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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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§4. Covariant Differentiation, Parallel Translation, <strong>and</strong> Geodesics 7312. a. Prove that if a geodesic is planar <strong>and</strong> not a l<strong>in</strong>e, then it is a l<strong>in</strong>e of curvature. (H<strong>in</strong>t: UseExercise 11.)b. Prove that if every geodesic of a (connected) surface is planar, then the surface is conta<strong>in</strong>ed<strong>in</strong> a plane or a sphere.13. Prove or give a counterexample:a. A l<strong>in</strong>e ly<strong>in</strong>g <strong>in</strong> a surface is both an asymptotic curve <strong>and</strong> a geodesic.b. If a curve is both an asymptotic curve <strong>and</strong> a geodesic, then it must be a l<strong>in</strong>e.c. If a curve is both a geodesic <strong>and</strong> a l<strong>in</strong>e of curvature, then it must be planar.14. Show that the geodesic curvature at P of a curve C <strong>in</strong> M is equal (<strong>in</strong> absolute value) to thecurvature at P of the projection of C <strong>in</strong>to T P M.15. Check us<strong>in</strong>g Clairaut’s relation, Proposition 4.4, that great circles are geodesics on a sphere.(H<strong>in</strong>t: The result of Exercise A.1.3 may be useful.)16. Let M be asurface <strong>and</strong> P ∈ M. WesayU, V ∈ T P M are conjugate if II P (U, V) =0.a. Let C ⊂ M be a curve. Def<strong>in</strong>e the envelope M ∗ of the tangent planes to M along C tobe the ruled surface whose generator at P ∈ C is the limit<strong>in</strong>g position as Q → P of the<strong>in</strong>tersection l<strong>in</strong>e of the tangent planes to M at P <strong>and</strong> Q. Prove that the generator at P isconjugate to the tangent l<strong>in</strong>e to C at P .b. Prove that if C is nowhere tangent to an asymptotic direction, then M ∗ is smooth (at leastnear C). Prove, moreover, that M ∗ is tangent to M along C <strong>and</strong> is a developable (flatruled) surface.c. Apply part b to give a geometric way of comput<strong>in</strong>g parallel translation. In particular, dothis for a latitude circle on the sphere. (Cf. Exercise 7.)17. Suppose that on a surface M the parallel translation of a vector from one po<strong>in</strong>t to anotheris <strong>in</strong>dependent of the path chosen. Prove that M must be flat. (H<strong>in</strong>t: Fix an orthonormalbasis e o 1 , eo 2 for T P M <strong>and</strong> def<strong>in</strong>e vector fields e 1 , e 2 by parallel translat<strong>in</strong>g. Choose coord<strong>in</strong>atesso that the u-curves are always tangent to e 1 <strong>and</strong> the v-curves are always tangent to e 2 . SeeExercise 10.)18. Use the Clairaut relation, Proposition 4.4, to describe the geodesics on the torus as parametrized<strong>in</strong> Example 1(c) of Section 1. (Start with a geodesic start<strong>in</strong>g at <strong>and</strong> mak<strong>in</strong>g angle φ 0 withthe outer parallel. Your description should dist<strong>in</strong>guish between the cases cos φ 0 ≤ a−ba+b <strong>and</strong>cos φ 0 > a−ba+b. Which geodesics never cross the outer parallel at all? Also, remember thatthrough each po<strong>in</strong>t there is a unique geodesic <strong>in</strong> each direction.)19. Use the proof of the Clairaut relation, Proposition 4.4, to show that a geodesic on a surface ofrevolution is given <strong>in</strong> terms of the st<strong>and</strong>ard parametrization <strong>in</strong> Example 7 of Section 2 by∫v = cduf(u) √ f(u) 2 − c 2 + const.

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