The Borneo Post

Sea level fears as more of giant Antarctic glacier floating than thought

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SYDNEY: More of a giant Francesize­d glacier in Antarctica is floating on the ocean than previously thought, scientists said yesterday, raising fears it could melt faster as the climate warms and have a dramatic impact on rising sea-levels.

The Totten Glacier is one of the fastest-flowing and largest glaciers in Antarctica with scientists keen to keep a close eye on how it melts given the enormous amount of water it could potentiall­y unleash.

Using artificial­ly created seismic waves that help scientists see through the ice, researcher­s have discovered that more of the Totten Glacier floats on the ocean than initially thought.

“In some locations we thought were grounded, we detected the ocean below indicating that the glacier is in fact f loating,” said Paul Winberry from Central Washington University.

The findings are important because recent studies have shown the Totten Glacier’s underbelly is already being eroded by warm, salty sea water flowing hundreds of kilometres in land after passing through underwater ‘gateways’.

As it does, the portion of the glacier resting on water rather than rock increases, accelerati­ng the pace of disintegra­tion.

Winberry said more of the glacier f loating on a warming ocean could help explain recent periods of accelerate­d melting.

Glaciers are huge bodies of dense ice that slowly move down valleys, mountains and slopes under their own weight over many centuries, sculpting the earth below as they go.

They hold the vast majority of Earth’s fresh water and are the main contributo­r to rising sea levels when they melt.

According to Nasa monitoring, between 2002 and 2016, Antarctica lost 125 gigatonnes of ice per year, causing sea levels worldwide to rise by 0.35 millimetre­s annually.

 ?? — AFP photo ?? Photo shows scientists setting up equipment on Totten Glacier to measure glacial flow speed and surface elevation.
— AFP photo Photo shows scientists setting up equipment on Totten Glacier to measure glacial flow speed and surface elevation.

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