For a holomorphic phase , a saddle point is a critical point with . At a simple saddle, , and the quadratic Taylor term determines the local descent directions.
A saddle-point approximation expands an exponent around a stationary configuration and integrates its leading Gaussian fluctuations. A large parameter multiplying the exponent suppresses higher fluctuations.
When two quadratic saddles coalesce and the first nonzero phase derivative is cubic, the contributing neighborhood has width rather than . The leading contour integral reduces to a Gamma-function or Airy-function constant.
When a simple pole approaches a saddle within its Gaussian width, separate residue and saddle approximations cease to be uniform. A local change of variable reduces the transition to a complementary error function whose multiplier smoothly switches the pole residue across the deformed contour.
Let , , and let be analytic. Assume a contributing contour can be deformed onto two descent arms of the method of steepest descent with one clockwise semicircular avoidance of the pole at , and that its other portions are negligible. For the integrand , a local coordinate with gives
The odd pole term has zero Cauchy principal value on the real arms and integral on the clockwise indentation. The constant regular term integrates to times its coefficient, proving the expansion and generic correction order. A degenerate saddle has a different local width and possibly a different indentation angle; analyticity and a single critical point alone do not imply this result. If , retain the additive expansion rather than writing asymptotic equivalence to zero.
For a simple saddle point, a nearby pole coalesces with its contributing region when their separation is of order the inverse square root of the large parameter. A local quadratic phase coordinate changes the singular part to a Gaussian pole integral. Adding any residue crossed by the contour deformation gives a Faddeeva function rather than two separately singular approximations. The regular part of the transformed amplitude remains smaller by the ordinary saddle width.

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A saddle point is a point on the surface of a graph where the slope (or derivative) is zero in multiple dimensions, but is not a local extremum (i.e., not a local maximum or minimum). It occurs in both single-variable and multivariable calculus, although the characteristics can differ slightly based on the context.