Researchers have commenced the investigation of the rapidly moving Thwaites Glacier. Their objective is to gather crucial information while the alterations are still reversible.
The glacier, nicknamed the “Doomsday Glacier,” is comparable in area to Great Britain and serves as a pivotal component stabilizing the West Antarctic ice sheet. Should it entirely melt, the global ocean level might rise by 0.5 meters or more. In the worst scenario, due to a chain reaction of adjacent glaciers melting, the water level could increase by 3–5 meters.
Satellite imagery reveals that warm ocean currents are eroding the glacier’s base, causing fissures and voids to form. Scientists from New Zealand journeyed to the glacier’s edge for a month-long scientific expedition to gauge the extent of the ongoing processes.
For this research, the team employs radar systems, drilling rigs, and sensors airlifted to the location by helicopters. This gear permits monitoring the glacier’s movement speed, the temperature, and the condition of the water masses beneath it. Final conclusions will be drawn following the analysis of all accumulated data.
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