Scientists are testing ways to thicken some Arctic sea ice in winter—not a plan to refreeze the whole Arctic. One method pumps seawater onto existing snow-covered ice so it freezes in a new surface layer and may encourage more ice to grow underneath. A 2024–25 trial in Cambridge Bay, Nunavut, measured up to 32 cm more ice in flooded areas than in controls by mid-May. That is evidence of local thickening under trial conditions, not proof the approach can restore Arctic-wide ice or cool the planet.
What does “refreezing the Arctic” actually mean?
The phrase is shorthand for experimental sea-ice management. The winter flooding approach starts with existing sea ice: pumps bring seawater onto its snow-covered surface. That water can freeze into an additional layer. Flooding can also reduce the snow’s insulation, potentially allowing the ocean to grow more ice at the bottom. Snow may later be added back to restore a brighter, more insulating surface. Ocean Visions describes the approach and its intended mechanisms.
It is not a way to freeze open ocean across the Arctic, and it does not directly address the greenhouse-gas emissions driving global warming. The relevant questions are whether a treatment can thicken ice locally, whether it can be deployed safely and reliably over a meaningful area, and whether that would make a measurable difference to climate.
What happened in the Cambridge Bay field trial?
A peer-reviewed study reports a 2024–25 field campaign in Cambridge Bay, Nunavut, Canada. Researchers worked within a 1 by 1 km site, dividing it into three areas that were never flooded and eight test areas. The flooded portions totaled 0.25 km²—one quarter of a square kilometre, not the whole study site.
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- By mid-May, before melt, flooded test areas were up to 32 cm thicker than the unflooded controls.
- Test areas had 1–13 cm less snow cover.
- Areas flooded twice thickened more than areas flooded once.
These are measured differences at a small experimental site; “up to” describes the greatest reported difference, not a uniform gain across every treated area. The trial shows that flooding can produce local thickening under those conditions. It does not establish how the technique would perform across different Arctic locations, over successive years, or at large operational scale. The study is published in Earth’s Future (2026).
What was observed during melt?
A University of Cambridge project update says the treated areas remained brighter during the melt season and appeared to melt more slowly than surrounding controls. That institutional description is an observation from the project update, not evidence that the method can preserve summer sea ice across a region. Read the University of Cambridge update, dated 26 May 2026.
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What other sea-ice intervention is being explored?
Not every group described as trying to “refreeze” the Arctic is using pumps. Reporting distinguishes winter surface flooding from a proposal to reinforce natural ice arches—structures in narrow straits that help hold back ice and limit its southward flow.
| Approach | Mechanism and target | Evidence described in reporting |
|---|---|---|
| Winter flooding and pumping | Pump seawater onto existing sea ice in winter, with the aim of adding a surface layer and encouraging basal growth. Real Ice is associated with this approach. | The Cambridge Bay field study measured local thickening; it did not test Arctic-wide deployment. |
| Ice-arch reinforcement | Strengthen natural ice arches in narrow straits to impede southward ice flow. Arctic Reflections has explored this approach. | A 2026 report described preliminary results as too early to assess whether it works. |
The approaches have different targets and evidence. Neither has been shown to work at Arctic scale. The Guardian’s 16 June 2026 report discusses the groups and the early status of the work.
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Could pumping matter at Arctic scale?
A 2025 review of five polar geoengineering concepts—including sea-ice management—concluded that all five are unlikely to be effective. It points to the scale and speed of climate change, potential harmful side effects, unresolved environmental protections, governance and financing challenges, and the danger of distracting from decarbonization. This is a critical assessment of large-scale prospects, not a finding that the Cambridge Bay experiment failed to thicken ice.
Engineering scale and estimated cost
The review cites engineering estimates of 10 million pumps to cover 10% of the Arctic Ocean and 100 million to cover the whole Arctic. It also cites estimated annual production and transport costs of US$50 billion for 10% coverage and US$500 billion for whole-Arctic coverage. These are estimates cited by the review, not observed costs for an operating program or costs measured in the Cambridge Bay trial.
Thicker ice is not the same outcome as less global warming
The same review reports a modeling result in which maintaining late-summer Arctic sea ice at its then-current extent for roughly 60 years would have a negligible effect on global warming. That modeled result concerns global temperature, not whether a particular patch of ice can be made thicker. Preserving some sea ice and mitigating global warming are distinct goals, and success at the first would not establish success at the second.
As University of Washington researcher Ed Marchand put it, “Whether you can do this on a scale that’s large enough to be climatically important is a difficult and open question.” The review’s conclusions and cited modeling and engineering estimates are in the 2025 Frontiers in Science assessment; the quotation and reporting on feasibility are covered by The Guardian.
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What should readers conclude?
- Demonstrated: In one small Cambridge Bay trial, winter flooding produced locally thicker ice than unflooded controls by mid-May.
- Not demonstrated: Arctic-wide restoration, reliable performance over many seasons, ecological safety at scale, or a global cooling effect.
- Major unresolved issues: the number of pumps and cost implied by broad coverage, environmental risks, reliable operation, and governance.
- Climate context: sea-ice interventions are not a substitute for cutting emissions; the 2025 review warns that they could distract from urgent decarbonization.
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