A recent study has heightened concerns about the future of a critical glacier in Antarctica and its contribution to rising sea levels.
Known as the "Doomsday Glacier," Thwaites Glacier, situated on the expansive West Antarctic Ice Sheet, holds the potential to elevate global sea levels by up to 10 feet, posing a significant threat to low-lying coastal areas and displacing millions.
While Thwaites' instability has long been recognized as a pivotal indicator of climate change, a fresh study published this week in the Proceedings of the National Academy of Sciences reveals new findings. It suggests that warm seawater is infiltrating beneath Thwaites' base, accelerating its erosion at a rate previously underestimated.
Monitoring the Meltdown: Rapid Dissolution of the Doomsday Glacier and Implications for Global Sea Level Rise.
Latest Findings: Thwaites' 'Doomsday Glacier' Melting at Accelerated Pace - Heightened Concerns over Rising Sea Levels.
Daily gravitational forces exert pressure on the glacier, facilitating the infiltration of seawater beneath the ice sheet and weakening the submerged ridges that anchor it in place. According to the report, this accelerated deterioration could lead to Thwaites retreating to deeper basin areas within 10 to 20 years, intensifying seawater interaction and expediting its demise.
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