  Models such as those involving abrupt changes in the Earth's reflectivity due
to ice melt and formation often use nonlinear terms (e.g., hyperbolic tangent)
to model the transition between two states. For various reasons, these models
are often approximated by "simplified" discontinuous piecewise-linear systems
that are obtained by letting the length of the transition region limit to zero.
The smooth versions of these models may exhibit equilibrium solutions that are
destroyed as parameter changes transition the models from smooth to nonsmooth.
Using one such model as motivation, we explore the persistence of local
behavior around saddle equilibria under these transitions. We find sufficient
conditions under which smooth models with saddle equilibria can become
nonsmooth models with "zombie saddle" behavior, and analogues of stable and
unstable manifolds persist.
