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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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CHAPTER 2<strong>Surfaces</strong>: Local Theory1. Parametrized <strong>Surfaces</strong> <strong>and</strong> the <strong>First</strong> Fundamental FormLet U be an open set <strong>in</strong> R 2 .Afunction f : U → R m (for us, m =1<strong>and</strong> 3 will be most common)is called C 1 if f <strong>and</strong> its partial derivatives ∂f ∂f<strong>and</strong> are all cont<strong>in</strong>uous. We will ord<strong>in</strong>arily use∂u ∂v(u, v) ascoord<strong>in</strong>ates <strong>in</strong> our parameter space, <strong>and</strong> (x, y, z) ascoord<strong>in</strong>ates <strong>in</strong> R 3 . Similarly, for anyk ≥ 2, we say f is C k if all its partial derivatives of order up to k exist <strong>and</strong> are cont<strong>in</strong>uous. We say fis smooth if f is C k for every positive <strong>in</strong>teger k. Wewill henceforth assume all our functions are C kfor k ≥ 3. One of the crucial results for differential geometry is that if f is C 2 , then(<strong>and</strong> similarly for higher-order derivatives).Notation: We will often also use subscripts to <strong>in</strong>dicate partial derivatives, as follows:f uf vf uuf uv =(f u ) v↔↔↔↔∂f∂u∂f∂v∂ 2 f∂u 2∂ 2 f∂v∂u∂2 f∂u∂v =Def<strong>in</strong>ition. A regular parametrization of a subset M ⊂ R 3 isa(C 3 ) one-to-one functionx: U → M ⊂ R 3 so that x u × x v ≠ 0∂2 f∂v∂ufor some open set U ⊂ R 2 . 1 A connected subset M ⊂ R 3 is called a surface if each po<strong>in</strong>t has aneighborhood that is regularly parametrized.We might consider the curves on M obta<strong>in</strong>ed by fix<strong>in</strong>g v = v 0 <strong>and</strong> vary<strong>in</strong>g u, called a u-curve,<strong>and</strong> obta<strong>in</strong>ed by fix<strong>in</strong>g u = u 0 <strong>and</strong> vary<strong>in</strong>g v, called a v-curve; these are depicted <strong>in</strong> Figure 1.1. Atthe po<strong>in</strong>t P = x(u 0 ,v 0 ), we see that x u (u 0 ,v 0 )istangent to the u-curve <strong>and</strong> x v (u 0 ,v 0 )istangentto the v-curve. We are requir<strong>in</strong>g that these vectors span a plane, whose normal vector is given byx u × x v .Example 1. We give some basic examples of parametrized surfaces. Note that our parametersdo not necessarily range over an open set of values.1 For technical reasons with which we shall not concern ourselves <strong>in</strong> this course, we should also require that the<strong>in</strong>verse function x −1 : x(U) → U be cont<strong>in</strong>uous.34

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