametrization map because its Jacobian matrix √ √ E √0 has non-zero determinant EG. The first fundamental form of 0 G σ (ũ, ṽ) of σ (u, v) is dũ2 + √2F dũdṽ +dṽ 2 . Now the reparametrization σ̃ EG √2F EG <1 since EG−F 2 > 0, so there is a smooth function θ(ũ, ṽ) with 0 < θ < π such that cos θ = √2F . This gives the first fundamental form as dũ2 + 2 cos θdũdṽ + dṽ 2 . EG 45 Since ũ = 12 (û + v̂), ṽ = 21 (û − v̂), the first fundamental form becomes 1 1 1 (dû + dv̂)2 + cos θ(dû2 − dv̂ 2 ) + (dû − dv̂)2 4 2 4 1 1 θ θ = (1 + cos θ)dû2 + (1 − cos θ)dv̂ 2 = cos2 dû2 + sin2 dv̂ 2 . 2 2 2 2 6.1.6 (i) σ u = (cos v, sin v, 1/u), σ v = (−u sin v, u cos v, 0) so E = 1 + u−2 , F = 0, G = u2 , The surface is obtained by rotating the curve z = ln x in the xz-plane around the z-axis. (ii) σ u = (cos v, sin v, 0), σ v = (−u sin v, u cos v, 1) so E = 1, F = 0, G = 1 + u2 . This is a helicoid (Exercise 4.2.6). (iii) σ u = (sinh u cos v, sinh u sin v, 1), σ v = (− cosh u sin v, cosh u cos v, 0) so E = 1 + sinh2 u = cosh2 u, F = 0, G = cosh2 u. This is a catenoid (Exercise 5.3.1). 6.1.7 The first fundamental form is 2du2 + u2 dv 2 . Hence, the length is √ Z π 2λ2 + 1 λπ (e − 1). (2(λeλt )2 + (eλt )2 )1/2 dt = λ 0 A ruling can be parametrized by u = t, v = constant, so the angle is ! r λt 2 2λ2 2(λe + u (0)) = cos−1 cos−1 p , √ 2λ2 + 1 (2λ2 + 1)e2λt 2 which is constant and independent of the ruling. b = t − τ vn n, σ v = b, so since t, n and b are 6.1.8 Denoting d/du by a dot, σ u = γ̇γ + vḃ 2 2 perpendicular unit vectors, E = 1 + τ v , F = 0, G = 1. σ u.σ uu . Hence, σ u.σ uu = 6.1.9 From E = σ u.σ u we get Eu = σ uu.σ u + σ u.σ uu = 2σ 1 2 Eu . Similarly, differentiating E with respect to v and G with respect to u and v gives σ u.σ uv = 12 Gu , σ u.σ uv = 12 Ev , σ v .σ vv = 12 Gv . Differentiating F = σ u.σ v with respect to u gives Fu = σ uu.σ v + σ u.σ uv and using the formula σ u.σ uv = 21 Ev gives σ uu.σ v = Fu − 21 Ev . The formula for σ u.σ vv is proved similarly. √ √ σ (u, v), say. The im6.2.1 The map is σ (u, v) 7→ u 2 cos √v2 , u 2 sin √v2 , 0 = σ̃ age of this map is √ the sector of the xy-plane whose polar coordinates (r, θ) satisfy 0 < θ < π 2. The first fundamental form of σ is 2 du2 + u2 dv 2 ; √ √ σu = σ v = −u sin √v , u cos √v , 0 , so k σ̃ σ u k2 = 2 cos √v2 , 2 sin √v2 , 0 , σ̃ σ̃ 2 2 σ v = 0, k σ v k2 = u2 and the first fundamental form of σ̃ σ is 2 du2 + u2 dv 2 . 2, σ u .σ √ 6.2.2 No: the part of the ruling (t, 0, t) with 1 ≤ t ≤ 2 (say) has length 2 and is mapped to the straight line segment (t, 0, 0) with 1 ≤ t ≤ 2, which has length 1. 46 6.2.3 A straightforward calculation shows that the first fundamental form of σ t is cosh2 u(du2 +dv 2 ); in particular, it is independent of t. Hence, σ (u, v) 7→ σ t (u, v) is an isometry for all t. Taking t = π/2 gives the isometry from the catenoid to the helicoid; under this map, the parallels u = constant on the catenoid go to circular helices on the helicoid, and the meridians v = constant go to the rulings of the helicoid. 6.2.4 The line of striction is given by v = −(γ̇γ .δ̇δ )δδ / k δ̇δ k2 (Exercise 5.3.4), where in this case δ = γ̇γ . Since γ is unit-speed, γ̇γ .γ̈γ = 0 so v = 0 and we get the curve γ itself. For the second part, we can assume that u0 = 0 and by applying an isometry of R3 that γ (0) = 0, t(0) = i, n(0) = j, b(0) = k (in the usual notation). Then, using ... Frenet-Serret, γ̈γ (0) = κ(0)jj, γ (0) = (−κ(0)2 , κ̇(0), κ(0)τ (0)) so, neglecting higher ... powers of u in each component, γ (u) = γ (0) +uγ̇γ (0) + 12 γ̈γ (0)u2 + 61 γ (0)u3 +. . . = (u, 12 κ(0)u2 , 61 κ(0)τ (0)u3 ). The intersection of the surface with the plane perpendicular to t(0) = i is given by setting the x-component of σ (u, v) equal to zero. This gives v = −u+ higher terms, so neglecting such terms, u = −v. Then the intersection is Γ(v) = σ (−v, v) = γ (−v) + vγ̇γ (−v) = (0, − 21 κ(0)v 2 , 31 κ(0)τ (0)v 3 ). 6.2.5 A generalized cylinder can be parametrized by σ (u, v) = γ (u) + vaa, where we can assume (see Exercise 5.3.3) that γ is unit-speed, a is a unit vector, and γ̇γ .a = 0, where the dot denotes d/du. Then, σ u = γ̇γ , σ v = a so the first fundamental form is du2 + dv 2 . This is the same as the first fundamental form of the plane (u, v, 0), so by Corollary 6.2.3 the map σ (u, v) 7→ (u, v, 0) is a local isometry. By applying an isometry of R3 (a translation), we can assume that the vertex of the cone is the origin. It can then be parametrized by σ (u, v) = vγγ (u), where γ is a unit-speed curve on S 2 . Then, σ u = vγ̇γ , σ v = γ so the first fundamental form is v 2 du2 + dv 2 . This is the same as the first fundamental form of the plane in polar coordinates (v cos u, v sin u, 0). 6.2.6 Assume that f satisfies the given condition and denote d/du by a dot. Define Rq g(u) = 1 − f˙2 du; then g is smooth since the term inside the square root is always > 0. The curve γ (u) = (f (u), 0, g(u)) in the xz-plane is unit-speed, and by Example 6.1.3 if we rotate γ around the z-axis, the resulting surface of revolution has first fundamental form du2 + f (u)2 dv 2 . By Corollary 6.2.3, the given surface is locally isometric to this surface of revolution. Rp U (u) du. The given condition on U implies that U (u) > 0 for all 6.2.7 Define ũ = values of u, so ũ is a smooth function of u and dũ/du is never zero. It follows that (u, v) 7→ (ũ, v) is a reparametrization map. The first fundamental form in terms of (ũ, v) is dũ2 + Ũ (ũ)dv 2 , where Ũ (ũ) = U (u). By Exercise 6.2.6, this df < 1 for all surface patch is locally isometric to a surface of revolution if dũ 47 values of ũ, where f = p Ũ . But, df 1 dŨ 1 dU/du 1 dU = p = √ = . dũ 2U du 2 U dũ/du 2 Ũ dũ 6.3.1 If the first fundamental forms of two surfaces are equal, they are certainly proportional, so any isometry is a conformal map. Stereographic projection is a conformal map from S 2 to the plane, but it is not an isometry since λ 6= 1 (see Example 6.3.5). 6.3.2 The first fundamental form of the given surface patch is (1+u2 +v 2 )2 (du2 +dv 2 ); this is a multiple of du2 + dv 2 so the patch is conformal. 2 σ (u, v) is dψ σ is 6.3.3 The first fundamental form of σ̃ du2 + cos2 ψ(u)dv 2 . So σ̃ du R conformal ⇐⇒ dψ/du = ± cos ψ. Taking the plus sign, we get u = sec ψdψ = ψ cos ψ ψ u u −u = 1+sin ln(sec ψ + tan ψ), so 1+sin cos ψ = e . Then 2 cosh u = e + e cos ψ + 1+sin ψ = σ (u, v) is the patch in Exercise 2 sec ψ. Hence, cos ψ = sechu, sin ψ = tanhu and σ̃ 5.3.2. 6.3.4 Φ is conformal if and only if fu2 + gu2 = fv2 + gv2 and fu fv + gu gv = 0. Let z = fu + igu , w = fv + igv ; then Φ is conformal if and only if zz̄ = ww̄ and z w̄ + z̄w = 0, where the bar denotes complex conjugate; if z = 0, then w = 0 and all four equations are certainly satisfied; if z 6= 0, the equations give z 2 = −w2 , so z = ±iw; these are easily seen to be equivalent to the first pair of equations in the statement of the exercise if the sign is +, and to the second pair if the f gu = ±(fu2 + fv2 ), with a plus sign if the sign is −. We have det(J(Φ)) = u fv g v first pair of equations hold and a minus sign if the second pair of equations hold. 6.3.5 Let S be an orientable surface. Fix a smooth choice of unit normal at each point of S, and let A be the atlas for S consisting of all the surface patches for S whose standard unit normal agrees with the chosen normal. On the other hand, by Theorem 6.3.6 S has an atlas consisting of conformal parametrizations; let à be the maximal such atlas (i.e. the set of all conformal parametrizations of S). Then, A ∩ à is an atlas for S. Indeed, if p ∈ S, let σ be any conformal parametrization of S containing p. If σ has the wrong orientation (so that σ (u, v) = σ (−u, v) is a conformal parametrization containing p σ ∈ / Ã), then σ̃ that has the correct orientation. Thus, in any case there is a surface patch of S containing p that is both conformal and correctly oriented. Let Φ be the transition map between two of the patches in the atlas A ∩ Ã. Then, Φ is a conformal diffeomorphism between open subsets of R2 . By Exercise 6.3.4, Φ is either holomorphic or anti-holomorphic, and in the latter case det(J(Φ)) < 0, contradicting the fact that Φ is the transition map between two correctly oriented surface patches. Hence, Φ must be holomorphic. 48 y x , z+1 , 0). Identifying (u, v) ∈ 6.3.6 Following Example 6.3.5, we find Π̃(x, y, z) = ( z+1 2 1−|w| σ 1 (w) = ( |w|2w R2 with w = u + iv ∈ C, we find σ̃ Then σ 1 (w) = 2 +1 , 1+|w|2 ). σ 1 (1/w̄), so the transition map is w 7→ 1/w̄. This is not holomorphic, so the atlas σ̃ σ 1 , σ̃ σ 1 } does not give S 2 the structure of a Riemann surface. If σ̂ σ 1 (w) = σ̃ σ 1 (w̄), {σ σ 1 is w 7→ 1/w. This is holomorphic (when the transition map between σ 1 and σ̂ σ 1 , σ̂ σ 1 } gives w 6= 0, which holds on the overlap of the two patches), so the atlas {σ 2 S the structure of a Riemann surface. 6.3.7 Any circle on S 2 is the intersection of S 2 with a plane, and so (see Appendix 2) has equation of the form aw + āw̄ + bz = c, where a ∈ C, b, c ∈ R are constants |ξ|2 −1 (and a and b are not both zero). Substituting w = |ξ|2ξ 2 +1 , z = |ξ|2 +1 gives (b − c)|ξ|2 + 2aξ + 2āξ̄ = b + c, which is the equation of a Circle in C∞ (a line if b = c, a circle otherwise). The converse is proved similarly. σ 1 , σ̃ σ 1 } of S 2 in Ex6.3.8 The expression of the map Π−1 ◦ M ◦ Π in terms of the atlas {σ ercise 6.3.6, which consists of conformal patches, is of the form w 7→ M (w), w 7→ −1 −1 M (1/w̄), w 7→ M (w) , or w 7→ M (1/w̄) , i.e. a Möbius or conjugate-Möbius transformation. Since such transformations are conformal (Appendix 2), the result follows. 6.3.9 The first fundamental form is (1 + f˙2 )du2√+ u2 dv 2 , where a dot denotes d/du. So σ √ is conformal if and only if f˙ = ± u2 − 1, i.e. if and only if f (u) = ±( 21 u u2 − 1 − 12 cosh−1 u) + c, where c is a constant. 6.3.10 The first fundamental form is (1 + 2vγ̇γ .δ̇δ + v 2δ̇δ .δ̇δ)du2 + 2γ̇γ .δδ dudv + dv 2 . So σ is conformal if and only if 1 + 2vγ̇γ .δ̇δ + v 2δ̇δ .δ̇δ = 1 and γ̇γ .δδ = 0 for all u, v; the first condition gives δ̇δ = 0, so δ is constant, and the second condition then says that γ .δδ is constant, say equal to d. Thus, σ is conformal if and only if δ is constant and γ is contained in a plane v.δδ = d. In this case, σ is a generalized cylinder. 6.3.11 From σ ∗u = σ1.σ σ u − 2((σσ..σσ)u2) σ , we get (in the obvious notation) E ∗ = σ ∗u.σ ∗u = σ.σ u )2 σ. σ u ) 2 4(σ 4(σ E E − + = . 2 3 3 σ. σ ) σ .σ ) σ. σ ) (σ (σ (σ k σ k4 Similarly, we find that F ∗ = F/ k σ k4 , G∗ = G/ k σ k4 . Hence, the first fundamental form of σ ∗ is a multiple of that of σ . 6.3.12 By Example 6.1.3, any surface of revolution has an atlas consisting of surface 2 2 2 patches σ (u, v) whose first fundamental R duform is du + f (u) dv for some positive smooth function f (u). Define ũ = f (u) . Then, the first fundamental form of σ (ũ, v) of σ (u, v) is f 2 (dũ2 + dv 2 ). This is a conformal the reparametrization σ̃ surface patch. 6.4.1 Parametrize the paraboloid by σ (u, v) = (u, v, u2 + v 2 ); its first fundamental form is (1 + 4u2 )du2 + 8uv dudv + (1 + 4v 2 )dv 2 . Hence, the required area is 49 RR p 1 + 4(u2 + v 2 ) dudv, taken over the disc u2 + v 2 < 1. Let the integral R1√ u = r sin θ, v = r cos θ; then the area is 2π 0 1 + 4r 2 r dr = π6 (53/2 − 1). This is less than the area 2π of the hemisphere. 6.4.2 If S is a sphere with centre the origin and radius R, the map S 2 → S given p multiplies the first fundamental form by R2 , and so is conformal by p 7→ Rp but multiplies areas by R2 . It follows from Theorem 6.4.7 that the sum of the angles of a spherical triangle of area A on S is π + A/R2 . In this case, R is the radius of the earth and A is ≥ the area of Australia, so the sum of the angles is 30 ≥ π + (7 500 000)/(6 500)2 = π + 169 radians. Hence, at least one angle of the 10 radians. triangle must be at least one third of this, i.e. π + 169 6.4.3 Take a point p inside the polygon and join it to each vertex of the polygon by an arc of a great circle. This gives n triangles whose sides are arcs of great circles. The sum of their angles is the sum of their areas (i.e. the area of the polygon) minus nπ by Theorem 6.4.7, and is also the sum of the angles of the polygon plus 2π (the angle around p). 6.4.4 The sum of the angles around any vertex is 2π, so the sum of the angles of all the polygons is 2πV . By the preceding exercise, the sum of the angles of a polygon with P n sides is (n − 2)π plus its area. Summing over all polygons gives 2πV = 4π + polygons (n − 2)π, since the sum of the areas of all the polygons is the area P 4π of the sphere. Since two polygons meet along each edge, polygons n = 2E, and since there are F polygons altogether we get 2πV = 2πE − 2πF + 4π, which is equivalent to V − E + F = 2. √ 6.4.5 (i) is obvious as a local isometry preserves E, F, G and hence EG − F 2 . If Ẽ = λE, F̃ = λF and G̃ = λG, and if Ẽ G̃ − F̃ 2 = EG − F 2 , then λ2 = 1 and so λ = 1 (as E, Ẽ are > 0). This proves (ii). The map from S 2 to the unit cylinder in the proof of Theorem 6.4.6 is an equiareal map that is not a local isometry. 6.4.6 Let σ : U → R3 ; f is equiareal ⇐⇒ ZZ ZZ 2 1/2 (E1 G1 − F1 ) dudv = (E2 G2 − F22 )1/2 dudv for all regions R ⊆ U . R R This holds ⇐⇒ the two integrands are equal everywhere, i.e. ⇐⇒ E1 G1 − F12 = E2 G2 − F22 . 6.4.7 Since N is perpendicular to the tangent plane, N × σ u is parallel to the tangent σ u + βσ σ v for some α, √ N × σ u ).σ σ u = 0, (N N × σ u )..σ v = plane, and so = ασ β. Now (N 2 σ u × σ v )..N = k σ u × σ v k N.N = EG − F by √ (σ Proposition 6.4.2. This gives the √ two equations αE + √ βF = 0, αF + βG = EG − F 2 , which imply 2 α = −F/ EG − F , β = E/ EG − F 2 . The formula for N × σ v is proved similarly. 50 6.4.8 By Exercise 6.1.6(ii), the first fundamental form is du2 + (1 + u2 )dv 2 . So the area is Z 2π Z 1 p √ √ 1 + u2 dudv = π( 2 + ln(1 + 2)). 0 0 (The integral can be evaluated by putting u = tan θ.) 6.4.9 If we count the m edges that meet at each vertex, and then sum over all vertices, we will have counted each edge twice, once from each end. Hence, mV = 2E. Similarly, counting the n edges of each polygon, and then summing over all the polygons, gives twice the total number of edges as each edge is an edge of two polygons. This gives nF = 2E. −1 1 + n1 − 12 , From V − E + F = 2 and V = 2E/m, F = 2E/n we get E = m and hence values for V and F . The desired inequality follows from the fact that V, E and F are all > 0. The inequality can be written (m − 2)(n − 2) < 4. Thus, m − 2 and n − 2 are two positive integers whose product is less than 4, giving the 5 possibilities 1 × 1, 1 × 2, 2 × 1, 3 × 1, 1 × 3. 6.4.10 We can assume that the sphere is the unit sphere S 2 . If such curves exist they would give a triangulation of S 2 with 5 vertices and 5 × 4/2 = 10 edges, hence 2 + 10 − 5 = 7 polygons. Since each edge is an edge of two polygons and each polygon has at least 3 edges, 3F ≤ 2E; but 3 × 7 > 2 × 10. If curves satisfying the same conditions exist in the plane, applying the inverse of the stereographic projection map (Example 6.3.5) would give curves satisfying the conditions on S 2 , which we have shown is impossible. 6.4.11 Such a collection of curves would give a triangulation of the sphere with V = 6, E = 9, and hence F = 5. The total number of edges of all the polygons in the triangulation is 2E = 18. Since exactly 3 edges meet at each vertex, going around each polygon once counts each edge 3 times, so there should be 18/3 = 6 polygons, not 5. 6.4.12 Parametrize the surface by σ (u, v) = (ρ(u) cos v, ρ(u) sin v, σ(u)), where γ (u) = 2 2 2 (ρ(u), 0, σ(u)).RRBy Example 6.1.3, R the first fundamental form is du + ρ(u) dv , so the area is ρ(u) dudv = 2π ρ(u) du. R π/2 (i) Take ρ(u) = cos u, σ(u) = sin u, with −π/2 ≤ u ≤ π/2; so 2π −π/2 cos u du = 4π is the area. (ii) For the torus, the profile curve is γ (θ) = (a + b cos θ, 0, b sin θ), but this is not unit-speed; a unit-speed reparametrisation is γ̃γ (u) = a + b cos ub , 0, b sin ub R 2πb with 0 ≤ u ≤ 2πb. So 2π 0 a + b cos ub du = 4π 2 ab is the area. 6.4.13 Using the parametrization in Exercise 4.2.7, the first fundamental form is found 51 to be ((1 − κa cos θ)2 + τ 2 a2 ) ds2 + 2τ a2 dsdθ + a2 dθ 2 , so the area is Z s1 s0 Z 2π 0 a(1 − κa cos θ)dsdθ = 2πa(s1 − s0 ). 6.4.14 If E1 = λE2 , F1 = λF2 , G1 = λG2 , and if E1 G1 − F12 = E2 G2 − F22 , then λ2 = 1 so λ = 1 (since λ > 0). 6.4.15 (i) Any linear map R2 → R2 is obviously smooth so M is a diffeomorphism if and only if M is bijective. This holds if and only if M takes a basis of R2 , such u, v} is as {ii, j}, to another basis. Hence, M is a diffeomorphism if and only if {u 2 u v a basis of R , i.e. if and only if and are linearly independent. u + vvv. The first fundamental form of σ (ii) M takes (u, v) ∈ R2 to σ (u, v) = uu 2 2 2 2 u.v)dudv+ k v k dv . This is equal to du2 + dv 2 if and only if is k u k du + 2(u k u k = k v k = 1 and u.v = 0, i.e. if and only if u and v are perpendicular unit vectors. u.v)dudv+ k v k2 dv 2 is a multiple of du2 + dv 2 if and only if (iii) k u k2 du2 + 2(u k u k = k v k and u.v = 0, i.e. if and only if u and v are perpendicular vectors of equal length. (iv) Since E = k u k2 , F = u.v, G =k v k2 , M is equiareal if and only if u.v)2 = 1. From the proof of Proposition EG − F 2 = 1, i.e. k u k2 k v k2 −(u 6.4.2, the left-hand side is equal to k u × v k2 . So M is equiareal if and only if k u × v k = 1. 6.4.16 From the solution to Exercise 6.3.9, the first fundamental form of σ is (denoting d/du by a dot) (1+ f˙2 )du2 +u2 dv 2 . So σ is equiareal if and only if u2 (1+ f˙2 ) = 1, √ 2 df = ± 1−u . Thus, i.e. du u f (u) = ± Z √ p 1 1 − u2 −1 du = ± 1 − u2 − cosh u u (up to adding an arbitrary constant). This is a parametrization of the tractrix, so σ is equiareal ⇐⇒ σ is a reparametrization of the pseudosphere (see §8.3). 6.4.17 The first fundamental form of σ 3 is cos2 θdθ 2 + 2f˙ cos θdθdϕ + (1 + f˙2 )dϕ2 , where the dot denotes d/dθ. With E = cos2 θ, F = f˙ cos θ, G = 1 + f˙2 , EG−F 2 = cos2 θ. As this does not depend on f , the fact that the map σ 1 (θ, ϕ) 7→ σ 3 (θ, ϕ) is equiareal follows from the fact, proved in Theorem 6.4.6, that the map σ 1 (θ, ϕ) 7→ σ 2 (θ, ϕ) is equiareal. 6.5.1 If the internal angles are equal to α, Theorem 6.4.7 gives 3α − π = 4π/4, so α = 2π/3. Corollary 6.5.6 then gives the length of a side as A = cos−1 (−1/3). 6.5.2 Using the notation following Proposition 6.5.8, there is a rotation R1 of S 2 that takes a′ to a; then a further rotation R2 around the diameter through a that 52 b′ ) coincide with the side through a and b. By makes the side through a and R1 (b Corollary 6.5.6 the two triangles have sides of the same length, so we must have b′ ). If c and c′ are on the same side of the plane containing the side b = R2 R1 (b through a and b, we shall then have c = R2 R1 (cc′ ) and the isometry R2 R1 takes the triangle with vertices a′ , b′ , c′ to the triangle with vertices a, b, c; if they are on opposite sides the isometry R3 R2 R1 does this, where R3 is reflection in the plane containing the side through a and b. 6.5.3 By applying an isometry of R3 , which leaves lengths and areas unchanged, we can assume that p is the north pole (0, 0, 1). The spherical circle of radius R and centre p is then the circle of latitude ϕ = π/2 − R (Example 4.1.4), which is a circle of radius sin R. The area inside it is, by Example 6.1.3 and Proposition R 2π R π/2 6.4.2, 0 π/2−R cos θdθdϕ = 2π(1 − cos R). The maximum value of R is π; if π/2 ≤ R ≤ π, one replaces R by π − R in (i) and (ii). ′ ′ w+b ′ 6.5.4 (i) If M ′ (w) = ac′ w+d ′ is another unitary Möbius transformation, (M ◦ M )(w) = Aw+B , where A = a′ a + b′ c, B = a′ b + b′ d, C = c′ a + d′ c, D = c′ b + d′ d. Thus, Cw+D Ā = ā′ ā + b¯′ c̄ = d′ d + (−c′ )(−b) = D and similarly C = −B̄. Inverses are dealt with similarly. (ii) Denoting (x, y, z) ∈ R3 by (ξ, z) with ξ = x + iy ∈ C, the plane through the origin perpendicular to (a, b) is w̄a + wā + 2bz = 0, and reflection in it |w 2 −1 is F (ξ, z) = (ξ, z) − 2 w̄a+wā+2bz (a, b). Taking ξ = |w|2w 2 +1 , z = |w|2 +1 , we |a|2 +b2 2(|a|2 +b2 )w−2a(w̄a+wā+b(|w|2 −1)) , z′ (|w|2 +1)(|a|2 +b2 ) −ab|w|2 +b2 w−a2 w̄+ab ξ′ giving w′ = 1−z ′ = b2 |w|2 +bāw+baw̄+|a|2 find that F (ξ, z) = (ξ ′ , z ′ ), where ξ ′ = 2 2 2 2 (|a| +b )(|w| −1)−2b(w̄a+wā+b(|w| −1)) , (|w|2 +1)(|a|2 +b2 ) (−aw̄+b)(bw+a) −aw̄+b (bw̄+ā)(bw+a) = bw̄+ā . = = (iii) By Proposition 6.5.7, if F is any isometry of S 2 , F∞ = (M1 ◦ J) ◦ (M2 ◦ J) ◦ · · · ◦ (Mk ◦ J) for some k. Since J ◦ M ◦ J is easily seen to be a unitary Möbius transformation if M is one, part (i) implies that F∞ is a unitary Möbius transformation if k is even, and of the form M ◦ J with M unitary Möbius if k is odd. aw+b (iv) If a ∈ C, b ∈ R, call the unitary Möbius transformation M (w) = −bw+ā special unitary. Then M = F∞ ◦ J where F is as in (ii). Since J = R∞ where R is reflection in the yz-plane, M = (F ◦ R)∞ corresponds to the isometry F ◦ R of S 2 . It therefore suffices to prove that every unitary Möbius transformation is a composite of finitely-many special unitary Möbius transformations. If M ′ (w) = Aw+B is any unitary Möbius tranformation, where A, B ∈ C, let B = beiθ with −B̄w+Ā Aw+b b, θ ∈ R. Then M ′ = ρ◦M ◦ρ−1 , where ρ(w) = eiθ and M (w) = −bw+ are both Ā aw+b iθ/2 special unitary Möbius transformations (ρ(w) = −bw+ā with a = e , b = 0). 6.5.5 The dilation v 7→ R−1v, followed by a suitable translation, takes the sphere S of radius R to S 2 . It takes a triangle on S with sides of length A, B, C to a triangle 53 on S 2 with sides of length A/R, B/R, C/R and the same angles. Applying the A B A B cosine rule to the triangle on S 2 gives cos C R = cos R cos R + cos γ sin R sin R , where γ is the angle opposite the side of length C (and two similar formulas). 2 x x x is approximately equal to 1 − 2R If R is large, cos R 2 and sin R is approximately x equal to R . Substituting into the cosine rule gives C2 1− = 2R2 B2 AB A2 1− + 2 cos γ, 1− 2 2 2R 2R R 2 2 which gives C 2 = A2 + B 2 − 2AB cos γ − A2RB2 . Letting R → ∞ gives the usual cosine rule for a plane triangle with sides of length A, B, C and with γ the angle opposite the side of length C. This happens because when R → ∞ and A, B, C are fixed, the triangle becomes more and more nearly planar. (When standing at a point on a sphere of very large radius, one seems to be standing on a plane - this is why the Ancients thought the Earth is flat!) 6.5.6 Let n, a, b be the North Pole, Athens and Bombay, respectively, and let R = 6500km be the radius of the Earth. The angle at n of the spherical triangle with vertices n, a, b is 73◦ − 24◦ = 49◦ , and the lengths of the sides opposite b and a are obtained by multiplying by R the radian equivalents of 90◦ − 19◦ = 71◦ and 90◦ − 38◦ = 52◦ , respectively. If d is the spherical distance between Athens and Bombay, applying the cosine rule in the preceding exercise thus gives cos d = cos 52◦ cos 71◦ + sin 52◦ sin 71◦ cos 49◦ = 0.6892. R Hence, d/R = 0.8104 (radians) and d = 0.8104R = 5267km. 6.5.7 Drawing the diagonal of the square gives two spherical triangles with angles α/2, α/2 and α, the sides opposite these angles being A, A and D (the length of the diagonal). Applying the cosine rule to one of these triangles gives 1 cos A = cos A cos D + sin A sin D cos α, 2 2 2 cos D = cos A + sin A cos α. Using the sine rule (Proposition 6.5.3(ii)) gives sin D = sin A sin α/ sin 21 α = 2 sin A cos 21 α. Substituting the formulas for cos D and sin D into the first equation above gives 1 cos A = cos3 A + cos A sin2 A cos α + 2 sin2 A cos2 α. 2 Hence, cos A sin2 A(1 − cos α) = 2 sin2 A cos2 12 α, and this gives the desired formula for cos A. 54 6.5.8 (i) This is obvious by the sine rule. (ii) This follows immediately from Corollary 6.5.6. Similarly one proves that cos β + cos α cos γ = λ sin γ sin A cos B. (iii) By (ii), (cos α + cos β)(1 + cos γ) = cos α + cos β cos γ + cos β + cos α cos γ = λ sin γ sin B cos A + λ sin γ sin A cos B by (ii), which = λ sin γ(sin A cos B + cos A sin B) = λ sin γ sin(A + B). (iv) Writing the formula in (iii) in terms of half-angles gives 1 1 1 1 1 cos (α + β) cos (α − β) = λ tan γ sin (A + B) cos (A + B). 