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DIFFERENTIAL GEOMETRY: A First Course in Curves and Surfaces

DIFFERENTIAL GEOMETRY: A First Course in Curves and Surfaces

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§2. An Introduction to Hyperbolic Geometry 89[ ] a b(i) Composition of functions corresponds to multiplication of the 2 × 2 matriceswith determ<strong>in</strong>ant 1, so we obta<strong>in</strong> a group.(ii) T maps H bijectively to H.(iii) T is an isometry of H.We leave it to the reader to check the first two <strong>in</strong> Exercise 6, <strong>and</strong> we check the third here. Giventhe po<strong>in</strong>t z = u + iv, wewant to compute the lengths of the vectors T u <strong>and</strong> T v at the image po<strong>in</strong>tT (z) =x + iy <strong>and</strong> see that the two vectors are orthogonal. Note thatso y =so we have(a(u + iv)+b)(c(u − iv)+d)az + b (az + b)(cz + d)=cz + d |cz + d| 2 =|cz + d| 2(ac(u 2 + v 2 )+(ad + bc)u ) + i ( (ad − bc)v )=v|cz + d| 2 .Nowwehave3<strong>and</strong>, similarly, ˜G =x 2 v + y 2 vy 2x u + iy u = −ix v + y v = T ′ (z) =|cz + d| 2 ,(cz + d)a − (az + b)c(cz + d) 2 =Ẽ = x2 u + yu2y 2 = 1 y 2 |T ′ (z)| 2 = 1 y 2 · 1|cz + d| 4 = 1 v 2 = E,= G. Onthe other h<strong>and</strong>,˜F = x uy u + x v y vy 2 = x u(−x v )+x v (x u )y 2 =0=F,1(cz + d) 2 ,as desired.Now, as we verify <strong>in</strong> Exercise 10 or <strong>in</strong> Exercise 12, l<strong>in</strong>ear fractional transformations carryl<strong>in</strong>es <strong>and</strong> circles <strong>in</strong> C to either l<strong>in</strong>es or circles. S<strong>in</strong>ce our particular l<strong>in</strong>ear fractional transformationspreserve the real axis (∪{∞}) <strong>and</strong> preserve angles as well, it follows that vertical l<strong>in</strong>es <strong>and</strong> semicirclescentered on the real axis map to one another. Thus, our isometries do <strong>in</strong> fact map geodesics togeodesics (how comfort<strong>in</strong>g!).If we th<strong>in</strong>k of H as model<strong>in</strong>g non-Euclidean geometry, with l<strong>in</strong>es <strong>in</strong> our geometry be<strong>in</strong>g thegeodesics, note that given any l<strong>in</strong>e l <strong>and</strong> po<strong>in</strong>t P /∈ l, there are <strong>in</strong>f<strong>in</strong>itely many l<strong>in</strong>es pass<strong>in</strong>gthrough P “parallel” to (i.e., not <strong>in</strong>tersect<strong>in</strong>g) l. Aswesee <strong>in</strong> Figure 2.3, there are also two specialcdlPFigure 2.3l<strong>in</strong>es through P that “meet l at <strong>in</strong>f<strong>in</strong>ity”; these are called ultraparallels.3 These are the Cauchy-Riemann equations from basic complex analysis.

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