Articles | Volume 25, issue 20
https://doi.org/10.5194/acp-25-13393-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-25-13393-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
How well are aerosol–cloud interactions represented in climate models? – Part 2: Isolating the aerosol impact on clouds following the 2014–2015 Holuhraun eruption
George Jordan
CORRESPONDING AUTHOR
Met Office Hadley Centre, Exeter, UK
Florent Malavelle
Met Office, Exeter, UK
Jim Haywood
Department of Mathematics and Statistics, University of Exeter, Exeter, UK
Ying Chen
School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham, UK
Ben Johnson
Met Office Hadley Centre, Exeter, UK
Daniel Partridge
Department of Mathematics and Statistics, University of Exeter, Exeter, UK
Amy Peace
Met Office Hadley Centre, Exeter, UK
Eliza Duncan
Department of Mathematics and Statistics, University of Exeter, Exeter, UK
Duncan Watson-Parris
Scripps Institution of Oceanography and Halıcıoğlu Data Science Institute, University of California San Diego, La Jolla, California, USA
David Neubauer
Institute for Climate and Atmospheric Science, ETH Zurich, Zurich, Switzerland
Anton Laakso
Atmospheric Research Centre of Eastern Finland, Finnish Meteorological Institute, Kuopio, Finland
Martine Michou
CNRM, Université de Toulouse, Météo-France, CNRS, Toulouse, France
Pierre Nabat
CNRM, Université de Toulouse, Météo-France, CNRS, Toulouse, France
Data sets
Volcanic Aerosol-Cloud Interaction (VolcACI) Experiment Part 2: Code and Dataset George Jordan https://doi.org/10.5281/zenodo.14891974
Model code and software
Volcanic Aerosol-Cloud Interaction (VolcACI) Experiment Part 2: Code and Dataset George Jordan https://doi.org/10.5281/zenodo.14891974
Short summary
The 2014–15 Holuhraun eruption created a vast aerosol plume that acted as a natural experiment to assess how well climate models capture changes in cloud properties due to increased aerosol. We find that climate models represent the observed shift to smaller, more numerous cloud droplets well. However, climate models diverge in their aerosol-induced changes to large-scale cloud properties, particularly cloud liquid water content. Our study shows that Holuhraun had a cooling effect on the Earth.
The 2014–15 Holuhraun eruption created a vast aerosol plume that acted as a natural experiment...
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