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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

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