https://egusphere.copernicus.org/preprints/2026/egusphere-2026-310/

*Authors: *Ewa M. Bednarz, Amy H. Butler, James M. Haywood, Matthew Henry,
Andy Jones, Ben Kravitz, Walker R. Lee, Douglas G. MacMartin, Amanda C.
Maycock, Takashi Sekiya, Shingo Watanabe, and Daniele Visioni

*27 January 2026*

*Abstract*
Owing to the crucial role of stratospheric ozone in shielding the Earth
from harmful solar ultraviolet radiation, impacts of human activities on
the ozone layer remain of interest. Here we provide an assessment of the
potential impacts of Stratospheric Aerosol Injection (SAI), a proposed
method to temporarily offset global warming, on stratospheric ozone
projections over the 21st century using the new multi-model GeoMIP
G6-1.5K-SAI experiment. The experiment injects SO2 at a pair of subtropical
latitudes and utilizes a more plausible middle-of-the-road greenhouse gas
emission pathway and SAI start date compared to earlier studies.

All three participating Earth system models show a decrease in global mean
total column ozone of a few Dobson units (1–2 %) under SAI compared to
no-SAI scenario. This decrease is dominated by heterogeneous halogen
activation on sulfate aerosol, most clearly evident in the Southern
Hemisphere mid- and high latitudes. This is unlike previous results using
strategies injecting at the equator, which show increased global mean
column ozone, partly due to larger ozone transport changes. As background
halogen levels continue to decrease, the potential of SAI to deplete ozone
is found to be a factor of ~2 larger in the earlier part of the 21st
century (2045–2064) than later (2065–2084). We further identify areas of
model disagreement and sources of uncertainty, but also areas of more
confidence and potential emergent constraints. Our results highlight the
need to assess any projected SAI impacts in the wider strategy and scenario
dimension using a multi-model framework.

*Source: EGUSphere*

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