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multiple time scale dynamics with two fast variables and one slow ...

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Figure 4.2: Illustration of transversal intersection of stable <strong>and</strong> unstable<br />

manifolds of the <strong>slow</strong> manifolds W s (S l,ǫ) (green) <strong>and</strong> W u (S r,ǫ)<br />

(magenta). The manifolds are truncated at the yellow section<br />

Σ <strong>and</strong> the trajectoryγ f w∪γbw started onΣat the transversal<br />

intersection point xsu is shown in red.<br />

had to be truncated almost immediately after they entered a neighborhood of<br />

a <strong>slow</strong> manifold. The final output of the algorithm after interpolation near the<br />

truncation points is shown in Figure 4.4.<br />

Now we consider the case of “<strong>slow</strong> waves” <strong>and</strong> work <strong>with</strong> smaller wave<br />

speeds s. Homoclinic orbits representing <strong>slow</strong> waves should be thought of as<br />

perturbations of singular limit orbits for the FitzHugh-Nagumo equation (3.6)<br />

<strong>with</strong> s=0. In this case the <strong>fast</strong> subsystem<br />

x ′<br />

1<br />

x ′<br />

2<br />

= x2<br />

= 1<br />

5 (− f (x1)+y− p) (4.9)<br />

is Hamiltonian. Singular homoclinic orbits exist in a single <strong>fast</strong> subsystem <strong>with</strong><br />

the y-coordinate of the equilibrium y= x∗ 1 . A direct application of Fenichel the-<br />

109

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