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

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whereµ∈R p are parameters. Usually it is assumed thatµis in some compact<br />

region in R p . The extended system <strong>with</strong> the trivial equation ˙µ = 0 does not<br />

satisfy the invariance assumptions but it is quite easy to modify the equation<br />

˙µ=0 near the boundary of the manifolds<br />

Ñ i :={(N i (µ),µ)} for i=1, 2<br />

to make the manifold Ñ 1 overflowing invariant <strong>and</strong> Ñ 2 inflowing invariant. The<br />

reason why the extended system (2.4) is important is the problem that for some<br />

fixedµ0 the manifolds N 1 <strong>and</strong> N 2 might be tangential. Varyingµcan poten-<br />

tially break this tangential intersection to make it transverse for Ñ 1 <strong>and</strong> Ñ 2 . This<br />

naturally leads to the main problem in applying Theorem 2.1.1 for a concrete<br />

example: the verification of the transversality hypothesis might be very diffi-<br />

cult. This will be our next step. Suppose we are in the situation described in<br />

Theorem 2.1.1. Since N 1 <strong>and</strong> N 2 intersect there exists a value y=y0 such that in<br />

the <strong>fast</strong> subsystem<br />

x ′ = f (x, y0, 0)<br />

there is a heteroclinic orbit between <strong>two</strong> equilibrium points, say p1 =<br />

(x1(y0), y0)∈W u (P 1 ) <strong>and</strong> p2= (x2(y0), y0)∈W s (P 2 ). Denote the heteroclinic orbit<br />

by (x0(t), y0)∈R m+n . The intersection between N 1 <strong>and</strong> N 2 at a point p=(x0(t), y0)<br />

for some t is transverse if <strong>and</strong> only if<br />

T pN 1 ⊕ T pN 2 = R m+n<br />

Direct dimension counting always gives:<br />

If we define<br />

dim(T pN 1 ⊕ T pN 2 )=dim(T pN 1 )+dim(T pN 2 )−dim(T pN 1 ∩ T pN 2 )<br />

d=dim(T pN 1 )+dim(T pN 2 )−m−n (2.5)<br />

20

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