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DIFFERENTIAL GEOMETRY: A First Course in Curves and Surfaces

DIFFERENTIAL GEOMETRY: A First Course in Curves and Surfaces

DIFFERENTIAL GEOMETRY: A First Course in Curves and Surfaces

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92 Chapter 3. <strong>Surfaces</strong>: Further Topics*4. Us<strong>in</strong>g Proposition 1.2, prove that horizontal l<strong>in</strong>es have constant geodesic curvature κ g =1<strong>in</strong>H; prove that this is also true for circles tangent to the u-axis. (These curves are classicallycalled horocycles.)5. Prove that every curve <strong>in</strong> H of constant geodesic curvature κ g =1is of the form given <strong>in</strong>Exercise 4. (H<strong>in</strong>ts: Assume we start with an arclength parametrization (u(s),v(s)), <strong>and</strong> useProposition 1.2 to show that we have 1 = u′v + θ′ <strong>and</strong> u ′2 + v ′2 = v 2 . Obta<strong>in</strong> the differentialequation(v d2 v( dv) ) 2 3/2 ( dv) 2du 2 = 1+− − 1,dudu<strong>and</strong> solve this by substitut<strong>in</strong>g z = dv/du <strong>and</strong> gett<strong>in</strong>g a separable differential equation fordz/dv.)6. Let T a,b,c,d (z) = az + b , a, b, c, d ∈ R, with ad − bc =1.cz + da. Suppose a ′ ,b ′ ,c ′ ,d ′ ∈ R <strong>and</strong> a ′ d ′ − b ′ c ′ =1. Check thatT a ′ ,b ′ ,c ′ ,d ′◦ T a,b,c,d = T a ′ a+b ′ c,a ′ b+b ′ d,c ′ a+d ′ c,c ′ b+d ′ d(a ′ a + b ′ c)(c ′ b + d ′ d) − (a ′ b + b ′ d)(c ′ a + d ′ c)=1.Show, moreover, that T d,−b,−c,a = T −1a,b,c,d . (Note that T a,b,c,d = T −a,−b,−c,−d . The readerwho’s taken group theory will recognize that we’re def<strong>in</strong><strong>in</strong>g an isomorphism between thegroup of l<strong>in</strong>ear fractional transformations <strong>and</strong> the group SL(2, R)/{±I} of 2 × 2 matriceswith determ<strong>in</strong>ant 1, identify<strong>in</strong>g a matrix <strong>and</strong> its additive <strong>in</strong>verse.)b. Let T = T a,b,c,d . Prove that if z = u + iv <strong>and</strong> v>0, then T (z) =x + iy with y>0.Deduce that T maps H to itself bijectively.7. Show that reflection across the geodesic u =0isgiven by r(z) =−z. Use this to determ<strong>in</strong>ethe form of the reflection across a general geodesic.8. The geodesic circle of radius R centered at P is the set of po<strong>in</strong>ts Q so that d(P, Q) =R. Provethat geodesic circles <strong>in</strong> H are Euclidean circles. One way to proceed is as follows: The geodesiccircle centered at P =(0, 1) with radius R =lna must pass through (0,a) <strong>and</strong> (0, 1/a), <strong>and</strong>hence ought to be a Euclidean circle centered at (0, 1 2(a +1/a)). Check that all the po<strong>in</strong>ts onthis circle are <strong>in</strong> fact a hyperbolic distance R away from P . (H<strong>in</strong>t: It is probably easiest towork with the cartesian equation of the circle.)Remark. This result can be established rather pa<strong>in</strong>lessly by us<strong>in</strong>g the Po<strong>in</strong>caré disk modelgiven <strong>in</strong> Exercise 15.<strong>and</strong>*9. What is the geodesic curvature of a geodesic circle of radius R <strong>in</strong> H? (See Exercises 4 <strong>and</strong> 8.)10. Recall (see, for example, p. 298 <strong>and</strong> pp. 350–1 of Shifr<strong>in</strong>’s Abstract Algebra: A GeometricApproach) that the cross ratio of four numbers A, B, P, Q ∈ C ∪ {∞} is def<strong>in</strong>ed to be[A : B : P : Q] = Q − A / Q − BP − A P − B .

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