EGU25-13668, updated on 15 Mar 2025
https://doi.org/10.5194/egusphere-egu25-13668
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Wednesday, 30 Apr, 09:45–09:55 (CEST)
 
Room 0.49/50
Forecasting the annual CO2 rise at Mauna Loa
Richard Betts1,2, Chris Jones1,3, Jeff Knight1, John Kennedy4, Ralph Keeling5, Yuming Jin6, James Pope1, and Caroline Sandford1
Richard Betts et al.
  • 1Met Office Hadley Centre, Exeter, UK (richard.betts@metoffice.gov.uk)
  • 2Global Systems Institute, University of Exeter, Exeter, UK
  • 3School of Geographical Sciences, University of Bristol, Bristol, UK
  • 4Independent researcher, Verdun, France
  • 5Scripps Institution of Oceanography, University of California San Diego, San Diego, USA
  • 6Earth Observing Laboratory, National Center for Atmospheric Research, Boulder, USA

For the last 9 years, the Met Office has issued forecasts of the annual increment in atmospheric carbon dioxide measured at Mauna Loa, accounting for both anthropogenic emissions and the effects of El Niño Southern Oscillation (ENSO) on natural carbon sinks and sources. The first forecast was produced when the 2015-2016 El Niño was emerging, and correctly predicted the largest annual CO2 increment on record at the time. In most years, the inclusion of ENSO provides a more skilful forecast than just considering emissions alone, except for 2022-2023 when La Niña conditions in late 2022 were followed by an early emergence of El Niño conditions in the second quarter of 2023. The impacts of interannual differences in emissions on the CO2 rise are usually smaller than those of ENSO variability, except in 2020 when the emergence of an unexpected large drop in global emissions due to societal responses to the COVID-19 pandemic required the forecast to be re-issued with a new estimate of the annual profile of emissions. Our forecast methodology also provides a simple means of tracking the changes in anthropogenic contributions to the annual atmospheric CO2 rise against policy-relevant scenarios. The Met Office forecast for 2023-2024 predicted a relatively large annual CO2 rise, but the observed rise was even larger, with exceptional wildfires in the Americas a likely contributor to the additional increase. Even without the effects of El Niño and other climatic influences on carbon sinks, the human-driven rise in CO2 in 2023-2024 would have been too fast to remain compatible with IPCC AR6 scenarios that limit global warming to 1.5°C with little or no overshoot. While the 2024-2025 rise is predicted to be smaller than 2023-2024, it will still be above these 1.5°C scenarios.

How to cite: Betts, R., Jones, C., Knight, J., Kennedy, J., Keeling, R., Jin, Y., Pope, J., and Sandford, C.: Forecasting the annual CO2 rise at Mauna Loa, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-13668, https://doi.org/10.5194/egusphere-egu25-13668, 2025.