EGU24-18277, updated on 11 Mar 2024
https://doi.org/10.5194/egusphere-egu24-18277
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Investigating the role of air mass history of Arctic black carbon in GCMs

Roxana S. Cremer1,2, Paul Kim3, Sara M. Blichner1, Emanuele Tovazzi3, Ben Johnson4, Zak Kipling5, Thomas Kühn6, Duncan Watson-Parris7,8, David Neubauer9, Phillip Stier7, Alistair Sellar4, Eemeli Holopainen6, Ilona Riipinen1, and Daniel G. Partridge3,4
Roxana S. Cremer et al.
  • 1Department of Environmental Science, Stockholm University, Stockholm, Sweden (cremer@tropos.de)
  • 2Leibniz Institute for Tropospheric Research, Leipzig, Germany
  • 3Department of Mathematics and Statistics, Faculty of Environment, Science and Economy, University of Exeter, Exeter, UK
  • 4Met Office, Exeter, UK
  • 5ECMWF, Reading, RG2 9AX, UK
  • 6Finnish Meteorological Institute, Climate Research Program, Helsinki, Finland
  • 7Atmospheric, Oceanic and Planetary Physics, Department of Physics, University of Oxford, Oxford, UK
  • 8Scripps Institution of Oceanography and Halıcıoğlu Data Science Institute, University of California San Diego, La Jolla, CA, USA
  • 9Institute of Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland

Black Carbon (BC) aerosols are known to be important for the Earth’s climate, yet their exact role to the changing of the Earth’s climate and Arctic amplification remains unclear. An accurate description of the BC life cycle in general circulation models (GCMs) can help reduce the uncertainties due to BC aerosols and specify BC's role in the Arctic.

In this study, several GCMs (ECHAM6.3-HAM2.3, ECHAM6.3-HAM2.3-P3, ECHAM6.3-HAM2.3-SALSA2 and UKESM1.0) are compared in terms of their representation of BC mass in the Arctic within the AeroCom project GCM Trajectory. A novel Lagrangian framework is employed to examine the history of air masses reaching the observational station Zeppelin, Svalbard. Therfore the removal processes were analysed along the trajectory and the GCMs compared with each other. The analysis emphasises the impact of remote emissions on local BC concentrations in the Arctic, indicating a longer BC lifetime compared to the global average. This underlines the importance of dry and wet scavenging parametrisations in the GCMs.

 

 

 

How to cite: Cremer, R. S., Kim, P., Blichner, S. M., Tovazzi, E., Johnson, B., Kipling, Z., Kühn, T., Watson-Parris, D., Neubauer, D., Stier, P., Sellar, A., Holopainen, E., Riipinen, I., and Partridge, D. G.: Investigating the role of air mass history of Arctic black carbon in GCMs, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-18277, https://doi.org/10.5194/egusphere-egu24-18277, 2024.