https://www.sciencedirect.com/science/article/abs/pii/S0165232X2500240X

*Authors*: Detelina Ivanova, Subarna Bhattacharyya, Anthony Strawa, Steve
Zornetzer, Stephanie Olinger, Leslie Field, Alexander Ivanov, Ethan
Kusnadi, Jacob Kim

*27 August 2025*

https://doi.org/10.1016/j.coldregions.2025.104657

*Highlights*
•Localized targeted solutions for climate intervention such as Surface
Albedo Modification are viable instrument for Arctic ice restoration

•Albedo enhancement in the Beaufort Gyre cools and thickens the ice cover,
aiding melt season survival and building multi-year sea ice.

•The BG SAM intervention can delay the transition to seasonal Arctic sea
ice by about 25 years

*Abstract*
CMIP6 projections show that Arctic could be ice-free by 2050, leading to
global climate disruptions like destabilizing polar jets, stronger storms
and prolonged droughts. Reducing greenhouse gas emissions alone will not be
sufficient to preserve Arctic sea ice, necessitating additional climate
restoration efforts. Field et al. (2018) proposed restoring sea ice by
artificially enhancing surface sea ice albedo with reflective hollow glass
microspheres (HGMs) and their modeling simulations show the potential of
this technology in Arctic sea ice recovery. While Arctic-wide application
is expensive, localized targeted deployments may be feasible. Here we
investigate the impacts and efficacy of regional surface albedo
modification (SAM) application in the Beaufort Gyre (BG) on the Arctic sea
ice and atmospheric radiation budget. We simulate SAM in the BG region
carrying out a ten-member ensemble of 50 years (2000–2050) integrations
using a global CESM2 climate model. Our results show that ~50 % albedo
enhancement in the BG region reduces absorbed surface radiation by ~5 W/m2
and increases outgoing radiation at the top of the atmosphere by ~4.34 W/m2
during summer, comparable to the global anthropogenic radiative forcing of
4.5 W/m2 in the underlying SSP2–4.5 scenario. These radiation budget
changes cool the surface of Arctic annually by 0.78 °C, BG area by 3 °C and
thicken the BG area summer sea ice by up to ~1 m. Our findings suggest that
targeted SAM could help preserve Arctic sea ice, and delay an ice-free
Arctic ocean, offering a viable interim climate intervention.

*Source: ScienceDirect *

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