https://www.frontiersin.org/journals/climate/articles/10.3389/fclim.2024.1426679/abstract

*Authors*
Ariel L. Morrison, Debanjali Pathak, Elizabeth A. Barnes, James W. Hurrell

*26 August 2024*

DOI: 10.3389/fclim.2024.1426679

*Abstract*
Rapid reductions in Arctic sea ice in response to warming have led to
increased interest in using the Arctic Ocean for commercial shipping. As
the world warms, however, different strategies are being considered to
stabilize or reduce surface temperatures in order to prevent critical
climate change impacts. One such strategy is stratospheric aerosol
injection (SAI), a form of solar climate intervention. Projected changes to
Arctic sea ice under SAI with specific regards to shipping have not yet
been assessed. We compare output from two SAI simulations that have
different global mean temperature targets with a non-SAI control simulation
to provide the first assessment of Arctic Ocean navigability under
potential SAI scenarios. We find that sea ice concentration and thickness
quickly stabilize or increase after SAI deployment. When sea ice thickness
stabilizes in response to SAI, the number of days when the Arctic Ocean is
navigable remains fairly constant, but increasing sea ice thickness leads
to reduced navigability compared to the non-SAI simulation. From 2035-2069,
both the Northwest Passage and Northern Sea Route are accessible from
July-November in all three simulations, but there are no navigable routes
under either SAI scenario from April-June. When the Arctic is navigable, it
can take 2-12 days longer to cross the Arctic Ocean in the SAI simulations
than in the non-SAI control simulation, and there are large year-to-year
variations in travel time. Overall, Arctic shipping may take longer and be
more difficult in an SAI vs a non-SAI world because of relatively thicker
sea ice, but the degree to which Arctic shipping may change in response to
SAI is dependent on the particular climate intervention strategy.

*Source: Frontiers *

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