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

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One can view this as a projection of the <strong>slow</strong> flow, which is constrained to the<br />

critical manifold in R 3 , onto the x1-axis. Observe that the <strong>slow</strong> flow is singu-<br />

lar at the fold points. Direct computation shows that the fixed point problem<br />

x1 = c(x1) has only a single real solution. This implies that the critical mani-<br />

fold intersects the diagonal y= x1 only in a single point x∗ 1 which is the unique<br />

equilibrium of the <strong>slow</strong> flow (3.8). Observe that q=(x ∗<br />

1 , 0, x∗<br />

1 ) is also the unique<br />

equilibrium of the full system (3.6) <strong>and</strong> depends on p. Increasing p moves the<br />

equilibrium from left to right on the critical manifold. The easiest practical way<br />

to determine the direction of the <strong>slow</strong> flow on C0 is to look at the sign of (x1− y).<br />

The situation is illustrated in Figure 3.2.<br />

y<br />

0.4<br />

0.3<br />

0.2<br />

0.1<br />

0<br />

−0.1<br />

−0.2<br />

−0.3<br />

eq. pt. q<br />

x 1,−<br />

Slow Flow in the plane x 2 =0<br />

y=x 1<br />

−0.4<br />

−0.4 −0.2 0 0.2 0.4<br />

x<br />

1<br />

0.6 0.8 1 1.2<br />

Figure 3.2: Sketch of the <strong>slow</strong> flow on the critical manifold C0<br />

3.3.1 The Slow Flow<br />

We are interested in the bifurcations of the <strong>slow</strong> flow depending on the parame-<br />

ter p. The bifurcations occur when x∗ 1 passes through the fold points. The values<br />

68<br />

x 1,+<br />

C 0

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