Articles | Volume 17, issue 24
https://doi.org/10.5194/acp-17-14871-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-17-14871-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
14 Dec 2017
Research article |
| 14 Dec 2017
Changing transport processes in the stratosphere by radiative heating of sulfate aerosols
Ulrike Niemeier
CORRESPONDING AUTHOR
Max Planck Institute for Meteorology, Bundesstr. 53, 20146 Hamburg, Germany
Hauke Schmidt
Max Planck Institute for Meteorology, Bundesstr. 53, 20146 Hamburg, Germany
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- Sensitivity of the radiative forcing by stratospheric sulfur geoengineering to the amount and strategy of the SO<sub>2</sub>injection studied with the LMDZ-S3A model C. Kleinschmitt et al. 10.5194/acp-18-2769-2018
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- Stratospheric ozone response to sulfate aerosol and solar dimming climate interventions based on the G6 Geoengineering Model Intercomparison Project (GeoMIP) simulations S. Tilmes et al. 10.5194/acp-22-4557-2022
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- The impact of recent changes in Asian anthropogenic emissions of SO<sub>2</sub> on sulfate loading in the upper troposphere and lower stratosphere and the associated radiative changes S. Fadnavis et al. 10.5194/acp-19-9989-2019
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- Exploring How Eruption Source Parameters Affect Volcanic Radiative Forcing Using Statistical Emulation L. Marshall et al. 10.1029/2018JD028675
- Revisiting the Agung 1963 volcanic forcing – impact of one or two eruptions U. Niemeier et al. 10.5194/acp-19-10379-2019
- Climate response to off-equatorial stratospheric sulfur injections in three Earth system models – Part 2: Stratospheric and free-tropospheric response E. Bednarz et al. 10.5194/acp-23-687-2023
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- The Interactive Stratospheric Aerosol Model Intercomparison Project (ISA-MIP): motivation and experimental design C. Timmreck et al. 10.5194/gmd-11-2581-2018
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- Comparing Surface and Stratospheric Impacts of Geoengineering With Different SO2 Injection Strategies B. Kravitz et al. 10.1029/2019JD030329
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- How the Hunga Tonga—Hunga Ha'apai Water Vapor Cloud Impacts Its Transport Through the Stratosphere: Dynamical and Radiative Effects U. Niemeier et al. 10.1029/2023GL106482
- 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
- On the magnitude and sensitivity of the quasi-biennial oscillation response to a tropical volcanic eruption F. Brown et al. 10.5194/acp-23-5335-2023
- The Circulation Response to Volcanic Eruptions: The Key Roles of Stratospheric Warming and Eddy Interactions K. DallaSanta et al. 10.1175/JCLI-D-18-0099.1
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- Evaluating climate geoengineering proposals in the context of the Paris Agreement temperature goals M. Lawrence et al. 10.1038/s41467-018-05938-3
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- Sensitivity of Total Column Ozone to Stratospheric Sulfur Injection Strategies S. Tilmes et al. 10.1029/2021GL094058
- Climate Response to Latitudinal and Altitudinal Distribution of Stratospheric Sulfate Aerosols M. Zhao et al. 10.1029/2021JD035379
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- Land Surface Cooling Induced by Sulfate Geoengineering Constrained by Major Volcanic Eruptions M. Plazzotta et al. 10.1029/2018GL077583
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Latest update: 20 Nov 2024
Short summary
An artificial stratospheric sulfur layer heats the lower stratosphere which impacts stratospheric dynamics and transport. The quasi-biennial oscillation shuts down due to the heated sulfur layer which impacts the meridional transport of the sulfate aerosols. The tropical confinement of the sulfate is stronger and the radiative forcing efficiency of the aerosol layer decreases compared to previous studies, as does the forcing when increasing the injection height.
An artificial stratospheric sulfur layer heats the lower stratosphere which impacts...
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