Gauss Curvature and Geodesic Curvature
📂GeometryGauss Curvature and Geodesic Curvature
Buildup
{T(s),N(s),B(s),κ(s),τ(s)}
Recall how we used the Frenet-Serret apparatus when analyzing curves. When studying surfaces, we will consider similar concepts. When α is the unit speed curve, the curvature of the curve was defined as the magnitude of acceleration κ=∣T′∣=∣α′′∣. It is natural to think about how curved a surface is by looking at how curved the curves on the surface are.
Consider the surface given as x:U⊂R2→M. Let α(s) be the unit speed curve on the simple surface x. Then let’s denote the Frenet-Serret apparatus for α as follows.
{T,N,B,κ,τ}
Let’s call the unit normal at point p∈M as n. Let’s define the set of all vectors that are point p as NpM.
NpM:={rn:r∈R}={all vectors perpendicular to M at p}
Then by definition of the tangent plane, TpM is the orthogonal complement of NpM.
NpM⊥=TpM
Therefore, R3 is orthogonally decomposed as follows, and α′′ can be expressed as the linear combination of vectors of the two spaces.
R3=NpM⊕TpMandα′′(s)=n1n(s)+n2n⊥(s)(n∈NpM, n⊥∈TpM)
Let’s call T=α′ the tangent vector. Since α is the unit speed vector, the following equation holds.
∣α′(s)∣2=∣T(s)∣2=⟨T,T⟩=1
Differentiating both sides gives the following result by the derivative of dot product.
⟹⟹⟨T,T⟩′=⟨T′,T⟩=⟨α′′,T⟩= 0 0 0
Therefore, α′′ is perpendicular to T. Separating α′′, since n and T are perpendicular to each other, we obtain the following.
⟹⟹⟹⟨α′′,T⟩=⟨n1n+n2n⊥,T⟩=⟨n1n,T⟩+⟨n2n⊥,T⟩=⟨n2n⊥,T⟩= 0 0 0 0
Therefore, it can be known that n⊥ is a vector perpendicular to both n and T. Let’s define the vector S as follows.
S:=n×Tandα′′=n1n+sS
S is called the intrinsic normal of α.
Definition
The component n1 of n is called the normal curvature of the unit speed curve α, denoted as κn.
κn:=⟨α′′,n⟩
The component s of S is called the geodesic curvature of the unit speed curve α, denoted as κg.
κg:=⟨α′′,S⟩
Therefore, the following equation holds.
κ(s)N(s)=T′(s)=α′′(s)=κn(s)n(s)+κg(s)S(s)
Explanation
The normal curvature κn is used to measure how much the surface M is curved at R3. The geodesic curvature κg is used to measure how much the curve α is curved on the surface M. For example, a curve with the geodesic curvature κg equal to 0 implies a straight line on the surface, i.e., a geodesic.
Since n,S is a unit vector, the following equation holds according to the definition above.
κ2=κn2+κg2