EGU2020-18190
https://doi.org/10.5194/egusphere-egu2020-18190
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Re-assessment of pre-industrial fires in CMIP6 models and the implications for radiative forcing

Ken Carslaw1, Cat Scott1, Masaru Yoshioka1, Douglas Hamilton2, Fiona O’Connor3, Gerd Folberth3, Jane Mulcahy3, Mohit Dalvi3, Yves Balkanski4, Ramiro Checa-Garcia4, Dirk Olivie5, Michael Schulz5, Martine Michou6, Pierre Nabat6, Lars Nieradzik7, Twan van Noije8, and Tommi Bergman8
Ken Carslaw et al.
  • 1University of Leeds, School of Earth and Environment, Institute for Climate and Atmospheric Science, Leeds, United Kingdom of Great Britain and Northern Ireland (k.s.carslaw@leeds.ac.uk)
  • 2Cornell University, USA
  • 3Met Office, UK
  • 4CNRS-LSCE, Paris, France)
  • 5MetNo, Oslo, Norway
  • 6Meteo France, France
  • 7Lund University, Lund, Swede
  • 8KNMI, Netherlands

Assessment of anthropogenic radiative forcing requires a robust understanding of the composition of the pre-industrial baseline atmosphere from which calculations are made

It is often assumed that fire activity and the associated aerosol emissions were lower in the pre-industrial period than in the present day. However, some lines of evidence suggest that fire activity may have halved since the pre-industrial period. 

Here we compare the simulated ratio of pre-industrial (c.1750CE and c.1850CE) to present-day black carbon surface concentrations in five ESMs (CNRM-ESM2-1, EC-Earth3, IPSL-CM6, NorESM1.2, UKESM1), using historical fire emissions from the Sixth Coupled Model Intercomparison Project (CMIP6), to the ratio in Northern Hemisphere ice-core records. 

We find that when forced with CMIP6 fire emissions all ESMs overestimate the present-day to pre-industrial black carbon ratio. This is consistent with previous studies and suggests that the contribution of fire to the composition of the pre-industrial atmosphere may be too low. If the contrast between the pre-industrial and present-day atmospheres in these models is too great, they are likely to overestimate the strength of the anthropogenic aerosol radiative forcing.  

We extend our analysis to include additional ESMs providing historical simulations for CMIP6, as included in the IPCC’s Sixth Assessment Report.

 

How to cite: Carslaw, K., Scott, C., Yoshioka, M., Hamilton, D., O’Connor, F., Folberth, G., Mulcahy, J., Dalvi, M., Balkanski, Y., Checa-Garcia, R., Olivie, D., Schulz, M., Michou, M., Nabat, P., Nieradzik, L., van Noije, T., and Bergman, T.: Re-assessment of pre-industrial fires in CMIP6 models and the implications for radiative forcing, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18190, https://doi.org/10.5194/egusphere-egu2020-18190, 2020

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