Global monsoon response to tropical and Arctic stratospheric aerosol injection

• Published in: Climate Dynamics
• Main Authors: Sun, Weiyi, Wang, Bin, Chen, Deliang, Gao, Chaochao, Lu, Guonian, Liu, Jian
• Other Authors: National Natural Science Foundation of China, National Key Research and Development Program of China, Priority Academic Program Development of Jiangsu Higher Education Institutions
• Format: Article in Journal/Newspaper
• Language: English
• Published: Springer Science and Business Media LLC 2020
• Subjects: Atmospheric Science; Arctic; Global warming
• Online Access: http://dx.doi.org/10.1007/s00382-020-05371-7; https://link.springer.com/content/pdf/10.1007/s00382-020-05371-7.pdf; https://link.springer.com/article/10.1007/s00382-020-05371-7/fulltext.html

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.