“…Tipping point transitions between different dynamical states where the pre-transition state dynamics is constrained to a smaller set of the system state space, or to a different region of the system state space, than the post-transition orbits are observed in a wide array of natural systems [1,2]. Such transitions are commonly found in various terrestrial climate models [35][36][37], ecosystem models [38][39][40], epidemics [41,42], and physical and engineering applications (e.g., intermittency [43] and crisis [44] transitions in plasmas [45][46][47][48], lasers [49,50], electrical and power systems [51][52][53][54], thermoacoustic systems [55][56][57], hydrodynamical systems [58,59], and electrochemical systems [60]). Thus, developing methods to predict the climate evolution of non-stationary dynamical systems which may tip into a state characterized by motion of the system that may visit previously unex-plored, or only sparsely explored, regions of its state space is a problem of very general importance.…”