2022/04/25 by F. Louchet, Louchet, Francois
Earth and Planetary Sciences · Environmental Science · Physics and Astronomy · #86A08 #Adaptation and Self-Organizing Systems (nlin.AO) #Advanced Thermodynamics and Statistical Mechanics #Atmospheric and Oceanic Physics (physics.ao-ph) #Earth Systems and Cosmic Evolution #Ecosystem dynamics and resilience #FOS: Physical sciences #Geophysics (physics.geo-ph)
paper · pdf · doi:10.48550/arxiv.2204.11619
openalex publication_date 2022/04/25 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/28
Current techniques for predicting climate change are mainly based on "massive" deterministic numerical modeling. However, the ocean-atmosphere system is a so-called "complex system", made up of a large number of interacting elements. We show that, in such systems, owing to the particularly large sensitivity to initial conditions, the approach of a possible tipping over a critical point cannot be evidenced "by construction" using numerical modeling, due to the divergence of computation time in the vicinity of the tipping point. On the other hand, the increasing amplitudes of observed climatic instabilities seem to be an obvious sign of the approach of such a tipping point, easily interpreted as a "critical softening", well known in the theory of dynamical systems, that would bring us irreversibly into a new and totally unexplored equilibrium state, except for a significantly higher temperature and in a much closer time than expected from numerical modeling extrapolations. Thus, maintaining climate warming around 1.5oC or 2oC by 2030 or 2050 appears fairly unrealistic unless worldwide drastic green house gases reduction measures are immediately taken and applied.