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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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§3. Surface Theory with Differential Forms 95{x21 + x 2 2 < 1, x 3 =0 } ,vertically project to the southern hemisphere of the unit sphere, <strong>and</strong>then stereographically project (from the north pole) back to the unit disk.a. Show that this mapp<strong>in</strong>g is given (<strong>in</strong> terms of polar coord<strong>in</strong>ates) by()Rx(R, θ) =(r, θ) =1+ √ 1 − R ,θ .2Compute that the first fundamental form of the Po<strong>in</strong>caré metric on D (see Exercise 15),4E =(1 − r 2 ) 2 , F =0,G = 4r 2(1 − r 2 ) 2 ,isgiven <strong>in</strong> (R, θ) coord<strong>in</strong>ates by Ẽ = 1(1 − R 2 ) 2 ,R˜F =0, ˜G 2= . (H<strong>in</strong>t: Compute carefully <strong>and</strong> economically!)1 − R2 b. Chang<strong>in</strong>g now to Euclidean coord<strong>in</strong>ates (u, v), show thatÊ =whence you derive1 − v 2(1 − u 2 − v 2 ) 2 , ˆF =uv(1 − u 2 − v 2 ) 2 , Ĝ =Γuu u 2u=1 − u 2 − v 2 , Γ uu v =0,Γuv u v=1 − u 2 − v 2 , Γ uv v u=1 − u 2 − v 2 ,Γ uvv =0,Γ vvv =1 − u 2(1 − u 2 − v 2 ) 2 ,2v1 − u 2 − v 2 .c. Use part b to show that the geodesics of the disk us<strong>in</strong>g the first fundamental form Î arechords of the circle u 2 + v 2 =1. (H<strong>in</strong>t: Show (by us<strong>in</strong>g the cha<strong>in</strong> rule) that the equationsfor a geodesic give d 2 v/du 2 = 0.) Discuss the advantages <strong>and</strong> disadvantages of this model(compared to Po<strong>in</strong>caré’s).d. Compute the distance from (0, 0) to (a, 0); compare with the formula for distance <strong>in</strong> thePo<strong>in</strong>caré model.e. Check your answer <strong>in</strong> part c by prov<strong>in</strong>g (geometrically?) that chords of the circle map byx to geodesics <strong>in</strong> the hyperbolic disk. (See Exercise 2.1.6.)3. Surface Theory with Differential FormsWe’ve seen that it can be quite awkward to work with coord<strong>in</strong>ates to study surfaces. (Forexample, the Codazzi <strong>and</strong> Gauss Equations <strong>in</strong> Section 3 of Chapter 2 are far from beautiful.) Forthose who’ve learned about differential forms, we can given a quick <strong>and</strong> elegant treatment that isconceptually quite clean.We start (much like the situation with curves) with a mov<strong>in</strong>g frame e 1 , e 2 , e 3 on (an open subsetof) our (oriented) surface M. Here e i are vector fields def<strong>in</strong>ed on M with the properties that(i) {e 1 , e 2 , e 3 } gives an orthonormal basis for R 3 at each po<strong>in</strong>t (so the matrix with thoserespective column vectors is an orthogonal matrix);(ii) {e 1 , e 2 } is a basis for the tangent space of M <strong>and</strong> e 3 = n.

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