The climate factors revealed in the study shed new light on Greenland’s climate and can help predict the future development of Greenland’s ice sheet.
The climate factors revealed in the study shed new light on Greenland’s climate and can help predict the future development of Greenland’s ice sheet.
In recent years, Greenland has warmed faster than the global average. A new study identifies clear-sky downwelling longwave radiation—heat radiated by the atmosphere to the surface—along with moisture advection, high-pressure anomalies, and surface albedo feedback, as key drivers of this accelerated warming. These factors are contributing to the rapid melting of Greenland's ice sheet. The findings are crucial for predicting future ice sheet behavior and its potential impact on global sea levels.
Global warming, driven by human activities, has led to rising average temperatures worldwide. However, Greenland has been warming at an even faster rate than the rest of the world, leading to accelerated ice sheet melting. This intensified warming in the northern regions, known as Arctic Amplification, has the potential to raise sea levels significantly, posing a threat to coastal areas and ecosystems globally. Understanding the drivers behind this phenomenon is crucial for predicting future climate impacts.
Read more at Pusan National University
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