2 2 2 2 2 Similarly, the first of the two equations in (i) can be written 1 1 1 1 sin (α + β) cos (α − β) = λ sin (A + B) cos (A − B). 2 2 2 2 Dividing this equation by the preceding one gives the first formula in (iv). The second follows similarly from (iii) and the second equation in (i). (v) Applying the first formula in (iv) to the polar triangle, we get cos 21 (π − α − π + β) 1 1 tan (π − A + π − B) = cot (π − C), 1 2 2 cos 2 (π − α + π − β) i.e., Similarly, cos 12 (α − β) 1 1 tan C. tan (A + B) = 1 2 2 cos 2 (α + β) sin 12 (α − β) 1 1 tan (A − B) = tan C. 1 2 2 sin 2 (α + β) 6.5.9 If a′ 6= ±aa a rotation through an angle 12 dS 2 (aa, a′ ) around the line through the origin parallel to a × a′ takes a ′ to a . If a ′ = −aa the same thing is achieved by v. Thus, in all cases there is an isometry of S 2 applying the isometry v 7→ −v that takes a ′ to a. Since composites of isometries are isometries, it is sufficient to prove the result when a′ = a . If θ is the angle between the great circles passing through a and b and through a and b′ , a rotation by θ about the line through the origin and a fixes a and takes b′ to a point b′′ on the great circle passing through a and b. Since b and b′ are equidistant from a, so are b and b′′ . It follows that either b′′ = b or b′′ is obtained 55 by reflecting b in the plane passing through the origin and a perpendicular to the great circle passing through a and b. It is therefore sufficient to prove the theorem when a = a′ and b = b′ . The great circle passing through a and c makes the same angle with that passing through a and b as does the great circle passing through a and c′ . Hence, either these great circles coincide or one is obtained from the other by reflecting in the plane containing a, b and the origin. It therefore suffices to prove the result in the case where the two great circles coincide. Since c and c′ are the same distance from a on the same great circle, either they coincide or c′ is obtained from c by reflecting in the plane passing through the origin and a perpendicular to the great circle passing through a and c. Chapter 7 7.1.1 σ u = (1, 0, 2u), σ v = (0, 1, 2v), so N = λ(−2u, −2v, 1), where λ = √1+4u12 +4v 2 ; σ uu = (0, 0, 2), σ uv = 0, σ vv = (0, 0, 2), so L = 2λ, M = 0, N = 2λ, and the second fundamental form is 2λ(du2 + dv 2 ). Nu = −σ σ uu .N N (since σ u .N N = 0), so Nu .σ σ u = 0; similarly, Nu .σ σ v = Nv .σ σu = 7.1.2 σ u .N σ v = 0; hence, Nu and Nv are perpendicular to both σ u and σ v , and so Nv .σ are parallel to N . On the other hand, Nu and Nv are perpendicular to N since N is a unit vector. Thus, Nu = Nv = 0, and hence N is constant. Then, σ .N N)u = σ u .N N = 0, and similarly (σ σ .N N)v = 0, so σ .N N is constant, say equal to (σ N = d. d, and then σ is an open subset of the plane v.N N = ±N N, the sign being that of det(J). From σ̃ σ ũ = σ u ∂∂uũ + σ v ∂∂vũ , 7.1.3 From §4.5, Ñ ∂v σ ṽ = σ u ∂u σ̃ ∂ ṽ + σ v ∂ ṽ , we get ∂ 2u ∂ 2v σ σ σ σ̃ ũũ = u 2 + v 2 + σ uu ∂ ũ ∂ ũ 2 ∂v + 2M ∂u +N So L̃ = ± L ∂u ∂ ũ ∂ ũ ∂ ũ ∂u ∂ ũ 2 ∂v 2 ∂ ũ ∂u ∂v σ uv + 2σ + σ vv ∂ ũ ∂ ũ ∂v ∂ ũ 2 . N = σ v .N N = 0. This, to, since σ u .N gether with similar formulas for M̃ and Ñ , are equivalent to the matrix equation in the question. 7.1.4 Let σ be a surface patch, P a 3 × 3 orthogonal matrix, a ∈ R3 a constant vector, σ = P σ +aa. Then, σ̃ σ u = P σ u , σ̃ σ v = P σ v , so σ̃ σ u ×σ̃ σ v = ±σ σ u ×σ σ v (Proposition and σ̃ A.1.6), the sign being + if the isometry v 7→ P v +aa is direct and − if it is opposite. It follows that (in the obvious notation), L̃ = ±L, M̃ = ±M, Ñ = ±N . The v, where a is a non-zero constant, multiplies σ by a and hence dilation v 7→ av multiplies each of L, M, N by a. 7.1.5 σ u = (cos v, sin v, 0), σ v = (−u sin v, u cos v, 1), so σ u × σ v = (sin v, − cos v, u) 1 and N = √1+u (sin v, − cos v, u). Then, σ uu = 0, σ uv = (− sin v, cos v, 0), σ vv = 2 56 1 (−u cos v, −u sin v, 0). This gives L = σ uu.N = 0, M = σ uv .N = − √1+u , 2 √ . N = σ vv .N = 0. So the second fundamental form is −2dudv 1+u2 7.1.6 The tangent developable is parametrized by σ (u, v) = γ (u) + vtt(u), where t = dγγ /du. Using the standard notation and the Frenet-Serret equations, we find v n, σ v = t, σ u × σ v = −κvb b, N = − |v| σ u = t + κvn b, n+ σ uu = κn dκ n + κv(−κtt + τb b), σ uv = κn n, σ vv = 0. vn du 2 v , M = N = 0. So the second fundamental form is −κτ |v|du2 . Hence, L = −κτ |v| This vanishes at all points of the surface if and only if τ = 0 at all points of γ , which holds if and only if γ is planar (Proposition 2.3.3). In that case, the tangent developable is part of a plane. Thus, for tangent developables, the second fundamental form vanishes everywhere if and only if the surface is part of a plane. This is a special case of Exercise 7.1.2. 7.2.1 The paraboloid is the level surface f = 0 where f (x, y, z) = z − x2 − y 2 and (fx ,fy ,fz ) N = k(f is the corresponding unit normal. So G(x, y, z) = (4x(−2x,−2y,z) 2 +4y 2 +1)1/2 . x ,fy ,fz )k 7.2.2 This is obvious since changing the orientation changes the Gauss map G to −G. 7.2.3 The hyperboloid of one sheet x2 + y 2 − z 2 = 1 is obtained by rotating the hyperbola x2 − z 2 = 1 in the xz-plane around the z-axis. For this hyperbola, dz = xz → ±1 as x → ±∞. The unit normal to the hyperbola therefore makes dx an angle θ with the x-axis, where the angle θ takes all values in the range − π4 < θ < π4 . Rotating around the z-axis, it follows that the image of the Gauss map of the hyperboloid is the region of S 2 for which the latitude θ satisfies − π4 < θ < π4 . This is an annulus on S 2 . The hyperboloid of two sheets x2 − y 2 − z 2 = 1 is obtained by rotating the same hyperbola as above around the x-axis. The image of G is the union of√ two ‘caps’ 2 2 2 2 on S , namely the parts of the sphere x + y + z = 1 with |x| > 1/ 2. 7.3.1 Let t be the parameter for γ , let s be arc-length along γ , and denote d/dt by a dot 2 ds 2 ′′ ′ γ γ + ddt2s γ ′ . By Proposition 7.3.5, and d/ds by a dash. Then, γ̇γ = ds dt γ , γ̈ = dt 1 1 γ̇γ , (ds/dt) γ̇γ ii = hhγ̇γ , γ̇γ ii/(ds/dt)2 = hhγ̇γ , γ̇γ ii/hγ̇γ , γ̇γ i. For the κn = hhγγ ′ , γ ′ ii = hh (ds/dt) 3 ′′ N × γ̇γ ) = ds N × γ ′ ) = 0, we have γ̈γ.(N N × γ ′) = second part, since γ ′.(N γ .(N dt hγ̇γ , γ̇γ i3/2 κg . 7.3.2 Let γ be a unit-speed curve on the sphere of centre a and radius r. Then, (γγ − a).(γγ − a ) = r 2 ; differentiating gives γ̇γ .(γγ − a ) = 0, so γ̈γ .(γγ − a ) = −γ̇γ .γ̇γ = −1. At the point γ (t), the unit normal of the sphere is N = ± r1 (γγ (t) − a), so N = ± 1r γ̈γ .(γγ − a ) = ∓ 1r . κn = γ̈γ .N 57 7.3.3 If the sphere has radius R, the parallel with latitude θ has radius r = R cos θ; if p is a point of this circle, its principal normal at p is parallel to the line through p perpendicular to the z-axis, while the unit normal to the sphere is parallel to the line through p and the centre of the sphere. The angle ψ in Eq. 7.10 is therefore equal to θ or π − θ so κg = ± 1r sin θ = ± R1 tan θ. Note that this is zero if and only if the parallel is a great circle. σ u )+v̇(F σ v −Gσ u ) , σ + v̇σ σ , so by Exercise 6.4.7, N × γ̇γ = u̇(Eσ v −F√ 7.3.4 We have γ̇γ = u̇σ u v σ u + v̈σ σ v + u̇2 σ uu + 2u̇v̇σ σ uv + v̇ 2σ vv . Hence, γ̈γ = üσ N × γ̇γ ) = (u̇v̈ − v̇ü) κg = γ̈γ .(N where p EG−F 2 EG − F 2 + Au̇3 + B u̇2 v̇ + C u̇v̇ 2 + Dv̇ 3 , 1 σ v − F σ u ) = E((σ σu .σ σ v )u − σ u .σ σ uv ) − F (σ σ u .σ σ u )u A = σ uu .(Eσ 2 1 1 = E(Fu − Ev ) − F Eu , 2 2 with similar expressions for B, C, D. p p If F = 0, we find by this method that A = − 12 Ev E/G, B = Gu E/G − p p p p 1 E G/E, C = 12 Gv E/G − Ev G/E, D = 21 Gu G/E. 2 u N1 .n n, κ2 = κN N2 .n n, so 7.3.5 κ1 = κN N1 .n n)N N2 − (N N2 .n n)N N1 ) = κ(N N1 × N 2 ) × n . κ1 N2 − κ2 N1 = κ((N Taking the squared length of each side, we get N2 = κ2 k (N N1 × N2 ) × n k2 . κ21 + κ22 − 2κ1 κ2 N1 .N N2 = cos α; γ̇γ is perpendicular to N1 and N2 , so N1 × N2 is parallel to Now, N1 .N N1 × N 2 ) × n k = k N 1 × N 2 kk n k = sin α. γ̇γ , hence perpendicular to n; hence, k (N 7.3.6 A straight line has a unit-speed parametrization γ (t) = p + t q (with q a unit N = 0. In general, κn = 0 ⇐⇒ γ̈γ is vector), so γ̈γ = 0 and hence κn = γ̈γ .N perpendicular to N ⇐⇒ N is perpendicular to n ⇐⇒ N is parallel to b (since N is perpendicular to t). √ 7.3.7 The second fundamental form is (−du2 + u2 dv 2 )/u 1 + u2 , so a curve γ (t) = σ (u(t), v(t)) is asymptotic if and only if −u̇2 + u2 v̇ 2 = 0, i.e. dv/du = v̇/u̇ = ±1/u, so ln u = ±(v + c), where c is a constant. 7.3.8 By Proposition 7.3.2, if κn = κg = 0 then κ = 0. But a curve with zero curvature everywhere is part of a straight line. 58 7.3.9 We find that, at the point where u = v = 1, the first and second fundamental √ , respectively. Taking u = v = t, so forms are 32 du2 + 2dudv + 32 dv 2 and 2dudv 5 that u̇ = v̇ = 1, Exercise 7.3.1 gives the normal curvature as 2√ u̇v̇ 5 3 2 2 u̇ + 2u̇v̇ + 3 2 2 v̇ 2 = √ . 5 5 7.3.10 From Examples 6.1.3 and 7.1.2, the first and second fundamental forms are du2 + f (u)2 dv 2 and (f˙g̈ − f¨ġ)du2 + f ġdv 2 , respectively (a dot denoting d/du. We use the formulas in Exercise 7.3.1. (i) For a meridian we use u as the parameter, so the curve is γ (u) = σ (u, v) (with v constant). Note that γ is unit-speed. The second formula in Exercise 7.3.1 gives κn = f˙g̈ − f¨ġ. Now, γ̇γ = (f˙ cos v, f˙ sin v, ġ), γ̈γ = (f¨ cos v, f¨ sin v, g̈), N×γ̇γ ) = 0. N = (−ġ cos v, −ġ sin v, f˙) (from Example 7.1.2 again), giving κg = γ̈γ. (N (ii) For a parallel we use v as the parameter, so the curve is Γ(v) = σ (u, v) Γ/dv = (with u constant). Note that Γ is not unit-speed in general. Now, dΓ 2Γ 2 Γ.(N N × Γ̇ Γ) = f 2 f˙. (−f sin v, f cos v, 0), d /dv = (−f cos v, −f sin v, 0), giving Γ̈ 2 ˙ ˙ Hence, κg = ff 3f = ff . 7.3.11 The paraboloid z = x2 + y 2 is obtained by rotating the parabola z = x2 in the xz-plane around the z-axis. We could therefore use the preceding exercise but we would need a unit-speed parametrization of the parabola, which is complicated. Proceeding directly, parametrize the paraboloid by σ (u, v) = (u cos v, u sin v, u2 ). 2 +2u2 dv 2 , The first and second fundamental forms are (1+4u2 )du2 +u2 dv 2 and 2du√1+4u 2 respectively. A curve u = constant can be parametrized by γ (v) = σ (u, v). 2 Hence, κn = √ 2u 1+4u2 u2 . Now, denoting d/dv by a dot, we find that γ̇γ = (−u sin v, u cos v, 0), γ̈γ = 1 (−2u cos v, −2u sin v, 1), which gives (−u cos v, −u sin v, 0), and N = √1+4u 2 N × γ̇γ ) = γ̈γ .(N 2 √ u . 1+4u2 Hence, κg = 1 u3 × 2 √ u 1+4u2 = √ 1 . u 1+4u2 7.3.12 σ u = t + vδ̇δ , σ v = δ , so along γ (where v = 0) we have σ u = t, σ v = δ and hence ×δ N = tsin θ . Hence, δ − cos θtt (tt × δ ) × t N×t= = , sin θ sin θ so ṫt.δ N × t) = κg = ṫt.(N , sin θ since ṫt.t = 0. Differentiating t.δ = cos θ gives ṫt.δ = − sin θ θ̇ − t.δ̇δ , hence the stated formula for κg . 59 7.3.13 A curve v = constant is parametrized by γ (u) = σ (u, v), so (denoting d/du by N × σ u ). Now, σ u.σ u = σ v .σ v = 1, a dot) γ̇γ = σ u , γ̈γ = σ uu and κ′g = σ uu.(N σ u ×σ v σ u.σ v = cos θ, so N = sin θ and 1 1 σu × σ v ) × σ u = σ v − cos θσ σ u ). N × σu = (σ (σ sin θ sin θ Hence, σ uu.σ u σ uu.σ v − cos θσ . κ′g = sin θ By Exercise 6.1.9, σ uu.σ u = 0, σ uu.σ v = −θu sin θ. Inserting these formulas in the preceding equation for κ′g gives κ′g = −θu . The formula for κ′′g is proved similarly. 7.3.14 From the solution to Exercise 7.3.4, √ X κg = EG(u̇v̈ − üv̇) + √ , EG where 1 1 1 1 3 2 EGv − GEv u̇v̇ 2 + GGu v̇ 3 X = − EEv u̇ + EGu − GEu u̇ v̇ + 2 2 2 2 1 1 = − Ev (1 − Gv̇ 2 )u̇ + EGu − GEu u̇2 v̇ 2 2 1 1 + EGv − GEv u̇v̇ 2 + Gu (1 − E u̇2 )v̇ 2 2 1 1 1 = (Gu v̇ − Ev u̇) − G(Eu u̇ + Ev v̇)u̇v̇ + E(Gu u̇ + Gv v̇)u̇v̇. 2 2 2 Substituting into the formula for κg gives the desired result. 7.3.15 A parameter curve v = constant can be parametrized by γ (u) = σ (u, v), but this curve will not be unit-speed in general. √Let s be the arc-length of γ and denote √ d/ds by a dot. Then, ds/du = k σ u k= E, so u̇ = 1/ E. Since v̇ = v̈ = 0, the formula in the preceding exercise gives Ev u̇ Ev κ′g = − √ =− √ . 2 EG 2E G ′′ The formula for κg is proved similarly. √ √ We have cos θ = u̇ E, sin θ = v̇ G, so d d θ̇ = cos θ (sin θ) − sin θ (cos θ) ds ds √ √ √ √ v̇ u̇ = u̇ E v̈ G + √ (Gu u̇ + Gv v̇) − v̇ G ü E + √ (Eu u̇ + Ev v̇) 2 G 2 E ! r r √ 1 E G = EG(u̇v̈ − üv̇) + u̇v̇ (Gu u̇ + Gv v̇) − (Eu u̇ + Ev v̇) . 2 G E 60 Using the preceding exercise and the first part of this exercise, we get √ √ 1 (Gu v̇ − Ev u̇) = κg + κ′g u̇ E + κ′′g v̇ G = κg − κ′g cos θ − κ′′g sin θ. θ̇ = κg − √ 2 EG 7.3.16 Let γ (t) be a unit-speed parametrization of C, and let p = γ (t0 ). Let N be a unit N. Denoting normal of S at p. Then, a parametrization of C˜ is γ̃γ = γ − (γγ .N )N ¨ ˙ N, so the curvature of γ̃γ N, γ̃γ = γ̈γ − (γ̈γ .N)N d/dt by a dot as usual, γ̃γ = γ̇γ − (γ̇γ.N)N at p is N) k = k γ̇γ (t0 ) × (N N × (γ̈γ (t0 ) × N)) k, κ̃ = k γ̇γ (t0 ) × (γ̈γ (t0 ) − (γ̈γ (t0 )..N)N since γ̃γ˙ (t0 ) = γ̇γ (t0 ) is a unit vector. Now, γ̈γ (t0 ) = κg N × γ̇γ (t0 ) + κn N, where κg and κn are the geodesic and normal curvatures of γ at p. Hence, γ̈γ (t0 ) × N = N × γ̇γ (t0 )) × N = κg γ̇γ (t0 ), so κg (N κ̃ = k γ̇γ (t0 ) × (κg N × γ̇γ (t0 )) k = |κg | k γ̇γ (t0 ) kk N × γ̇γ (t0 ) k = |κg | as N and γ̇γ (t0 ) are perpendicular unit vectors. 2 2 −dv 7.3.17 The second fundamental form is √du , so a curve γ (t) = σ (u(t), v(t)) is 1+u2 +v 2 2 2 asymptotic if and only if u̇ − v̇ = 0, i.e. u + v or u − v is constant. If u + v = c, say, where c is a constant, then σ (u, v) = (u, c − u, 12 c(2u − c)), which is a parametrization of a straight line. Similarly if u − v is constant. Geometrically, the surface is a hyperbolic paraboloid and is doubly ruled (Exercise 5.2.5). Both of the straight lines on the surface passing through a given point are asymptotic curves (Exercise 7.3.6). b) = t along γ ; σ v = n. Hence, along 7.3.18 In the usual notation, σ u = t + v(−κtt + τb n + v τ̇b b = κn n γ , σ u × σ v = b. Next, we find that σ uu = −v κ̇tt + (κ − (κ2 + τ 2 )v)n along γ . The parameter curve v = 0 is asymptotic if and only if L = 0. But, n.b = 0. along γ , L = σ uu.N = κn 7.3.19 Parametrize the surface by σ (u, v) = (u2 cos v, u2 sin v, 2u). The second funda2 +2u2 dv 2 mental form is −2du√1+u , so the asymptotic curves are given by 2 −2u̇2 + 2u2 v̇ 2 = 0. This gives v = ± ln u + c, where c is an arbitrary constant. The projection of this asymptotic curve on the xy-plane is given by x = u2 cos v, y = u2 sin v. Since u2 = e±2(v−c) , this is a logarithmic spiral. 7.3.20 Let γ be a unit-speed parametrization of C. Then, γ is asymptotic ⇐⇒ γ̈γ .N = 0 ⇐⇒ n.N = 0, where N is a unit normal to S and n is the principal normal of 61 γ . Since γ̇γ = t is perpendicular to N, γ is asymptotic ⇐⇒ N is perpendicular to both t and n. But the osculating plane is spanned by t and n. 7.3.21 If every curve on a surface is asymptotic, Lu̇2 + 2M u̇v̇ + N v̇ 2 = 0 for all curves γ (t) = σ (u(t), v(t)) on the surface. This is possible only if L = M = N = 0 everywhere. By Exercise 7.1.2 this implies the surface is an open subset of a plane. 7.3.22 N.n = cos ψ, N.t = 0, so N.b = sin ψ; hence, N = n cos ψ + b sin ψ and B = n cos ψ + b sin ψ) = b cos ψ − n sin ψ. Hence, t × (n N = ṅ n cos ψ + ḃ b sin ψ + ψ̇(−n n sin ψ + b cos ψ) Ṅ b) cos ψ − nτ sin ψ + ψ̇(−n n sin ψ + b cos ψ) = (−κtt + τb b cos ψ − n sin ψ) = −κ cos ψtt + (τ + ψ̇)(b = −κn t + τg B. B is proved similarly. Since {tt, N, B} is a right-handed orthonorThe formula for Ḃ 3 N, Ḃ B in terms mal basis of R , Exercise 2.3.6 shows that the matrix expressing ṫt, Ṅ of t, N, B is skew-symmetric, hence the formula for ṫt. N; then, B = t × N = ∓n n. Hence, 7.3.23 By Exercise 7.3.6, b is parallel to N, so b = ±N B = ∓ṅ n = ∓(−κtt + τb b) = ±κtt − τN N; comparing with the formula for Ḃ B in the Ḃ preceding exercise shows that τg = τ (and κn = ±κ). 7.4.1 ṽv is a smooth function of t and lies in Tγ (ϕ(t)) S = Tγ̃γ (t) S, so ṽv is a tangent vector v dϕ , field along γ̃γ . The formula follows from Eq. (7.11) and the fact that ddtv = ddṽ t̃ dt v = 0 ⇐⇒ ∇γ v = 0. where t̃ = ϕ(t). The last part follows since ϕ̇ 6= 0 so ∇γ̃γ ṽ 7.4.2 If p and q correspond to the parameter values t = a and t = b, respectively, let qp is Γ(t) = γ (a + b − t) (thus, Γ is γ ‘traversed backwards’). We show that Π Γ pq the inverse of Πγ . Let w ∈ Tp S and let v be the tangent vector field parallel pq w ) = v(b). By Exercise 7.4.1, V (t) = along γ such that v(a) = w. Then, Πγ (w qp qp V(a)) = V(b) = v(a) = w . v(b)) = Π (V v(a + b − t) is parallel along Γ so Π (v Γ Γ pq qp This proves that Π ◦ Πγ is the identity map on Tp S. One proves similarly Γ qp pq is the identity map (or by interchanging the roles of γ and Γ) that Πγ ◦ Π Γ on Tq S. 7.4.3 Let α, β, γ be the internal angles of the triangle at p, q, r, respectively. Since the arc through p and q is part of a great circle, the tangent vector of the arc is parallel along the arc (Example 7.4.7). So the result of parallel transporting v0 to q along the arc pq through p and q is a vector v1 tangent to pq at q. Now v1 makes an angle π − β with the arc qr at q, so parallel transporting v1 along qr 62 to r gives a vector v2 which makes an angle (π − β) + (π − γ) with the arc rp at r. Parallel transporting v2 along rp to p then gives a vector v3 which makes an angle (π − β) + (π − γ) + (π − α) with v0 . Since v0 , v1 , v2 , v3 all have the same length (Proposition 7.4.9(ii)), the result follows from Theorem 6.4.7. 7.4.4 Putting E = G = 1, F = cos θ in the formulas in Proposition 7.4.4 gives Γ111 = θu cot θ, Γ211 = −θu cosec θ, Γ122 = −θv cosec θ, Γ222 = θv cot θ, Γ112 = Γ212 = 0. 7.4.5 In the notation of Proposition 7.4.5, the tangent vector σ v to the parameter curves u = constant are given by α = 0, β = 1, and a curve v = constant corresponds to v̇ = 0 (and u̇ 6= 0). From Eq. 7.13, σ v is parallel along the curves v = constant if and only if Γ112 = Γ212 = 0; from the formulas in Proposition 7.4.4, this holds if and only if (*) GEv = F Gu and EGu = F Ev . If the parameter curves form a Chebyshev net, Ev = Gu = 0 (Exercise 6.1.5), so (*) holds. Conversely, if (*) holds than (EG − F 2 )Gu = G(EGu ) − F (F Gu ) = G(F Ev ) − F (GEv ) = 0 and so Gu = 0; then GEv = 0 by (*) again, so Ev = 0. Hence, if (*) holds the parameter curves form a Chebyshev net. This proves that (i) is equivalent to (ii). That (i) is equivalent to (iii) is proved similarly. .σ v = F/√EG, so A = √EG − EG cos2 θ = √EG sin θ. 7.4.6 We have cos θ = kσσuukk σv k Differentiating the first equation with respect to u and using the second equation gives √ 2EGFu − F GEu − EF Gu EG F √ −θu = = . A 2AEG EG u On the other hand, the formulas in Proposition 7.4.4 give Γ211 Γ112 1 2EFu − EEv − F Eu GEv − F Gu + = + E G 2A2 E G 2EGFu − F GEu − EF Gu = . 2A2 EG 7.4.7 From A2 = EG − F 2 we get 2AAu = EGu + GEu − 2F Fu . On the other hand, u −2F Fu . By the the formulas in Proposition 7.4.4 give Γ111 + Γ212 = GEu +EG 2A2 preceding formula, this is equal to 2AAu /2A2 = Au /A. The other formula is proved similarly. 63 Chapter 8 8.1.1 Parametrize the surface by σ (x, y) = (x, y, f (x, y)). Then, σ x = (1, 0, fx), σ y = (0, 1, fy ), N = (1 + fx2 + fy2 )−1/2 (−fx , −fy , 1), σ xx = (0, 0, fxx), σ xy = (0, 0, fxy ), σ yy = (0, 0, fyy ). This gives E = 1 + fx2 , F = fx fy , G = 1 + fy2 and L = (1 + fx2 + fy2 )−1/2 fxx , M = (1 + fx2 + fy2 )−1/2 fxy , N = (1 + fx2 + fy2 )−1/2 fyy . By Corollary 8.1.3, K = 2 fxx fyy −fxy , (1+fx2 +fy2 )2 H= (1+fy2 )fxx −2fx fy fxy +(1+fx2 )fyy . 2(1+fx2 +fy2 )3/2 8.1.2 For the helicoid σ (u, v) = (v cos u, v sin u, λu), σ u = (−v sin u, v cos u, λ), σ v = (cos u, sin u, 0), 1 (−λ sin u, λ cos u, −v), N= √ λ2 + v 2 σ uu = (−v cos u, −v sin u, 0), σ uv = (− sin u, cos u, 0), σ vv = 0. √ This gives E = λ2 + v 2 , F = 0, G = 1 and L = N = 0, M = λ/ λ2 + v 2 . Hence, K = (LN − M 2 )/(EG − F 2 ) = −λ2 /(λ2 + v 2 )2 . For the catenoid σ (u, v) = (cosh u cos v, cosh u sin v, u), σ u = (sinh u cos v, sinh u sin v, 1), σ v = (− cosh u sin v, cosh u cos v, 0), N = sech u(− cos v, − sin v, sinh u), σ uu = (cosh u cos v, cosh u sin v, 0), σ uv = (− sinh u sin v, sinh u cos v, 0), σ vv = (− cosh u cos v, − cosh u sin v, 0). This gives E = G = cosh2 u, F = 0 and L = −1, M = 0, N = 1. Hence, K = (LN − M 2 )/(EG − F 2 ) = −sech4 u. σ v is never zero, N = σ u ×σ σ v / k σ u ×σ σ v k is smooth. 8.1.3 Since σ is smooth and σ u ×σ Hence, E, F, G, L, M and N are smooth. Since EG − F 2 > 0 (by the remark following Proposition 6.4.2), the formulas in Corollary 8.1.3 show that H and K are smooth. N = 0 ⇐⇒ δ̇δ .((tt +vδ̇δ )×δδ ) = 0 ⇐⇒ δ̇δ .(tt ×δδ ) = 8.1.4 From Example 8.1.5, K = 0 ⇐⇒ δ̇δ .N b, t × δ = b, so K = 0 ⇐⇒ τ = 0 ⇐⇒ γ is planar (by 0. If δ = n, δ̇δ = −κtt + τb n, t × δ = −n n, so again K = 0 ⇐⇒ τ = 0. Proposition 2.3.3). If δ = b, δ̇δ = −τn 64 8.1.5 The dilation (x, y, z) 7→ (ax, ay, az), where a is a non-zero constant, multiplies E, F, G by a2 and L, M, N by a, hence H by a−1 and K by a−2 (using Corollary 8.1.3). 8.1.6 This follows immediately from Definition 8.1.1 and the hint. 8.1.7 Suppose that the cone is the union of the straight lines joining points of a curve C to a vertex v. It is clear that the Gauss map G is constant along the rulings of the cone, so the image of the cone under G is the same as the image of C under G, which is a curve. 8.1.8 By Eq. 8.2, the area of σ (R) is ZZ R k Nu × Nv k dudv = ZZ R |K| k σ u × σ v k dudv = ZZ R |K|dAσ . 8.1.9 Using the parametrization σ in Exercise 4.2.5, we find that E = b2 , F = 0, G = cos θ (a+b cos θ)2 and L = b, M = 0, N = (a+b cos θ) cos θ. This gives K = b(a+b cos θ) . + − It follows that S and S are the annular regions on the torus given by −π/2 ≤ u ≤ π/2 and π/2 ≤ u ≤ 3π/2, respectively. S+ S− It is clear that as a point p moves over S + RR (resp. S − ), the unit normal at p RR covers the whole of S 2 . Hence, S + |K|dA = S − |K|dA = 4π by the preceding exercise; since |K| = ±K on S ± , this gives the result. wu.N)N N so 8.1.10 ∇uw = wu − (w wuv .N)N N − (w wu .Nv )N N − (w wu .N)N Nv − (w wuv .N)N N ∇v (∇u w) = wuv − (w wuv .N)N N + (w wu.N v )N N + (w wu.N)(N Nv .N)N N + (w wuv .N)N N − (w wu.N)N Nv . = wuv − (w 65 Interchanging u and v and subtracting gives the first formula. Replacing w by w in this formula gives λw wv .N)N Nu −(w wu.N)N Nv }+λv (w w.N)N Nu −λu (w w.N )N Nv = λ{(w wv .N )N Nu −(w wu.N)N Nv } λ{(w since w.N = 0. It is also obvious that w1 + w 2 )) − ∇u (∇v (w w1 + w 2 )) = (∇v (∇uw 1 ) − ∇u (∇v w1 )) ∇v (∇u (w + (∇v (∇uw2 ) − ∇u (∇v w 2 )) for any two tangent vector fields w1 , w2 . σ uv .N)N Nu − (σ σ uu.N )N Nv = MN Nu − LN Nv (in the Now ∇v (∇uσ u ) − ∇u (∇v σ u ) = (σ σ σ σ u + dσ σv ) usual notation). Using Proposition 8.1.2, this = M (aσ u + bσ v ) − L(cσ and using the explicit expressions for a, b, c, d in Proposition 8.1.2 this becomes σv − F σ u ). Similarly, ∇v (∇uσ v ) − ∇u (∇v σ v ) = K(−Gσ σ u + F σ v ). K(Eσ If (*) ∇v (∇uw) − ∇u (∇v w) = 0 for all w, then taking w = σ u gives K = 0 since E 6= 0, σ v 6= 0. Conversely, if K = 0 then (*) holds for w = σ u and σ v , and hence by the first part of the σ u + βσ σ v for all smooth functions α, β of (u, v). But every exercise it holds for ασ tangent vector field w is of this form. 8.1.11 σ u = (1, 1, v), σ v = (1, −1, u), σ uu = σ vv = 0, σ uv = (0, 0, 1). When√u = v = 1, we find from this that E = 3, F = 1, G = 3 and L = N = 0, M = −1/ 2. Hence, K =√(LN − M 2 )/(EG − F 2 ) = −1/16, H = (LG − 2M F + N G)/2(EG − F 2 ) = 1/8 2. 