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Weakening ice shelf has caused crucial Antarctic glacier ...

The flow of ice at Pine Island Glacier in West Antarctica has sped up dramatically because of the disintegration of the ice shelf in fron...

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Saturday, February 7, 2026 ๐Ÿ“– 2 min read
Weakening ice shelf has caused crucial Antarctic glacier ...
Image: New Scientist

Whatโ€™s Happening

Alright so The flow of ice at Pine Island Glacier in West Antarctica has sped up dramatically because of the disintegration of the ice shelf in front of it, and this could lead to faster sea level rise Environment Weakening ice shelf has caused crucial Antarctic glacier to accelerate The flow of ice at Pine Island Glacier in West Antarctica has sped up dramatically because of the disintegration of the ice shelf in front of it, and this could lead to faster sea level rise By James Woodford 6 February 2026 Facebook / Meta Twitter / X icon Linkedin Reddit Email Giant icebergs have been breaking off the edge of Pine Island ice shelf NASA/Brooke Medley A large and fast-melting glacier in West Antarctica has sped up dramatically since 2017.

This may be a sign that the floating ice shelf in front of it is no longer helping to hold back the ice. Pine Island glacier is the fastest-flowing glacier in Antarctica and the largest contributor to sea-level rise of all Antarctic glaciers. (it feels like chaos)

It is a key part of the West Antarctic ice sheet, which holds enough ice to raise the global sea level by 5.

The Details

3 metres if melted completely. City-sized iceberg has turned into a giant swimming pool The Pine Island ice shelf lies in front of the glacier and juts out over the ocean.

It is thought to play a crucial role in holding back the inland ice and shielding it from warm water, buttressing an amount of ice equivalent to 51 centimetres of sea-level rise. The instability of Pine Island glacier and the neighbouring Thwaites glacier, nicknamed the Doomsday glacier, poses a major threat to the long-term viability of the broader West Antarctic ice sheet.

Why This Matters

Sarah Wells-Moran at the University of Chicago and her colleagues tracked the movement of Pine Island glacier using imagery from the Copernicus Sentinel-1 Satellite and observations going back to the early 1970s. Free to The Earth Edition Unmissable news about our planet, delivered straight to your inbox each month. To The glacierโ€™s velocity increased from 2.

The scientific community tends to find developments like this significant.

The Bottom Line

To The glacierโ€™s velocity increased from 2. 2 kilometres per year in 1974 to 4 kilometres per year by 2008.

Whatโ€™s your take on this whole situation?

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Originally reported by New Scientist

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