Articles | Volume 11, issue 7
https://doi.org/10.5194/gmd-11-2633-2018
© 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/gmd-11-2633-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Model evaluation paper
| 
06 Jul 2018
Model evaluation paper |
| 06 Jul 2018
| 06 Jul 2018
Stratospheric aerosol evolution after Pinatubo simulated with a coupled size-resolved aerosol–chemistry–climate model, SOCOL-AERv1.0
Timofei Sukhodolov
CORRESPONDING AUTHOR
Physikalisch-Meteorologisches Observatorium Davos and World Radiation Center, Davos, Switzerland
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
Jian-Xiong Sheng
School of Engineering and Applied Sciences, Harvard University, Cambridge, MA, USA
Aryeh Feinberg
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
Bei-Ping Luo
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
Thomas Peter
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
Laura Revell
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
Bodeker Scientific, Christchurch, New Zealand
Andrea Stenke
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
Debra K. Weisenstein
School of Engineering and Applied Sciences, Harvard University, Cambridge, MA, USA
Eugene Rozanov
Physikalisch-Meteorologisches Observatorium Davos and World Radiation Center, Davos, Switzerland
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
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22 citations as recorded by crossref.
- Importance of microphysical settings for climate forcing by stratospheric SO2 injections as modeled by SOCOL-AERv2 S. Vattioni et al. 10.5194/gmd-17-4181-2024
- Temperature and Ozone Response to Different Forcing in the Lower Troposphere and Stratosphere M. Usacheva et al. 10.3390/atmos15111289
- Evaluating the simulated radiative forcings, aerosol properties, and stratospheric warmings from the 1963 Mt Agung, 1982 El Chichón, and 1991 Mt Pinatubo volcanic aerosol clouds S. Dhomse et al. 10.5194/acp-20-13627-2020
- Atmosphere–ocean–aerosol–chemistry–climate model SOCOLv4.0: description and evaluation T. Sukhodolov et al. 10.5194/gmd-14-5525-2021
- Modeling the Sulfate Aerosol Evolution After Recent Moderate Volcanic Activity, 2008–2012 C. Brodowsky et al. 10.1029/2021JD035472
- Interactive stratospheric aerosol models' response to different amounts and altitudes of SO2 injection during the 1991 Pinatubo eruption I. Quaglia et al. 10.5194/acp-23-921-2023
- Extreme Solar Events: Setting up a Paradigm I. Usoskin et al. 10.1007/s11214-023-01018-1
- CREST: a Climate Data Record of Stratospheric Aerosols V. Sofieva et al. 10.5194/essd-16-5227-2024
- Possible impact of the 43 BCE Okmok volcanic eruption in Alaska on the climate of China as revealed in historical documents P. Wang et al. 10.5194/cp-20-1513-2024
- Sensitivity of stratospheric ozone to the latitude, season, and halogen content of a contemporary explosive volcanic eruption F. Østerstrøm et al. 10.1038/s41598-023-32574-9
- Model physics and chemistry causing intermodel disagreement within the VolMIP-Tambora Interactive Stratospheric Aerosol ensemble M. Clyne et al. 10.5194/acp-21-3317-2021
- Validating a microphysical prognostic stratospheric aerosol implementation in E3SMv2 using observations after the Mount Pinatubo eruption H. Brown et al. 10.5194/gmd-17-5087-2024
- Evaluating the Response of Global Column Resistance to a Large Volcanic Eruption by an Aerosol-Coupled Chemistry Climate Model Y. Xie et al. 10.3389/feart.2021.673808
- Dependency of the impacts of geoengineering on the stratospheric sulfur injection strategy – Part 1: Intercomparison of modal and sectional aerosol modules A. Laakso et al. 10.5194/acp-22-93-2022
- A fully coupled solid-particle microphysics scheme for stratospheric aerosol injections within the aerosol–chemistry–climate model SOCOL-AERv2 S. Vattioni et al. 10.5194/gmd-17-7767-2024
- Exploring accumulation-mode H<sub>2</sub>SO<sub>4</sub> versus SO<sub>2</sub> stratospheric sulfate geoengineering in a sectional aerosol–chemistry–climate model S. Vattioni et al. 10.5194/acp-19-4877-2019
- Stratospheric aerosol size reduction after volcanic eruptions F. Wrana et al. 10.5194/acp-23-9725-2023
- Impact of the Hunga Tonga volcanic eruption on stratospheric composition D. Wilmouth et al. 10.1073/pnas.2301994120
- Interactive Stratospheric Aerosol Microphysics‐Chemistry Simulations of the 1991 Pinatubo Volcanic Aerosols With Newly Coupled Sectional Aerosol and Stratosphere‐Troposphere Chemistry Modules in the NASA GEOS Chemistry‐Climate Model (CCM) P. Case et al. 10.1029/2022MS003147
- Unknown Eruption Source Parameters Cause Large Uncertainty in Historical Volcanic Radiative Forcing Reconstructions L. Marshall et al. 10.1029/2020JD033578
- Improved tropospheric and stratospheric sulfur cycle in the aerosol–chemistry–climate model SOCOL-AERv2 A. Feinberg et al. 10.5194/gmd-12-3863-2019
- The effect of ash, water vapor, and heterogeneous chemistry on the evolution of a Pinatubo-size volcanic cloud M. Abdelkader et al. 10.5194/acp-23-471-2023
1 citations as recorded by crossref.
Latest update: 23 Nov 2024
Short summary
The Pinatubo eruption in 1991 is the strongest directly observed volcanic event. In a series of experiments, we simulate its influence on the stratospheric aerosol layer using a state-of-the-art aerosol–chemistry–climate model, SOCOL-AERv1.0, and compare our results to observations. We show that SOCOL-AER reproduces the most important atmospheric effects and can therefore be used to study the climate effects of future volcanic eruptions and geoengineering by artificial sulfate aerosol.
The Pinatubo eruption in 1991 is the strongest directly observed volcanic event. In a series of...