8.1.12 r We write the equation of the quadric in the form z = f (x, y), where f (x, y) = 2 2 c 1 − xa − yb . The result of the calculation will give the value of the Gauss- ian curvature K on the part of the quadric where z > 0. Similar calculations (with the same result) give K on the parts of the surface where z < 0, x > 0, x < 0, y > 0 and y < 0. Together these regions cover the whole surface. r 2 2 Taking f (x, y) = c 1 − xa − yb , and applying the first formula in Exercise 8.1.1, we get, after straightforward calculation, 2 2 2 y x z 1 a + b + c K= 2 . abc x2 y2 z2 + b2 + c2 a2 66 The vector ∇ x2 a + y2 b + z2 c =2 x y z a, b, c (x, y, z).. xa , yb , zc d= q y2 x2 z2 a2 + b2 + c2 =q This gives the stated formula for K. For the paraboloid we take f (x, y) = 8.1.1 gives K= The vector x y 2a , 2b , −1 (x, y, z).. q d= x2 4a2 x2 a 4ab 1 + + 1 x2 a2 y2 b 1 x2 4a2 + + y2 b2 + z2 c2 . . The first formula in Exercise y2 4b2 2 . is normal to the surface, so x y 2a , 2b , −1 + 1 4 is normal to the surface, so y2 4b2 +1 x2 2a =q + x2 4a2 y2 2b + −z y2 4b2 +1 =q x2 4a2 |z| + y2 4b2 . +1 Hence, K = d4 /4abz 4 . 8.1.13 Taking f (x, y) = 1/xy, we get fx = −z/x, fy = −z/y, fxx = 2z/x2 , fxy = z/xy, fyy = 2z/y 2 . The first formula in Exercise 8.1.1 gives K= 4z 2 x2 y 2 1+ − z2 x2 z2 x2 y 2 + z2 y2 2 = 3x−2 y −2 z −2 , (x−2 + y −2 + z −2 )2 hence the stated formula for K. Similarly, the second formula in Exercise 8.1.1 gives 2z z2 2z 3 2z z2 1 + − + 1 + x2 y2 x2 y 2 y2 x2 1 xyz(x2 + y 2 + z 2 ) p H= = = . 2 2 + y 2 + z 2 )3/2 2 + y 2 + z 2 )3/2 2 + y2 + z2 (x (x x 3 3 x y We showed in Exercise 5.1.3 that the smallest value of X 2 + Y 2 + Z 2 subject to the condition XY Z = 1 is 3, and that it is attained precisely when (X, Y, Z) = (1, −1, −1), (−1, 1, −1), (−1, −1, 1) or (1, 1, 1). Taking X = 1/x, Y = 1/y, Z = 1/z, it follows that the largest value of K is 3(1+1+1)−2 = 1/3, and that it is attained precisely when (1/x, 1/y, 1/z) = (1, −1, −1), (−1, 1, −1), (−1, −1, 1) or (1, 1, 1), i.e. when (x, y, z) = (1, −1, −1), (−1, 1, −1), (−1, −1, 1) or (1, 1, 1). As noted in the solution to Exercise 5.1.3, these points lie at the vertices of a regular tetrahedron. 67 8.1.14 If the circle in the xz-plane has radius a and touches the z-axis at the point (0, 0, c), it can be parametrized by γ (u) = (a(1 + cos u), 0, a sin u + c). Rotating γ (u) around the z-axis through an angle v gives the point (a(1 + cos u) cos v, a(1 + cos u) sin v, a sin u + c). Since the circle rotates at constant angular velocity and moves parallel to the z-axis at constant speed, the distance it moves parallel to the z-axis in the time taken to rotate through an angle v is a constant multiple of v, say bv. Hence, after the circle has rotated through an angle v the point initially at γ (u) will have moved to the point σ (u, v) in the statement of the exercise. If a = b and c = 0 we have σ (u, v) = a((1 + cos u) cos v, (1 + cos u) sin v, sin u + v). We find that the first fundamental form is a2 (du2 + 2 cos ududv + ((1 + cos u)2 + 1)dv 2 ). Let A = k σ u × σ v k = fundamental form is √ EG − F 2 , so that A2 = 2a4 (1 + cos u). The second a3 ((1 + cos u)du2 − 2 sin2 ududv + (1 + cos u)2 cos udv 2 ). A The first formula in Corollary 8.1.3 now gives K= a6 ((1 + cos u)3 cos u − sin4 u) . A4 Writing c = cos u we get K= c(1 + c) − (1 − c)2 3 cos u − 1 c(1 + c)3 − (1 − c2 )2 = = . 4a2 (1 + c)2 4a2 4a2 Since d = a(1 + cos u), this agrees with the formula in the statement of the exercise. 8.1.15 Using the parametrization in Example 8.1.5, we have σ u × σ v = γ̇γ × δ + vδ̇δ × δ . √ Recalling that k σ u × σ v k = EG − F 2 , the formula for K in that example becomes −(δ̇δ. (γ̇γ × δ ))2 K= . k γ̇γ × δ + vδ̇δ × δ k4 If δ̇δ ×δδ 6= 0, K → 0 as v → ∞ (with u fixed); thus, if K is constant we must have K = 0. On the other hand, if δ̇δ × δ = 0, δ̇δ is parallel to δ , hence δ̇δ.(γ̇γ × δ ) = 0 and again K = 0. 68 8.1.16 We use the parametrization σ (s, θ) in Exercise 4.2.7, a dot to denote d/ds, and the standard notation relating to the Frenet-Serret data for γ . Then, σ s = n + τ a cos θb b, σ θ = −a sin θn n + a cos θb b. Hence, (1 − κa cos θ)tt − τ a sin θn n + sin θb b), σ s × σ θ = −a(1 − κa cos θ)(cos θn n + sin θb b), E = (1 − κa cos θ)2 + τ 2 a2 , F = τ a2 , G = a2 and so N = −(cos θn EG − F 2 = a2 (1 − κa cos θ)2 . Next, n σ ss = (κτ a sin θ − κ̇a cos θ)tt + (κ(1 − κa cos θ) − τ̇ a sin θ − τ 2 a cos θ)n b, + (τ̇ a cos θ − τ 2 a sin θ)b n − τ a sin θb b, = κa sin θtt − τ a cos θn σ sθ n − a sin θb b. σ θθ = −a cos θn Hence, L = aτ 2 − κ cos θ(1 − κa cos θ), M = τ a, N = a, Thus, K= −κa cos θ(1 − κa cos θ) −κ cos θ = . 2 2 a (1 − κa cos θ) a(1 − κa cos θ) (i) We have dA = k σ s × σ θ k dsdθ = a(1 − κa cos θ)dsdθ, so Z ℓZ 0 (ii) Since R 2π 0 2π KdA = 0 Z ℓZ 0 | cos θ|dθ = 2 R π/2 −π/2 Z ℓZ 0 2π (−κ cos θ)dsdθ = 0. 0 cos θdθ = 4, we get 2π 0 |K|dA = 4 Z ℓ κ(s)ds. 0 8.1.17 It follows from Exercises 6.1.2 and 7.1.4 that applying a direct isometry of R3 leaves both H and K unchanged, while applying an opposite isometry leaves K unchanged but changes the sign of H. 8.1.18 From the proof of Proposition 7.3.3, if γ is unit-speed its normal curvature is κn = N.γ̇γ = W(γ̇γ )..γ̇γ . Hence, γ is asymptotic if and only if W(γ̇γ ) is perpendicular to −Ṅ γ̇γ at each point of γ . Since −W(γ̇γ ) is the tangent vector of the image of γ under the Gauss map of S, the result follows. N = −W(γ̇γ ), and that W is self-adjoint (Corollary 7.2.4), we have 8.1.19 Recalling that Ṅ to prove that hW 2 (γ̇γ ) − 2HW(γ̇γ ) + K γ̇γ , γ̇γ i = 0. This follows from the preceding exercise. 69 We can assume that γ is unit-speed. As in the solution of Exercise 8.1.18, if γ N.γ̇γ = 0 and the first part gives Ṅ N.Ṅ N = −K. But by Exercise is asymptotic then Ṅ b so Ṅ N = ∓τn n (where n is the principal normal 7.3.6, if γ is asymptotic, N = ±b 2 N.Ṅ N=τ . of γ and b is its binormal). Hence, Ṅ 8.2.1 For the helicoid σ (u, v) = (v cos u, v sin u, λu), √ the first and second fundamental 2 2 2 2 forms are (λ + v )du + dv and 2λdudv/ λ2 + v 2 , respectively. Hence, the −κ(λ2 + v 2 ) √λ2λ+v 2 = 0, i.e. κ = principal curvatures are the roots of √ λ −κ λ2 +v 2 ±λ/(λ2 + v 2 ). For the catenoid σ (u, v) = (cosh u cos v, cosh u sin v, u), the first and second fundamental forms are cosh2 u(du2 +dv 2 ) and −du2 +dv 2 , so the principal curvatures −1 − κ cosh2 u 0 are the roots of = 0, i.e. κ = ±sech2 u. 0 1 − κ cosh2 u N. 8.2.2 This is obvious, since W(γ̇γ ) = −Ṅ σ u + v̇σ σ n is a principal vector for all t ⇐⇒ 8.2.3 γ is a line of curvature ⇐⇒ γ̇γ = u̇σ L M E F =κ for some scalar κ. Writing this matrix equation as two L N F G scalar equations and then eliminating κ gives the stated equation. For the second part, if the second fundamental form is a multiple of the first, the Weingarten map is a scalar multiple of the identity map, so every tangent vector is principal and every curve on the surface is a line of curvature. If F = M = 0 the matrices FI and FII are diagonal, hence so is the matrix FI−1 FII of the σ u , σ v }. This means that σ u and Weingarten map with respect to the basis {σ σ v are principal vectors, i.e. that the parameter curves v = constant and u = constant are lines of curvature. Conversely, if every parameter curve is a line of curvature, the stated equation must hold if u̇ = 0 and if v̇ = 0. This gives EM = F L and F N = GM , which imply that (EN −GL)F = EGM −EGM = 0 and so either EN = GL or F = 0. If F = 0 then GM = 0 so M = 0 and (ii) holds. If EN = GL the equation in the exercise implies that every curve is a line of curvature, so every tangent vector is principal, so (i) holds. Condition (i) implies that the two principal curvatures are equal everywhere, i.e. every point is an umbilic, so σ is an open subset of a plane or a sphere by Proposition 8.2.9. From Examples 6.1.3 and 7.1.2, the first and second fundamental forms of a surface of revolution are du2 + f (u)2 dv 2 and (f˙g̈ − f¨ġ)du2 + f ġdv 2 , respectively. Since the terms dudv are absent, the vectors σ u and σ v are principal; but these are tangent to the meridians and parallels, respectively. 70 N1.(tt × N 1 ) = 0. Since Ṅ N1 is 8.2.4 Let N 1 be a unit normal of S. Then, K = 0 ⇐⇒ Ṅ N1 perpendicular to N1 and N1 is perpendicular to t , this condition holds ⇐⇒ Ṅ N1 = −λγ̇γ for some scalar λ. Now use Exercise 8.2.2. is parallel to t, i.e. ⇐⇒ Ṅ 8.2.5 Let N 1 and N2 be unit normals of the two surfaces; if γ is a unit-speed parametrizaN1 = −λ1 γ̇γ for some scalar λ1 by Exercise 8.2.2. If C is a line tion of C, then Ṅ N2 = −λ2 γ̇γ for some scalar λ2 , and then (N N1 .N N2 )˙ = of curvature of S2 , then Ṅ N2 − λ2 γ̇γ .N N1 = 0, so N1 .N N2 is constant along γ , showing that the angle −λ1γ̇γ .N N2 is constant, then N1 .Ṅ N2 = 0 between S1 and S2 is constant. Conversely, if N1 .N N1 .N N2 = −λ1 γ̇γ .N N2 = 0; thus, Ṅ N2 is perpendicular to N1 , and is also persince Ṅ pendicular to N2 as N 2 is a unit vector; but γ̇γ is also perpendicular to N1 and N2 must be parallel to γ̇γ , so there is a scalar λ2 (say) such that N2 ; hence, Ṅ N2 = −λ2 γ̇γ . Ṅ 8.2.6 (i) Differentiate the three equations in (8.5) with respect to w, u and v, respectively; this gives σ v + σ u .σ σ vw = 0, σ uv .σ σ w + σ v .σ σ uw = 0, σ vw .σ σ u + σ w .σ σ uv = 0. σ uw .σ σ vw = 0, Subtracting the second equation from the sum of the other two gives σ u .σ σ uw = σ w .σ σ uv = 0. and similarly σ v .σ σ w = 0, it follows that the matrix FI for the u = u0 surface is (ii) Since σ v .σ diagonal (and similarly for the others). Let N be the unit normal of the u = u0 surface; N is parallel to σ v × σ w by definition, and hence to σ u since σ u , σ v and σ u = 0, hence σ vw .N N = 0, proving that the σ w are perpendicular; by (i), σ vw .σ matrix FII for the u = u0 surface is diagonal. (iii) By part (ii), the parameter curves of each surface u = u0 are lines of curvature. But the parameter curve v = v0 , say, on this surface is the curve of intersection of the u = u0 surface with the v = v0 surface. 8.2.7 On the open subset of the ellipsoid qwith z 6= 0, we can use the parametrization 2 2 σ (x, y) = (x, y, z), where z = ±r 1 − xp2 − yq 2 . By Proposition 8.1.2 and the remarks following Proposition 8.2.1, the condition for an umbilic is that FII = κFI for some scalar κ. The formulas in the solution of Exercise 8.1.1 lead to the equations zxx = λ(1 + zx2 ), zxy = λzx zy , zyy = λ(1 + zy2 ), where q λ = κ 1 + zx2 + zy2 . If x and y are both non-zero, the middle equation gives λ = −1/z, and substituting into the first equation gives the contradiction p2 = r 2 . Hence, either x = 0 or y = 0. If x = 0, the equations have the four solutions x = 0, y = ±q s q2 p2 − , z = ±r 2 q − r2 s r 2 − p2 . r2 − q2 71 Similarly, one finds the following eight other candidates for umbilics: s s 2 2 p −q r2 − q2 , y = 0, z = ±r , x = ±p p2 − r 2 r 2 − p2 s s p2 − r 2 q2 − r2 x = ±p , y = ±q , z = 0. p2 − q 2 q 2 − p2 Of these 12 points, exactly 4 are real, depending on the relative sizes of p2 , q 2 and r 2 . If p = q 6= r, the only umbilics are the two points (0, 0, ±r). If p = q = r every point of the ellipsoid (now a sphere) is an umbilic. 8.2.8 By Proposition 8.2.3, the principal curvatures are the roots of κ2 −2Hκ+K = 0, √ i.e. H ± H 2 − K. If there are no umbilics, we must have H 2 > K, and then the principal curvatures are smooth because H and K are (Exercise 8.1.3). The second part follows from Exercises 6.1.4 and 7.1.3 and Proposition 8.2.6. 8.2.9 Setting x = r cos θ, y = r sin θ gives z = aθ so a parametrization of the surface is σ (r, θ) = (r cos θ, r sin θ, aθ). Then σ r = (cos θ, sin θ, 0), σ θ = (−r sin θ, r cos θ, a), so E = 1, F = 0, G = r 2 + a2 . Next, σ r × σ θ = (a sin θ, −a cos θ, r) so N = G−1/2 (a sin θ, −a cos θ, r). From σ rr = 0, σ rθ = (− sin θ, cos θ, 0), σ θθ = (−r cos θ, −r sin θ, 0) we get L = 0, M = −aG−1/2 , N = 0. The principal curvatures are the roots of −κ −aG−1/2 i.e. κ = ±a/G = ±a r2 +a2 = −aG−1/2 = 0, −κG ±a . x2 +y 2 +a2 8.2.10 In the notation of Proposition 8.2.3, H 2 −K = 41 (κ1 +κ2 )2 −κ1 κ2 = 14 (κ1 −κ2 )2 . 8.2.11 The condition H 2 = K gives x2 + y 2 + z 2 = 3. We showed in Exercise 5.1.3 that the points (x, y, z) which satisfy this condition as well as xyz = 1 are precisely the four points (1, −1, −1), (−1, 1, −1), (−1, −1, 1) and (1, 1, 1), and we found in Exercise 8.1.13 that these are the points where the Gaussian curvature attains its maximum value. 8.2.12 If K > 0, then since K = κ1 κ2 , either κ1 > 0 and κ2 > 0, or κ1 < 0 and κ2 < 0. It follows from Euler’s theorem 8.2.4 that the normal curvature κn of any curve γ on the surface is > 0 in the first case and < 0 in the second (since sin θ and cos θ cannot be zero simultaneously). By Eq. 7.9, the curvature of γ is > 0. 8.2.13 Changing the sign of N changes the sign of the Weingarten map W. With the notation in Proposition 8.2.1, (−W)(tt1 ) = (−κ1 )tt1 , (−W)(tt2 ) = (−κ2 )tt2 , which shows that −κ1 and −κ2 are the principal curvatures and t1 and t 2 are corresponding principal vectors. 72 v) = P v + a be an isometry of R3 , where P 8.2.14 Let σ (u, v) be a surface patch, let T (v σ = T (σ σ ). Then, σ̃ σ u = P (σ σ u ), etc. is an orthogonal matrix and a ∈ R3 , and let σ̃ σ . σ σ . σ so in the obvious notation Ẽ = P (σ u ).P (σ u ) = u u (since P is orthogonal) so N = εN N, the sign ε Ẽ = E. Similarly, F̃ = F, G̃ = G. By Proposition A.1.6, Ñ being + if T is direct and − if T is opposite, so L̃ = εL, M̃ = εM , Ñ = εN . The result now follows from Proposition 8.2.6. 8.2.15 Let κ1 and κ2 be the principal curvatures of a surface patch of S at p and θ the oriented angle between a principal vector corresponding to κ1 and the tangent vector of one of the m curves at p. By Euler’s Theorem 8.2.4, the sum of the normal curvatures of the m curves at p is m−1 X r=0 rπ rπ κ1 cos2 θ + + κ2 sin2 θ + . m m Using cos θ = 21 (eiθ + e−iθ ), sin θ = 1 iθ 2i (e − e−iθ ), etc., the sum becomes m−1 m−1 X 1 1 X (κ1 + κ2 ) + (κ1 − κ2 ) e2i(θ+rπ/m) + e−2i(θ+rπ/m) . 2 r=0 4 r=0 But, Pm−1 r=0 ±2iπ 1=e e±2i(θ+rπ/m) = e±2iθ 1−e ±2iπ/m = 0, so the desired sum is simply m−1 1 X 1 (κ1 + κ2 ) = m(κ1 + κ2 ) = mH, 2 r=0 2 where H is the mean curvature of S at p. 8.2.16 Using Proposition 6.2.5 and Exercise 7.1.6 (and the notation there), E = 1+v 2 κ2 , F = G = 1, L = −κτ v, M = N = 0 (we work in the part of the surface in which v > 0; the region v < 0 is treated similarly). By Exercise 8.2.3 the lines of curvature are given by κτ v u̇2 + κτ v u̇v̇ = 0, so u̇ = 0 or u̇ + v̇ = 0, i.e. u = constant or u + v = constant; the first of these corresponds to the tangent lines to the given curve. N1 (u) in the notation of Exercise 8.2.17 The surface is parametrized by σ (u, v) = γ (u)+vN N1 = −κγ̇γ , where κ is the principal 8.2.4. Since γ is a line of curvature, we have Ṅ curvature corresponding to the principal vector γ̇γ . (i) If the surface is a generalized cone, the rulings all pass through some fixed point, so there is a function v(u) such that σ (u, v(u)) is independent of u. DifN1 − κvγ̇γ = 0. Since γ̇γ is perpendicular ferentiation with respect to u gives γ̇γ + v̇N to N1 , this gives 1 − κv = 0 and v̇ = 0, so κ = 1/v is a non-zero constant. Conversely, if κ is constant, σ (u, 1/κ) is constant so the surface is a generalized cone. 73 (ii) If the surface is a generalized cylinder, the rulings are all parallel, so N1 is N1 = 0, and since Ṅ N1 = −κγ̇γ we have κ = 0. Conversely, constant along γ . So Ṅ N1 = 0 so N1 is constant along γ and the rulings are parallel. if κ = 0 then Ṅ 8.2.18 The image of γ under the Gauss map is the curve N, so the condition is that N, i.e. Ṅ N = λγ̇γ for some scalar λ. The result now follows from γ̇γ is parallel to Ṅ Exercise 8.2.2. The second part follows from the last sentence of Proposition 8.2.1. 8.2.19 If every curve on S is a line of curvature, every tangent vector of S at p is a principal vector. By Proposition 8.2.6, it is enough to prove that every point of S is an umbilic. Suppose for a contradiction that p ∈ S is not an umbilic, and let κ1 6= κ2 be the principal curvatures at p with corresponding non-zero principal vectors t 1 and t 2 . If W is the Weingarten map of S at p, we have W(tt1 + t2 ) = κ1 t1 + κ2 t2 . Since every tangent vector is principal, there is a scalar λ such that W(tt1 + t2 ) = λ(tt1 + t2 ); then (κ1 − λ)tt1 + (κ2 − λ)tt2 = 0. But t 1 and t 2 are linearly independent, so this equation forces κ1 = λ = κ2 , a contradiction. N.(tt × N). By Exercise 8.2.2, if γ is 8.2.20 In the notation of Exercise 7.3.22, τg = Ṅ N is parallel to t, so τg = 0. Conversely, if τg = 0 then a line of curvature Ṅ N × t ) = 0; but Ṅ N and t are both perpendicular to N, so Ṅ N × t is parallel to N.(Ṅ N × t = 0, so Ṅ N is parallel to t and γ is a line of curvature by Exercise N; hence, Ṅ 8.2.2 again. 8.2.21 We use the usual Frenet-Serret notation for γ and let N be the unit normal of S. n.N = b.Ṅ N. If κ is the principal curvature We are given that b.N is constant, so τn N = −κtt so b.N = 0. If τ 6= 0 at some point of S corresponding to γ , we have Ṅ γ (t0 ) of γ , say, then for some ǫ > 0 we have τ (t) 6= 0 if t0 − ǫ < t < t0 + ǫ. For values of t in this interval, n is perpendicular to N, so b is parallel to N, hence b = ±N N. But then ḃ b = ±Ṅ N so τn n = ±κtt; this forces τ = κ = 0, contradicting assumption. It follows that τ = 0 at all points of γ , so γ is a plane curve. The converse is a special case of Exercise 8.2.5, since every curve in a plane is a line of curvature of the plane. 8.2.22 In the notation of the proof of Euler’s Theorem 8.2.4, t = cos θtt1 + sin θtt2 , so N = −W(tt) = −κ1 cos θtt1 − κ2 sin θtt2 . Since t2 × N = t1 and t 1 × N = −tt2 , we Ṅ have t × N = − cos θtt2 + sin θtt1 so since t1 and t2 are perpendicular unit vectors, N.(tt × N ) = −κ1 sin θ cos θ + κ2 sin θ cos θ = (κ2 − κ1 ) sin θ cos θ. τg = Ṅ 8.2.23 By Euler’s Theorem 8.2.4, for an asymptotic curve we have κ1 cos2 θ +κ2 sin2 θ = 0, so κ1 κ2 = −κ22 tan2 θ ≤ 0 (if θ is a multiple of π/2 Euler’s Theorem gives κ1 = 0 or κ2 = 0, and the condition again holds). If S is ruled, we must have κ1 κ2 ≤ 0 because the rulings are asymptotic curves (Exercise 7.3.6). If κ1 κ2 < 0, Euler’s theorem gives tan2 θ = −κ1 /κ2 , so there are two asymptotic 74 p curves each of which makes an angle tan−1 −κ1 /κ2 with a principal vector corresponding to κ1 , so the angle between them is as stated. If κ1 = κ2 = 0 everywhere, every curve is asymptotic. If κ1 = 0 but κ2 6= 0, say, Euler’s Theorem gives sin θ = 0 so there is one asymptotic curve through each point, namely the line of curvature corresponding to κ1 (it is proved in Proposition 8.4.2 that these curves are, in fact, straight lines). 8.2.24 Part (i) follows from the fact that hh , ii is symmetric; part (ii) follows from the fact that it is linear in its second argument (since it is actually bilinear). 8.2.25 This is an immediate consequence of Proposition 7.3.3. 8.2.26 hhtt1 , t2 ii = hW(tt1 ), t2 i = κ1 htt1 , t2 i. But if κ1 6= κ2 then t1 is perpendicular to t2 (Proposition 8.2.1). 8.2.27 By Proposition 8.2.1, we can assume that t 1 is perpendicular to t2 (whether or not κ1 and κ2 are distinct). Then t = cos θtt1 + sin θtt2 , t̃t = cos θ̃tt1 + sin θ̃tt2 , so hhtt, t̃tii = cos θ cos θ̃hhtt1 , t1 ii + (cos θ sin θ̃ + cos θ̃ sin θ)hhtt1 , t2 ii + sin θ sin θ̃hhtt2 , t2 ii. Now hhtti , tj ii = hW(tti ), tj i = κi htti , tj i = κi if i = j and = 0 otherwise. Hence, hhtt, t̃tii = κ1 cos θ cos θ̃ + κ2 sin θ sin θ̃, from which the result follows. 8.2.28 Using the notation and result of the preceding exercise, 1 1 1 1 + = + 2 κn κ̃n κ1 cos2 θ + κ2 sin θ κ1 cos2 θ̃ + κ2 sin2 θ̃ 1 + tan2 θ 1 + tan2 θ̃ = + κ1 + κ2 tan2 θ κ1 + κ2 tan2 θ̃ κ2 1 − κ1 tan2 θ 1 − κκ21 1 1 + = + + κ2 κ1 κ2 κ1 + κ2 tan2 θ κ1 + 1 cot2 θ κ2 1 1 + . = κ1 κ2 v, γ̇γ ii = hv v, W(γ̇γ )i = −hv v, Ṅ Ni = −v v.Ṅ N = v̇ v.N (since v.N = 0). 8.2.29 hhv 8.2.30 The formulas for E ∗ , F ∗ and G∗ were proved in Exercise 6.3.11, where it was also shown that σ u.σ )σ σ 2(σ σu − . σ ∗u = 2 4 kσ k kσ k Hence, σ ∗uu = σ u.σ )σ σ uu.σ + σ u.σ u )σ σ u.σ )2σ σu σ 8(σ 4(σ 2(σ σ uu − − + . k σ k2 k σ k4 k σ k4 k σ k6 75 Using the formula for N∗ in Exercise 4.5.5, this gives σ u.σ )σ σ uu.σ + σ u.σ u )σ σ u .σ )2 σ σu σ 8(σ σ.N )σ σ 4(σ 2(σ 2(σ σ uu ∗ . − − + −N , L = k σ k2 k σ k4 k σ k4 k σ k6 k σ k2 which simplifies to give L∗ = − σ .N N)(σ σ u .σ u ) σ .N N)σ σ σ uu.N) 2(σ L 2E(σ (σ − =− − E. 2 4 2 4 kσ k kσ k kσk kk Similar calculations give the stated formulas for M ∗ and N ∗ . In the usual notation, the preceding formulas can be written FI∗ = p.N) 1 1 2(p ∗ FI , FII =− FII − FI . 4 2 kpk kpk k p k4 Hence, for any κ ∈ R, ∗ p.N))FI∗ = − FII + (k p k2 κ + 2(p 1 (FII − κFI ). k p k2 Parts (i) and (ii) follow immediately from this equation, and part (iii) is an immediate consequence of (ii). σ u + bσ σv , 8.2.31 In the notation of the proof of Proposition 8.1.2, we have Nu = aσ σ u + dσ σ v , so Nv = cσ Nu Nu .N Nv Nu .N FIII = Nv Nv .N Nv N u .N Ea2 + 2F ab + Gb2 Eac + F (ad + bc) + Gbd = Eac + F (ad + bc) + Gbd Ec2 + 2F cd + Gd2 a b E F a c = = (−FI−1 FII )t FI (−FI−1 FII ) c d F G b d = FII FI−1 FI FI−1 FII = FII FI−1 FII . 8.2.32 We can assume that the profile curve of σ is unit-speed. From Examples 6.1.3 and 7.1.2, the principal curvatures are −f¨ġ + f˙g̈ = −f¨/ġ (if ġ 6= 0) and ġ/f . (i) If ġ(u0 ) = 0 the first principal curvature must be non-zero when u = u0 , so g̈(u0 ) 6= 0. Since g̈ is a continuous function of u, there is an ǫ > 0 such that g̈(u) 6= 0 if 0 < |u − u0 | < ǫ. Then, ġ(u) 6= 0 if 0 < |u − u0 | < ǫ by the intermediate value theorem. (ii) Assume that ġ is never zero. Then the first principal curvature must be zero everywhere, so f¨ = 0, i.e. f (u) = au + b for some constants a, b. Then, 76 √ ġ 2 = 1 − f˙2 = 1 − a2 so (up to a sign) g(u) = 1 − a2 u + c for some constant c. Since ġ 6= 0, a2 < 1. If a = 0 we have a circular cylinder; if a 6= 0 then making the reparametrization ũ = au + b and a suitable√translation parallel to the z-axis σ (ũ, v) = ũ(cos v, sin v, 1 − a2 ). gives the circular cone σ̃ 8.2.33 The first and second fundamental forms are (1 + zx2 )dx2 + 2zx zy dxdy + (1 + zy2 )dy 2 , zxx dx2 + 2zxy dxdy + zyy dy 2 q . 2 2 1 + zx + zy At an umbilic we have FII = κFI , where κ is the principal curvature. This is equivalent to zxx = λ(1 + zx2 ), zxy = λzx zy , zyy = λ(1 + zy2 ), q where λ = κ 1 + zx2 + zy2 . 8.2.34 By Exercises 6.1.2 and 7.1.4, applying an isometry of R3 does not change the first fundamental form, and either leaves the second fundamental form unchanged (if the isometry is direct) or changes its sign (if the isometry is opposite). It follows that the principal curvatures stay the same (if the isometry is direct) or both change sign (if the isometry is opposite). All the assertions in the exercise follow immediately from this. 8.2.35 (i) By applying an isometry of R3 , we can assume (Theorem 5.2.2) that the hyperboloid is of the form x2 y2 z2 + = − 1, p2 q2 r2 where p, q, r are positive constants, and by the preceding exercise it suffices to consider this case. Differentiating implicitly we find zxx r2 x r2 y zx = 2 , zy = 2 , p z q z 2 2 2 r x r2 y 2 r 4 xy r2 r 1 − 2 2 , zxy = − 2 2 3 , zyy = 2 1− 2 2 . = 2 p z p z p q z q z q z By Exercise 8.2.33 the conditions for an umbilic are r 2 x2 r 4 x2 r2 1− 2 2 =λ 1+ 4 2 , p2 z p z p z r 4 xy λr 4 xy − 2 2 3 = 2 2 2, p q z p q z 2 2 2 r r y r4 y 2 1− 2 2 =λ 1+ 4 2 . q2 z q z q z 77 The second equation gives x = 0, y = 0 or λ = −1/z; but substituting λ = −1/z in the first equation leads to r 2 /p2 = −1, which is absurd; so x = 0 or y = 0. If x = 0, the first equation gives λ = r 2 /p2 z and then the last equation gives r4 y 2 r2 y 2 2 p 1− 2 2 =q 1+ 4 2 . q z q z 2 q q 2 +r 2 z = ±r pq 2 +r 2 (with any q q 2 2 q 2 −p2 combination of signs). Similarly, y = 0 leads to x = ±p p2 +r2 , z = ±r pq 2 +r +r2 . Using y 2 /q 2 = z 2 /r 2 − 1, this leads to y = ±q p2 −q 2 , q 2 +r2 If p2 6= q 2 , this gives four distinct (real) points of the surface; if p2 = q 2 we get the two points (0, 0, ±r). (ii) We can take the surface to be z= x2 y2 + . p2 q2 Proceeding as in (i), we find that the conditions for an umbilic are 2 4λxy 4x2 2 4y 2 =λ 1+ 4 , 0= 2 2 , 2 =λ 1+ 4 . p2 p p q q q The second equation gives x = 0, y = 0 or λ = 0, p and λ = 0 is impossible by the other two equations. If x = 0 we get y = ± 21 q p2 − q 2 , z = ± 14 (p2 − q 2 ). p If y = 0 we get x = ± 12 p q 2 − p2 , z = ± 14 (q 2 − p2 ). If p2 6= q 2 this gives two (real) points of the surface; if p2 = q 2 we get the origin as the only umbilic. (iii) The calculation is simplified by noting that these surfaces are ruled, so that, if κ1 , κ2 are the principal curvatures, κ1 κ2 ≤ 0 everywhere (Exercise 8.2.23). Hence, if κ1 = κ2 we must have κ1 = κ2 = 0, and hence FII = 0, so we are looking for the points at which the second fundamental form is zero. For the hyperboloid of one sheet x2 y2 z2 + = + 1, p2 q2 r2 we can use x, y as parameters on the open subset of the surface where z 6= 0. The formulas for zxx , zxy and zyy are the same as in part (i); the condition zxy = 0 forces x = 0 or y = 0, but neither of these is consistent with the conditions zxx = zyy = 0. Hence, there are no umbilics for which z 6= 0. To deal with the ‘waist’ z = 0 of the hyperboloid, we can use x, z as parameters if x 6= 0 and y, z if y 6= 0. In the first case, for example, the condition for an 78 umbilic is yxx = yxz = yzz = 0; proceeding as above, we find that there are no umbilics. Similarly in the last case. Finally, for the hyperbolic paraboloid z= x2 y2 − , p2 q2 zxx = 2/p2 is never zero, so there are no umbilics. 