Figure 7.4. The vector qr
2
(sr
1
) is the vector ps ( pq) parallel transported to q (s). In
general, r
1
= r
2
and the torsion measures the difference r
2
r
1
.
Thus, the torsion tensor measures the failure of the closure of the parallelogram
made up of the small displacement vectors and their parallel transports.
Example 7.2. Suppose we are navigating on the surface of the Earth. We define a
vector to be parallel transported if the angle between the vector and the latitude is
kept fixed during the navigation. [Remarks: This definition of parallel transport
is not the usual one. For example, the geodesic is not a great circle but a straight
line on Mercator’s projection. See example 7.5.] Suppose we navigate along
a small quadrilateral pqrs made up of latitudes and longitudes (figure 7.5(a)).
We parallel transport a vector at p along pqr and psr, separately. According
to our definition of parallel transport, two vectors at r should agree, hence the
curvature tensor vanishes. To find the torsion, we parametrize the points p, q, r
and s as in figure 7.5(b). We find the torsion by evaluating the difference between
pr
1
and pr
2
as in (7.45). If we parallel transport the vector pq along ps,we
obtain a vector sr
1
, whose length is R sin θdφ. However, a parallel transport
of the vector ps along pq yields a vector qr
2
= qr.Sincesr has a length
R sin(θ − dθ)dφ R sin θ dφ − R cos θ dθ dφ,wefindthatr
1
r
2
has a length
R cos θ dθ dφ.Sincer
1
r
2
is parallel to −∂/∂φ, the connection has a torsion
T
φ
θφ
, see (7.45). From g
φφ
= R
2
sin
2
θ,wefindthatr
1
r
2
has components
(0, −cot θ dθ dφ). Since the φ-component of r
1
r
2
is equal to T
φ
θφ
dθdφ,we
obtain T
φ
θφ
=−cot θ.
Note that the basis {∂/∂θ, ∂/∂φ} is not well defined at the poles. It is known
that the sphere S
2
does not admit two vector fields which are linearly independent
everywhere on S
2
. Any vector field on S
2
must vanish somewhere on S
2
and