2.4 The Sigma Model 155
surfaces with singularities. Those singularities were then removed by compactifying
the resulting surfaces by two points, one for each side of the closed geodesic. This
now connects well with the behavior of the functional S, because its critical points,
the solutions of (2.4.20), (2.4.21), are harmonic functions. And bounded harmonic
functions can be smoothly extended across isolated singularities. That means that if
we consider a sequence of degenerating Riemann surfaces
n
and controlled har-
monic functions u
n
(with some suitable norm bounded independently of n) on them,
we can pass to the limit (of some subsequence) that then defines a harmonic func-
tion u on the Riemann surface obtained by the described compactification of the
limit of the Riemann surfaces. That harmonic function is then smooth on all of ,
and in particular, it does not feel the presence or the position of the puncture, that
is, of the points added for the compactification. In particular, the functional S then
naturally extends not only to the Deligne–Mumford compactification, but also to
the Baily–Satake compactification
M
p
(see Sect. 1.4.3 of the moduli space M
p
).
For more details, see [62].
There is one point here that will become important below in Sect. 2.5. While the
equation of motion, our Euler–Lagrange equation (2.4.20), is conformally invariant
in the sense that the conformal factor
1
λ
2
plays no role, the corresponding differential
operator, the Laplace–Beltrami operator
4
λ
2
∂
2
∂z∂¯z
, is not conformally invariant itself.
From (2.4.20), we see directly that the energy–momentum tensor as given by
(2.4.19) is holomorphic at a solution of (2.4.20):
∂T
zz
∂ ¯z
=0. (2.4.22)
In conclusion, the energy–momentum tensor yields a holomorphic quadratic differ-
ential T
zz
dz
2
=(
∂φ
∂z
)
2
dz
2
on our Riemann surface .
There is a deeper reason why T is holomorphic. As we shall now explain, S
is invariant under diffeomorphisms, and by Noether’s theorem, this yields a con-
served current, that is, a divergence-free quantity. That latter equation then turns
out to be equivalent to (2.4.22). The reason is simply that (2.4.6), or equivalently
(2.4.16), is invariant under coordinate changes. In mathematical terms, as explained
in Sect. 1.1.1, this means that we compose the field φ with a diffeomorphism h of
our surface and simultaneously pull the metric γ in (2.4.6) or the area form dx ∧dy
in (2.4.16) back by that diffeomorphism. In other words, we have
S(φ ◦h, h
γ)=S(φ,γ). (2.4.23)
In the formalism of physics, we move the points in the domain by an infinitesimal
diffeomorphism, that is, a vector field, and consider the variation
x
α
+δx
α
or, in complex coordinates, z +δz. (2.4.24)
By (2.3.28), the conserved current is
j
z
=−
∂φ
∂ ¯z
2
δ¯z, j
¯z
=−
∂φ
∂z
2
δz, (2.4.25)