A new ice sheet model developed by glaciologists at the University of California, Irvine and NASA's Jet Propulsion Laboratory projects that the melting of Thwaites Glacier in West Antarctica will contribute up to 30 millimeters (1.2 inches) of sea level rise by 2100—twice previous estimates—even without additional climate warming.
Thwaites Glacier's Melting Could Lead to Significant Sea-Level Rise by 2100
A new model by researchers from the University of California, Irvine and NASA predicts that Thwaites Glacier's melting could lead to a sea level rise of up to 30 millimeters by 2100, which is double previous estimates. This projection is significant as it highlights the potential impacts of climate change on global sea levels. For Iran, rising sea levels could exacerbate coastal flooding and affect its economy and population.
👥 Key Players
📰 What Happened
Researchers from the University of California, Irvine and NASA have developed a new model predicting that the melting of Thwaites Glacier will lead to a sea level rise of up to 30 millimeters by 2100, which is double previous estimates. This finding underscores the urgency of addressing climate change impacts.
- Thwaites Glacier is located in West Antarctica.
- The projected sea level rise could occur even without additional climate warming.
💡 Why It Matters
📚 Background
Thwaites Glacier is often referred to as the 'doomsday glacier' due to its potential to significantly raise sea levels if it collapses. Understanding its melting is critical for predicting future climate scenarios.
🏷️ Entities Mentioned
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