https://essopenarchive.org/doi/full/10.22541/essoar.177100420.06303100/v1

*Authors*: Isaline Businger, Rhonda Müller, Raleigh Grysko, Jacqueline
Oehri, Jin-Soo Kim, Gabriela Schaepman-Strub

*13 February 2026*

*Abstract*
The Arctic is warming about four times faster than the global average, with
permafrost thaw representing a potential global climate tipping element.
Given the insufficient rate of carbon emission reductions, stratospheric
aerosol injection (SAI) has emerged as a strategy to abate climate warming.
However, its effects on permafrost thaw drivers remain uncertain. The
G6sulfur experiment, part of the Geoengineering Model Intercomparison
Project (GeoMIP6), aims to reduce radiative forcing in the high-emission
scenario (ssp585) to levels comparable to those in the moderate-emission
scenario (ssp245) by injecting stratospheric aerosols near the equator.
Analyzing the G6sulfur results, we find that this intervention alters
atmospheric circulation, modifying winds, cloud properties, and the North
Atlantic Oscillation, which affect temperature patterns and longwave
radiation. These changes shift the relative importance of mechanisms
driving summer permafrost thaw, resulting in a distinct spatial pattern:
increased thaw depth in the Eastern Hemisphere (+0.51 ± 0.07 m) and
decreased thaw in the Western Hemisphere (-0.26 ± 0.06 m), compared to the
ssp245 scenario targeted by the intervention. While G6sulfur reduces
radiative forcing to levels similar to ssp245 and slows permafrost decline
by 2080–2099 relative to ssp585 (+4.61 ± 0.21 × 106 km2), it fails to
preserve as much permafrost area as ssp245 (-1.08 ± 0.18 × 106 km2). By
altering the drivers of permafrost dynamics, G6sulfur creates spatial
variations in thaw patterns, resulting in an overall reduction in
permafrost area compared to ssp245. Our findings underscore the need to
better understand and optimize SAI deployment to avoid unintended regional
impacts.

*Source: ESS Open Archive *

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