Estimated effect of the permafrost carbon feedback on the zero emissions commitment to climate change

• Published in: Biogeosciences Vol. 18; no. 17; pp. 4937 - 4952
• Main Author: MacDougall, Andrew H
• Format: Journal Article
• Language: English
• Published: Katlenburg-Lindau Copernicus GmbH 10.09.2021; Copernicus Publications
• Subjects: Air pollution; Analysis; Anthropogenic factors; Atmosphere; Atmospheric models; Benchmarks; Carbon; Carbon cycle; Carbon dioxide; Carbon dioxide emissions; Climate change; Design of experiments; Emissions; Environmental aspects; Experiments; Feedback; General circulation models; Global temperature changes; Global temperatures; Greenhouse effect; Greenhouse gases; Human influences; Intercomparison; Permafrost
• ISSN: 1726-4189; 1726-4170; 1726-4189
• DOI: 10.5194/bg-18-4937-2021

Zero Emissions Commitment (ZEC), the expected change in global temperature following the cessation of anthropogenic greenhouse gas emissions, has recently been assessed by the Zero Emissions Commitment Model Intercomparison Project (ZECMIP). ZECMIP concluded that the component of ZEC from CO2 emissions will likely be close to zero in the decades following the cessation of emissions. However, of the 18 Earth system models that participated in ZECMIP only 2 included a representation of the permafrost carbon feedback to climate change. To better assess the potential impact of permafrost carbon decay on ZEC, a series of perturbed parameter experiments are here conducted with an Earth system model of intermediate complexity. The experiment suggests that the permafrost carbon cycle feedback will directly add 0.06 [0.02 to 0.14] ∘C to the benchmark the ZEC value assesses 50 years after 1000 Pg C of CO2 has been emitted to the atmosphere. An additional 0.04 [0 to 0.06] ∘C is likely to been added relative to the benchmark ZEC value from the thaw-lag effect unaccounted for in the ZECMIP experiment design. Overall I assess that the permafrost carbon feedback is unlikely to change the assessment that ZEC is close to zero on decadal timescales; however, the feedback is expected to become more important over the coming centuries.