8.2.36 We have to show that the umbilics on the surface xyz = 1 are the four points (1, 1, 1), (1, −1, −1), (−1, 1, −1) and (−1, −1, 1). Using x, y as parameters, we find as in the preceding exercise that the conditions for an umbilic are 1 2 =λ 1+ 4 2 , x3 y x y 1 λ = 3 3, 2 2 x y x y 2 1 =λ 1+ 2 4 , xy 3 x y for some λ. The second equation gives λ = xy and then the other equations give x4 y 2 = x2 y 4 = 1; these equations force x2 = y 2 = 1, so x = ±1, y = ±1 (with any combination of signs). Then z = 1/xy = ±1 and we obtain the four points required. 8.2.37 On the open subset of S on which z 6= 0 we can use x, y as parameters. Differentiating implicitly we find that zxx = (y 2 + z 2 )(2x2 z 2 − y 2 z 2 − x2 y 2 ) , z 3 (x2 + y 2 )2 so zxx = 0 when x2 = y 2 = z 2 = 1, and in particular at p. Similarly, zxy = zyy = 0 at p. It follows that the second fundamental form of S is zero at p (Exercise 8.2.33), i.e., p is a planar point. The argument actually proves that the eight points (±1, ±1, ±1) are all planar, but this can also be deduced from Exercise 8.2.34 and the fact that S is preserved by the isometries (x, y, z) 7→ (±x, ±y, ±z) of R3 (with any combination of signs). (i) S is a level surface of f (x, y, z) = x2 y 2 + y 2 z 2 + z 2 x2 , so ∇ f = (2x(y 2 + z 2 ), 2y(x2 + z 2 ), 2z(x2 + y 2 )) n is normal is normal to S at (x, y, z). Taking x = y = 1 we find that (4, 4, 4) = 4n to S at p, and hence so is n. Since t 1 and t2 are perpendicular to n, they are tangent to S at p. 79 (ii) Since the vectors t1 , t2 , n are linearly independent, scalars X, Y, Z as in the statement of the exercise exist, and are small if (x, y, z) is near p. When we substitute x = 1 + X + Z, y = 1 − X + Y + Z, z = 1 − Y + Z in the equation of S, we know that all quadratic and lower order terms will cancel, and the quartic terms can be discarded as they will be small compared to the cubic terms. Retaining only the cubic terms, we find after some algebra the equation 6Z − 3X 2 Y + 3XY 2 = 0, hence the stated equation. √ √ (iii) Making the linear transformation X = −X̃ + 3Ỹ , Y = X̃ + 3Ỹ , Z̃ = Z, we get Z̃ = X̃(X̃ 2 − 3Ỹ 2 ), which is a monkey saddle. 8.3.1 (i) Setting ũ = v, ṽ = w = e−u , we have u = − ln ṽ, v = ũ so, in the nota0 − ṽ1 tion of Exercise 6.1.4, J = . Since J is invertible, (u, v) 7→ (v, w) 1 0 is a reparametrization map. w is form in terms of v, Thefirst fundamental 1 1 0 0 − E F 0 1 Ẽ F̃ ṽ = given by = Jt J = 1 2 1 0 0 0 f (u) F G − F̃ G̃ ṽ 1 0 w2 , so the first fundamental form is (dv 2 + dw2 )/w2 . 0 w12 (ii) We find that the matrix ∂v ∂v 1 2 (v − (w + 1)2 ) v(w + 1) ∂V ∂W 2 ˜ J = ∂w ∂w = , v(w + 1) − 21 (v 2 − (w + 1)2 ) ∂V ∂W 1 0 2 t w so the first fundamental form in terms of V and W is J˜ J˜ = 0 w12 (v 2 +(w+1)2 )2 I 4w 2 = (1−U 24−V 2 )2 I, after some tedious algebra. In (i), u < 0 and −π < v < π corresponds to −π < v < π and w > 1, a semi-infinite rectangle in the upper half of the vw-plane. 111111111111111111 000000000000000000 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 w 1 0 v To find the corresponding region in (ii), it is convenient to introduce the complex numbers z = v + iw, Z = U + iV . Then, the equations in (ii) are equivalent to 80 Z= z−i z+i , z= Z+1 i(Z−1) . The line v = π in the vw-plane corresponds to z + z̄ = 2π (the bar denoting complex conjugate), i.e. Z+1 i(Z−1) = 2π, which simplifies − i(Z̄+1 Z̄−1) to |Z − (1 − πi )|2 = π12 ; so v = π corresponds to the circle in the U V -plane with centre 1 − πi and radius π1 . Similarly, v = −π corresponds to the circle with centre 1 + πi and radius π1 . Finally, w = 1 corresponds to z − z̄ = 2i, i.e. Z+1 1 2 Z̄+1 1 i(Z−1) + i(Z̄−1) = 2i. This simplifies to |Z − 2 | = 4 ; so w = 1 corresponds to the circle with centre 1/2 and radius 1/2 in the U V -plane. The required region in the U V -plane is that bounded by these three circles: V U2 + V 2 = 1 11111 00000 00000 11111 00000 11111 O 00000 11111 00000 11111 U For (iii) we follow the hint and make use of polar coordinates on the disc, V = r cos θ, W = r sin θ, V̄ = r̄ cos θ̄, W̄ = r̄ sin θ̄. We find that r̄ = r22r+1 , θ̄ = θ. Suppose that the first fundamental form in terms of these param2(1−r2 ) eters is Edr̄ 2 + 2F dr̄dθ̄ + Gdθ̄ 2 . Since dr̄ dr = (1+r2 )2 , the first fundamental 2 4(1−r2 )2 ) Edr 2 + 4(1−r F drdθ + Gdθ 2 . (1+r2 )4 (1+r2 )2 (1+r2 )4 4(dr2 +r2 dθ2 ) , we get E = = (1−r̄1 2 )2 , F 2 2 (1−r ) (1−r2 )4 form is Equating this to 2 4(dV 2 +dW 2 ) = (1−V 2 −W 2 )2 2 r̄ = 1−r̄ 2 . Con2 4r = 0, G = (1−r 2 )2 verting back to the parameters (V̄ , W̄ ), we have r̄dr̄ = V̄ dV̄ + W̄ dW̄ , r̄ dθ̄ = 81 V̄ dW̄ − W̄ dV̄ , so the first fundamental form becomes (V̄ dV̄ + W̄ dW̄ )2 + (1 − r̄ 2 )(V̄ dW̄ − W̄ dV̄ )2 r̄ 2 (1 − r̄ 2 )2 (V̄ 2 + (1 − r̄ 2 )W̄ 2 )dV̄ 2 + 2r̄ 2 V̄ W̄ dV̄ dW̄ + (W̄ 2 + (1 − r̄ 2 )V̄ 2 )dW̄ 2 = r̄ 2 (1 − r̄ 2 )2 (1 − W̄ 2 )dV̄ 2 + 2V̄ W̄ dV̄ dW̄ + (1 − V̄ 2 )dW̄ 2 . = (1 − V̄ 2 − W̄ 2 )2 8.3.2 √ The parametrisation is σ (u, v) = (f (u) cos v, f (u) sin v, g(u)), f (u) = eu , g(u) = 1 − e2u − cosh−1 (e−u ), −∞ < u < 0. (i) A parallel u = constant is a circle of radius f (u) = eu , so has length 2πeu . (ii) From Example 7.1.2, E = 1, F = 0, G = f (u)2 , so dAσ = f (u)dudv and the R 2π R 0 area is 0 −∞ eu dudv = 2π. (iii) From Examples 7.1.2 and 8.1.4, the principal curvatures are κ1 = f˙g̈ − f¨ġ = −f¨/ġ = −(e−2u − 1)−1/2 , κ2 = f ġ/f 2 = ġ/f = (e−2u − 1)1/2 . (iv) κ1 < 0, κ2 > 0. 8.3.3 Let γ (u) = (f (u), 0, g(u)) and denote d/du by a dot; by Example 8.1.4, f¨+Kf = √ √ 0. If K < 0, the general solution is f = ae− −Ku + be −Ku where a, b are constants; the condition f (π/2) = f (−π/2) = 0 forces a = b = 0, so γ coincides with the z-axis, contradicting the assumptions. If K = 0,√f = a + bu√and again a = b = 0 is forced. So we must have K > 0 and f = a cos Ku+b sin Ku. This time, f (π/2) = f (−π/2) = 0 and a, b not both zero implies that the determinant √ √ cos √Kπ/2 sin √Kπ/2 = 0. cos Kπ/2 − sin Kπ/2 √ This gives sin Kπ = 0, so K = n2 for some integer n 6= 0. If n = 2k is even, f = b sin 2ku, but then f (0) = 0, contradicting the assumptions. If n = 2k + 1 is odd, f = a cos(2k + 1)u and f (π/2(2k + 1)) = 0, which contradicts the assumptions unless k = 0 or −1, i.e. unless K = (2k+1)2 = 1. Thus, f = a cos u, q p ġ = 1 − f˙2 = 1 − a2 sin2 u. Now, γ̇γ = (f˙, 0, ġ) is perpendicular to the z√ axis ⇐⇒ ġ = 0. So the assumptions give 1 − a2 = 0, i.e. a = ±1. Then, γ (u) = (± cos u, 0, ± sin u) (up to a translation along the z-axis) and S is the unit sphere. σ (ũ, ṽ) be a patch of S containing p = σ̃ σ (ũ0 , ṽ0 ). The Gaussian curvature 8.4.1 Let σ̃ K of S is < 0 at p; since K is a smooth function of (ũ, ṽ) (Exercise 8.1.3), K(ũ, ṽ) < 0 for (ũ, ṽ) in some open set Ũ containing (ũ0 , ṽ0 ); then every point of σ (Ũ ) is hyperbolic. Let κ1 , κ2 be the principal curvatures of σ̃ σ , let 0 < θ < π/2 σ̃ 82 p be such that tan θ = −κ1 /κ2 , and let e1 and e2 be the unit tangent vectors of σ making angles θ and −θ, respectively, with the principal vector corresponding σ̃ to κ1 (see Theorem 8.2.4). Applying Proposition 8.4.3 gives the result. For the last part, put v̇ = 0 in the formula for κn in Proposition 7.3.5: this shows that L = 0 if the parameter curves v = constant are asymptotic. Similarly N = 0 if the parameter curves u = constant are asymptotic. 8.4.2 The first and √ second fundamental forms are (2 + v 2 )du2 + 2uvdudv + (2 + u2 )dv 2 and −4dudv/ 4 + 2u2 + 2v 2 . By Exercise 8.2.3, the lines of curvature are given by −(2 + v 2 )u̇2 + (2 + u2 )v̇ 2 = 0, so and hence Z dv =± 2 + v2 Z du , 2 + u2 v u sinh−1 √ ± sinh−1 √ = constant. 2 2 We can take s = sinh−1 √v2 + sinh−1 √u2 , t = sinh−1 √v2 − sinh−1 √u2 , so u = √ √ 2 sinh 12 (s − t), v = 2 sinh 12 (s + t). 8.4.3 Assume that γ is unit-speed. Then, the ruled surface is σ (u, v) = γ (u) + vδδ (u), N, t = γ̇γ (a dot denoting d/du), and N is the unit normal of (a patch where δ = t ×N N)..N = 0. of) S. By Example 8.1.5, the flatness condition is δ̇δ.N = 0, i.e., (tt × Ṅ N is tangent to S, so t × Ṅ N is parallel to N . Hence, S̃ is flat if and only if Now, Ṅ N = 0, i.e. if and only if Ṅ N is parallel to γ̇γ . By Exercise 8.2.2, this is precisely t × Ṅ the condition for γ to be a line of curvature of S. 8.5.1 By Corollary 8.1.3 and the fact that σ is conformal, the mean curvature of σ is , so H = L+N 2E (*) σ is minimal ⇐⇒ L + N = 0 ⇐⇒ (σ σ uu + σ vv )..N = 0. σ = σ uu +σ σ vv = 0. For the converse, we have to Obviously, then, σ is minimal if ∆σ σ = 0 if (*) holds. It is enough to prove that ∆σ σ.σ u = ∆σ σ.σ v = 0, show that ∆σ σ u , σ v , N} is a basis of R3 . We compute ∆σ σ.σ u = σ uu.σ u + σ vv .σ u = since {σ 1 1 σ σ σ σ σ 2 (σ u .σ u )u + (σ v .σ u )v − (σ v .σ uv ) = 2 (σ u .σ u − σ v .σ v )u + (σ v .σ u )v . But, since σ is conformal, σ u .σ u = σ v .σ v and σ u .σ v = 0. Hence, ∆σ σ .σ u = 0. Similarly, σ.σ v = 0. ∆σ The first fundamental form of the given surface patch is (1 + u2 + v 2 )2 (du2 + dv 2 ), so it is conformal, and σ uu + σ vv = (−2u, 2v, 2) + (2u, −2v, −2) = 0. 83 8.5.2 Using the formula in Exercise 8.1.1 with f (x, y) = ln cos y − ln cos x gives H= sec2 x(1 + tan2 y) − sec2 y(1 + tan2 x) = 0. 2(1 + tan2 x + tan2 y)3/2 Nu , Σv = σ v + wN Nv , Σ w = N. Σ u .Σ Σw = 0 since σ u .N N = Nu .N N = 0, 8.5.3 Σ u = σ u + wN Σ Σ and similarly v .Σw = 0. Finally, Σv = σ u .σ σ v + w(σ σ u .N Nv + σ v .N Nu ) + w2N u .N Nv Σ u .Σ Nv = w2 Nu .N Nv . = F − 2wM + w2 Nu .N L N σ u , Nv = − N By the proof of Proposition 8.1.2, Nu = − E G σ v , so N u .Nv = LN F = 0. Every surface u = u0 (a constant) is ruled as it is the union of EG the straight lines given by v = constant; by Exercise 8.2.4, this surface is flat provided the curve γ (v) = σ (u0 , v) is a line of curvature of S, i.e. if σ v is a principal vector; but this is true since the matrices FI and FII are diagonal. Similarly for the surfaces v = constant. 8.5.4 We take the ruled surface to be σ (u, v) = γ (u) + vδδ (u), where γ is unit-speed and δ is a unit vector. Denoting d/du by a dot and γ̇γ by t, the coefficients of the first and second fundamental forms are E = k t + vδ̇δ k2 , F = t.δ , G = 1, ˙ L = (ṫt + vδ̈δ )..N, M = δ̇δ.N, N = 0, where N = (t+vδ˙ )×δ . Then, the mean k(t +vδ )×δ k curvature LG − 2M F + N E (ṫt − 2(tt.δ )δ̇δ + vδ̈δ )..N H= = . 2 2(EG − F ) 2(EG − F 2 ) If δ̇δ (u0 ) 6= 0 for some value of u0 , H(u0 , v) → 0 as v → ±∞, since the numerator in the expression for H is independent of v while the denominator → ∞ as v → ±∞. As H is constant, H = 0 everywhere, contradicting the assumption. Hence, δ̇δ = 0 everywhere, δ is constant, and the surface is a generalized cylinder. We can now assume that γ lies in a plane perpendicular to δ (Exercise 5.3.3). Then, t × δ is a unit vector and the formula for the mean curvature simplifies to H= ṫt.(tt × δ ) . 2 k t × δ k2 n where κ is the curvature of γ and n is its principal normal. Also, t ×δδ Now ṫt = κn n. is perpendicular to t and parallel to the plane containing γ ; hence, t × δ = ±n It follows that H = ±κ/2, so if H is a non-zero constant then κ is constant and the plane curve γ is a circle. Thus, the surface is a circular cylinder. 8.5.5 We use the notation and results of Proposition 8.5.2. If γ is a curve on σ , the N. Now, γ λ ‘corresponding’ curve γ λ on the parallel surface σ λ is γ λ = γ + λN 84 λ N = −κγ̇γ λ for some scalar κ (Exercise 8.2.2) is a line of curvature on σ λ ⇐⇒ Ṅ N = −κ(γ̇γ + λṄ N). But this last equation holds if and only if Ṅ N is a scalar ⇐⇒ ǫṄ multiple of γ̇γ , i.e. if and only if γ is a line of curvature on σ . In this case, N = (1 − κλ)γ̇γ is parallel to γ̇γ . γ̇γ λ = γ̇γ + λṄ σ (u, v) = σ (u, v)+λ(u, v)N N(u, v) is 8.5.6 Let σ (u, v) be a patch of S. We are given that σ̃ a patch of S̃, for some function λ, where N(u, v) is the unit normal of σ at σ (u, v), σ (u, v). Now σ̃ σ u = σ u + λN Nu + λuN; since and that N (u, v) is also normal to S̃ at σ̃ σ u and N u are all perpendicular to N, this implies that λu = 0; similarly σ u , σ̃ λv = 0. Hence, λ is constant and S̃ = S λ is a parallel surface of S. Chapter 9 9.1.1 By Exercise 4.1.3, there are two straight lines on the hyperboloid passing through (1, 0, 0); by Proposition 9.1.4, they are geodesics. The circle z = 0, x2 + y 2 = 1 and the hyperbola y = 0, x2 − z 2 = 1 are both normal sections, hence geodesics by Proposition 9.1.6. N × γ̇γ ). Note that if Γ(t) = γ (ϕ(t)) is a reparametrization of γ , 9.1.2 Let κ(γγ ) = γ̈γ. (N 3 Γ) = dϕ Γ) = 0. then κ(Γ κ(γγ ). In particular, κ(γγ ) = 0 ⇐⇒ κ(Γ dt For (i), let γ be a pre-geodesic and let Γ be a geodesic reparametrization of γ . Γ(t) = Γ(t/v) is By Proposition 9.1.2 Γ has constant speed, say v, and then Γ̃ Γ) = 0, hence κ(Γ Γ) = 0, hence a unit-speed geodesic. By Proposition 9.1.3, κ(Γ̃ κ(γγ ) = 0. Conversely, if κ(γγ ) = 0 and if Γ is a unit-speed reparametrization of Γ) = 0 so Γ is a geodesic by by Proposition 9.1.3. γ , then κ(Γ Part (ii) is obvious. For (iii), let γ be a constant speed pre-geodesic, say with speed v. Then Γ(t) = γ (t/v) is a unit-speed pre-geodesic, hence a geodesic by (i) and Proposition 9.1.3. Γ, γ̈γ is perpendicular to the surface, so γ is a geodesic. Since γ̈γ = v 2Γ̈ Finally, (iv) follows from (iii) and Proposition 9.1.2. 9.1.3 Let Πs be the plane through γ (s) perpendicular to t(s); the parameter curve s = constant is the intersection of the surface with Πs . From the solution to Exercise 4.2.7, the standard unit normal of σ is N = −(cos θ n + sin θ b). Since this is perpendicular to t, the circles in question are normal sections. 2 2 2 9.1.4 Take the ellipsoid to be xp2 + yq 2 + zr2 = 1; the vector ( px2 , qy2 , rz2 ) is normal to the ellipsoid by Exercise 5.1.2. If γ (t) = (f (t), g(t), h(t)) is a curve on the ellipsoid, 2 2 2 2 2 ˙2 R = ( fp2 + ġq 2 + ḣr2 )−1/2 , S = ( fp4 + gq 4 + hr4 )−1/2 . Now, γ is a geodesic ⇐⇒ γ̈γ is parallel to the normal ⇐⇒ (f¨, g̈, ḧ) = λ( f2 , g2 , h2 ) for some scalar λ(t). From p g2 f2 + 2 p q2 2 + hr2 = 1 we get f f˙ g ġ hḣ p2 + q 2 + r2 = 0, hence q r f˙2 ġ 2 f f¨ gg̈ ḣ2 hḧ + 2 p q 2 + r2 + p2 + q 2 + r2 = 0, i.e. 85 f˙2 p2 ġ 2 q2 ḣ2 r2 f2 p4 g2 q4 h2 r4 = 0, which gives λ = −S 2 /R2 . The curvature 2 1/2 2 2 S k γ̈γ k = (f¨2 + g̈ 2 + ḧ2 )1/2 = |λ| fp4 + gq 4 + hr4 = |λ| S = R2 . Finally, ! ! 1 f˙2 ġ 2 ḣ2 1 d f f˙ g ġ hḣ = + 4 + 4 + 2+ 2 2 dt R2 S 2 p4 q r p2 q r ! ˙¨ 2 ff g 2 h2 ġg̈ ḣḧ f + 4 + 4 + 2 + 2 + p4 q r p2 q r ! ! 1 λ f f˙ g ġ hḣ f f˙ g ġ hḣ = 2 + 4 + 4 + 2 + 4 + 4 = 0, R p4 q r S p4 q r + + +λ + + since λ = −S 2 /R2 . Hence, RS is constant. 9.1.5 Suppose that a geodesic γ lies in the plane v.a = b, where a and b are constants. Then γ̇γ .a = γ̈γ.a = 0. Since γ̈γ is parallel to N (the unit normal of the surface), N.a = 0, so Ṅ N.a = 0. Since N, γ̇γ and Ṅ N are all parallel to the plane and the last two vectors are perpendicular to the first, they are parallel. Hence γ is a line of curvature by Exercise 8.2.2. Conversely, if γ is both a geodesic and a line of curvature, we may assume γ has unit-speed (for the unit-speed reparametrization of γ would still be a geodesic and a line of curvature). Let a = N × γ̇γ . Then N × γ̇γ +N N × γ̈γ = 0 since the first term vanishes because γ is a line of curvature ȧa = Ṅ and the second because γ is a geodesic. So a is constant. And γ̇γ.a = 0 so γ .a is a constant, say b. Hence γ lies in the plane v.a = b. 9.1.6 For (i) note that γ̈γ is a non-zero vector parallel to both N1 and N2 , so N 1 and N2 must be parallel. For an example, take S1 and S2 to be the sphere and cylinder in Theorem 6.4.6. (ii) Now suppose that S1 and S2 intersect perpendicularly. Then, N1 , N2 and γ̇γ N2 = 0. If γ is are perpendicular unit vectors. From γ̇γ.N2 = 0 we get γ̈γ.N2 + γ̇γ .Ṅ N2 is perpendicular to a geodesic on S1 , γ̈γ .N2 = 0 since γ̈γ is parallel to N1 , so Ṅ γ N N γ̇ . Since Ṅ2 is also perpendicular to 2 , it must be parallel to N1 . Conversely, if N2 is parallel to N1 , then γ̇γ .Ṅ N2 = 0 so γ̈γ is perpendicular to N 2 . Since γ̈γ is also Ṅ perpendicular to γ̇γ , it must be parallel to N 1 . Finally, if γ is a geodesic on both N1 is parallel to N2 and Ṅ N2 is parallel to N1 . It follows that S1 and S2 , then Ṅ N1 × N2 )˙ = Ṅ N1 × N 2 + N1 × Ṅ N2 = 0 so N1 × N2 is a constant vector. Since γ̇γ is (N a unit vector parallel to N1 × N2 , γ̇γ is constant, so C is part of a straight line. 9.1.7 The ellipses formed by the intersections of the ellipsoid with thethree coordinate x y z planes are normal sections. Indeed, a normal to the ellipsoid is p2 , q 2 , r2 . The plane z = 0 (say) has normal (0, 0, 1), so the intersection with the plane z = 0 is a normal section if and only if px2 , qy2 , rz2 .(0, 0, 1) = z/r 2 = 0 when z = 0, which is true. 86 9.1.8 The intersections of the surface with each of the planes x = ±y, y = ±z and z = ±x are normal sections. Indeed, by the solution to Exercise 8.2.37, a normal to the surface is (x(y 2 + z 2 ), y(x2 + z 2 ), z(x2 + y 2 )). The planes x = ±y have normals (1, ∓1, 0) so the intersection of the surface with x = ±y is a normal section if and only if x(y 2 + z 2 ) ∓ y(x2 + z 2 ) = 0 when x = ±y, which is evidently true. Similarly for the other four planes. 9.1.9 Assume that γ is unit-speed with tangent vector t. Then (with the usual notan.a = 0. Since κ 6= 0, n is perpendicular tion), t.a is constant, so ṫt.a = 0, i.e. κn to a. As γ is a geodesic, ṫt is parallel to N, so n is parallel to N. Hence, a is perpendicular to N , hence tangent to S. 9.1.10 From the solution to Exercise√7.3.3., a circle of radius r on a sphere of radius R has geodesic curvature κg = R2 − r 2 /rR. Hence, κg = 0 ⇐⇒ r = R ⇐⇒ the circle is a great circle. 9.1.11 The osculating plane is perpendicular to the binormal b of γ , and so is perpendicular to S at p if and only if b is perpendicular to N at p. Since t and N are perpendicular, b is perpendicular to N ⇐⇒ n is parallel to N ⇐⇒ γ is a geodesic. 9.1.12 γ is asymptotic ⇐⇒ γ̈γ is perpendicular to N; γ is a geodesic ⇐⇒ γ̈γ is parallel to N. Hence, if γ is both asymptotic and a geodesic, we must have γ̈γ = 0, so γ (t) = taa + b for some constant vectors a, b, i.e. γ is a straight line. 9.1.13 γ is a geodesic on σ ⇐⇒ γ̈γ is parallel to σ u × σ v = (γ̇γ + vδ̇δ ) × δ when v = 0, i.e. γ̈γ × (γ̇γ × δ ) = 0. Since γ̈γ is perpendicular to γ̇γ , γ is a geodesic ⇐⇒ γ̈γ .δ = 0 ⇐⇒ δ n. is perpendicular to γ̈γ = κn 9.1.14 Denoting by t, n and b the unit tangent vector, principal normal and binormal N since Γ is a geodesic so of Γ, and by κ its curvature, we have n = ±N Γ.(N N × Ṅ N) = t.(n n × ṅ n) = t.(n n × (−κtt + τb b)) = t.(κb b + τtt) = τ. Γ̇ We can assume that γ is unit-speed; denote by a dash differentiation with respect to the arc-length of γ . By Exercise 7.3.22, the geodesic torsion of γ is N × N′ ). τg = (γγ ′ × N)..N′ = γ ′ .(N Γ at p, and we can assume that the sign is + Since γ and Γ touch at p, γ ′ = ±Γ̇ by changing the sign of the parameter of γ if necessary. Since γ ′ = u′σ u + v ′ σ v , N′ = u′N u + v ′ Nv , etc., it follows that u′ = u̇ and v ′ = v̇ at p, and hence that N at p. Hence, τg = Γ̇ Γ.(N N × Ṅ N) and the result now follows from the first N′ = Ṅ part of the exercise. 87 Since Γ touches itself at each of its points (!), its torsion is equal to its geodesic torsion. N so τ = 9.1.15 If γ is an asymptotic curve, then (with the usual notation) b = ±N b.n = ∓Ṅ N.n. Since n = b × t = ±N N × t, we get −ḃ N. (N N × t ) = t. (N N × Ṅ N). τ = −Ṅ The last part follows from the preceding exercise. 9.1.16 We use the notation of Exercise 9.1.14 and assume that γ is a line of curvature. Γ = γ ′ and N′ = Ṅ N at p. By Rodrigues’ formula, Ṅ N = −κγ̇γ We can assume that Γ̇ where κ is the principal curvature corresponding the line of curvature γ , so N′ = −κγγ ′ . Hence, the torsion of Γ is Γ. (N N × Ṅ N) = −κγγ ′ .(N N × γ ′ ) = 0. τ = Γ̇ 9.1.17 (i) By Exercise 9.1.14, the torsion τ of a geodesic γ on a surface S is equal to its geodesic torsion which, by Exercise 8.2.22, is equal to (κ2 − κ1 ) sin θ cos θ in the notation there. At an umbilic κ1 = κ2 so τ = 0. (ii) By (i), the torsion is given by τ = (κ2 − κ1 ) sin θ cos θ. If a second geodesic γ̃γ intersects γ at right angles at p, then in the obvious notation θ̃ = θ ± π/2 and hence τ̃ = −τ . (iii) If γ is a geodesic, its curvature κ is equal, up to sign, to its normal curvature, so κ = ±(κ1 cos2 θ + κ2 sin2 θ) by Euler’s Theorem 8.2.4. Taking the + sign, κ − κ1 = (κ2 − κ1 ) sin2 θ, κ − κ2 = (κ1 − κ2 ) cos2 θ, so (κ − κ1 )(κ − κ2 ) = −(κ1 − κ2 )2 sin2 θ cos2 θ = −τ 2 . Taking the − sign gives the other expression for τ 2 . (iv) If the surface is flat, either κ1 = 0 or κ2 = 0 at p. If κ2 = 0, then κ = ±κ1 cos2 θ, τ = −κ1 sin θ cos θ, so τ = ∓κ tan θ. The other formula results if κ1 = 0 at p. 9.1.18 We can assume that γ is unit-speed as conditions (i) - (iii) are unchanged by reparametrization. Let δ (u) be a non-zero vector parallel to the ruling through γ (u). Then (i) says that γ is a geodesic, and by Exercise 9.1.13 this holds ⇐⇒ ṫt.δ = 0. By Exercise 5.3.4, (ii) holds ⇐⇒ t.δ̇δ = 0. And (iii) obviously holds ⇐⇒ t.δ is a constant. Everything now follows immediately. 9.1.19 Suppose that every geodesic on a surface S is a plane curve. By Proposition 8.2.9, it suffices to show that every point of S is an umbilic. Suppose for a contradiction that p ∈ S is not an umbilic, let κ1 , κ2 be the distinct principal 88 curvatures of S at p, and let t be a non-zero principal vector corresponding to the principal curvature κ1 at p. Choose an angle θ such that (i) θ is not an integer multiple of π/2, and (ii) κ1 cos2 θ + κ2 sin2 θ 6= 0. Let γ be the unit-speed geodesic on S passing through p and making an angle θ with t. By condition (ii) and Euler’s Theorem 8.4.2, γ has non-zero curvature at p, and γ is a plane curve by the hypothesis. By Exercise 9.1.5, γ is a line of curvature, but this contradicts property (i). 9.1.20 Assume that γ is unit-speed, and let r be the radius of the sphere. Then, (γγ − c)..(γγ − c) = r 2 so γ̇γ .(γγ − c) = 0, γ̈γ .(γγ − c) = −γ̇γ .γ̇γ = −1. But, as γ is N, where κ is the curvature of γ , so the last equation gives a geodesic, γ̈γ = ±κN N.(γγ − c) = ±1/κ, i.e. 1 , κ= N.(γγ − c)| |N as required. 9.2.1 If p and q lie on the same parallel of the cylinder, there are exactly two geodesics joining them, namely the two circular arcs of the parallel of which p and q are the endpoints. If p and q are not on the same parallel, there are infinitely-many circular helices joining p and q (see Example 9.2.8). 9.2.2 Take the cone to be σ (u, v) = (u cos v, u sin v, u). By Exercise 6.2.1, σ is locally isometric to an open subset of the xy-plane by √ √ v v σ (u, v) 7→ u 2 cos √ , u 2 sin √ , 0 . 