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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. The Gauss Map <strong>and</strong> the Second Fundamental Form 43be able to f<strong>in</strong>d parametric equations for the curve <strong>in</strong> which the bitangent plane <strong>in</strong>tersects thetorus.)2. The Gauss Map <strong>and</strong> the Second Fundamental FormGiven a regular parametrized surface M, the function n: M → Σ that assigns to each po<strong>in</strong>tP ∈ M the unit normal n(P ), as pictured <strong>in</strong> Figure 2.1, is called the Gauss map of M. Asweshallsee <strong>in</strong> this chapter, most of the geometric <strong>in</strong>formation about our surface M is encapsulated <strong>in</strong> thePnn(P)Figure 2.1mapp<strong>in</strong>g n.Example 1. A few basic examples are these.(a) On a plane, the tangent plane never changes, so the Gauss map is a constant.(b) On a cyl<strong>in</strong>der, the tangent plane is constant along the rul<strong>in</strong>gs, so the Gauss map sends theentire surface to an equator of the sphere.(c) On a sphere centered at the orig<strong>in</strong>, the Gauss map is merely the (normalized) positionvector.(d) On a saddle surface (as pictured <strong>in</strong> Figure 2.1), the Gauss map appears to “reverse orientation”:As we move counterclockwise <strong>in</strong> a small circle around P ,wesee that the unit vectorn turns clockwise around n(P ). ▽Recall from the Appendix that for any function f on M (scalar- or vector-valued) <strong>and</strong> anytangent vector V ∈ T P M,wecan compute the directional derivative D V f(P )bychoos<strong>in</strong>g a curveα: (−ε, ε) → M with α(0) = P <strong>and</strong> α ′ (0) = V <strong>and</strong> comput<strong>in</strong>g (f ◦α) ′ (0).To underst<strong>and</strong> the shape of M at the po<strong>in</strong>t P , might try to underst<strong>and</strong> the curvature at P ofvarious curves <strong>in</strong> M. Perhaps the most obvious th<strong>in</strong>g to try is various normal slices of M. That is,we slice M with the plane through P spanned by n(P ) <strong>and</strong> a unit vector V ∈ T P M.Various suchnormal slices are shown for a saddle surface <strong>in</strong> Figure 2.2. Let α be the arclength-parametrizedcurve obta<strong>in</strong>ed by tak<strong>in</strong>g such a normal slice. We have α(0) = P <strong>and</strong> α ′ (0) = V. Then s<strong>in</strong>ce thecurve lies the plane spanned by n(P ) <strong>and</strong> V, the pr<strong>in</strong>cipal normal of the curve at P must be ±n(P )(+ if the curve is curv<strong>in</strong>g towards n, − if it’s curv<strong>in</strong>g away). Apply<strong>in</strong>g Lemma 2.1 of Chapter 1

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