Global monsoon response to tropical and Arctic stratospheric aerosol injection
Open accessAbstract
Abstract Stratospheric aerosol injection (SAI) is considered as a backup approach to mitigate global warming, and understanding its climate impact is of great societal concern. It remains unclear how differently global monsoon (GM) precipitation would change in response to tropical and Arctic SAI. Using the Community Earth System Model, a control experiment and a suite of 140-year experiments with CO 2 increasing by 1% per year (1% CO 2 ) are conducted, including ten tropical SAI and ten Arctic SAI experiments with different injecting intensity ranging from 10 to 100 Tg yr −1 . For the same amount of injection, a larger reduction in global temperature occurs under tropical SAI compared with Arctic SAI. The simulated result in the last 40 years shows that, for a 10 Tg yr −1 injection, GM precipitation decreases by 1.1% (relative to the 1% CO 2 experiment) under Arctic SAI, which is weaker than under tropical SAI (1.9%). Further, tropical SAI suppresses precipitation globally, but Arctic SAI reduces the Northern Hemisphere monsoon (NHM) precipitation by 2.3% and increases the Southern Hemisphere monsoon (SHM) precipitation by 0.7%. Under the effect of tropical SAI, the reduced GM precipitation is mainly due to the thermodynamic term associated with the tropical cooling-induced decreased moisture content. The hemispheric antisymmetric impact of Arctic SAI arises from the dynamic term related to anomalous moisture convergence influenced by the anomalous meridional temperature gradient.
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Arctic SAI would have less of an effect on Monsoon precipitation.
“Arctic SAI for instance would have less of an effect on Monsoon precipitation (Sun et al., 2020).”
From A Fate Worse Than Warming? Stratospheric Aerosol Injection and Global Catastrophic Risk (2021) · cites this paper as Sun et al., 2020
The Abstract reports a smaller reduction in global monsoon precipitation under Arctic than tropical SAI at the same 10 Tg yr⁻¹ injection rate (1.1% versus 1.9%). But Section 4 reports stronger suppression under Arctic SAI in some Northern Hemisphere monsoon regions, so the claim is supported for global monsoon precipitation, not uniformly for monsoon precipitation across regions. (LLM, conf=0.83)
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“Impacts discussed in section: Directly Catastrophic Impacts: Ecological Blowback? also can change with a non-equatorial injection – Arctic SAI for instance would have less of an effect on Monsoon precipitation (Sun et al., 2020).”
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Self-citation
- Authors
- Sun, W., Wang, B., Chen, D., Gao, C., Lu, G., & Liu, J.
- Affiliations
- Nanjing Normal University (CN)
- University of Hawaiʻi at Mānoa (US)
- University of Gothenburg (SE)
- Zhejiang University (CN)
- Corresponding author
- Liu, Jian
- Venue
- Climate Dynamics
- Published
- 2020-07-29
- Volume
- 55
- Issue
- 7-8
- Pages
- 2107-2121
- ISSN
- 0930-7575 (ISSN-L)
- 1432-0894
- OpenAlex
- W3046035471
- Cited by
- 42
- References
- 56
- Citations by year
- 2026: 3 · 2025: 6 · 2024: 9 · 2023: 7 · 2022: 10 · 2021: 6 · 2020: 1
- FWCI
- 2.23
- Type
- journal article
- Language
- en
- Open access
- hybrid
- doi.org
- Locations
- Climate Dynamics (publishedVersion, cc-by)
- Funders
- National Natural Science Foundation of China (41971108, 41420104002, 41671197, 41971021)
- National Key Research and Development Program of China (2016YFA0600401)
- Priority Academic Program Development of Jiangsu Higher Education Institutions (164320H116)
- Topics
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate Change and Geoengineering
- Physical Sciences › Environmental Science › Global and Planetary Change › Atmospheric aerosols and clouds
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Keywords
- stratospheric aerosol injection, global monsoon, monsoon rainfall, geoengineering, climate change mitigation, moisture convergence, meridional temperature gradient
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