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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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100 Chapter 3. <strong>Surfaces</strong>: Further Topicsb. Compute ω 12 <strong>and</strong> dω 12 <strong>and</strong> verify that K = −1.9. Use mov<strong>in</strong>g frames to redoa. Exercise 3.1.9b. Exercise 3.1.1010. a. Use mov<strong>in</strong>g frames to reprove the result of Exercise 2.3.13.b. Suppose there are two families of geodesics <strong>in</strong> M mak<strong>in</strong>g a constant angle θ. Prove ordisprove: M is flat.11. Recall that locally any 1-form φ with dφ =0can be written <strong>in</strong> the form φ = df for somefunction f.a. Prove that if a surface M is flat, then locally we can f<strong>in</strong>d a mov<strong>in</strong>g frame e 1 , e 2 on M sothat ω 12 =0. (H<strong>in</strong>t: Start with an arbitrary mov<strong>in</strong>g frame.)b. Deduce that if M is flat, locally we can f<strong>in</strong>d a parametrization x of M with E = G =1<strong>and</strong> F =0. (That is, locally M is isometric to a plane.)12. (The Bäcklund transform) Suppose M <strong>and</strong> M are two surfaces <strong>in</strong> R 3 <strong>and</strong> f : M → M is asmooth bijective function with the properties that(i) the l<strong>in</strong>e from P to f(P )istangent to M at P <strong>and</strong> tangent to M at f(P );(ii) the distance between P <strong>and</strong> f(P )isaconstant r, <strong>in</strong>dependent of P ;(iii) the angle between n(P ) <strong>and</strong> n(f(P )) is a constant θ, <strong>in</strong>dependent of P .Prove that both M <strong>and</strong> M have constant curvature K = −(s<strong>in</strong> 2 θ)/r 2 . (H<strong>in</strong>ts: Write P = f(P ),<strong>and</strong> let e 1 , e 2 , e 3 (resp. e 1 , e 2 , e 3 )bemov<strong>in</strong>g frames at P (resp. P ) with e 1 = e 1 <strong>in</strong> the directionof −→P P . Lett<strong>in</strong>g x <strong>and</strong> x = f ◦x be local parametrizations, we have x = x + re 1 . Differentiatethis equation <strong>and</strong> deduce that ω 12 = cot θω 13 − 1 r ω 2.)4. Calculus of Variations <strong>and</strong> <strong>Surfaces</strong> of Constant Mean CurvatureEvery student of calculus is familiar with the necessary condition for a differentiable functionf : R n → R to have a local extreme po<strong>in</strong>t (m<strong>in</strong>imum or maximum) at P :Wemust have ∇f(P )=0.Phrased slightly differently, for every vector V, the directional derivativef(P + εV) − f(P )D V f(P )=limε→0 εshould vanish. Moreover, if we are given a constra<strong>in</strong>t set M = {x ∈ R n : g 1 (x) =0,g 2 (x) =0,...,g k (x) =0}, the method of Lagrange multipliers tells us that at a constra<strong>in</strong>ed extreme po<strong>in</strong>tP we must havek∑∇f(P )= λ i ∇g i (P )i=1for some scalars λ 1 ,...,λ k . (There is also a nondegeneracy hypothesis here that ∇g 1 (P ),...,∇g k (P )be l<strong>in</strong>early <strong>in</strong>dependent.)Suppose we are given a regular parametrized surface x: U → R 3 <strong>and</strong> want to f<strong>in</strong>d—without thebenefit of the analysis of Section 4 of Chapter 2—a geodesic from P = x(u 0 ,v 0 )toQ = x(u 1 ,v 1 ).

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