An interior layer is a narrow region of rapid variation lying inside a singular perturbation domain, separated from its boundary. Away from it, a slowly varying outer approximation is valid; a stretched inner variable resolves the transition near the layer location.
For example,has the exact solution . As , it approaches for fixed negative and for fixed positive . Neither constant outer branch describes the transition at zero. The inner coordinate gives and .
Thus the transition has width proportional to and central slope . Matching requires as and as . The same principle can describe thin internal fronts in differential equations; boundary layers instead lie near boundary data or a domain edge.
New to topics? Read the docs here!