Put
On the specified branch, is positive for and negative for . The saddle points of the phase are therefore , with
and
Applying the method of steepest descent at the two simple saddles gives
This formula is valid while the pole and positive saddle remain separated by much more than their saddle width.
The pole crosses the positive saddle when
Because the original contour passes above the pole, deformation onto the steepest-descent contour contributes
when , or . It contributes no residue when , or . Hence, away from the transition,
The residue is exponentially oscillatory and , whereas each ordinary saddle contribution is .
At the pole and saddle coalesce, so the displayed saddle formula is singular and must not be used. Passing above the coincident point gives one half of the switched residue at leading order:
If , a uniform saddle-point approximation with a nearby pole replaces the discontinuous switch by a complementary-error-function multiplier.
As , , , and the pole lies in the no-residue regime. Each saddle coefficient is , so the leading approximation tends to
For , the stationary-point equation would require
so the two saddles leave the real axis. The contour can be deformed through the appropriate complex saddle or saddles, and their contributions become exponentially small or large according to the sign of the real part of . The real-axis oscillatory saddle contributions present for therefore disappear across the turning point . The admissible deformation and the pole's residue must still respect the prescribed branch cuts and the instruction that the contour pass above .
At , the two saddles have receded to infinity and the ordinary quadratic saddle approximation is nonuniform. One should first use an asymptotic expansion of the phase and amplitude for large :
so
The phase varies on the scale rather than in an neighbourhood of a finite saddle. Rescaling in the positive and negative tails, retaining the corresponding large- amplitude, and matching these tail integrals to the finite part of the deformed contour produces the leading approximation. This is an endpoint at infinity problem; a uniform calculation may equivalently begin from the saddle representation and take the coalescing-at-infinity limit.
Away from , the outer solution is obtained by setting :
It already satisfies both endpoint conditions, but its derivative jumps at . Introduce the inner variable
and write . The inner equation is
Matching to the outer cusp requires as . The even solution is
Subtracting the common part gives the composite asymptotic expansion
Its endpoint errors are exponentially small.
At , the first and second derivatives from the two sides agree, but the third derivatives have opposite signs. The composite expansion is therefore but not .
For , the reduced first-order outer equation is
The condition at selects
Indeed as , while as . The boundary condition at must therefore be supplied by a boundary layer.
Set
Since in this layer, the convection term is lower order. The leading inner equation and matching conditions are
Thus
The leading uniformly valid expression is
Near diffusion regularizes the divergent derivative of the outer approximation on the thinner scale , but the leading value there remains the already matched constant .
For , the formal outer family is
Every nonzero member diverges as , so bounded matching selects the outer solution . Boundary layers are now required at both endpoints.
The layer still has width and leading profile
Near , diffusion and the logarithmically vanishing convection balance on the thinner scale
At leading order the reaction term is smaller there. Using the supplied first integral with , define
The left layer that equals at the endpoint and matches zero is
Consequently a leading composite description is
Its sketch has value at each endpoint, drops sharply to an almost-zero outer plateau just to the right of , and rises through an layer just before .
The linear mode has frequency squared , so . To resolve the small frequency near threshold, write
The leading equation
and the initial data give
At , the equation for has a forcing whose component is
The Fredholm solvability condition removes this secular term and yields the slow amplitude equation
It has the conserved energy
The potential has maxima at
A periodic orbit launched from , exists only when that turning point lies inside the two maxima, namely
At equality the orbit is the separatrix; below it, the assumed real periodic oscillation is lost. Therefore

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