On the climate sensitivity and historical warming evolution in recent coupled model ensembles

• Published in: Atmospheric Chemistry and Physics
• Main Authors: C. M. Flynn, T. Mauritsen
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2020
• Subjects: Physics; QC1-999; Chemistry; QD1-999; Antarctic; Southern Ocean; Antarc*; Sea ice
• Online Access: https://doi.org/10.5194/acp-20-7829-2020; https://doaj.org/article/f8df15dddb74434a83137b7abd878971

The Earth's equilibrium climate sensitivity (ECS) to a doubling of atmospheric CO 2 , along with the transient climate response (TCR) and greenhouse gas emissions pathways, determines the amount of future warming. Coupled climate models have in the past been important tools to estimate and understand ECS. ECS estimated from Coupled Model Intercomparison Project Phase 5 (CMIP5) models lies between 2.0 and 4.7 K (mean of 3.2 K ), whereas in the latest CMIP6 the spread has increased to 1.8–5.5 K (mean of 3.7 K ), with 5 out of 25 models exceeding 5 K . It is thus pertinent to understand the causes underlying this shift. Here we compare the CMIP5 and CMIP6 model ensembles and find a systematic shift between CMIP eras to be unexplained as a process of random sampling from modeled forcing and feedback distributions. Instead, shortwave feedbacks shift towards more positive values, in particular over the Southern Ocean, driving the shift towards larger ECS values in many of the models. These results suggest that changes in model treatment of mixed-phase cloud processes and changes to Antarctic sea ice representation are likely causes of the shift towards larger ECS. Somewhat surprisingly, CMIP6 models exhibit less historical warming than CMIP5 models, despite an increase in TCR between CMIP eras (mean TCR increased from 1.7 to 1.9 K ). The evolution of the warming suggests, however, that several of the CMIP6 models apply too strong aerosol cooling, resulting in too weak mid-20th century warming compared to the instrumental record.