Synchronization phenomena observed in glacial-interglacial cycles simulated in an Earth system model of intermediate complexity

Abstract

Abstract. The glacial-interglacial cycles of the Quaternary exhibit 41-kyr periodicity before the Mid-Pleistocene Transition (MPT) around 1.2–0.8 Myr ago and ~100-kyr periodicity after that. From the viewpoint of dynamical systems, proposed mechanisms generating these periodicities are broadly divided into two types: (i) nonlinear forced responses of a mono- or multi-stable climate system to the astronomical forcing, or (ii) synchronization of internal self-sustained oscillations to the astronomical forcing. In this study, we investigate the dynamics of glacial cycles simulated by the Earth system model of intermediate complexity CLIMBER-2 with a fully interactive carbon cycle, which reproduces the MPT under gradual changes in volcanic CO2 degassing and regolith cover. We report that, in this model, the dominant frequency of glacial cycles is set in line with the principle of synchronization. It is found that the model exhibits self-sustained oscillations in the absence of astronomical forcing. Before the MPT, glacial cycles synchronize to the 41-kyr obliquity cycles because the self-sustained oscillations have periodicity relatively close to 41 kyr. After the MPT the time scale of internal oscillations becomes too long to follow every 41-kyr obliquity cycle, and the oscillations synchronize to the 100-kyr eccentricity cycles that modulate the amplitude of climatic precession. The latter synchronization occurs with the help of the 41-kyr obliquity forcing through a mechanism that we term vibration-enhanced synchronization. While we interpret the dominant periodicities of glacial cycles as the result of synchronization of internal self-sustained oscillations with the astronomical forcing, the Quaternary glacial cycles show facets of both synchronization and forced response.