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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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§1. Holonomy <strong>and</strong> the Gauss-Bonnet Theorem 77e 2α ′θe 1αFigure 1.2Suppose now that α is an arclength-parametrized curve <strong>and</strong> let’s write α(s) =x(u(s),v(s)) <strong>and</strong>T(s) =α ′ (s) =cos θ(s)e 1 + s<strong>in</strong> θ(s)e 2 , s ∈ [0,L], for a C 1 function θ(s) (cf. Lemma 3.6 of Chapter1), as <strong>in</strong>dicated <strong>in</strong> Figure 1.2. A formula fundamental for the rest of our work is the follow<strong>in</strong>g:Proposition 1.2. When α is an arclength-parametrized curve, the geodesic curvature of α isgiven byκ g (s) =φ 12 (s)+θ ′ 1(s) =2 √ (−Ev u ′ (s)+G u v ′ (s) ) + θ ′ (s).EGProof. Recall that κ g = κN · (n × T) =T ′ · (n × T). Now, s<strong>in</strong>ce T = cos θe 1 + s<strong>in</strong> θe 2 ,n × T = − s<strong>in</strong> θe 1 + cos θe 2 (why?), <strong>and</strong> soκ g = ∇ T T · (− s<strong>in</strong> θe 1 + cos θe 2 )= ∇ T (cos θe 1 + s<strong>in</strong> θe 2 ) · (− s<strong>in</strong> θe 1 + cos θe 2 )= ( cos θ∇ T e 1 + s<strong>in</strong> θ∇ T e 2)· (− s<strong>in</strong> θe1 + cos θe 2 )+ ( (− s<strong>in</strong> θ)θ ′ (− s<strong>in</strong> θ)+(cos θ)θ ′ (cos θ) )= (cos 2 θ + s<strong>in</strong> 2 θ)(φ 12 + θ ′ )=φ 12 + θ ′ ,as required.Next, we have (tak<strong>in</strong>g full advantage of the orthogonality of x u <strong>and</strong> x v )φ 12 = d ( )xu x√ · √ vds E Gby the formulas (‡) onp.55.= 1 √EG(xuu u ′ + x uv v ′) · x v= 1 √EG((Γuuu x u +Γ v uux v )u ′ +(Γ u uvx u +Γ v uvx v )v ′) · x v= G √EG(Γvuu u ′ +Γ v uvv ′) =□12 √ EG(−Ev u ′ + G u v ′) ,Remark. The first equality <strong>in</strong> Proposition 1.2 should not be surpris<strong>in</strong>g <strong>in</strong> the least. Curvatureof a plane curve measures the rate at which its unit tangent vector turns relative to a fixed referencedirection. Similarly, the geodesic curvature of a curve <strong>in</strong> a surface measures the rate at which itsunit tangent vector turns relative to a parallel vector field along the curve; θ ′ measures its turn<strong>in</strong>grelative to e 1 , which is itself turn<strong>in</strong>g at a rate given by φ 12 ,sothe geodesic curvature is the sum ofthose two rates.

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