In mathematics, an ancient solution to a differential equation is a solution that can be extrapolated backwards to all past times, without singularities. That is, it is a solution "that is defined on a time interval of the form ."[1]
The term was introduced by Richard Hamilton in his work on the Ricci flow.[2] It has since been applied to other geometric flows[3] [4] [5] [6] as well as to other systems such as the Navier–Stokes equations[7] [8] and heat equation.[9]