Abstract
The Antarctic ice sheet is integral to Earth's climate system, influencing global energy and water cycles, and ecosystems. Enough ice is stored in regions most vulnerable to rapid retreat to cause sea levels to rise by ∼15 m if they completely melted, making their stability a key concern. As global temperatures approach and look to surpass 1.5°C (Box 1) above pre-industrial levels, Antarctic ice loss is accelerating, with the potential to trigger significant climatic shifts. Yet, the complex processes governing its stability in a warming climate remain insufficiently understood, limiting society's preparedness. Given the accelerating rate of ice loss and its profound implications, urgent and coordinated efforts to reduce uncertainties around future Antarctic ice changes are essential for policymakers and society, as the resulting melt will have global consequences, especially for coastal areas already facing rising flood risks.
Published Version
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call