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Figure 9.25.
Defining geodesic curvature.
n(g(s))
g ¢¢(s)
T(s)
p = g(s)
S
n S (s)
T p (S)
parameterized by arc-length . See Figure 9.25. As a curve in R 3 we know that g(s) can
be described in terms of its Frenet frame (T(s),N(s),B(s)), its curvature k(s), and
its torsion t(s). Define a unit vector n S (s) so that (T(s),n S (s), n (g(s))) is a frame that
defines the standard orientation in R 3 . The vector n S (s) will be tangent to S at g(s)
and is defined by the equation
() =
(
()
) ¥
()
ns
n
g
s
Ts
.
(9.63)
S
Recall that the second derivative g≤(s) is closely related to the curvature of the space
curve g(s). Since the tangent space to R 3 at g(s) is the direct sum of the tangent space
of S at g(s) and the one-dimensional orthogonal subspace with basis n (g(s)), we can
write any vector, in particular g≤(s), in the form
g≤ () =
() +
()
sWsVs
(9.64)
where V(s) lies in the tangent space of S at g(s) and W(s) is a multiple of n (g(s)). The
vector V(s) can also be described more explicitly. Since T(s) is tangent to S , W(s) • T(s)
= 0. But g(s) is arc-length parameterization, so that g≤(s) • T(s) = 0. It follows from this
and equation (9.64) that V(s) • T(s) = 0, that is, V(s) is orthogonal to T(s). In other
words, the vector V(s) is orthogonal to both n (g(s)) and T(s). Equation (9.63) now
implies that V(s) is a multiple of n S (s). Putting all these facts together implies that
there are unique functions k n (s) and k g (s), so that
() =
() () =
()
(
()
) +
()
()
g
s
k
s Ns
k
s
ns
g
k
s ns
.
(9.65)
n
g
S
The value k n (s) =g≤(s) • n (g(s)) is of course just the normal curvature of the curve g(s)
at s.
Definition. The value k g (s) is called the geodesic curvature of the arc-length para-
meterized curve g(s) at s.
The geodesic curvature function was introduced by F. Minding in 1830. Because
we have orthonormal vectors, the following relation holds between k, k n , and k g :
2
2
2
kkk
= ng .
(9.66)
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