A new UN-backed report warns that overshooting 1.5°C, even briefly, could lead to irreversible melting across Earth’s glaciers and polar ice caps. As ice in Greenland and Antarctica melts six times faster than just a few decades ago, experts stress the urgent need for deeper emissions cuts to safeguard coastal communities and vital water sources.
Cryosphere Faces Permanent Damage When World Overshoots 1.5C, Scientists Warn
Key Takeaways:
- Rapid melting of Greenland and Antarctic ice sheets has accelerated sixfold since the 1990s.
- Even a short overshoot of 1.5°C risks permanent damage to glaciers and polar ice.
- Scientists argue the long-term temperature limit for ice sheets should be nearer to 1.0°C.
- Current policies leading to 2.8°C warming could leave less than 10% of glacier mass in the Rockies, Alps, Iceland, and Scandinavia.
- Significant emissions reductions by 2030 and 2035 are crucial to averting the worst impacts.
The Looming Threat to Global Ice
A UN-backed report has sounded an alarm over the unprecedented pace of melting in Earth’s polar regions. Greenland and Antarctic ice sheets, in particular, are losing ice at a rate roughly six times faster than in the 1990s. The danger is not limited to the poles: glaciers around the world are also melting rapidly, with broad implications for environmental balance and human livelihoods.
Overshooting 1.5°C: What It Means
Scientists have long warned that keeping global warming below 1.5°C is critical. According to the report, even a temporary overshoot of that threshold could lock in irreversible changes, rendering subsequent climate mitigation efforts insufficient to save large portions of the cryosphere. “Snow and ice respond rapidly to every fraction of a degree of warming,” said James Kirkham, lead author of the report. However, once certain tipping points are crossed, the recovery could span centuries—if it happens at all.
Damage Already Underway
Released in conjunction with the 31st annual COP climate conference, the report highlights rapidly melting sea ice, glaciers, and permafrost. Thawing permafrost releases more greenhouse gases, compounding climate change. As the pace of warm-weather records grows, so too does the risk to hundreds of millions of people living in low-lying areas threatened by rising seas.
Regional Implications
The consequences vary across regions. For instance, if warming reaches 2.8°C under current policies, glaciers in the Rockies, Alps, Iceland, and Scandinavia could lose more than 90% of their mass. Limiting warming to 1.5°C would preserve 20–35% of those glaciers. In the Hindu Kush Himalayas—key for water supplies to nearly a quarter of humanity—only 41% of ice mass would remain under business-as-usual scenarios, whereas 83% could endure with strict climate action.
Emission Reductions: The Only Path Forward
A separate UNEP report advises that the world needs to lower carbon emissions by 18% by 2030 and by 45% by 2035 to avoid a disastrous temperature spike of 1.7°C or more. This aligns with the cryosphere report’s call for setting a safe temperature limit closer to 1.0°C to prevent the permanent melting of polar ice. As leaders deliberate on climate action, the decisions made now may determine the future of global ice and, in turn, the stability of coastlines, water sources, and weather patterns worldwide.