A tighter constraint on Earth-system sensitivity from long-term temperature and carbon-cycle observations.

ABSTRACT: The long-term temperature response to a given change in CO₂ forcing, or Earth-system sensitivity (ESS), is a key parameter quantifying our understanding about the relationship between changes in Earth's radiative forcing and the resulting long-term Earth-system response. Current ESS estimates are subject to sizable uncertainties. Long-term carbon cycle models can provide a useful avenue to constrain ESS, but previous efforts either use rather informal statistical approaches or focus on discrete paleoevents. Here, we improve on previous ESS estimates by using a Bayesian approach to fuse deep-time CO₂ and temperature data over the last 420 Myrs with a long-term carbon cycle model. Our median ESS estimate of 3.4 °C (2.6-4.7 °C; 5-95% range) shows a narrower range than pr

SUBMITTER: Wong TE 

PROVIDER: S-EPMC8154887 | biostudies-literature | 2021 May

REPOSITORIES: biostudies-literature