Articles | Volume 21, issue 2
https://doi.org/10.5194/acp-21-1287-2021
© Author(s) 2021. 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-21-1287-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
North Atlantic Oscillation response in GeoMIP experiments G6solar and G6sulfur: why detailed modelling is needed for understanding regional implications of solar radiation management
Met Office Hadley Centre, Exeter, EX1 3PB, UK
Jim M. Haywood
Met Office Hadley Centre, Exeter, EX1 3PB, UK
Global Systems Institute, College of Engineering, Mathematics and
Physical Sciences, University of Exeter, Exeter, EX4 4QE, UK
Anthony C. Jones
Met Office, Exeter, EX1 3PB, UK
Simone Tilmes
Atmospheric Chemistry, Observations and Modeling Laboratory, National
Center for Atmospheric Research, Boulder, CO 80307, USA
Ben Kravitz
Department of Earth and Atmospheric Sciences, Indiana University,
Bloomington, IN 47405-1405, USA
Atmospheric Sciences and Global Change Division, Pacific Northwest
National Laboratory, Richland, WA 99352, USA
Alan Robock
Department of Environmental Sciences, Rutgers University, New
Brunswick, NJ 08901-8551, USA
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- Identifying Climate Impacts From Different Stratospheric Aerosol Injection Strategies in UKESM1 A. Wells et al. 10.1029/2023EF004358
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- Climate change modulates the stratospheric volcanic sulfate aerosol lifecycle and radiative forcing from tropical eruptions T. Aubry et al. 10.1038/s41467-021-24943-7
Latest update: 20 Nov 2024
Short summary
Two different methods of simulating a geoengineering scenario are compared using data from two different Earth system models. One method is very idealised while the other includes details of a plausible mechanism. The results from both models agree that the idealised approach does not capture an impact found when detailed modelling is included, namely that geoengineering induces a positive phase of the North Atlantic Oscillation which leads to warmer, wetter winters in northern Europe.
Two different methods of simulating a geoengineering scenario are compared using data from two...
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