2 2 By Corollary 9.2.7, the geodesics on the cone correspond to the straight lines in the xy-plane. Any such line, other than the axes x = 0 and y = 0, has equation ax + by = 1, where a, b are constants; this line corresponds to the curve v 7→ cos v sin v 1 √ ,√ ,√ v v v v v 2(a cos √2 + b sin √2 ) 2(a cos √2 + b sin √2 ) 2(a cos √2 + b sin √v2 ) the x− and y-axes correspond to straight lines on the cone. 9.2.3 Parametrize the cylinder by σ (u, v) = (cos u, sin u, v). Then, E = G = 1, F = 0, so the geodesic equations are ü = v̈ = 0. Hence, u = a + bt, v = c + dt, where a, b, c, d are constants. If b = 0 this is a straight line on the cylinder; otherwise, it is a circular helix. ! ; 89 9.2.4 For the first part, (E u̇2 + 2F u̇v̇ + Gv̇ 2 )˙ = (Eu u̇ + Ev v̇) u̇2 + 2(Fu u̇ + Fv v̇)u̇v̇ + (Gu u̇ + Gv v̇)v̇ 2 + 2E u̇ü + 2F (u̇v̈ + üv̇) + 2Gv̇v̈ = u̇(Eu u̇2 + 2Fu u̇v̇ + Gu v̇ 2 ) + v̇(Ev u̇2 + 2Fv u̇v̇ + Gv v̇ 2 ) + 2E u̇ü + 2F (u̇v̈ + üv̇) + 2Gv̇v̈ = 2(Eu u̇ + F v̇)˙ u̇ + 2(F u̇ + Gv̇)˙ v̇ + 2(E u̇ + F v̇)ü + 2(F u̇ + Gv̇)v̈ by the geodesic equations = 2[(E u̇ + F v̇)u̇]˙+ 2[(F u̇ + Gv̇)v̇]˙ = 2(E u̇2 + 2F u̇v̇ + Gv̇ 2 )˙. Hence, (E u̇2 + 2F u̇v̇ + Gv̇ 2 )˙ = 0 and so k γ̇γ k2 = E u̇2 + 2F u̇v̇ + Gv̇ 2 is constant. Suppose now that (i) and (ii) hold. Differentiating E u̇2 +2F u̇v̇ +Gv̇ 2 = constant gives (Eu u̇ + Ev v̇)u̇2 + 2(Fu u̇ + Fv v̇))u̇v̇ + (Gu u̇ + Gv v̇)v̇ 2 = −2(E u̇ + F v̇)ü − 2(F u̇ + Gv̇)v̈, i.e., (Eu u̇2 + 2Fu u̇v̇ + Gu v̇ 2 )u̇ + (Ev u̇2 + 2Fv u̇v̇ + Gv v̇ 2 )v̇ = −2(E u̇ + F v̇)ü − 2(F u̇ + Gv̇)v̈. Using (i) we get 2u̇ d (E u̇ + F v̇) + 2(E u̇ + F v̇)v̈ = −2(F u̇ + Gv̇)v̈ − (Ev u̇2 + 2Fv u̇v̇ + Gv v̇ 2 )v̇. dt The left-hand side of this equation equals 2 d d d (u̇(E u̇ + F v̇)) = −2 (F u̇v̇ + Gv̇ 2 ) = −2(F u̇ + Gv̇)v̈ − 2v̇ (F u̇ + Gv̇). dt dt dt Combining the last two equations gives (ii) provided v̇ 6= 0. 9.2.5 E = 1, F = 0, G = 1+u2 , so γ is unit-speed ⇐⇒ u̇2 +(1+u2 )v̇ 2 = 1. The second a d ((1 +u2 )v̇) = 0, i.e. v̇ = 1+u equation in (9.2) gives dt 2 , where a is a constant. So 2 a dv v̇ a 2 u̇ = 1 − 1+u2 and, along the geodesic, du = u̇ = ± √ . If a = 0, (1−a2 +u2 )(1+u2 ) √ then v = constant and we have a ruling. If a = 1, then dv/du = ±1/u 1 + u2 , which can be integrated to give v = v0 ∓ sinh−1 u1 , where v0 is a constant. 90 2 (u2 +1)(u2 +1−a2 ) so = For the last part, note that du dv a2 √ 2 2 (i) if a > 1 then du/dv = 0 for u = ± a − 1 and this is the minimum distance of the geodesic from the z-axis; (ii) if a2 < 1 then |du/dv| > a−2 − 1 so u will decrease to zero and the geodesic will cross the z-axis; (iii) if a2 = 1 then du/dv = ±(u2 + 1) so u = ± tan(v + c) where c is a constant. The information given implies that, when u = D, cos α = γ̇γ.σ u = u̇ (since E = 1, F = 0) so a2 = (1 + D2 ) sin2 α. Then, a2 is > 1, < 1 or = 1 according as D is >, < or = cot α. 9.2.6 This is straightforward algebra. 9.2.7 By Exercise 5.3.3 we can parametrize the generalized cylinder S by σ (u, v) = γ (u) + vδδ , where γ is a unit-speed curve, δ is a constant unit vector parallel to the rulings, and γ̇γ = dγγ /du is perpendicular to δ for all values of u. Then the first fundamental form of σ is du2 + dv 2 , so the map σ (u, v) 7→ (u, v, 0) is a local isometry from S to the xy-plane. The curves on S that make a constant angle with δ correspond to the curves in the plane that make a constant angle with the axes. These are, of course, exactly the straight lines in the plane, i.e. the geodesics in the plane. It follows from Corollary 9.2.7 that the geodesics on S are exactly the curves on S making a constant angle with δ . 9.2.8 Let γ be a parameter curve v = constant, and √assume that γ is unit-speed. Then, in the usual notation, E u̇2 = 1 so u̇ = ±1/ E. By Theorem 9.2.1, γ is a geodesic if and only if (*) 1 d 1 d (E u̇) = Eu u̇2 and (F u̇) = Ev u̇2 . dt 2 dt 2 The second equation in (*) holds ⇐⇒ i.e. F ±√ E 1 √ E u̇ = u F √ E u = Ev , 2E Ev . 2E This is equivalent to the stated condition. One checks in the same way that the first equation in (*) holds identically. 9.2.9 Let γ be the unit-speed curve on the surface corresponding to u + v = c, where c is a constant. Then, u̇ + v̇ = 0 so the unit-speed condition gives (1 + u2 + 2uv + 1 + v 2 )u̇2 = 1, 91 i.e., (2 + c2 )u̇2 = 1, so u̇ (and hence also v̇) is constant. The geodesic equations are d ((1 + u2 )u̇ − uv v̇) = u̇(uu̇ − v v̇), dt d (−uv u̇ + (1 + v 2 )v̇) = v̇(v v̇ − uu̇). dt Using v̇ = −u̇ the first equation becomes d ((1 + cu)u̇) = cu̇2 , dt i.e. (1 + cu)ü = 0. Similarly, the second geodesic equation is equivalent to (1 + cv)v̈ = 0. Both equations are obviously satisfied when u̇ and v̇ are constant. 9.2.10 The geodesic equations ü = 1 d 1 Gu v̇ 2 , (Gv̇) = Gv v̇ 2 2 dt 2 must be satisfied if v = cu and c is any constant. It is easy to see that these equations are satisfied if c = 0 (since in that case u̇ = ±1 from the unit-speed condition), so we assume that c 6= 0 from now on. Then the second equation is 1 d 2 dt (Gu̇) = 2 cGv u̇ , i.e. 1 Gü + (Gu + cGv )u̇2 = 0. 2 Using the first geodesic equation and writing c = v/u we get the stated equation for G. Substituting G = f (u)/v 2 leads to the ordinary differential equation (f + 2u2 ) df = 2uf, du which can be solved for the function f (u). (The solution is 2u3 = 3f 3 ln af , where a is an arbitrary constant.) 9.2.11 Assume that the geodesic is unit-speed. The second geodesic equation in Theorem 9.2.1 gives F u̇+Gv̇ = Ω, a constant. Using this and the unit-speed condition E u̇2 + 2F u̇v̇ + Gv̇ 2 = 1 gives r G − Ω2 u̇ = ± . EG − F 2 Hence, either u = constant or, along the geodesic, r v̇ Ω − F u̇ F Ω EG − F 2 dv = = =− ± . du u̇ Gu̇ G G G − Ω2 92 b(u), where b is the binormal 9.2.12 The surface is parametrized by σ (u, v) = γ (u) + vb n, σ v = b and the first of γ (we assume that γ is unit-speed). Then σ u = t − τ vn fundamental form is (1 + τ v 2 )du2 + dv 2 . Let Γ(t) be a unit-speed geodesic on S, and denote d/dt by a dot. The first geodesic equation in Theorem 9.2.1 gives (1 + τ 2 v 2 )u̇ = c, where c is a constant. To determine c, note that, at the intersection point p Γ.t = cos α, which gives (say), Γ̇ n) + v̇b b)..t = cos α, (u̇(tt − τ vn i.e. u̇ = cos α at p. Since v = 0 at p, we have c = cos α and so u̇ = cos α . 1 + τ 2v2 The unit-speed condition (1 + τ 2 v 2 )u̇2 + v̇ 2 = 1 now gives v̇ 2 = sin2 α + τ 2 v 2 , 1 + τ 2v2 and hence du = ±q dv cos α (sin2 α + τ 2 v 2 )(1 + τ 2 v 2 ) . If τ 6= 0, |du/dv| decreases as |v| increases and, for large |v|, |du/dv| is approximately cos α/τ 2 v 2 . It follows that u approaches limits u± (say) as v → ±∞ and that u is always between these limits. If τ is always zero, then du/dv = ± cot α. If cot α 6= 0 then u → ±∞ as v → ±∞ and then γ is not contained between two rulings. If cot α = 0 then u is constant and γ is a ruling. √ √ 9.2.13 Writing E = (U + V )P , G = (U + V )Q, we have cos θ = u̇ E, sin θ = v̇ G so we have to prove that U Gv̇ 2 − V E u̇2 is constant along γ . Now 2 d d d d d (U Gv̇ 2 − V E u̇2 ) = 2U v̇ (Gv̇) − 2V u̇ (E u̇) + 2Gv̇ (U v̇) − 2E u̇ (V u̇). dt dt dt dt dt 93 Using the geodesic equations in Theorem 9.2.1, this becomes d d (U v̇) − 2E u̇ (V u̇) dt dt 2 2 = u̇ v̇(U Ev − 2EVv ) + u̇v̇ (2GUu − V Gu ) + 2GU v̇v̈ − 2EV u̇ü v̇U (Ev u̇2 + Gv v̇ 2 ) − u̇V (Eu u̇2 + Gu v̇ 2 ) + 2Gv̇ + Gv U v̇ 3 − Eu V u̇3 = u̇2 v̇(U Ev − 2EVv ) + u̇v̇ 2 (2GUu − V Gu ) d d + U (Gv̇ 2 ) − U Gu u̇v̇ 2 − V (E u̇2 ) + V Ev u̇2 v̇ dt dt = u̇2 v̇((U + V )Ev − EVv ) + u̇v̇ 2 (GUu − (U + V )Gu ) d d + U (Gv̇ 2 ) + Uu Gu̇v̇ 2 − V (E u̇2 )Vv E u̇2 v̇ dt dt d = (U Gv̇ 2 − V E u̇2 ) + u̇2 v̇((U + V )Ev − EVv ) + u̇v̇ 2 (GUu − (U + V )Gu ). dt Thus, d (U Gv̇ 2 − V E u̇2 ) = u̇2 v̇((U + V )Ev − EVv ) + u̇v̇ 2 (GUu − (U + V )Gu ). dt But, since U and P depend only on u, Ev = Vv P and so (U + V )Ev − EVv = (U + V )(Vv P − Vv P ) = 0. Similarly, GUu − (U + V )Gu = 0. 9.2.14 The first part can be verified directly. Alternatively, this parametrization can be deduced from that in (5.12) by putting a = p2 − u, b = q 2 − u, c = r 2 − u and then reparametrizing by ũ = u − v, ṽ = u − w. Straightforward algebra gives the first fundamental form as vdv 2 udu2 . (u − v) − (a + u)(b + u)(c + u) (a + v)(b + v)(c + v) Thus, the quadric is a Liouville surface with U = u, V = −v. The result now follows from the preceding exercise. 9.3.1 They are normal sections. 2 2 9.3.2 (i) Let the spheroid be obtained by rotating the ellipse xp2 + zq 2 = 1 around the z-axis, where p, q > 0. Then, p is the maximum distance of a point of the spheroid from the z-axis, so the angular momentum Ω of a geodesic must be ≤ p (we can assume that Ω ≥ 0). If Ω = 0, the geodesic is a meridian. If 0 < Ω < a, the geodesic is confined to the annular region on the spheroid contained between q 2 the circles z = ±q 1 − Ωp2 , and the discussion in Example 9.3.3 shows that the geodesic ‘bounces’ between these two circles (see diagram below). 94 If Ω = p, Eq. 9.10 shows that the geodesic must be the parallel z = 0. (ii) Let the torus be as in Exercise 4.2.5. If Ω = 0, the geodesic is a meridian (a circle). If 0 < Ω < a − b, the geodesic spirals around the torus. If Ω = a − b, the geodesic is either the parallel of radius a − b or spirals around the torus approaching this parallel asymptotically (but never crossing it): 0 <Ω< a−b Ω=a−b If a − b < Ω < a + b, the geodesic is confined to the annular region consisting of the part of the torus a distance ≥ Ω from the axis, and bounces between the two parallels which bound this region: 95 If Ω = a + b, the geodesic must be the parallel of radius a + b. q 9.3.3 The two solutions of Eq. 9.14 are v = v0 ± Ω12 − w2 , so the condition for a q self-intersection is that, for some w > 1, 2 Ω12 − w2 = 2kπ for some integer q k > 0. This holds ⇐⇒ 2 Ω12 − 1 > 2π, i.e. Ω < (1 + π 2 )−1/2 . In this case, there q are k self-intersections, where k is the largest integer such that 2kπ < 2 Ω12 − 1. 9.3.4 From the solution to Exercise 8.3.1, Z = U + iV = z−i z+i , where z = v + iw. This is a Möbius transformation, so it takes lines and circles to lines and circles and preserves angles (Appendix 2). Since the geodesics on the pseudosphere correspond to straight lines and circles in the vw-plane perpendicular to the vaxis, they correspond in the V W -plane to straight lines and circles perpendicular to the image of the V -axis under the transformation z 7→ z−i z+i , i.e. the unit circle 2 2 V + W = 1. A straight line aV̄ + bW̄ = c in the V̄ W̄ -plane (where a, b, c are constants) corresponds to the curve 2aV + 2bW = c(V 2 + W 2 + 1) in the V W -plane. If c = 0 this is a straight line through the origin, which corresponds to a geodesic on the pseudosphere by the first part. If c 6= 0 it is the equation of a circle with centre (a/c, b/c) and squared radius (a2 + b2 − c2 )/c2 . This circle intersects the boundary circle V 2 + W 2 = 1 orthogonally because the square of the distance between the centres of the two circles is equal to the sum of the squares of their radii. Hence this circle also corresponds to a geodesic on the pseudosphere. This proves that every straight line in the V̄ W̄ -plane corresponds to a geodesic on the pseudosphere. That every geodesic on the pseudosphere arises from a straight line in the V̄ W̄ -plane in this way can be proved by similar arguments, or by noting that there is a straight line in the V̄ W̄ -plane passing through any point of the disc V̄ 2 + W̄ 2 < 1 in any direction and using Proposition 9.2.4. 9.3.5 By Proposition 9.3.1(ii), a surface of revolution for which every parallel is a geodesic would have df /du = 0 for all values of u, and hence f = constant. 96 Then the surface would be a circular cylinder. 9.3.6 By Exercise 6.1.6(iii), the first fundamental form is cosh2 u(du2 + dv 2 ), so the result is a special case of Exercise 9.2.11. 9.3.7 By Clairaut’s Theorem 9.3.2, ρ is constant along every geodesic. It follows that ρ is actually a constant (and hence the surface is a circular cylinder). For if not, then dρ/dz 6= 0 for some value of z, say z = z0 . But then a geodesic passing through a point on the parallel z = z0 and not tangent to that parallel would have non-constant ρ, contrary to hypothesis. 9.3.8 By Clairaut’s Theorem, a geodesic on the unit cylinder (for which ρ is a constant) must have ψ = constant, i.e. the geodesic must intersect the meridians (i.e. the rulings) of the cylinder at a constant angle. By Exercise 4.1.6, the curves on the cylinder that have this property are the straight lines (rulings), circles (parallels) and helices. 9.3.9 The first fundamental form is du2 + k 2 cos2 udv 2 . By Clairaut’s Theorem, (k 2 cos2 u)v̇ = Ω, where Ω is a constant. As in Exercise 9.2.11, we find that, along any geodesic that is not a parallel, dv du 2 = Ω2 . k 2 cos2 u(k 2 cos2 u − Ω2 ) The geodesic γ makes an angle α with the parallel u = 0 at the point σ (0, 0) = (k, 0, 0). Hence, γ̇γ .σ v = cos α, k which gives v̇ = cos α/k at (k, 0, 0). On the other hand, v̇ = Ω/k 2 cos2 u = Ω/k 2 at (k, 0, 0). Hence, Ω = k cos α and we get dv du 2 = cos2 α . k 2 cos2 u(cos2 u − cos2 α) This gives k Integrating, dv sec2 u = ±√ 2 . du tan α − tan2 u kv = ± sin −1 tan u tan α , 97 and hence tan u = ± tan α sin kv. Since | sin kv| ≤ 1, the maximum value of u along the geodesic is α, so the maximum height above the xy-plane is Z α 0 p 1 − k 2 sin2 θ dθ. 9.3.10 (i) We note that all geodesics γ (t) on the pseudosphere, except meridians, are defined only for t in some finite interval α ≤ t ≤ β, say, whereas meridians are defined on a semi-infinite interval. Since f (γγ (t)) is a geodesic defined on the same interval as γ (t), it follows that f takes meridians to meridians, i.e. if v is constant, so is ṽ. Hence, ṽ does not depend on w. (ii) f preserves angles and takes meridians to meridians, so must take parallels to parallels. Hence, w̃ does not depend on v. (iii) The parallel w = constant has length 2π/w by Exercise 8.3.2(i) (w = e−u ). As f preserves lengths, part (ii) implies that 2π/w = 2π/w̃, so w = w̃. σ(u, v)) = σ (F (v), w)for some smooth (iv) We now know that f (σ function F (v). 2 The first fundamental form of σ (F (v), w) is w−2 dF dv 2 + dw2 ; since f is an dv isometry, this is equal to w−2 (dv 2 + dw2 ), hence dF/dv = ±1, so F (v) = ±v + α, where α is a constant. If the sign is +, f is rotation by α around the z-axis; if the sign is −, f is reflection in the plane containing the z-axis making an angle α/2 with the xz-plane. 9.4.1 From Exercise 6.2.1, the cone is√ isometric to the ‘sector’ S of the plane with vertex at the origin and angle π 2: 111111111111111111 000000000000000000 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 O 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 000000000000000000 111111111111111111 Geodesics on the cone correspond to possibly broken line segments in S: if a line segment meets the boundary of S at a point A, say, it may continue from the point B on the other boundary line at the same distance as A from the origin and with the indicated angles being equal: 98 B O A (i) TRUE: if two points P and Q can be joined by a line segment in S there is no problem; otherwise, P and Q can be joined by a broken line segment satisfying the conditions above: q1 Q q2 O p1 S R P p2 To see that this is always possible, let p1 , p2 , q1 and q2 be the indicated distances, and let R and S be the points on the boundary of the sector at a distance (p2 q1 + p1 q2 )/(p2 + q2 ) from the origin. Then, the broken line segment joining P and R followed by that joining S and Q is the desired geodesic. (ii) FALSE: Q P (iii) FALSE: many meet in two points, such as the two geodesics joining P and Q in the diagram in (ii). (iv) TRUE: the meridians do not intersect (remember that the vertex of the cone has been removed), and parallel straight lines that are entirely contained in S 99 do not intersect. (v) TRUE: since (broken) line segments in S can clearly be continued indefinitely in both directions. (vi) TRUE: a situation of the form O in which the indicated angles are equal is clearly impossible. But the answer to this part of the question depends on the angle of the cone: if the angle is α, instead of π/4, lines can self-intersect if α < π/6, for then the corresponding sector in the plane has angle < π: O 9.4.2 We consider the intersection of S 2 with the plane passing through p and q and making an angle θ with the xy-plane, where −π/2 < θ < π/2. This intersection is a circle Cθ but it is not a great circle unless θ = 0. Hence, if θ 6= 0, the short segment of Cθ joining p and q is not a geodesic and so has length > π/2 (the length of the shortest geodesic joining p and q). Since the length of Cθ is ≤ 2π, the length of the long segment of Cθ joining p and q has length < 3π/2 if θ 6= 0, i.e. strictly less than the length of the long segment of the geodesic C0 joining p and q. So the long geodesic segment is not a local minimum of the length of curves joining p and q. 2 2 9.4.3 (i) This is obvious if n ≥ 0 since e−1/t → 0 as t → 0. We prove that t−n e−1/t → 0 as t → 0 by induction on n ≥ 0. We know the result if n = 0, and if n > 0 100 t−n 2 e1/t we can apply L’Hopital’s rule: limt→0 = limt→0 nt−n−1 2 1/t2 3e = limt→0 t n t−(n−2) 2 e1/t2 , which vanishes by the induction hypothesis. (ii) We prove by induction on n that θ is n-times differentiable with dn θ = dtn Pn (t) −1/t2 t3n e 0 if t 6= 0, if t = 0, where Pn is a polynomial in t. For n = 0,the assertion holds with P0 = 1. Pn′ 2Pn −3nPn dn+1 θ −1/t2 if t 6= Assuming the result for some n ≥ 0, dtn+1 = t3n+1 + t3n + t3n+3 e 0, so we take Pn+1 = (2 −3nt2 )Pn +t3 Pn′ . If t = 0, Pn (0) limt→0 −1/t2 e t3n+1 dn+1 θ dtn+1 = limt→0 Pn (t) −1/t2 e t3n+1 = = 0 by part (i). Parts (iii) and (iv) are obvious. 9.4.4 For the circular cylinder, the answers are: (i) true; (ii) false; (iii) false; (iv) true; (v) true; (vi) false; (vii) true. For the sphere: (i) true; (ii) false; (iii) false; (iv) false; (v) true; (vi) false; (vii) true. RR σ r dr = R. Differentiating with σ r = 1, so 0 σ r .σ 9.5.1 Since γ θ is unit-speed, σ r .σ RR σ rθ dr = 0, and then integrating by parts gives respect to θ gives 0 σ r .σ σ r |r=R σ θ .σ r=0 − Z R σ rr dr = 0. σ θ .σ 0 Now σ (0, θ) = p for all θ, so σ θ = 0 when r = 0. So we must show that the integral in the last equation vanishes. But, σ rr = γ̈γ θ , the dot denoting the derivative with respect to the parameter r of the geodesic γ θ , so σ rr is parallel N = 0, it follows that σ θ .σ σ rr = 0. The first to the unit normal N of σ ; since σ θ .N σ r = 1 and σ r .σ σ θ = 0. fundamental form is as indicated since σ r .σ R1q R1q 2 2 ˙ γ p q 9.5.2 (i) The length of the part of between and is 0 f + Gġ dt ≥ 0 f˙2 dt = f (1) − f (0) = R. (ii) Use the hint, noting that the length of the part of γ between p and q′ is ≥ R. (iii) If the part of γ between p and q has length R, then it must stay inside theqgeodesic circle with centre p and radius R by (ii), and then we must have R1q R1 f˙2 + Gġ 2 dt = f˙2 dt. Then Gġ = 0 for all t ∈ (0, 1), so ġ = 0 (as G > 0) 0 0 and so g is a constant which must be α as γ passes through q. This means that γ is a parametrization of the radial line θ = α. 9.5.3 The first fundamental form is dr 2 + Gdθ 2 and a geodesic circle is a parameter curve r = constant. By Exercise 7.3.15, its geodesic curvature is Gr /2G. We are 101 given that this is a function of r only, say A(r). Then, ∂ (ln G) = A(r) ∂r Z ln G = ∴ ∴ R where f (r) = e A(r)dr A(r)dr + B(θ) (say) G = f (r)g(θ), and g(θ) = eB(θ) . Chapter 10 σ u , σ v } is FI−1 FII = 10.1.1 The matrix of the Weingarten map with respect to the basis {σ −1 cos2 v 0 − cos2 v 0 = = −I, so Nu = σ u , Nv = σ v . Thus, N = 0 1 0 −1 σ −aa, where a is a constant vector. Hence, k σ −aa k = 1, showing that the surface is an open subset of the sphere S of radius 1 and centre a. The standard latitudelongitude parametrization σ (u, v) of S 2 has first and second fundamental forms both given by du2 + cos2 udv 2 , so the parametrization σ (v, u) + a of S has the given first and second fundamental forms (the second fundamental form changes σ u × σ v ). sign because σ v × σ u = −σ 10.1.2 Γ122 = sin u cos u and the other Christoffel symbols are zero; the second Codazzi– Mainardi equation is not satisfied. 10.1.3 The Christoffel symbols are Γ111 = 0, Γ211 = 1/w, Γ112 = −1/w, Γ212 = 0, Γ122 = 0, Γ222 = −1/w. Using the first equation in Proposition 10.1.2 we get K = −1. The Codazzi-Mainardi equations are Lw = −(L + N )/w, Nv = 0. Hence, N depends only on w, and since −1 = K = LN/EG, we have LN = −1/w4 so L also depends only on w; the first Codazzi-Mainardi equation gives dL/dw = −L/w + 1/Lw5 , which is the stated differential equation. Putting P = Lw2 we 2 2 get dP/dw = (1 + P 2 )/wP √ which integrates to give 1 + P = Cw , where C > 0 is a constant, i.e. L = ± Cw2 − 1/w. Hence, the second fundamental form is only defined for w ≥ C −1/2 or w ≤ −C −1/2 . The first fundamental form is this exercise is the same as that of a suitable parametrization of the pseudosphere (see Exercise 8.3.1(i)). We saw that the pseudosphere corresponds to (part of) the region w > 1. 10.1.4 The Christoffel symbols are Γ111 = Eu /2E, Γ211 = −Ev /2G, Γ112 = Ev /2E, Γ212 = Gu /2G, Γ122 = −Gu /2E, Γ222 = Gv /2G. The first Codazzi–Mainardi equation is LEv 1 −Ev L N Lv = = Ev , −N + 2E 2G 2 E G 102 and similarly for the other equation. Finally, LEv Ev N Ev N L Ev L − 2 = = + − (κ2 − κ1 ), (κ1 )v = 2E E G E 2E G E 2E and similarly for (κ2 )u . 10.1.5 If E, F, G, L, M, N are constant, the Christoffel symbols are all zero so Eqs. 10.1 are obviously satisfied, and the Gauss equations (Proposition 10.1.2) are satisfied ⇐⇒ K = 0, i.e. LN = M 2 . Of course, we must also have E > 0, G > 0 and EG − F 2 > 0. a b E F L M Let C be the constant matrix , and let FI = , FII = . c d F G M N By Exercises 6.1.4 and 7.1.3, the reparametrization (u, v) 7→ (ũ, ṽ) leads to the stated first and second fundamental forms if and only if κ 0 t t C FI C = I, C FII C = . 0 0 To prove the existence of an invertible matrix C satisfying these conditions, note first that since FI is symmetric, there is an orthogonal matrix P such λ 0 that P t FI P = , where λ, µ are the eigenvalues of FI (see Appendix 0 µ 0). Since the trace E + G and the determinant EG − F 2 of FI are both > 0, it follows that the sum and product −1/2 of λ, µ are both > 0, and hence that λ, µ λ 0 are both > 0. Letting A = , we have At P t FI P A = I. The 0 µ−1/2 matrix At P t FII P A issymmetric, so there is an orthogonal matrix Q such that κ 0 1 Qt (At P t FII P A)Q = , for some (constants) κ1 , κ2 . The matrix C = 0 κ2 κ 0 1 P AQ has the property that C t FI C = I, C t FII C = . 0 κ2 By Proposition 8.2.6, the principal curvatures are the roots of det(FII − κFI ) = 0. Since C is invertible, these are the same as the roots of det(C t FII C − κC t FI C) = 0, i.e. κ1 , κ2 . Since K = κ1 κ2 , one of κ1 , κ2 is zero, and we might as well assume 0 1 that κ2 = 0 (if κ1 = 0, we can replace C by C ). This gives the stated 1 0 result, with κ1 = κ. 103 If κ = 0, the surface has the same first and second fundamental forms as a plane, so by Theorem 10.1.3 the surface can be obtained from a plane by applying a direct isometry of R3 . It follows that the surface is a plane. If κ 6= 0, then by the reparametrization v 7→ |κ|−1/2 v we can assume that κ = ±1. By Examples 6.1.4, 7.1.2 and 10.1.4, in both cases there is a parametrization of the unit cylinder with these first and second fundamental forms. By Theorem 10.1.3 again, the surface is obtained by applying to this cylinder a direct isometry of R3 , and so is a circular cylinder. Ev u v u , Γ211 = − 2G , Γ112 = E , Γ212 = G , 10.1.6 (i) The Christoffel symbols are Γ111 = E 2E 2E 2G Gv Gu 2 1 Γ22 = − 2E , Γ22 = 2G . Eqs. 10.1 (with L = N = 0, M = 1) now state that (E/G)u = 0 and (E/G)v = 0. Hence, E/G is constant. (ii) If E/G = λ4 , the reparametrization ũ = λu, ṽ = λ−1 v leads to the first and second fundamental forms Ẽ(dũ2 + dṽ 2 ) and 2dũdṽ, respectively, where Ẽ = λ−2 E. (iii) If E = G, the first of the Gauss equations in Proposition 10.1.2 gives 1 − =− E i.e. Ev 2E v − Eu 2E + u Eu 2E Eu 2E 2 − Ev 2E + u v Ev 2E = 2 + Ev 2E 2 − Eu 2E 2 , 2 , E which is the stated equation. 