https://www.essoar.org/doi/abs/10.1002/essoar.10512047.1

High-latitude stratospheric aerosol injection to preserve the Arctic
Authors
Walker RaymondLee
iD
Douglas GMacMartin
iD
DanieleVisioni
iD
BenKravitz
iD
YatingChen
John ChristopherMoore
iD
GunterLeguy
David MLawrence
iD
David AnthonyBailey
iD
See all authors
Published Online:Sun, 7 Aug 2022
DOI:https://doi.org/10.1002/essoar.10512047.1
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Abstract
Stratospheric aerosol injection (SAI) has been shown in climate models to
reduce some impacts of global warming in the Arctic, including the loss of
sea ice, permafrost thaw, and reduction of Greenland Ice Sheet (GrIS) mass;
SAI at high latitudes could preferentially target these impacts. In this
study, we use the Community Earth System Model to simulate two
Arctic-focused SAI strategies, which inject at 60°N latitude each spring
with injection rates adjusted to either maintain September Arctic sea ice
at 2030 levels (“Arctic Low”) or restore it to 2010 levels (“Arctic High”).
Both simulations maintain or restore September Arctic sea ice to within 10%
of their respective targets, reduce permafrost thaw, and increase GrIS
surface mass balance by reducing runoff. Arctic High reduces these impacts
more effectively than a globally-focused SAI strategy that injects similar
quantities of SO<sub>2</sub> at lower latitudes. However, Arctic-focused
SAI is not merely a “reset button” for the Arctic climate, but brings about
a novel climate state, including changes to the seasonal cycles of Northern
Hemisphere temperature and sea ice and less high-latitude carbon uptake
relative to SSP2-4.5. Additionally, while Arctic-focused SAI predominantly
cools the Arctic, its effects are not confined to the Arctic, including
detectable cooling throughout most of the northern hemisphere for both
simulations, increased mid-latitude sulfur deposition, and a southward
shift of the location of the Intertropical Convergence Zone (ITCZ

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