The Asian Age

Scientists click foundation of ‘notorious’ Antarctic glacier

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New York: Using a robotic submarine, researcher­s have taken the first-ever images of the Antarctic Thwaites glacier’s foundation­s, a step towards better monitoring of the ice sheet which is notorious for its contributi­ons to sea-level rise.

According to the researcher­s, including those from Georgia Institute of Technology in the US, Thwaites accounts for about four per cent of global sealevel rise, causing concerns that a tipping point in its stability may result in a run-away collapse of the glacier, and boost sea levels by as much as 25 inches.

A particular area of concern, visited by the robotic submarine, named Icefin, is a boundary called the grounding line between where the glacier rests on the ocean bed, and where it floats over water.

The scientists noted that this grounding line is important to the stability of Thwaites Glacier’s footing

since the farther it recedes, the faster the ice can flow into the sea, pushing up sea-level.

“Visiting the grounding line is one of the reasons work like this is important because we can drive right up to it and actually measure where it is,” said Britney Schmidt, a

researcher from Georgia Institute of Technology, who is part of the project.

“It’s the first time anyone has done that or has ever even seen the grounding zone of a major glacier under the water, and that’s

the place where the greatest degree of melting and destabilis­ation can

occur,” Schmidt said.

As part of the project, Icefin swam over 15 kilometers round trip during five missions, including two passes up to the grounding zone — one where it got extremely close to the place where the seafloor meets the ice.

 ??  ?? An aerial view Thwaites Glacier. The scientists noted that the grounding line (inset) is important to the stability of the Glacier’s footing since the farther it recedes, the faster the ice can flow into the sea, pushing up sea-level.
An aerial view Thwaites Glacier. The scientists noted that the grounding line (inset) is important to the stability of the Glacier’s footing since the farther it recedes, the faster the ice can flow into the sea, pushing up sea-level.

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