10.1.7 The assumption is that L = N = 0. The Codazzi-Mainardi equations are −Mu = M (Γ212 − Γ111 ), Mv = M (Γ222 − Γ112 ). 10.1.8 (i) By Proposition 8.4.1, there is a patch σ (U, V ) of S containing p such that F = M = 0. If κ1 = L/E is a constant κ, Exercise 10.1.4 implies that EV = 0 (since the principal curvatures are distinct by assumption). So E is a function R√ of U only. Define u = E dU , v = V . Then the first and second fundamental 2 forms are of the form du + Gdv 2 and κdu2 + N dv 2 , respectively. (ii) The Christoffel symbols are Γ111 = Γ211 = Γ112 = 0, Γ212 = Gu /2G, Γ122 = −Gu /2G, Γ222 = Gv /2G. (iii) The parameter curve v = constant is parametrized by Γ(u) = σ (u, v). DeΓ = σ u , Γ̈ Γ = σ uu ... N, by Proposition 7.4.4 noting d/du by a dot, we have Γ̇ = κN Nu = −κ2 σ u . Since and part√(ii). By the proof of Proposition 8.1.2, Γ = κN σ u , σ v / G, N} is a right-handed orthonormal basis of R3 , {σ Γ × Γ̈ Γk κ k Γ̇ = k √ σ v k = |κ|. 3 Γk G k Γ̇ 104 The torsion of Γ is ... √ Γ .(Γ̇ Γ × Γ̈ Γ) σ v / G) (−κ2 σ u )..(−κσ = 0, = κ2 Γ × Γ̈ Γ k2 k Γ̇ since σ u.σ v = 0. It follows that Γ is a circle of radius r = 1/|κ|. Nu = −κ2 σ u , so σ uu + r12 u is a function of v only. Hence, σ (u, v) = (iv) σ uuu = κN γ (v) + C (v) cos ur + D(v) sin ur for some smooth functions C , D, γ of v. We may assume that the curve γ is unit-speed, since replacing v by a smooth function of v does not change the coefficients E, F, L, M (as F = M = 0). By (iii), k σ (u, v) k2 = r 2 for all u, v. This implies that C and D are perpendicular vectors of length r. Let c = r −1C , d = r −1D. (v) Using the fact that c(v) and d(v) are perpendicular unit vectors for all values of v, we get dcc u u dγγ + r .d . −cc sin + d cos σ u .σ v = dv r r dv dγ dγ for all u, v. Hence, .c = .d = 0 (= dc .d). It follows that, for some angle α dv dv (possibly depending on v), we have dv d = −n n sin α + b cos α, c = n cos α + b sin α, ±d where n and b denote the principal normal and binormal of γ , respectively. dγ (The condition dv .d = 0 implies that dα/dv = −τ , where τ is the torsion of γ .) Writing s = v, θ = α ± κu shows that σ is a reparametrization of the tube of radius r around γ (Exercise 4.2.7). 10.1.9 Since p−1Σ u , q −1Σ v and r −1Σ w are perpendicular unit vectors, Σu + bΣ Σv + cΣ Σw , Σuu = aΣ for some scalars a, b, c. We have p2 a = Σ uu.Σ u = 1 1 Σu.Σ u )u = (p2 )u = ppu , (Σ 2 2 so a = pu /p. Next, 1 Σu.Σ v )u − Σ u.Σuv = − (Σ Σu.Σu )v = −ppv , q 2 b = Σuu.Σv = (Σ 2 so b = −ppv /q 2 . Similarly, c = −ppw /r 2 , hence the stated formula for Σuu . The other formulas for the second derivatives of Σ are proved similarly. Σuu )v = We now use these formulas to compute both sides of the equation (Σ Σuv )u ; both sides are then linear combinations of Σu , Σ v and Σw . We find that (Σ 105 the coefficients of Σu are automatically equal, while equating coefficients of Σv and Σw on the two sides yields the third and fourth of Lamé’s equations. The others are proved similarly. 10.2.1 By Corollary 10.2.3(i), 1 K=− λ 2e ∂ ∂u Ẽ F̃ (eλ )u eλ F̃ G̃ ∂ + ∂v (eλ )v eλ E F F G t =− 1 (λuu + λvv ). 2eλ ∂r ∂u ∂θ ∂u ∂r ∂v ∂θ ∂v = 10.2.2 By Exercise 6.1.4, = J J, where J = u v r r . By Exercise 9.5.1, E = 1, F = 0, and we get the stated foru −v r2 r2 2 2 mulas for Ẽ, F̃ , G̃. From Ẽ − 1 = vr2 rG2 − 1 , G̃ − 1 = ur2 rG2 − 1 , we get u2 (Ẽ − 1) = v 2 (G̃ − 1). Since Ẽ and G̃ are smooth functions of (u, v), they have P P i j 2 i j 2 Taylor expansions Ẽ = i+j≤2 eij u v + o(r ), G̃ = i+j≤2 gij u v + o(r ), where o(r k ) denotes terms such that o(r k )/r k → 0 as r → 0. Equating coefficients on both sides of u2 (Ẽ − 1) = v 2 (G̃ − 1) shows that all the e’s and g’s are zero except e02 = g20 = k, say. Then, Ẽ = 1 + kv 2 + o(r 2 ), √which implies 2 that G = r 2 + kr 4 + o(r 4 ). By Corollary 10.2.3(ii), K = − √1G ∂∂r2G . From the √ first part, G = r + 21 kr 3 + o(r 3 ), hence K = −3k + o(1). Taking r = 0 gives p) = −3k. K(p R 2π R 2π √ R 2π p)R3 + o(R3 ) dθ = G dθ = 0 R − 16 K(p 10.2.3 (i) CR = 0 k σ θ k dθ = 0 p)R3 + o(R3 ) . 2π R − 16 K(p √ R R R 2π √ G drdθ is equal to (ii) Since dAσ = G drdθ, the area AR = 0 0 2π Z 0 R p) 2 1 K(p 3 3 2 2 p)r + o(r ) dr = πR 1 − r − K(p R + o(R ) . 6 12 If S = S 2 , Exercise 6.5.3 gives CR = 2π sin R = 2π(R = 61 R3 + o(R3 )), AR = 1 R4 + o(R4 )). Since K = 1 these formulas agree 2π(1 − cos R) = 2π( 21 R2 − 24 with those in (i) and (ii). 10.2.4 (i) Let s be the arc-length of γ , so that ds/dθ = λ, and denote d/ds by a dot. The first of the geodesic equations (9.2) applied to γ gives r̈ = 12 Gr θ̇ 2 . Since r = f (θ), ′ this gives λ1 λ1 f ′ = 2λ1 2 Gr . This simplifies to give the stated equation. (ii) Since σ r and γ̇γ are unit vectors, cos ψ = σ r .γ̇γ = λ1 σ r .(f ′σ r + σ θ ) = f ′ /λ. ′ ′ √ √ σ r ×σ σ θ ) = λG N, so sin ψ = G/λ. Hence, fλ = −ψ ′ sin ψ = Also, σ r ×γ̇γ = λ1 (σ √ √ ′ ′ ∂ G = − . − λG ψ ′ , and so ψ ′ = − √1G f ′′ − f λλ = − 2√1G ∂G ∂r ∂r 106 (iii) Using the formula for K in Corollary 10.2.3(ii) and the expression for the first fundamental form of σ in Exercise 9.5.1, we get ZZ T √ 1 ∂2 G √ −√ G drdθ KdAσ = G ∂r 2 0 0 √ Z α Z α √ r=f (θ) ∂ G ∂ G ′ dθ = ψ + =− ∂r ∂r 0 0 Z α Z f (θ) r=0 r=0 ! dθ. √ √ By Exercise 10.2.2, G = r +o(r) so ∂ G/∂r = 1 at r = 0, where o(r)/r → 0 as RR r → 0. Hence, ABC KdAσ = ψ(α) −ψ(0) +α = γ −(π −β) +α = α +β +γ −π. ( 6 A) C (0) B A 10.2.5 With the notation of Example 4.5.3 we have, on the median circle t = 0, θ θ θ σ t = − sin cos θ, − sin sin θ, cos , σ θ = (− sin θ, cos θ, 0), 2 2 2 hence E = 1, F = 0, G = 1 and N = − cos 2θ cos θ, − sin 2θ sin θ, − sin 2θ ; σ tt = 0, σ tθ = θ θ 1 θ θ 1 θ 1 − cos cos θ + sin sin θ, − cos sin θ − sin cos θ, − sin 2 2 2 2 2 2 2 2 giving L = 0, M = 21 . Hence, K = (LN −M 2 )/(EG−F 2 ) = −1/4. Since K 6= 0, the Theorema Egregium implies that the Möbius band is not locally isometric to a plane. 10.2.6 The catenoid has first fundamental form cosh2 u(du2 + dv 2 ) and its Gaussian curvature is K = −sech4 u (Exercise 8.1.2). If f is an isometry of the catenoid, let σ(u, v)) = σ (ũ, ṽ). By the Theorema Egregium, sech4 u = sech4 ũ, so ũ = ±u; f (σ reflecting in the plane z = 0 changes u to −u, so assume that the sign is +. Let ṽ = f (u, v); the first fundamental form of σ (u, f (u, v)) is (cosh2 u + fu2 )du2 + 2fu fv dudv + fv2 cosh2 udv 2 . , 107 Hence, cosh2 u = cosh2 u + fu2 , fu fv = 0 and fv2 cosh2 u = cosh2 u. So fu = 0, fv = ±1 and f = ±v + α, where α is a constant. If the sign is + we have a rotation by α about the z-axis; if the sign is − we have a reflection in the plane containing the z-axis and making an angle α/2 with the xz-plane. 10.2.7 Using Corollary 10.2.3(i), we find that 1 K= 4 m(2 − m) n(2 − n) + un v 2 u2 v m . Hence, the surface is flat if and only if (m, n) = (0, 0), (2, 0), (0, 2) or (2, 2). If m = n = 0 the first fundamental form is du2 + dv 2 so the surface is locally isometric to a plane (Corollary 6.2.3). If (m, n) = (2, 0), we get v 2 du2 + dv 2 , which is the first fundamental form pf a cone (Example 6.1.5), and this is locally isometric to a plane by Exercise 6.2.5. Similarly if (m, n) = (0, 2). The case in which m = n = 2 is less obvious, but the reparametrization U = 2−1/2 uv, V = ln uv transforms the first fundamental form v 2 du2 +u2 dv 2 into dU 2 +U 2 dV 2 , which is the first fundamental form of a cone. 10.2.8 Using the Christoffel symbols calculated in Exercise 7.4.4, the second of the Gauss equations (Proposition 10.1.2) gives K cos θ = 0 − (θu cot θ)v + 0 − (−θu cosec θ)(−θv cosec θ) = −θuv cot θ, hence the result. 10.2.9 By Exercise 6.2.5 and the Theorema Egregium, K = 0 for a generalized cylinder and a generalized cone. But K 6= 0 for a sphere so by the Theorema Egregium again, there can be no local isometry between a sphere and a generalized cylinder or cone. σ are 10.2.10 The first fundamental forms of σ and σ̃ 1 1 + 2 du2 + u2 dv 2 and du2 + (u2 + 1)dv 2 , u σ (u, v) is not an respectively. Since these are different, the map σ (u, v) 7→ σ̃ isometry. Nevertheless, by Corollary 10.2.3(i), the Gaussian curvatures are equal: ∂ 1 K = K̃ = − √ 2 u2 + 1 ∂u 2u √ 1 + u2 =− 1 . (1 + u2 )2 1 σ (ũ, ṽ) is an isometry, the Theorema Egregium tells us that − (1+u If σ (u, v) 7→ σ̃ 2 )2 1 = − (1+ũ2 )2 , so ũ = ±u; let ṽ = f (u, v). The first fundamental form of σ (±u, f (u, v)) is (1 + (1 + u2 )fu2 )du2 + 2(1 + u2 )fu fv dudv + (1 + u2 )fv2 dv 2 ; this σ̃ 108 is equal to the first fundamental form of σ (u, v) ⇐⇒ 1 + (1 + u2 )fu2 = 1 + 1/u2 , fu fv = 0 and (1 + u2 )fv2 = u2 . The middle equation gives fu = 0 or fv = 0, but these are both impossible by the other two equations. Hence, the isometry does not exist. 10.2.11 From the solution of Exercise 8.1.9, the Gaussian curvature of the torus (in the parametrization of Exercise 4.2.5) is K= cos θ 1 a = 2− 2 . b(a + b cos θ) b b (a + b cos θ) If σ (θ, ϕ) 7→ σ (θ̃, ϕ̃) is an isometry of the torus, the Theorema Egregium implies that we must have cos θ = cos θ̃, and hence θ̃ = ±θ (up to adding integer multiples of 2π). Since the first fundamental form is b2 dθ 2 + (a + b cos θ)2 dϕ2 , we must therefore have dϕ̃2 = dϕ2 , and hence ∂ ϕ̃/∂θ = 0, ∂ ϕ̃/∂ϕ = ±1. Hence, ϕ̃ = ±ϕ + constant. 10.2.12 Since all parameter curves are pre-geodesics we have, by Exercise 9.2.8, EEv + F Eu = 2EFu , GGu + F Gv = 2GFv . If the parameter curves intersect orthogonally, F = 0 so these equations give 2 2 Ev = Gu = 0, p the first fundamental R p form is E(u)du +G(v)dv . ReparametrizR so E(u)du, V = G(v)dv, the first fundamental form becomes ing by U = dU 2 + dV 2 . Hence, the surface is locally isometric to the plane, and so is flat by the Theorema Egregium. The result is not true without the assumption of orthogonality. Example 10.4.3 gives a parametrization σ (u, v) of S 2 (actually of a hemisphere) with the property that the pre-geodesics on S 2 correspond exactly to the straight lines in the uvplane. In particular, all the parameter curves are pre-geodesics. 10.3.1 Arguing as in the proof of Theorem 10.3.4, we suppose that J attains its maximum value > 0 at some point p ∈ S contained in a patch σ of S. We can assume that the principal curvatures κ1 and κ2 of σ satisfy κ1 > κ2 > 0 everywhere. Since H = 12 (κ1 + κ2 ), κ1 > H and J = 4(κ1 − H)2 . Thus, J increases with κ1 when κ1 > H, so κ1 must have a maximum at p, and then κ2 = 2H − κ1 has a minimum there. By Lemma 10.3.5, K ≤ 0 at p, contradicting the assumption that K > 0 everywhere. 10.3.2 We start with the parametrization σ (U, V ) = (f (U ) cos V, f (U ) sin V, g(U )), where R√ U 2U 1 − e dU . The first and second fundamental forms are f (U ) = e , g(U ) = √ U −e 2 2U 2 dU + e dV and √ 2U dU 2 + eU 1 − e2U dV 2 , respectively. In the notation 1−e √ √ of the proof of Proposition 10.3.2, κ1 = −1/eU√ 1 − e2U , κ2 = e−U 1 − e2U . So we are in case (ii) of the proof and tan ω = e−2U − 1. We find that e(U ) = 109 E/ sin2 ω = 1 1−e2U , g(V ) = G sec2 ω = 1. So Ṽ = V and Ũ = R √ dU 1−e2U = − cosh−1 (e−U ) − c for some constantqc. So U = − ln(cosh(Ũ + c)). Hence, θ = √ 2ω = 2 tan−1 e−2U − 1 = 2 tan−1 cosh2 (Ũ + c) − 1 = 2 tan−1 sinh(Ũ + c). Finally, u = 12 (Ũ + Ṽ ), v = 12 (Ṽ − Ũ ), so Ũ = u − v. √ 10.3.3 We have E = G = 1, F = cos θ and θuv = sin θ. Hence, EG − F 2 = θuv . Consider the quadrilateral bounded by the parameter curves u = u0 , u = u1 , v = v0 and v = v1 , and let α1 be the angle between the parameter curves u = u0 and v = v0 , α2 be the angle between the parameter curves u = u0 and v = v1 , α3 be the angle between the parameter curves u = u1 and v = v0 , α4 be the angle between the parameter curves u = u1 and v = v1 . The area of the quadrilateral is Z v1 v0 Z u1 θuv dudv = u0 Z v1 v0 (θv (u1 , v) − θv (u0 , v))dv = θ(u1 , v1 ) − θ(u1 , v0 ) − θ(u0 , v1 ) + θ(u0 , v0 ) = α4 − (π − α3 ) − (π − α2 ) + α1 = α1 + α2 + α3 + α4 − 2π. 10.4.1 Let f : S → S̃ be a local diffeomorphism that takes unit-speed geodesics to unitspeed geodesics. Let p ∈ S and let 0 6= v ∈ Tp S. There is a unique geodesic γ (t) on S such that γ (0) = p and γ̇γ (0) = v/ k v k. Then γ is unit-speed so γ̃γ = f ◦ γ v/ k v k) is a unit vector, i.e. is a unit-speed geodesic. In particular, γ̃γ˙ = Dp f (v v) k = k v k. This means that Dp f : Tp S → Tf (p) S̃ is an isometry, so f k Dp f (v is a local isometry. 10.4.2 Local isometries take geodesics to geodesics by Corollary 9.2.7. If we apply a v, where a 6= 0 is a constant, to a surface, the first fundamental dilation v 7→ av form is multiplied by a2 so the Christoffel symbols are unchanged (see Proposition 7.4.4). By Proposition 9.2.3, the geodesic equations are unchanged. It follows that dilations take geodesics to geodesics. Hence, any composite of local isometries and dilations also takes geodesics to geodesics. The converse is false: the map from the xy-plane to itself given by (x, y) 7→ (x, 2y) takes geodesics to geodesics (as it takes straight lines to straight lines) but is not the composite of a dilation and a local isometry. 10.4.3 (i) This is true because F is conformal. 110 (ii) The parameter curve u 7→ σ (u, v0 ) is a geodesic on σ for any fixed v0 by construction of the geodesic patch σ . Since F is a geodesic local diffeomorphism, σ (u, v0 )) is a pre-geodesic on σ̃ σ . Hence, for some smooth function u(t), u 7→ F (σ σ (u(t), v0 )) is a geodesic on σ̃ σ . The second geodesic equation in Theorem t 7→ F (σ 2 9.2.1 gives λv u̇ = 0, so λv = 0 and λ is independent of v. (iii) Let γ (t) = σ (u(t), v(t)); we can assume that γ is unit-speed. Since the first fundamental form of σ is du2 + Gdv 2 , the parameter curves v = constant and u =√ constant intersect orthogonally and unit vectors parallel to them are σ u and σ v / G, respectively. If the oriented angle between γ̇γ and the curve v = constant σ u + G−1/2 sin θσ σ v = u̇σ σ u + v̇σ σ v . Hence, u̇ = cos θ and is θ, we have γ̇γ = cos θσ sin θ v̇ = √G . The first geodesic equation in Theorem 9.2.1 gives ü = 12 Gu v̇ 2 , i.e. √ dθ u v̇ θ̇ sin θ = 21 Gu v̇ 2 . Substituting for v̇ gives dv = v̇θ̇ = 2Gsin = Gu /2 G. θ (iv) Apply (iii) to F ◦ γ and use the fact that F is conformal. (v) Parts (iii) and (iv) imply (λG)u = λGu , hence λu G = 0, hence λu = 0, i.e. λ is independent of u. By (ii), λ is constant. (vi) If Dλ−1/2 is the dilation by a factor λ−1/2 , the composite Dλ−1/2 ◦F preserves the first fundamental form and so is a local isometry, say G. Then, F = Dλ1/2 ◦G. Chapter 11 11.1.1 Let l meet the real axis at b and suppose that Re(a) > b (the case Re(a) < b is similar). The semicircle with centre c on the real axis and radius |a − d| passes through a and does not meet l provided that |a − d| ≤ |d − b|, i.e. provided d ≥ (|a|2 − b2 )/(Re(a) − b). 11.1.2 Suppose that a and b lie on a half-line geodesic, say a = r + is, b = r + it, where Rt d = ln(t/s) = d, say, so t/s r, s, t ∈ R and t > s. Then, dH (a, b) = s dw w =e . On the other hand, the formula in Proposition 11.1.4 gives 2tanh−1 d 2tanh−1 eed −1 = 2tanh−1 (tanh d2 ) = d. +1 t−s t+s = 11.1.3 The required hyperbolic line cannot be a half-line, so must be a semicircle with centre the origin, and it must have radius |a|. 11.1.4 By Proposition 11.1.4, z ∈ Ca,R ⇐⇒ 2tanh−1 2 2 2 z−a z−ā = R. If λ = tanh(R/2), this is equivalent to (1 − λ )|z| − (ā − λ a)z − (a − λ2 ā)z̄ + (1 − λ2 )|a|2 = 0. According to Proposition A.2.3, this is the equation of a circle provided that λ2 < 1, which is obvious, and |ā − λ2 a|2 > (1 − λ2 )2 |a|2 . This condition reduces to 2|a|2 > a2 + ā2 . Writing a = |a|eiθ this becomes cos 2θ < 1, which is true because a ∈ H implies 0 < θ < π. Cic,R will be a circle with centre on the imaginary axis, say at ib. Then Ca,R intersects the imaginary axis at the points i(b ± r), so these two points must 111 be a hyperbolic distance 2R apart, i.e. 2R = 2tanh−1 2ir 2ib . This gives r = 1 b+r b tanhR, which is equivalent to R = 2 ln b−r . Next, the points i(b ± r) are the same hyperbolic distance from ic, so i(b+r)−ic i(b+r)+ic = i(b−r)−ic i(b−r)+ic . This gives (b + r − c)(b − r + c) = (c + r − b)(c + r + b), which simplifies to c2 = b2 − r 2 . Parametrizing Cic,R by v = r cos θ, w = b+r sin θ, and denoting d/dθ by a dot, the R 2π √v̇ 2 +ẇ2 R 2π circumference of Cic,R is 0 dθ = 0 b+rrsin θ dθ = √b2πr = 2π sinh R. 2 −r 2 w2 R RR = Cic,R dv The area inside Cic,R is int(Cic,R ) dvdw w w by Green’s theorem, which R 2π −r sin θ = 0 b+r sin θ dθ = √b2πb − 2π = 2π(cosh R − 1). 2 −r 2 11.1.5 11.1.6 11.2.1 11.2.2 11.2.3 The circumference is 2π sinh R = 2π(R+ 61 R3 +o(R3 )) and the area is 2π(cosh R− 1 1) = 2π( 21 R2 + 24 R4 + o(R4 ))). Since K = −1 these formulas are consitent with those in Exercise 10.2.7. (See Exercise 10.2.4 for the o( ) notation.) Suppose that l is the imaginary axis for simplicity. If a = reiθ , with 0 < θ < π/2, the distance of a from l is the distance of a from the point ir on l. From the proof of Proposition 11.1.4, this distance is − ln tan θ2 . Hence, the points at a fixed distance from l are those with a constant value of θ, i.e. the straight halflines passing through the origin. Of course, there are two such half-lines for any given distance, each being the (Euclidean) reflection of the other in l. These lines are not geodesics (unless the distance is zero, in which case they coincide with l), as they are not perpendicular to the real axis. The region {(u, v) | u < 0, −π < v < π} in the parametrization of the pseudosphere corresponds to the region {(v, w) | − π < v < π, w > 1} in H, a semi-infinite rectangle in the upper half of the vw-plane. By Proposition 11.2.3, there is an isometry that takes a to i and b to ir, say, where r > 0. Since isometries leave distances unchanged, we need only prove the result for a = i, b = ir. Assume that r > 1 (the case r < 1 is similar). Then, dH (a, b) = ln r. On the other hand, if γ (t) = v(t) + iw(t) is any curve in H with√γ (t0 ) = i, γ (t1 ) = ir, say, the length of the part of γ between a and b is R t1 ẇ R r dw R t1 v̇ 2 +ẇ2 dt ≥ dt = = ln r. w 1 w t0 w t0 By applying an isometry we can assume that l is a half-line, and then the result was proved in Exercise 11.1.1. By applying an isometry, we can assume that l is the imaginary axis. Then, m must be the semicircle with centre the origin and radius |a|. Let a = ρeiθ , where ρ > 0, −π < θ < π, and let c = it, t > 0. Since tanh−1 x is a strictly increasing function of x, we have to show that a−it > a−iρ if t 6= ρ. The a+it a+iρ 2 θ sin θ second expression equals 1−sin , and the difference is 2(ρ−t) , which is 1+sin θ |a+it|2 1+sin θ > 0 if t 6= ρ. 11.2.4 (i) If a ∈ H, let l′ and m′ be the unique hyperbolic lines passing through a and perpendicular to l and m, respectively (Exercise 11.2.3). Let b and c be 112 the intersections of l′ and m′ with l and m, respectively. We are given that F (b) = b and F (c) = c, so F (l′ ) = l′ and F (m′ ) = m′ as l′ and m′ are the unique hyperbolic lines passing through b and c and perpendicular to l and m. Since a is the unique point of intersection of l′ and m′ , we must have F (a) = a. (ii) Either F or I0,1 ◦ F fixes l, m and the interior of the semicircle m. Next, either F , I0,1 ◦ F , R0 ◦ F or R0 ◦ I0,1 ◦ F fixes l, m, the interior of the semicircle m and the region H>0 = {z ∈ H | Re(z) > 0} to the right of l. Let G be this isometry. Then, G fixes each point of m because there is a unique point of m at any given distance d > 0 from i in the region H>0 . Similarly, G fixes each point of l. Hence, G is the identity by (i). (iii) Let F be any isometry of H. By the proof of Proposition 11.2.3, there is an isometry G that is a composite of elementary isometries and which takes F (i) to i and F (l) to l. Then, G ◦ F is an isometry that fixes l and i. As m is the unique hyperbolic line intersecting l perpendicularly at i, G ◦ F fixes m. By (iii), G ◦ F is one of four composites of elementary isometries. It follows that F is a composite of elementary isometries. (iv) By (iii) it suffices to prove that every elementary isometry is a composite of reflections and inversions in lines and circles perpendicular to the real axis. For reflections and inversions there is nothing to prove, so we need only consider translations and dilations. But, if a ∈ R, Ta = R0 ◦R1 , where R1 is the reflection in the line Re(z) = a/2; and if a > 0, D√a = I0 ◦ I, where I is inversion in the circle with centre the origin and radius a. 11.2.5 (i) This is obvious from the proof of Proposition A.1.2(ii). ad−bc If (ii) If a, b, c, d ∈ R, a calculation shows that Im(M (z)) = |cz+d| 2 Im(z). ad − bc > 0 this is > 0 whenever Im(z) > 0. Conversely, suppose that M takes H to itself. Assume that c 6= 0 and d 6= 0 (the cases in which c = 0 or d = 0 are similar but easier). Then, M must take the real axis to itself (as it must take the lower half-plane −H to itself), i.e. az+b cz+d ∈ R if z ∈ R. Taking z = 0 gives b/d = λ ∈ R, say. Letting z → ∞ gives a/c = µ ∈ R, λ−µ say. Then, az+b cz+d = µ + dc z+1 . This is real whenever z is real, so c/d = ν ∈ R, say. Hence, a, b, c, d are, up to an overall multiple, equal to the real numbers µν, λ, ν, 1, respectively. The condition ad − bc > 0 now follows from the previous calculation. (iii) Following the proof (and the notation) of Proposition A.2.2, we have M = Tb/d ◦ Da/d if c = 0 (and then d 6= 0), while if c 6= 0, M = Ta/c ◦ D(ad−bc)/c2 ◦ (−K) ◦ Td/c . Hence, it suffices to show that −K is a composite of elementary isometries. But −K = R0 ◦ I0,1 in the notation of Exercise 11.2.4. (iv) J is reflection in the imaginary axis and hence an isometry of H, so the result follows from (i). 113 (v) This follows from the fact that, if M is a real Möbius transformation, so is J ◦ M ◦ J. For example, if M1 , M2 are real Möbius transformations, then (M1 ◦ J) ◦ (M2 ◦ J) = M1 ◦ (J ◦ M2 ◦ J) is a composite of real Möbius transformations, hence a real Möbius tranformation by (i). (vi) By (v) and Exercise 11.2.4(iii), it suffices to prove that every elementary isometry of H is a Möbius isometry. If a ∈ R, Ta is real Möbius and Ra = T2a ◦J. If a > 0 then Da is real Möbius. Finally, if a ∈ R, r > 0 then Ia,r = Ta ◦ Dr2 ◦ I0,1 ◦ T−a (see the proof of Proposition 11.2.1), so it suffices to prove that I0,1 is a Möbius isometry; but I0,1 = (−K) ◦ J, where −K(z) = −1/z is real Möbius. 11.2.6 By Proposition 11.1.3(i), there is a unique hyperbolic line l, say, passing through a and b. By Proposition 11.2.3, by applying a suitable isometry of H we can assume that l is the imaginary axis. Let C and C ′ be the hyperbolic circles with centres a and b, respectively, which pass through c (Exercise 11.1.4). These are Euclidean circles with centres on the imaginary axis. Suppose for a contradiction that the stated inequality is false, and let a = iw, b = iw′ , where w′ > w (interchanging the roles of a, b if necessary). Then, C intersects the imaginary axis at a point ir, say, with r > w; we must have r < w′ since r ≥ w′ implies that d(a, b) ≤ d(a, ir) = d(a, c), which contradicts our assumption. Similarly, C ′ intersects the imaginary axis at a point is, say, between a and b. Since C and C ′ intersect, we must have s ≤ r; in fact, s < r for if s = r then C and C ′ touch, contradicting the fact that a, b, c do not lie on a geodesic. Then, d(a, c) + d(c, b) = d(a, ir) + d(is, b) > d(a, ir) + d(ir, b) = d(a, b), a contradiction. 11.2.7 Let F be an isometry of H that takes l to the imaginary axis. By Exercise 11.1.5, the equidistant curves are then a pair of Euclidean half-lines l1 , l2 passing through the origin. The isometry F −1 of H, being a composite of reflections and inversions (Exercise 11.2.4), takes Euclidean lines and circles to Euclidean lines and circles (Appendix 2). Since the real axis is the only Euclidean straight line passing through a and b, F −1 must take l1 , l2 to a pair of circular arcs passing through a and b. We observed in Exercise 11.1.5 that these are not geodesics. 