Conformally Invariant Variational Problems. - SAM
Conformally Invariant Variational Problems. - SAM
Conformally Invariant Variational Problems. - SAM
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Note that Example 1 is contained as a particular case.<br />
Verifying that E g is indeed conformally invariant may be done<br />
analogously to the case of the Dirichlet energy, via introducing<br />
the complex variable z = x+iy. No new difficulty arises, and<br />
the details are left to the reader as an exercise.<br />
TheweakcriticalpointsofE g arethefunctionsu ∈ W 1,2 (D 2 ,R m )<br />
which satisfy<br />
∀ξ ∈ C ∞ 0 (D 2 ,R m )<br />
d<br />
dt E g(u+tξ) |t=0 = 0 .<br />
An elementary computation reveals that u is a weak critical<br />
point of E g if and only if the following Euler-Lagrange equation<br />
holds in the sense of distributions:<br />
m∑<br />
∀i = 1···m ∆u i + Γ i kl (u)∇uk ·∇u l = 0 . (VI.4)<br />
k,l=1<br />
Here, Γ i kl aretheChristoffelsymbolscorrespondingtothemetric<br />
g, explicitly given by<br />
Γ i kl(z) = 1 2<br />
m∑<br />
g is (∂ zl g km +∂ zk g lm −∂ zm g kl ) ,<br />
s=1<br />
(VI.5)<br />
where (g ij ) is the inverse matrix of (g ij ).<br />
Equation (VI.4) bears the name harmonic map equation 6<br />
with values in (R m ,g).<br />
Just as in the flat setting, if we further suppose that u is<br />
conformal, then (VI.4) is in fact equivalent to u(D 2 ) being a<br />
minimal surface in (R m ,g).<br />
6 One wayto interpret(VI.4) asthe two-dimensionalequivalent ofthe geodesicequation<br />
in normal parametrization,<br />
d 2 x i<br />
dt 2 + m ∑<br />
k,l=1<br />
Γ i dx k<br />
kl<br />
dt<br />
dx l<br />
dt = 0 .<br />
44