https://acp.copernicus.org/articles/25/6001/2025/

*Authors*
Simone Tilmes, Ewa M. Bednarz, Andrin Jörimann, Daniele Visioni, Douglas E.
Kinnison, Gabriel Chiodo, and David Plummer

*18 June 2025*

*Abstract*
A new Stratospheric Aerosol Intervention (SAI) experiment has been designed
for the Chemistry–Climate Model Initiative (CCMI-2022) to assess the
impacts of SAI on stratospheric chemistry and dynamical responses and
inter-model differences using a constrained setup with a prescribed
stratospheric aerosol distribution and fixed sea surface temperatures and
sea ice. This paper serves a dual purpose: first, it describes the details
of the experimental setup and the prescribed aerosol distribution and
demonstrates the suitability of the simplified setup to study SAI impacts
in the stratosphere in a multi-model framework. The experiment allows
attributing inter-model differences to the resulting impacts on atmospheric
chemistry, radiation, and dynamics rather than the model uncertainty
arising from differences in aerosol forcing and feedbacks from the ocean
and sea ice under SAI. Second, we use the Whole Atmosphere Community
Climate Model (WACCM6) to compare the interactive stratospheric aerosol
configuration with coupling to land, ocean, and sea ice used to produce the
stratospheric aerosol distribution with the results of the constrained SAI
experiment. With this, we identify and isolate the stratosphere-controlled
SAI-induced impacts from those influenced by the coupling with the ocean.
Overall, this comparison facilitates an advanced process-level
understanding of the drivers of SAI-induced atmospheric responses. For
example, we confirm earlier suggestions that the SAI-induced positive phase
of the North Atlantic Oscillation in winter, with the corresponding winter
warming over Eurasia and related changes, is driven by
stratosphere–troposphere coupling. Future multi-model comparisons will thus
provide an important contribution to upcoming scientific assessments of
ozone depletion.

*Source: EGU*

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