Unraveling the Mystery: New Clue Found in Tidewater Glacier Retreat
Tidewater glaciers are retreating at unprecedented rates, and new research suggests that the bursting of tiny, pressurized bubbles in underwater glacier ice may be a key factor. The study found that bubbly glacier ice melts more than twice as fast as non-bubbly ice, indicating the need to adjust current climate models. These bubbles, which are filled with pressurized air, have not been accounted for in previous models. Understanding the role of these bubbles in ice melt could lead to more accurate predictions of glacier retreat and sea level rise.