11.2.8 By applying a suitable isometry, we can assume that a and d are on the imaginary axis. The centre of the semicircle geodesic passing through a and b is (R, 0), 114 where a = iR cot 12 α, and its radius is Rcosec 21 α. Let d = it. We must have Rcosec 12 α < R + t. Then, d(a, d) = ln 1 R cot α t 2 < ln cot 12 α cosec 12 α − 1 = f (α). 11.2.9 As in the proof of Theorem 11.2.4, we can assume that a = a′ , that a, c and c′ are all on the imaginary axis, that b and b′ are on the same side of the imaginary axis, and that c and c′ are either both ‘above’ or both ‘below’ a on the imaginary axis. Then, clearly, c = c′ . Since the angles of the two triangles at a are equal, the geodesic through a and b is the same as that through a and b′ . Since d(a, b) = d(a, b′ ) and since b and b′ are on the same side of the imaginary axis, we must have b = b′ . 11.2.10 The proof is the same as in Euclidean geometry. Let a, b ∈ H, let d be the mid-point of the geodesic l passing through a and b, and let m be the geodesic passing through d perpendicular to l. If c is any point on m then, by the preceding exercise, the triangles with vertices a, d, c and b, d, c are congruent. In particular, d(a, c) = d(b, c). Hence, m is the set of points equidistant from a and b. 11.3.1 The distance we want is 2tanh−1 The algebra is straightforward. P −1 (b)−P −1 (a) P −1 (b)−P −1 (a) . Now use P −1 (z) = z+1 . i(z−1) 11.3.2 By Proposition 11.2.3, there is an isometry F that takes l to the real axis and the point of intersection of l and m to the origin. Then F must take m to the imaginary axis as this is the unique hyperbolic line through the origin perpendicular to the real axis. The number of such isometries is the number of isometries that take the real axis to itself and the imaginary axis to itself. If G is such an isometry, then either G, R0 ◦ G, R1 ◦ G or R1 ◦ R0 ◦ G fix the real and imaginary axes and also each quadrant into which the disc DP is divided by the axes. If H is this isometry, the argument used in the solution of Exercise 11.2.4(ii) shows that H must be the identity map. Hence, G = R0 , R1 , R0 ◦ R1 or the identity map. 11.3.3 Let us call a Möbius transformation of the type in the statement of the exercise a hyperbolic Möbius transformation. Since P is a Möbius transformation, the Möbius transformations that take DP to itself are those of the form PM P −1 , where M is a Möbius transformation that takes H to itself, i.e. a real Möbius , where a, b, c, d ∈ R and transformation (Exercise 11.2.5). If M (z) = az+b cz+d ad − bc > 0, we find that PM P −1 (z) = (a+d+i(b−c))z+a−d−i(b+c) (a−d+i(b+c))z+a+d−i(b−c) . Since |a + d + i(b − c)|2 − |a − d − i(b + c)|2 = 4(ad − bc) > 0, 115 PM P −1 is hyperbolic. Conversely, we have to show that if M is a hyperbolic Möbius transformation, then P −1 M P is a real Möbius transformation. The calculation is similar to that already given. 11.3.4 By Exercise 11.2.5(iii), the isometries of H are of the form M or M ◦ J where M is real Möbius and J(z) = −z̄. Hence, the isometries of DP are PM P −1 and −1 −1 −1 −1 −1 P(M ◦ J)P = PM P ◦ PJP . But PM P is hyperbolic and PJP (z) = z̄+1 z+1 = P i(z̄−1) = P(P −1 (z̄)) = z̄. PJ i(z−1) 11.3.5 We know that every isometry of H is the composite of reflections Ra and inversions Ia,r with a ∈ R, r > 0 (Exercise 11.2.4(iv)). Now, Ia,r = Ta ◦Dr2 ◦I0,1 ◦T−a and any translation Ta (a ∈ R) is the composite of reflections R0 ◦Ra/2 . It therefore suffices to show that, if F is any isometry of H of the form Ra (a ∈ R), Da (a > 0) or I0,1 , then P ◦ F ◦ P −1 is a composite of isometries of DP of the types in Proposition 11.3.3. We find that (a) if a 6= 0, P ◦ Ra ◦ P −1 = Ib,r , where −1 is reflection in the real axis; (c) P ◦I0,1 ◦P −1 b = 1+ia ia , r = 1/|a|; (b) P ◦R0 ◦P is reflection in the imaginary axis; (d) if a > 0, P ◦ Da ◦ P −1 is the composite of two inversions of the type in Proposition 11.3.3(i), namely Ic,√c2 −1 ◦ Ib,√b2 −1 , where b, c are real numbers such that b2 > 1, c2 > 1 and a = f (c)/f (b) where x+1 . (We can take b to be any real number > 1 and distinct from 1/f (a), f (x) = x−1 then choose c = f (af (b)); then, f (c) = f (f (af (b))) = af (b) using the property f (f (x)) = x for all x 6= 1.) 11.3.6 Suppose first that γ = π/2. The cosine rule gives cosh C = cosh A cosh B and cosh A = cosh B cosh C − sinh B sinh C cos α. Eliminating cosh C gives cos α = cosh A sinh B/ sinh C. Hence, sin2 α sinh2 C = sinh2 C − cosh2 A sinh2 B = cosh2 A cosh2 B − 1 − cosh2 A sinh2 B = cosh2 A − 1 = sinh2 A, so sin α sinh A = 1 sinh C . Interchanging the roles of A and B gives sin β sinh B = 1 sinh C . In the general case suppose that the hyperbolic line through the vertex of the triangle with angle α intersects the opposite side at a point which divides that side into segments of lengths A′ and A′′ , so that β is the angle between the sides of lengths C and A′ . Suppose also that this hyperbolic line segment has length D. Then the original triangle is divided into two triangles, one with angles π/2, β, α′ and sides of lengths C, D, A′ and the other with angles π/2, γ, α′′ and sides of lengths B, D, A′′ . Applying the first part to each of these triangles gives sin β/ sinh D = 1/ sinh C and sin γ/ sinh D = 1/ sinh B. Hence, sin β/ sinh B = sin γ/ sinh C. The other equation is proved by interchanging the roles of A and B (for example). The case in which the hyperbolic line through a vertex meets 116 the hyperbolic line through the other two vertices in a point outside the triangle is similar. 11.3.7 (i) This was established in the solution of the preceding exercise. B cosh C−cosh A B and cos α = coshsinh . (ii) Using the sine and cosine rules, sin β = sinh sinh C B sinh C 2 cos α cosh B cosh C−cosh A cosh B cosh A−cosh A Hence, sin β = = = cosh A. sinh2 B sinh2 B (iii) Using sin β = sinh B/ sinh C and the cosine rule for cos β, we get cot β = sinh2 A cosh B sinh A cosh A cosh C−cosh B = sinh A sinh B sinh A sinh B = tanhB . 11.3.8 If γ = π/2 the formula we want is that in Exercise 11.3.7(ii). In the general case, we use the method (and notation) of the solution of Exercise 11.3.6. In the case where the hyperbolic line through a vertex perpendicular to the opposite side meets that side at a point inside the triangle, applying Exercise 11.3.7(ii) to the two right-angled triangles gives cosh A′ = cos α′ / sin β, cosh A′′ = cos α′′ / sin γ, so cosh A = cosh(A′ + A′′ ) = cosh A′ cosh A′′ + sinh A′ sinh A′′ = cos α′ cos α′′ tanh2 D + sin β sin γ tan β tan γ using Exercise 11.3.7(iii). By Exercise 11.3.7(ii), cosh D = cos β sin α′ = cos γ sin α′′ so cosh A sin β sin γ = cos α + sin α′ sin α′′ + tanh2 D cos β cos γ = cos α + sech2 D cos β cos γ + tanh2 D cos β cos γ = cos α + cos β cos γ. The case in which the perpendicular meets the opposite side at a point outside the triangle is similar. 11.3.9 Let γ (t) = (x(t), y(t), z(t)) be a curve on S 2 . Then, Π(γγ (t)) = (u(t), v(t)), where ẋ+xż y x u = 1−z , v = 1−z . Denoting d/dt by a dot, u̇ = (1−z) with a similar formula (1−z)2 for v̇, which give 4 u̇2 + v̇ 2 1 2 2 2 2 2 2 = (1 − z) ( ẋ + ẏ ) + (x + y ) ż + 2(x ẋ + y ẏ) ż(1 − z) . 1 + u2 + v 2 (1 − z)2 Using x2 +y 2 = 1−z 2 , which implies xẋ+y ẏ = −z ż, this expression simplifies to ẋ2 +ẏ 2 +ż 2 . Hence, the length ofpΠ◦γγ calculated using the given first fundamental R 2√u̇2 +v̇ 2 R 2 form on R is 1+u2 +v 2 dt = ẋ2 + ẏ 2 + ż 2 dt, which is the length of γ . Hence, Π is an isometry. 11.3.10 Since P : H → DP is an isometry, P −1 (l1 ) and P −1 (l2 ) are geodesics in H. By Proposition 11.2.3, there is an isometry F of H that takes P −1 (l1 ) to P −1 (l2 ) 117 and P −1 (z1 ) to P −1 (z1 ). Then, PF P −1 is an isometry of DP that takes l1 to l2 and z1 to z2 . 11.3.11 Draw the radii of DP given by arg(z) = 2πk/n with k = 0, 1, . . . , n − 1, and let a0 , a1 , . . . , an−1 be the points at a Euclidean distance r (with 0 < r < 1) from the origin on these radii. For each value of r, we then have a regular hyperbolic n-gon with vertices a0 , a1 , . . . , an−1 . It is clear that the interior angle α of this n-gon is an increasing function of r and depends continuously on r. When r tends to zero, the area of the n-gon also tends to zero, so α must approach its Euclidean value (Theorem 11.1.5), namely (n − 2)π/n. On the other hand, as r tends to 1, α tend to zero. By the intermediate value theorem, when 0 < r < 1, α take every value in the interval 0 < α < (n − 2)π/n. By Exercise 11.3.8, cosh A = ∴ 2 cos 2π n + cos sin2 α2 α 2 2 cos2 πn sin2 α2 cos nπ A cosh = . 2 sin α2 1 + cosh A = ∴ 11.3.12 Let D be the length of the diagonal of the quadrilateral, and let β be the angle between the diagonal and the side of length B. By Corollary 11.3.7, cosh D = cosh A cosh B, and by the cosine rule (Theorem 11.3.6), cosh C = cosh A cosh D − sinh A sinh D sin β. By the sine rule (Exercise 11.3.6), sinh A = sinh D sin β so cosh C = cosh A cosh D − sinh2 A = cosh2 A cosh B − sinh2 A. By the sine rule, the other two (equal) angles α of the quadrilateral are given by sin α = sinh D cos β . sinh C By the cosine rule, cosh A = cosh B cosh D − sinh B sinh D cos β. 118 Hence, sin α = cosh A sinh B cosh B cosh D − cosh A = . sinh B sinh C sinh C 11.3.13 Let n be one of the geodesics bisecting the angle between l and m, and let a be a point on n. We will show that a is equidistant from l and m. By applying an isometry we can assume that n is the real axis in DP . Let j and k be the geodesics through a meeting l and m at right angles, and let b and c be the points in which j meets l and k meets m, respectively. Reflection R in the real axis is an isometry of DP that interchanges l and m and fixes each point of n. If R(c) 6= b, the hyperbolic triangle with vertices a, b and R(c) would have two angles equal to π/2, contradicting Theorem 11.1.5. It follows that R interchanges b and c, and hence that d(a, b) = d(a, c). Consider a hyperbolic triangle with vertices a, b, c and let l, m, n be the geodesics bisecting the angles at a, b, c, respectively. Let d be the point of intersection of l and m. Then, d is equidistant from all three sides of the triangle, and hence lies on n. 11.3.14 By applying an isometry of DP , we can assume that l is the imaginary axis, m is the real axis, a = 0 and c = 1. By Proposition 11.1.4, the hyperbolic circle with centre b > 0 and radius R is |z − b| R = tanh . |1 − bz| 2 If this circle passes through the origin, b = tanh R 2 so the hyperbolic circle is |z − b| = b|1 − bz|, which can be written as |z|2 − b (z + z̄) = 0. 1 + b2 As b → 1 this tends to the circle |z|2 = 12 (z + z̄), i.e. 1 z− 2 2 = 1 , 4 which is a circle Γ touching C at 1. A circle Γ̃ that intersects C perpendicularly at 1 also intersects Γ perpendicularly at 1, and hence the other intersection of Γ and Γ̃ is also at right angles. 11.4.1 Let l and m be two distinct hyperbolic lines in H that do not intersect at any point of H. If l and m are both half-lines they are parallel as they do not have 119 a common perpendicular. If at least one of l and m is a semicircle, then l and m are parallel if they intersect at a point of the real axis, and ultra-parallel otherwise. 11.4.2 We work in H and assume that l is the imaginary axis (by applying a suitable isometry). If a = v + iw, the semicircle geodesic through a intersects l at √ i v 2 + w2 = ir, say. The distance of a from l is 2tanh−1 ir−v−iw ir−v+iw . Setting this equal to a constant, say D, gives (after some algebra) v 2 /w2 = 2 sinh2 (D/2). This is the equation of a pair of lines passing through the origin. As they are not perpendicular to the real axis (unless D = 0), they are not hyperbolic lines. 11.4.3 We work in DP . By applying an isometry we can assume that a is the origin and b > 0. Suppose that the hyperbolic triangle with vertices a, b, c has internal angles α, β, γ, and assume that Re(c) > 0. The hyperbolic line through b and c is part of a circle Γ with centre d and radius r, say. The line through b and d makes an angle π/2 − β with the real axis, so d = b + r sin β + ir cos β. Similarly, d = c + r sin(α + γ) − ir cos(α + γ) = c + r sin(A + β) + ir cos(A + β) using A = π − α − β − γ. Writing c = v + iw we get v = b − r sin A cos β + r(1 − cos A) sin β, w = r(1 − cos A) cos β + r sin A sin β. Then, v(1 − cos A) + w sin A = (b + 2r sin β)(1 − cos A). But, since γ intersects the boundary C of DP perpendicularly, r 2 + 1 = |d|2 = (b + r sin β)2 + r 2 cos2 β = A r 2 + b2 + 2br sin β, so 2br sin β = 1 − b2 . Hnece, v(1 − cos A) + w sin A = 1−cos . b This is the equation of a straight line that interescts the real axis at 1/b and makes an angle A/2 with the (negative) real axis. The set of points c for which the triangle with vertices a, b, c has area A is the union of this line together with its reflection in the real axis. These lines are not hyperbolic lines as they do not pass through the origin. 11.4.4 In the first two parts of this exercise it is slightly easier to work in H (by applying P −1 ). (i) By applying a suitable isometry of H, we can assume that one of the sides of the triangle is the imaginary axis. Then the other sides must be a semicircle passing through the origin and some point a ∈ R, together with the half-line Re(z) = a. By further applying a suitable translation parallel to the real axis and a positive dilation (which are isometries of H), we can assume that the three sides are the half-lines Re(z) = ±1 and the semicircle |z|2 = 1. Then, the area of the triangle is Z 1 −1 dv Z ∞ √ 1−v 2 dw = w2 Z 1 −1 √ dv = π. 1 − v2 (ii) Let a be the vertex of the biasymptotic triangle in H, and let l be the geodesic through a perpendicular to the opposite side, meeting it at a′ , say. By applying an isometry of H, we can assume that l is the imaginary axis and that a′ = i. 120 Then, the side opposite a is the semicircle |z|2 = 1. The side joining 1 and a is an arc of a circle with centre b < 0, say, where cos α −b = . 2 1−b The equation of the circle is (v − b)2 + w2 = (1 − b)2 , so the area of the triangle is ! Z 1 1 1 √ −p dv. 2 1 − v2 (1 − v)(1 + v − 2b) 0 The second integral can be evaluated using the substitution u = v − b. This gives the area as π−2 Z 1−b −b p du −b du = 2 sin−1 1−b (1 − b)2 − u2 −b −1 = π − α. = π − 2 cos 1−b That a bisymptotic triangle with angle α exists for any 0 < α < π is proved using the method of Exercise 11.3.11. (iii) We now switch back to DP . Assume that the vertex at which the angle is α is 0, let b be the other vertex of the triangle in DP . Let the side of the triangle passing through 0 and b meet C at c, and let the other side passing through 0 meet C at d (these sides are radii of C). The area of the asymptotic triangle with vertices 0, b, d is the difference between the areas of the biasymptotic triangles with vertices 0, c, d and b, c, d, which by part (ii) is (π − α) − (π − (π − β)) = π − α − β. Let a be a point on the radius joining 0 and d and consider the triangle with vertices 0, a, b. Let the angle of this triangle at b be β ′ and the angle at a be α′ . Thus, α′ tends to zero and β ′ tends to β as a tends to d along the radius (‘tends to’ in the Euclidean sense). By Exercise 11.3.8, the length A of the side joining 0 and b is given by cos α′ + cos α cos β ′ cosh A = . sin α sin β ′ Letting a tend to c, we obtain cosh A = 1 + cos α cos β . sin α sin β 121 11.4.5 (i) Let a, b ∈ DP be the vertices of one of the triangles, let l be the geodesic passing through a, b and let m be the other side of the triangle passing through a; define a′ , b′ , l′ , m′ similarly for the other triangle. By applying an isometry to one of the triangles, we can assume that a = a′ , m = m′ and that l and l′ are on the same side of m. As the triangles have the same angle at a, l = l′ and by Exercise 11.4.4(iii) the lengths of the finite sides of the two triangles are equal. It follows that b = b′ , and since the two triangles have the same angle at b their third sides must also coincide. (ii) As in (i), by applying an isometry to one of the triangles we can assume that their vertices in DP coincide, as do the two sides passing through this vertex. But then the two triangles coincide. (iii) This was established in the solution of Exercise 11.4.4(i). 11.4.6 We consider the biasymptotic triangle with vertices 0, 1 and e3iπ/4 , where the two sides meeting at the origin are radii of DP and the side joining 1 and e3iπ/4 is an arc of a circle meeting C at right angles at 1 and e3iπ/4 . The ‘altitude’ of this triangle passing through 1 is a circular arc that meets C at −i, and that through e3iπ/4 is a circular arc meeting C at e5iπ/4 . These two geodesics are clearly ultraparallel (one is confined to the region v > 0, the other to the region v < 0). If we now replace the vertices 1 and e3iπ/4 with nearby points a, b ∈ DP , the altitudes of the hyperbolic triangle with vertices 1, a, b passing through a and b will still be ultraparallel. 2w v 2 +w 2 −1 2v −1 11.5.1 From Example 6.3.5, Π (v, w) = v 2 +w2 +1 , v 2 +w2 +1 , v 2 +w2 +1 , so K(v, w) = 2(v,w) . v 2 +w 2 +1 11.5.2 From Appendix 2, every Möbius transformation is a composite of transformations of the form z 7→ 1/z, z 7→ z + λ, z 7→ λz (where λ 6= 0 in the last case). Hence, it suffices to establish Eq. 11.11 when M is of this form. For the last two types this (a−1 −c−1 )(b−1 −d−1 ) is obvious; for the first, (a−1 , b−1 ; c−1 , d−1 ) = (a −1 −d−1 )(b−1 −d−1 ) = (a, b; c, d) on multiplying numerator and denominator by abcd. This argument is only valid provided none of a, b, c, d is 0 or ∞, but a similar argument works in the other cases. For example, if a = ∞ but b, c, d 6= 0, we have to show that (0, b−1 ; c−1 , d−1 ) = (∞, b; c, d). This is proved by multiplying numerator and −c−1 (b−1 −d−1 ) denominator of (0, b−1 ; c−1 , d−1 ) = −d −1 (b−1 −c−1 ) by bcd. If M : C∞ → C∞ is a bijection satisfying Eq. 11.11, let b, c, d ∈ C∞ be such that M (b) = 1, M (c) = 0, M (d) = ∞. Then, M (z) = (M (z), 1; 0, ∞) = (M (z), M (b); M (c), M (d)) = (z, b; c, d), so M is a Möbius transformation. 11.5.3 It is enough to prove the existence when a′ = ∞, b′ = 0, c′ = 1. For if M and M ′ are Möbius transformations taking (a, b, c) and (a′ , b′ , c′ ) to (∞, 0, 1), −1 then M ′ ◦ M is a Möbius transformation taking (a, b, c) to (a′ , b′ , c′ ). But M (z) = (a, b; c, z) is a Möbius transformation that takes (a, b, c) to (∞, 0, 1). For 122 the uniqueness, note that if M is a Möbius transformation that takes (a, b, c) to (∞, 0, 1), then M (z) = (∞, 0; 1, M (z)) = (a, b; c, z). 2 (a−b)(− 1 + 1 ) (a−b)(b̄−ā) a−b b̄ = − tan2 21 d by = (1+āb)(1+a = − 1+āb 11.5.4 (a, −1/ā; b, −1/b̄) = (a+ 1 )(−ā1 −b) b̄) ā b̄ Proposition 6.5.2. 11.5.5 The reflection in the line through the origin making an angle θ with the real axis 2e2iθ z̄ 2iθ is R(z) = e2iθ z̄. Then, K(R(z)) = |z| K(z) = R(K(z)). 2 +1 = e 11.5.6 This follows from Exercises 11.3.5 and 11.5.5 and Proposition 11.5.4. 11.5.7 Since K = pr ◦ Π−1 , and since Π is conformal (Example 6.3.5), it suffices 2 to show that pr : S− → D preserves the angles between curves intersecting at pr(0, 0, −1) = p (0, 0, 0). But the first fundamental form of the patch 2 is pr−1 (x, y, 0) = (x, y, − 1 − x2 − y 2 ) of S− 1 ((1 − y 2 )dx2 + 2xydxdy + (1 − x2 )dy 2 ), 1 − x2 − y 2 which reduces to dx2 + dy 2 when x = y = 0. 11.5.8 Suppose first that a, b, c, d lie on a Circle C. Let M be the Möbius transformation such that M (a) = ∞, M (b) = 0, M (c) = 1 (Exercise 11.5.3), and let M (d) = z. ˜ say (Proposition A.2.4); since C˜ passes through ∞ it Now M (C) is a Circle C, must be a straight line, and as this line passes through 0 and 1 it must be the real axis; hence z ∈ R. But (a, b; c, d) = (∞, 0; 1, z) = z (Exercise 11.5.2). Conversely, assume that (a, b; c, d) ∈ R, and let M be as above. Then, M (d) ∈ R and 0, 1, ∞, M (d) lie on a Circle C, namely the real axis. But then a, b, c, d lie on the Circle M −1 (C). 11.5.9 Let M be the Möbius transformation taking ∞, 0, 1 to a, b, c, respectively. Then, M (d) = λ. By Exercise 11.5.2, if we subject a, b, c, d to any permutation, the resulting cross-ratio will be the cross-ratio of the points obtained by subjecting ∞, 0, 1, λ to the same permutation. It therefore suffices to check that the six stated values are the values of the cross-ratios of the points ∞, 0, 1, λ taken in any order. This is straightforward. Chapter 12 12.1.1 κ1 + κ2 = 0 =⇒ κ2 = −κ1 =⇒ K = κ1 κ2 = −κ21 ≤ 0. K = 0 ⇐⇒ κ21 = 0 ⇐⇒ κ1 = κ2 = 0 ⇐⇒ the surface is an open subset of a plane (by Proposition 8.2.9). σ u × σ v , where κ1 , κ2 are the 12.1.2 From Eq. 8.15, σ λu × σ λv = (1 − λκ1 )(1 − λκ2 )σ principal curvatures of σ . Since σ is minimal, κ2 = −κ1 so ZZ Aσ λ (U ) = (1 − λ2 κ21 ) k σ u × σ v k dudv U ZZ 2 κ21 k σ u × σ v k dudv. = Aσ (U ) − λ U 123 Since the integrand in the last integral is ≥ 0 everywhere, the stated inequality follows. Equality holds ⇐⇒ the last integral vanishes, which happens ⇐⇒ the integrand vanishes everywhere, i.e. ⇐⇒ κ1 = 0 everywhere. In that case κ2 = −κ1 = 0 also, and σ is an open subset of the plane by Proposition 8.2.9. 12.1.3 By Proposition 8.6.1, a compact minimal surface would have K > 0 at some point, contradicting Exercise 12.1.1. 12.1.4 The first part follows from Exercises 6.1.2 and 7.1.4. The map which wraps the plane onto the unit cylinder (Example 6.2.4) is a local isometry, but the plane is a minimal surface and the cylinder is not. 12.1.5 If κ1 , κ2 are the principal curvatures at the point, we have κ1 + κ2 = 0 as the surface is minimal, and κ1 = κ2 as the point is an umbilic. Hence, κ1 = κ2 = 0. 12.1.6 Let Σ0 be the minimal surface and let S = Σλ in the notation of Definition 8.5.1. Let k1 , k2 be the principal curvatures of Σ. By Proposition 8.5.2(ii), we have 1 1 − λk1 1 − λk2 2λ 1 + = + =− , κ1 κ2 ǫk1 ǫk2 ǫ since 1 k1 + 1 k2 = 0 (because k1 + k2 = 0). 12.1.7 The condition for a minimal surface is LG − 2M F + N E = 0 (Corollary 8.1.3). From the solution of Exercise 8.1.16, E = (1−κa cos θ)2 +τ 2 a2 , F = τ a2 , G = a2 , L = aτ 2 − κ cos θ(1 − κa cos θ), M = τ a, N = a, and we find that the condition for the tube to be a minimal surface is a(1 − κa cos θ)(1 − 2a cos θ) = 0, which obviously cannot hold at all points of the surface. 12.1.8 Let t1 , t2 be orthonormal principal vectors of S at p corresponding to principal curvatures κ1 , κ2 (Corollary 8.2.2). Then, t = a1t 1 + a2t2 for some a1 , a2 ∈ R, so W(tt) = κ1 a1t1 + κ2 a2t2 (where W is the Weungarten map of S at p). Hence, hW(tt), W(tt)i κ2 a2 + κ22 a22 hhhtt, tiii . = = 1 12 htt, ti htt, ti a1 + a22 But, as S is a minimal surface, κ2 = −κ1 , so hhhtt, tiii = κ21 = −κ1 κ2 = −K. htt, ti Alternatively, this exercise can be deduced from Exercise 8.1.6. 12.2.1 By the solution of Exercise 8.1.2, the helicoid σ (u, v) = (v cos u, v sin u, λu) has 124 E = λ2 + v 2 , F = 0, G = 1, L = 0, M = λ/(λ2 + v 2 )1/2 , N = 0, so H = LG−2M F +NG = 0. 2(EG−F 2 ) 12.2.2 A straightforward calculation shows that the first and second fundamental forms of σ t are cosh2 u(du2 + dv 2 ) and − cos t du2 − 2 sin t dudv + cos t dv 2 , respectively, 2 u+cos t cosh2 u = 0. so H = − cos t cosh 2 cosh4 u 12.2.3 From Example 5.3.1, the cylinder can be parametrized by σ (u, v) = γ (u) + vaa, where γ is unit-speed, k a k = 1 and γ is contained in a plane Π perpendicular to a. We have σ u = γ̇γ = t (a dot denoting d/du), σ v = a, so E = 1, F = 0, G = 1; n, σ uv = σ vv = 0, so L = κn n.(tt × a), M = N = 0. Now N = t × a, σ uu = ṫt = κn t × a is a unit vector parallel to Π and perpendicular to t, hence parallel to n; so L = ±κ and H = ±κ/2. So H = 0 ⇐⇒ κ = 0 ⇐⇒ γ is part of a straight line ⇐⇒ the cylinder is an open subset of a plane. 