https://acp.copernicus.org/articles/25/18449/2025/

*Authors: *Pengfei Yu, Yifeng Peng, Karen H. Rosenlof, Ru-Shan Gao, Robert
W. Portmann, Martin Ross, Eric Ray, Jianchun Bian, Simone Tilmes, and Owen
B. Toon

*18 December 2025*

*Abstract*
Stratospheric aerosol injection (SAI) using sulfur has been proposed to
cool the planet by reflecting sunlight back to space. A commonly proposed
SAI, with sulfur dioxide injection rate of 10 Tg yr−1 at 25 km, accumulates
aerosols in the tropical lower stratosphere, causing a 6 K warming of the
tropical lower stratosphere that impact the entry value of stratospheric
water vapor and jet positions. This approach could also delay October
Antarctic total column ozone (TCO) recovery to 1980s values by 25–55 years.
We propose a novel SAI approach of injecting sulfur at 50 km (SAI50) that
substantially reduces these negative impacts. In SAI50, the mean meridional
overturning circulation near the stratopause rapidly transports gaseous SO2
to mid-high latitudes, preventing sulfate aerosol accumulation in the
tropical lower stratosphere. This approach reduces tropical stratospheric
warming to 3 K and shortens the Antarctic ozone recovery delay to 5 years.
Furthermore, SAI50 demonstrates greater cooling efficiency, enhancing
global and polar surface cooling by 22 % and 40 % respectively.
Consequently, SAI50 preserves 20 % more Arctic September sea ice compared
to lower-altitude SAI. These findings suggest that SAI50 could offer a more
effective and less disruptive approach to climate intervention.

*Source: EGU*

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