Comment on egusphere-2026-310

<strong class="journal-contentHeaderColor">Abstract.</strong> 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 21^st 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&ndash;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 21^st century (2045&ndash;2064) than later (2065&ndash;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.