Parabolic implosion - from discontinuity to renormalization
Parabolic implosion - from discontinuity to renormalization
Parabolic implosion - from discontinuity to renormalization
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Return map and Renormalization<br />
f<br />
g<br />
Rf<br />
Renormalization<br />
f Rf = first return map f (after rescaling)<br />
If f is infinitely renormalizable, ...<br />
f 0 = f f 1 = Rf 0 f 2 = Rf 1<br />
h 0<br />
g 0 g 1<br />
h 1 h 2<br />
˜g 0 ˜g 1<br />
f Rf<br />
as a “meta dynamical system”<br />
on a space of dynamical systems<br />
Often one expects a hyperbolic<br />
f ↔ (α, f<br />
dynamics 0 ) Rf(z) = e −2πi 1 α R α f 0 (z) R : (α,<br />
f 0 α α ↦→ − 1 α mod Z R 0 R<br />
R 0 contracting? R hyperbolic? (R α contrac<br />
f = P ◦ ϕ −1<br />
˜f 0 = ˜f ˜f1 = R ˜f 0<br />
˜f2 = R ˜f 1<br />
rigidity: weak conj. upgraded <strong>to</strong> nicer one<br />
f = Q ◦ ϕ −1<br />
0 ∞ (−∞, −1]