Articles | Volume 18, issue 3
https://doi.org/10.5194/acp-18-2307-2018
© Author(s) 2018. 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-18-2307-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
15 Feb 2018
Research article |
| 15 Feb 2018
| 15 Feb 2018
Multi-model comparison of the volcanic sulfate deposition from the 1815 eruption of Mt. Tambora
Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds, UK
Anja Schmidt
Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds, UK
now at: Department of Chemistry, University of Cambridge, UK and Department of Geography, University of Cambridge, UK
Matthew Toohey
GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany
Max Planck Institute for Meteorology, Hamburg, Germany
Ken S. Carslaw
Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds, UK
Graham W. Mann
Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds, UK
National Centre for Atmospheric Science, University of Leeds, UK
Michael Sigl
Laboratory of Environmental Chemistry, Paul Scherrer Institut, 5232 Villigen, Switzerland
Myriam Khodri
Laboratoire d'Océanographie et du Climat: Expérimentations et Approches Numériques, Sorbonne Universités,
UPMC, IPSL, UMR CNRS/IRD/MNHN, 75005 Paris, France
Claudia Timmreck
Max Planck Institute for Meteorology, Hamburg, Germany
Davide Zanchettin
Department of Environmental Sciences, Informatics and Statistics, University Ca' Foscari of Venice, Mestre, Italy
William T. Ball
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
PMOD/WRC, Davos, Switzerland
Slimane Bekki
LATMOS-IPSL, UPMC/Paris-Sorbonne, UVSQ/Paris Saclay, CNRS/INSU, Paris, France
James S. A. Brooke
School of Chemistry, University of Leeds, UK
Sandip Dhomse
Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds, UK
Colin Johnson
Met Office Hadley Centre, Exeter, UK
Jean-Francois Lamarque
Atmospheric Chemistry Observations and Modeling Laboratory, National Center for Atmospheric Research, Boulder, CO, USA
Allegra N. LeGrande
NASA Goddard Institute for Space Studies, New York, NY, USA
Center for Climate Systems Research, Columbia University, New York, NY, USA
Michael J. Mills
Atmospheric Chemistry Observations and Modeling Laboratory, National Center for Atmospheric Research, Boulder, CO, USA
Ulrike Niemeier
Max Planck Institute for Meteorology, Hamburg, Germany
James O. Pope
British Antarctic Survey, Cambridge, UK
Virginie Poulain
Laboratoire d'Océanographie et du Climat: Expérimentations et Approches Numériques, Sorbonne Universités,
UPMC, IPSL, UMR CNRS/IRD/MNHN, 75005 Paris, France
Alan Robock
Department of Environmental Sciences, Rutgers University, New Brunswick, NJ, USA
Eugene Rozanov
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
PMOD/WRC, Davos, Switzerland
Andrea Stenke
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
Timofei Sukhodolov
PMOD/WRC, Davos, Switzerland
Simone Tilmes
Atmospheric Chemistry Observations and Modeling Laboratory, National Center for Atmospheric Research, Boulder, CO, USA
Kostas Tsigaridis
Center for Climate Systems Research, Columbia University, New York, NY, USA
NASA Goddard Institute for Space Studies, New York, NY, USA
Fiona Tummon
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
now at: Faculty of Biosciences, Fisheries, and Economics, UiT The Arctic University of Norway, Tromsø, Norway
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Latest update: 06 Dec 2025
Short summary
We use four global aerosol models to compare the simulated sulfate deposition from the 1815 Mt. Tambora eruption to ice core records. Inter-model volcanic sulfate deposition differs considerably. Volcanic sulfate deposited on polar ice sheets is used to estimate the atmospheric sulfate burden and subsequently radiative forcing of historic eruptions. Our results suggest that deriving such relationships from model simulations may be associated with greater uncertainties than previously thought.
We use four global aerosol models to compare the simulated sulfate deposition from the 1815 Mt....
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