12.2.4 The first fundamental form is (cosh v + 1)(cosh v − cos u)(du2 + dv 2 ), so σ is conformal. By Exercise 8.5.1, to show that σ is minimal we must show that σ vv = 0; but this is so, since σ uu = (sin u cosh v, cos u cosh v, sin u2 sinh v2 ) = σ uu +σ σ vv . −σ (i) σ (0, v) = (0, 1 − cosh v, 0), which is the y-axis. Any straight line is a geodesic. (ii) σ (π, v) = (π, 1 + cosh v, −4 sinh v2 ), which is a curve in the plane x = π such that z 2 = 16 sinh2 v2 = 8(cosh v − 1) = 8(y − 2), i.e. a parabola. The d d geodesic equations are dt (E u̇) = 12 Eu (u̇2 + v̇ 2 ), dt (E v̇) = 12 Ev (u̇2 + v̇ 2 ), where a dot denotes the derivative with respect to the parameter t of the geodesic and E = (cosh v + 1)(cosh v − cos u). When u = π, the unit-speed condition is E v̇ 2 = 1, so v̇ = 1/(cosh v + 1). Hence, the first geodesic equation is 0 = 12 Eu v̇ 2 , which holds because Eu = sin u(cosh v + 1) = 0 when u = π; the second geodesic d (cosh v + 1) = (cosh v + 1) sinh v v̇ 2 = sinh v v̇, which obviously equation is dt holds. (iii) σ (u, 0) = (u −sin u, 1 −cos u, 0), which is the cycloid of Exercise 1.1.7 (in the xy-plane, with a = 1 and with t replaced by u). The second geodesic equation is satisfied because Ev = sinh v(2 cosh v + 1 − cos u) = 0 when v = 0. The unit-speed condition is 2(1 − cos u)u̇2 = 1, so u̇ = 1/2 sin u2 . The first geodesic d d equation is dt (4 sin2 u2 u̇) = sin uu̇2 , i.e. dt (2 sin u2 ) = cos u2 u̇, which obviously holds. 12.2.5 Using Exercise 8.1.1, the surface is minimal ⇐⇒ 2 (1 + g ′ )f¨ + (1 + f˙2 )g ′′ = 0, where a dot denotes d/dx and a dash denotes d/dy; hence the stated equation. Since the left-hand side of the stated equation depends only on x and the righthand side only on y, we must have f¨ 1 + f˙2 = a, g ′′ = −a, 1 + g′2 125 for some constant a. Suppose that a 6= 0. Let r = f˙; then f¨ = rdr/df and the first equation is rdr/df = a(1 + r 2 ), which can be integrated to give af = 1 2 corresponds to translating 2 ln(1 + r ), up to adding an arbitary constant (which √ the surface parallel to the z-axis). So df /dx = ± e2af − 1, which integrates to give f = − a1 ln cos a(x + b), where b is a constant; we can assume that b = 0 by translating the surface parallel to the x-axis. Similarly, g = a1 ln cos ay, after translating the surface parallel to the y-axis. So, up to a translation, we have cos ay , az = ln cos ax which is obtained from Scherk’s surface by the dilation (x, y, z) 7→ a(x, y, z). If a = 0, then f¨ = g ′′ = 0 so f = b + cx, g = d + ey, for some constants b, c, d, e, and we have the plane z = b + d + cx + ey. −1 12.2.6 Using p Exercise 8.1.1, taking f (x, y) = sin (sinh x sinh y), and writing λ = 1/ 1 − sinh2 x sinh2 y, we find that fx = λ cosh x sinh y, fy = λ cosh y sinh x, fxx = λ3 sinh x sinh y cosh2 y, fxy = λ3 cosh x cosh y, fyy = λ3 sinh x sinh y cosh2 x. It is easy to check that (1 + fy2 )fxx − 2fx fy fxy + (1 + fx2 )fyy = 0. 12.3.1 (i) From the proof of Theorem 12.3.2, the Gauss map is conformal ⇐⇒ W 2 = λ..id, where λ is a smooth function on S. If H 6= 0 at p, then H 6= 0 on an open 2 +K subset O of S containing p. By Exercise 8.1.6, W = λ 2H .id, so every point of O is an umbilic and O is an open subset of a plane or a sphere by Proposition 8.2.9. Since H 6= 0 the planar case is impossible. Part (ii) is now obvious. For (iii), assume that S is not minimal. Then, there is a point p ∈ S at which H 6= 0, say H = µ. The argument in (i) and (ii) shows that the set Sµ of points of S at which H = µ is a (non-empty) open subset of S; it is also a closed subset because H is a continuous function on S. Since S is connected, Sµ = S. Hence, every point of S is an umbilic, and so S is an open subset of a sphere (the planar case is impossible as µ 6= 0). 12.3.2 (i) From Example 12.1.4, N = (−sech u cos v, −sech u sin v, tanh u). Hence, if N(u, v) = N (u′ , v ′ ), then u = u′ since u 7→ tanh u is injective, so cos v = cos v ′ and sin v = sin v ′ , hence v = v ′ ; thus, N is injective. If N = (x, y, z), then x2 +y 2 = sech2 u 6= 0, so the image of N does not contain p the poles. Given a point −1 2 (x, y, z) ∈ S other than the poles, let u =p±sech x2 + y 2 , thepsign being that of z, and let v be such that cos v = −x/ x2 + y 2 , sin v = −y/ x2 + y 2 ; then, N(u, v) = (x, y, z). (ii) By the solution of Exercise 8.1.2, N = (λ2 + v 2 )−1/2 (−λ sin u, λ cos u, −v). Since N(u, v) = N (u + 2kπ, v) for all integers k, the infinitely-many points σ (u + 2kπ, v) = σ (u, v) + (0, 0, 2kπ) 126 of the helicoid all have the same image under the Gauss map. (Of course, this is geometrically obvious because the helicoid itself is left unchanged by the translation by 2π parallel to the z-axis.) If N = (x, y, z), then x2 +y 2 = λ2 /(λ2 +v 2 ) 6= 0, 2 2 2 so the image of pN does not contain the poles. If (x, y, z) ∈ Spand x + y 6= 0, let vp= −λz/ x2 + y 2 and let u be such that sin u = −x/ x2 + y 2 , cos u = −y/ x2 + y 2 ; then N(u, v) = (x, y, z). 12.4.1 By Proposition 12.3.2, if K 6= 0 then the Gauss map G : S → S 2 is a conformal p) local diffeomorphism. Let R be a rotation of R3 about the origin that takes G(p to the south pole of S 2 (or any point other than the north pole). There is an open subset O of S containing p such that G(O) does not contain the north pole. By Example 6.3.5, Π ◦ R ◦ G is a conformal diffeomorphism from O to an open subset U of R2 . The inverse of this diffeomorphism is the desired surface patch σ. 12.4.2 Writing x = r cos θ, y = r sin θ gives z = aθ, so we have the parametrization σ (r, θ) = (r cos θ, r sin θ, aθ). The first fundamental form of σ is dr 2 +(r 2 +a2 )dθ 2 , so σ is not a conformal parametrization. However, noting that Z r dr √ = sinh−1 , 2 2 a r +a we let ϕ = sinh−1 r a so that r = a sinh ϕ. The reparametrization σ (θ, ϕ) = σ (a sinh ϕ, θ) = (a sinh ϕ cos θ, a sinh ϕ sin θ, aθ) σ̃ has first fundamental form (r 2 + a2 )(dϕ2 + dθ 2 ) = a2 cosh2 ϕ(dθ 2 + dϕ2 ), σ is a conformal parametrization of the surface. so σ̃ 12.5.1 We have σv ϕ = σ u − iσ = (1 − u2 + v 2 − 2iuv, 2uv − i(1 − v 2 + u2 ), 2u + 2iv) = (1 − ζ 2 , −i(1 + ζ 2 ), 2ζ). So the conjugate surface is, up to a translation, Z σ (u, v) = Re (i(1 − ζ 2 ), 1 + ζ 2 , 2iζ) dζ σ̃ ζ3 2 ζ3 , ζ + , iζ = Re i ζ − 3 3 3 v u3 2 2 = −v + u v − , u + − uv , −2uv . 3 3 127 √ √ σ (U, V ) = σ (u, v); then, Let U = (u − v)/ 2, V = (u + v)/ 2, σ̃ 1 3 1 3 1 2 2 σ (U, V ) = √ U − V + UV − U V + V − U , σ̃ 3 3 2 1 1 3 1 3 2 2 2 2 √ . U + V + UV + U V − V − U , U − V 3 3 2 σ (U, V ) then Applying the π/4 rotation (x, y, z) 7→ √12 (x + y), √12 (y − x), z to σ̃ gives U − 31 U 3 + U V 2 , V − 31 V 3 + U 2 V, U 2 − V 2 , which is Enneper’s surface again. 12.5.2 ϕ = 12 (1 − ζ −4 )(1 − ζ 2 ), 2i (1 − ζ −4 )(1 + ζ 2 ), ζ(1 − ζ −4 ) , so 2 1 ζ3 i ζ3 ζ ζ −3 ζ −3 ζ −2 −1 −1 σ = Re ζ− , ζ+ , −ζ + +ζ + + 2 3 3 2 3 3 2 2 i 1 1 = Re − (ζ − ζ −1 )3 , (ζ + ζ −1 )3 , (ζ + ζ −1 )2 , 6 6 2 σ (ũ, ṽ), where up to a translation. Put ζ = eζ̃ , ζ̃ = ũ + iṽ. Then, σ (u, v) = σ̃ 4 4i σ (ũ, ṽ) = Re − sinh3 ζ̃, cosh3 ζ̃, 2 cosh2 ζ̃ σ̃ 3 3 1 = 4 sinh ũ cos ṽ(cosh2 ũ sin2 ṽ − sinh2 ũ cos2 ṽ) , 3 1 4 sinh ũ sin ṽ( sinh2 ũ sin2 ṽ − cosh2 ũ cos2 ṽ), 3 2(cosh2 ũ cos2 ṽ − sinh2 ũ sin2 ṽ) . 12.5.3 The first part is obvious. σ qv = a(σ σ u − iσ σ v ) implies that σ a = aσ σ + a, where (i) If a ∈ R, the identity σ au − iσ a a is a constant vector. Hence, σ is obtained from σ by applying the dilation Da followed by the translation Ta (Appendix 1). (ii) If f and g are the functions in the Weierstrass representation of σ (Proposition 12.5.4), those in the Weierstrass representation of σ a are af and g (see Eq. 12.23). By Eq. 12.25, replacing f by af leaves the first fundamental form unchanged, so the map σ (u, v) 7→ σ a (u, v) is an isometry, and by Eq. 12.26 N does not depend on f , so the tangent planes of σ and σ a at corresponding points are parallel. it it σ ev = eit (σ σ u − iσ σ v ). Since σ (u, v) = cosh u cos v, cosh u sin v, u), 12.5.4 We have σ eu − iσ we get it σ eu = (cos t sinh u cos v − sin t cosh u sin v, sin t cosh u cos v + cos t sinh u sin v, cos t), it σ ev = (− cos t cosh u sin v − sin t sinh u cos v, cos t cosh u cos v − sin t sinh u sin v, − sin t). 128 Integrating gives it σ e (u, v) = cos t(cosh u cos v, cosh u sin v, u) + sin t(− sinh u sin v, sinh u cos v, −v) σ (u, v) + sin tσ̂ σ (u, v), = cos tσ σ (sinh u, π2 + v) = say (up to a translation). In the notation of Exercise 6.2.3, σ̃ π (− sinh u sin v, sinh u cos v, 2 +v). Reflecting in the xy-plane and then translating σ (u, v). σ (sinh u, π2 + v) to σ̂ by π/2 along the z-axis takes σ̃ 12.5.5 (i) ϕ is never zero since we have arranged that F ′ and G′ are never both zero. Condition (ii) in Theorem 12.5.2 is obvious. ∂ d (ii) When v = 0, F ′ (z) = ∂u F (u, 0) = Fu , etc, so du σ (u, 0) = (f˙, ġ, 0) = γ̇γ (a dot denoting d/du). This proves q (ii). (−ġ,f˙,0) (iii) When v = 0, ϕ = (f˙, ġ, i f˙2 + ġ 2 ). Using Eq. 12.26, N = √ . Then, f˙2 +ġ 2 q N × γ̇γ ) = 0. It follows that γ is a N × γ̇γ = (0, 0, − f˙2 + ġ 2 ) and finally γ̈γ .(N pre-geodesic on σ (Exercise 9.1.2). σv = ϕ = (iv) If γ is the cycloid, F (z) = z − sin z, G(z) = 1 − cos z, so σ u − iσ (1 − cos z, sin z, 2i sin z). This gives u v sinh ), 2 2 v u σ v = (− sin u sinh v, − cos u sinh v, −2 sin cosh ). 2 2 σ u = (1 − cos u cosh v, sin u cosh v, −2 cos Integrating gives σ (u, v) = (u − sin u cosh v, − cos u cosh v, −4 sin u2 sinh v2 ), up to a translation. Translating by (0, 1, 0) gives Catalan’s surface. ϕ = ( 21 if (1 − g 2 ), 2i if (1 + g 2 ), if g), which 12.5.6 ϕ = ( 21 f (1 − g 2 ), 2i f (1 + g 2 ), f g) =⇒ iϕ corresponds to the pair if and g. 12.5.7 From Example 12.5.3, for the catenoid we have ϕ1 = sinh ζ, ϕ2 = −i cosh ζ, ϕ3 = 1, so f = ϕ1 − iϕ2 = sinh ζ − cosh ζ = −e−ζ , g = ϕ3 /(ϕ1 − iϕ2 ) = −eζ . Since the helicoid is the conjugate surface of the catenoid (Example 12.5.3 again), the preceding exercise gives f = −ie−ζ , g = −eζ for the helicoid. 12.5.8 By Example 6.3.5, Π(x, y, z) = (x + iy)/(1 − z). From Eq. 12.26, G(ζ) = 1 2 |g|2 +1 (g + ḡ, −i(g − ḡ), |g| − 1), so π(G(ζ)) = g + ḡ + g − ḡ = g(ζ). |g|2 + 1 − (|g|2 − 1) 12.5.9 By Eq. 12.22, i 2 1 2 −2 −2 ϕ = − (ζ − ζ ), (ζ + ζ ), 1 , 2 2 129 so the parametrization is, up to a translation, Z σ (u, v) = Re ϕ(ζ)dζ (u + iv)3 u − iv i(u + iv)3 i(u − iv) = Re − − , − , u + iv 6 2(u2 + v 2 ) 6 2(u2 + v 2 ) u 1 v 1 3 2 2 3 , (−3u v + v ) − ,u . = − (u − 3uv ) − 6 2(u2 + v 2 ) 6 2(u2 + v 2 ) By Proposition 12.5.5, the Gaussian curvature is K= −64|ζ|6 , (1 + |ζ|4 )4 √ and this tends to zero as |ζ| = u2 + v 2 → ∞. 12.5.10 Using the conformal parametrization in Exercise 12.4.2, we get σϕ ϕ = σ θ − iσ = a(− sinh ϕ sin θ − i cosh ϕ cos θ, sinh ϕ cos θ − i cosh ϕ sin θ, 1) = a(−i cos ζ, −i sin ζ, 1), where ζ = θ + iϕ. Then, f = ϕ1 − iϕ2 = −iae−iζ , ϕ3 g= = ieiζ . ϕ1 − iϕ2 By Proposition 12.5.5, 16|eiζ |2 a2 |e−iζ |2 (1 + |eiζ |2 )4 16e−2ϕ = − 2 2ϕ a e (1 + e−2ϕ )4 16 =− 2 ϕ a (e + e−ϕ )4 K=− = −a−2 sech4 ϕ. 130 Chapter 13 RR 13.1.1 If γ is a simple closed geodesic, Theorem 13.1.2 gives int(γ ) KdA = 2π; since K ≤ 0, this is impossible. The parallels of a cylinder are not the images under a π) surface patch σ : U → R3 of a simple closed curve π in the plane such that int(π is contained in U . Note that the whole cylinder can actually be covered by a single patch (see Exercise 4.1.4) in which U is an annulus, but that the parallels correspond to circles going ‘around the hole’ in the annulus. n, the geodesic curvature κg of n 13.1.2 Since the unit normal N of S 2 is equal to ±n ′′ . n ′ n n is, up to a sign, (n × ). Let t be the arc-length of γ and denote d/dt by √ 2 2 n k = k −κtt + τb b k = κ + τ = R, say, where t = a dot. Then, ds/dt = k ṅ γ̇γ . −κt +τ b d b)/R, n × n′ = (κb b + τtt)/R, and n′′ = R1 dt Then, n′ = (−κtt + τb = R b − R−2 (κ2 + τ 2 )n n. These formulas give −R−1 (κ/R)˙tt + R−1 (τ /R)˙b n × n′ ) = −R−2 τ (κ/R)˙+ R−2 κ(τ /R)˙ = (κτ̇ − τ κ̇)/R3 . n′′. (n ′ ′ d κ = ± ds tan−1 κτ . Applying Theorem 13.1.2 Since κ̇ = Rκ′ , etc, κg = ± κτκ2 −τ +τ 2 R ℓ(n) κg dt = 0 to the curve n on S 2 , and noting that K = 1 for S 2 and that 0 n)-periodic function (where ℓ(n n) is the length because κg is the derivative of an ℓ(n of the closed curve n), we get that the area inside n is 2π. 13.1.3 Before smoothing K = 0 so the total curvature is zero. To compute the total curvature after smoothing, we apply Theorem 13.1.2 to the smoothed cone with γ being the circle on the cone given by z = a for some constant a > 0. The radius of this circle is a tan α so its curvature is κ = 1/a tan α. Since the angle of the cone is α, the geodesic curvature of γ is κg = κ sin α = a−1 cos α. The part of the cone with z > a still has K = 0 so does not contribute to the total curvature. Integrating K over the part of the cone with z < a, Gauss-Bonnet gives the total curvature as ZZ Z KdA = 2π − κg ds = 2π − (a−1 cos α)(2πa tan α) = 2π(1 − sin α). γ 13.2.1 The parallel u = u1 is the circle γ 1 (v) = (f (u1 ) cos v, f (u1 ) sin v, g(u1 )); if s is the arc-length of γ 1 , ds/dv = f (u1 ). Denote d/ds by a dot and d/du by a dash. Then, γ̇γ = (− sin v, cos v, 0), γ̈γ = − f (u1 1 ) (cos v, sin v, 0), and the unit normal of the surface is N = (−g ′ cos v, −g ′ sin v, f ′ ). This gives the geodesic R ℓ(γ 1 ) ′ (u1 ) γ N × γ̇γ ) = ff (u κg ds = . Since ℓ(γ ) = 2πf (u ), curvature of γ as κg = γ̈γ .(N 1 1 0 1) RR ′ ′′ 2πf (u1 ). Similarly for γ 2 . By Example 8.1.4, K = −f /f , so R KdAσ = R 2π R u2 f ′′ − f f dudv = 2π(f ′ (u1 ) − f ′ (u2 )). Hence, 0 u1 ZZ Z ℓ(γ 2 ) Z ℓ(γ 1 ) κg ds = KdAσ . κg ds − 0 0 R 131 This equation is the result of applying Theorem 13.2.2 to the curvilinear polygon shown below. B u = u2 A u = u1 13.2.2 Applying Theorem 12.2.2 to the curvilinear n-gon, and noting the −K ≥ 1, we get X A(int(γγ )) ≤ (n − 2)π − αi . i If n ≤ 2 the right-hand side is < 0, which is absurd. If n = 3 the right hand-side is < π. 13.2.3 Consider a small curvilinear quadrilateral on S bounded by parameter curves u = a, u = a + h, v = b, v = b + k, say, where h and k are small. The internal angles are α, α, π − α, π − α, where α is the angle between the parameter curves u = a and v = b. Let A be the (small) area of the quadrilateral. Since the sides of the quadrilateral are geodesics, Theorem 13.2.2 gives K(a, b)A = (4 − 2)π − (α + α + π − α + π − α) = 0. 13.3.1 This can be proved by expressing a, b, c in component form and computing both sides. Alternatively, one may observe that both sides of the equation are linear in each of a, b, c (separately), and change sign when any two of a, b, c are interchanged. This means that it is enough to prove the formula when a = i, b = j, c = k, when both sides are obviously equal to 1. 13.3.2 Define ϕk as in the hint. The stated properties are easily checked. RR 13.4.1 By Corollary 13.4.8, S KdA = 4π(1 − g), and g = 1 since S is diffeomorphic to T1 . By Proposition 8.6.1, K > 0 at some point of S. RR 13.4.2 K > 0 =⇒ S KdA > 0 =⇒ g < 1 by Corollary 13.4.8; since g is a non-negative integer, g = 0 so S is diffeomorphic to a sphere. The converse is false: for 132 example, a ‘cigar tube’ is diffeomorphic to a sphere but K = 0 on the cylindrical part. 13.4.3 The ellipsoid is diffeomorphic to S 2 by the map (x, y, x) 7→ (x/a, y/a, RR z/b), so the genus of the ellipsoid is zero. Hence, Corollary 13.4.8 gives S KdA = 4π(1 − 0) = 4π. Parametrising the ellipsoid by σ (θ, ϕ) = (a cos θ cos ϕ, a cos θ sin ϕ, b sin θ) (cf. the latitude-longitude parametrization of S 2 ), the first and second fundamental forms of σ are (a2 sin2 θ+b2 cos2 θ)dθ 2 +a2 cos2 θdϕ2 and p ab a2 2 sin θ + b2 cos2 θ (dθ 2 +cos2 θdϕ2 ), respectively. This gives b2 , (a2 sin2 θ + b2 cos2 θ)2 p dAσ = a cos θ a2 sin2 θ + b2 cos2 θdθdϕ. K= Hence, ZZ S KdAσ = Z 0 2π Z π/2 −π/2 ab2 cos θ dθdϕ . (a2 sin2 θ + b2 cos2 θ)3/2 13.4.4 The surface in Exercise 5.4.1(ii) is diffeomorphic to S 2 , hence its Euler number is 2. 13.5.1 Assuming that every country has ≥ 6 neighbours, the argument in the proof of Theorem 13.5.1 gives E ≥ 3F and 2E ≥ 3V , so V − E + F ≤ 2E − E + E3 = 0, 3 contradicting V − E + F = 2. 13.5.2 3F = 2E because each face has three edges and each edge is an edge of two faces. From χ = V − E + F , we get χ = V − E + 32 E, so E = 3(V − χ). 133 Since each edge has two vertices and two edges cannot intersect in more than one vertex, E ≤ 12 V (V − 1); hence, 3(V − χ) ≤ 21 V (V − 1), which is equivalent √ 1 to V 2 − 7V + 6χ ≥ 0. The roots of the quadratic are 7 ± 49 − 7χ , so 2 √ √ 1 1 V ≤ 2 7 − 49 − 7χ or V ≥ 2 7 + 49 − 7χ . Since χ = 2, 0, −2, . . . , the first condition gives V ≤ 3, which would allow only one triangle; hence, the second condition must hold. 13.5.3 This is obvious since a diffeomorphism S → S̃ takes an n-coloured map on S to an n-coloured map on S̃. 13.5.4 Since three edges meet at each vertex and each edge has two vertices, we have 3V = 2E. As each edge is an edge of two countries, 2E = ∞ X ncn . n=2 Hence, E = 1 2 P P P ncn , V = 31 ncn , and since F = cn we get ∞ ∞ X 1 1X 1 (6 − n)cn . n − n + 1 cn = χ= 3 2 6 n=2 n=2 13.5.5 (i) In the notation of the preceding exercise, for a soccer ball we have cn = 0 unless n = 5 or 6 so the formula in the preceding exercise gives c5 = 12 (since χ = 2 for a sphere). (ii) This time we are given that cn = 0 unless n = 4 or 6, so the formula gives 2c4 = 12. 13.6.1 The circle θ = θ0 is a circle in the plane z = b sin θ0 with centre on the zaxis, so its principal normal is a unit vector perpendicular to the circle and in this plane, hence equal (up to a sign) to (cos ϕ, sin ϕ, 0). The unit normal of σ is N = (− cos θ cos ϕ, − cos θ sin ϕ, − sin θ), so the angle between N and n at a point of the circle θ = θ0 is θ0 . The radius of the circle is a + b cos θ0 , so its R sin θ0 geodesic curvature is a+b cos θ0 . Hence, κg ds = 2π sin θ0 and the holonomy is 2π − 2π sin θ0 . The circles ϕ = constant are geodesics (as they are meridians on a surface of revolution) so κg = 0 and the holonomy is 2π − 0 = 2π. 13.6.2 For the circle v = 1 on the cone, the radius is 1 and the angle between the principal normal n of the√circle and√the unit normal N of the cone is π/4, so the holonomy is 2π − 2π/ 2 = (2 − 2)π. The cone is flat so if the converse of Proposition 13.6.5 were true the holonomy around any closed curve on the cone would be zero. R ℓ(γ ) dϕ 13.6.3 For a general closed curve, 0 ds ds is an integer multiple of 2π, say 2nπ. Then, (13.28) is replaced by Z ℓ(γ ) κg ds. 2nπ − 0 134 13.6.4 As in the proof of Proposition 13.6.1, v = cos ϕtt + sin θtt1 , where t1 = N × t, so v = ϕ̇(− sin ϕtt + cos ϕtt1 ) + cos ϕṫt + sin ϕṫt1 . v̇ By Exercise 7.3.22, ṫt = κn N + κg t1 , ṫt1 = −κg t + τg N, so N = (κn cos ϕ + τg sin ϕ)N N, v̇v = (ϕ̇ + κg )(− sin ϕtt + cos ϕtt1 ) + (κn cos ϕ + τg sin ϕ)N by Proposition 13.6.1, and hence k v̇v k2 = (κn cos ϕ + τg sin ϕ)2 . 13.7.1 Take the reference tangent vector field to be ξ = (1, 0), and take the simple closed curve γ (s) = (cos s, sin s). At γ (s), we have V = (α, β), where (cos s + i sin s)k if k > 0, α + iβ = −k (cos s − i sin s) if k < 0. By de Moivre’s theorem, α = cos ks, β = sin ks in both cases. Hence, the angle ψ between V and ξ is equal to ks, and Definition 13.7.2 shows that the multiplicity is k. σ (ũ, ṽ), where (ũ, ṽ) 7→ (u, v) is a reparametrization map, then 13.7.2 If σ (u, v) = σ̃ ∂ ṽ ∂ ṽ σ u + βσ σ v = α̃σ̃ σ ũ + β̃σ̃ σ ṽ =⇒ α̃ = α ∂∂uũ + β ∂u , β̃ = α ∂∂vũ + β ∂v . Hence, α̃ V = ασ and β̃ are smooth if α and β are smooth. Since the components of the vectors σ u and σ v are smooth, if V is smooth so are its components. If the components σ v + βσ σ v are smooth, then V.σ σ u and V.σ σ v are smooth functions, hence of V = ασ V σ V σ V σ V σ . u) u )−F ( . v ) v )−F ( α = G( . EG−F , β = E( . EG−F are smooth functions, so V is 2 2 smooth. 13.7.3 If ψ̃ is the angle between V and ξ̃ξ , we have ψ̃ − ψ = θ (up to multiples of 2π); so R ℓ(γ ) θ̇ ds = 0 (a dot denotes d/ds). This is not obvious since we must show that 0 θ is not a well defined smooth function of s (although dθ/ds is well defined). However, ρ = cos θ is well defined and smooth, since ρ = ξ .ξ̃ξ / k ξ kk ξ̃ξ k. Now, R ℓ(γ ) ρ̇ √ ρ̇ = −θ̇ sin θ, so we must prove that 0 ds = 0. Using Green’s theorem, 2 1−ρ this integral is equal to Z Z ρu du + ρv dv p = 1 − ρ2 int(π ) π ∂ ∂u ρv p 1 − ρ2 ! ∂ − ∂v ρu p 1 − ρ2 !! dudv, π (s)); and this line integral vanishes where π is the curve in U such that γ (s) = σ (π because ! ! ∂ ρuv (1 − ρ2 ) + ρρu ρv ∂ ρv ρu p p = = . ∂u ∂v (1 − ρ2 )3/2 1 − ρ2 1 − ρ2 135 σ be 13.8.1 Let F : S → R be a smooth function on a surface S, let p ∈ S, let σ and σ̃ σ (ũ0 , ṽ0 ) = p, and let f = F ◦ σ and patches of S containing p, say σ (u0 , v0 ) = σ̃ ∂u ∂v ˜ ˜ ˜ σ f = F ◦ σ̃ . Then, fũ = fu ∂ ũ + fv ∂ ũ , fṽ = fu ∂u + fv ∂∂vṽ , so if fu = fv = 0 at ∂ ṽ (u0 , v0 ), then f˜ũ = f˜ṽ = 0 at (ũ0 , ṽ0 ). 2 2 + 2fuv ∂∂uũ ∂∂vũ + fvv ∂∂vũ , with Since fu = fv = 0 at p, we have f˜ũũ = fuu ∂u ∂ ũ ˜ similar expressionsfor f˜ũṽ and fṽṽ . This gives, in an obvious notation, H̃ = J t HJ, where J = ∂u ∂ ũ ∂v ∂ ũ ∂u ∂ ṽ ∂v ∂ ṽ is the Jacobian matrix of the reparametrization map (ũ, ṽ) 7→ (u, v). Since J is invertible, H̃ is invertible if H is invertible. Since the matrix H is real and symmetric, it has eigenvectors v1 , v2 , with eigenvalues λ1 , λ2 , say, such that vtivj = 1 if i = j and = 0 if i 6= j. Then, if v = α1v1 + α2v2 is any vector, where α1 , α2 are scalars, vt Hvv = λ1 α21 + λ2 α22 ; hence, vt Hvv > 0 (resp. < 0) for all v 6= 0 ⇐⇒ λ1 and λ2 are both > 0 (resp. both < 0) ⇐⇒ p is a local minimum (resp. local maximum); and hence p is a saddle point ⇐⇒ vt Hvv can be both > 0 and < 0, depending on the choice of v. Since vt J t HJ ṽv = vt Hvv. J is invertible, a vector ṽv 6= 0 ⇐⇒ v = J ṽv 6= 0; and ṽvt H̃ṽv = ṽ The assertions in the last sentence of the exercise follow from this. 13.8.2 (i) fx = 2x − 2y, fy = −2x + 8y, so fx = fy = 0 at the origin. fxx = 2, fxy = 2 −2 −2, fyy = 8, so H = . H is invertible so the origin is non-degenerate; −2 8 √ of H are and the eigenvalues 5 ± 13 both > 0, so it is a local minimum. 2 4 (ii) fx = fy = 0 and H = at the origin; detH = −16 < 0, so the 4 0 eigenvalues of H are of opposite sign and the origin is a saddle point. (iii) fx = fy = 0 and H = 0 at the origin, which is therefore a degenerate critical point. 13.8.3 Using the parametrization σ in Exercise 4.2.5 (with a = 2, b = 1) gives f (θ, ϕ) = σ (θ, ϕ)) = (2+cos θ) cos ϕ+3. Then, fθ = − sin θ cos ϕ, fϕ = −(2+cos θ) sin ϕ; F (σ since 2 + cos θ > 0, fϕ = 0 =⇒ ϕ = 0 or π, and then fθ = 0 =⇒ θ = 0 or π; p = (3, 0, 0), q = (1, 0, 0), r= (−1, so there are four critical points, 0, 0) and − cos θ cos ϕ sin θ sin ϕ −1 0 s = (−3, 0, 0). Next, H = = −(2 + cos 0 −3 sin θ sin ϕ θ) cosϕ 1 0 −1 0 1 0 at p, = at q, = at r, and = at s; hence, p is a 0 −1 0 1 0 3 local maximum, q and r are saddle points, and s is a local minimum (all of which is geometrically obvious). 13.8.4 Since the torus is compact, any smooth function f on the torus must achieve its maximum and minimum values, and these are of course critical points of multiplicity 1. Since the Euler number of the torus is zero, Theorem 13.8.6 implies that f must have at least two saddle points (more if f has other local 136 maxima or minima). 13.8.5 The position of the two rods can be specified by giving the angles θ and ϕ made by the rods with the vertical. The bijection takes this configuration of the rods to the point σ (θ, ϕ) of the torus, in the notation of the solution of Exercise 4.2.5. The potential energy is E = 21 aα cos θ + (a + 21 b)β cos ϕ + constant, where a, b are the lengths of the two rods and α, β are positive constants; write this as E = λ cos θ + µ cos ϕ + ν for simplicity (where λ, µ > 0 and ν are constants). For a critical point we must have ∂E/∂θ = ∂E/∂ϕ = 0, which gives sin θ = sin ϕ = 0. Thus, there are four critical points, namely (θ, ϕ) = (0, 0), (π, 0), (0, π), (π, π). In the notation of Definition 13.8.3, H= −λ cos θ 0 0 −λ cos ϕ , which is obviously invertible if θ, ϕ = 0 or π, so all the critical points are nondegenerate. At (0, 0) the matrix H has two negative eigenvalues, at (π, 0) and (0, π) it has one, and at (π, π) it has none. So (0, 0) is a local maximum, (π, 0) and (0, π) are saddle points and (π, π) is a local minimum. The left-hand side of the equation in the statement of Theorem 13.8.6 is 1 − 2 + 1 = 0, which is indeed the Euler number of the torus (Example 13.8.7). http://www.springer.com/978-1-84882-890-2