Home / News and Events / Media Releases / Ross Ice Shelf

New Antarctic research “a big step forward” in predicting impacts of climate change - 29/05/2019

The Ross Ice Shelf holds the key to avoiding catastrophic sea-level rises as the planet warms – and new research will help scientists monitor its future health.

An international team of researchers including New Zealand’s GNS Science took part in the ROSETTA-Ice project, mapping the sea floor under the ice shelf.

"

These observations can then guide computer models to predict how the Ross Ice Shelf and the West Antarctic Ice Sheet will change as our climate warms

Dr Richard Levy

"

Their findings are published in Nature Geoscience magazine today.

The Ross Ice Shelf occupies an area twice the size of New Zealand and is within the Ross Dependency, the region of Antarctica over which New Zealand claims a right of sovereignty.

The shelf helps to slow the flow of Western Antarctica’s grounded sea ice into the ocean.

Most of the ice in West Antarctica sits on ground below sea level and is particularly vulnerable to increases in ocean temperature.

If all of this marine-based ice were released into the ocean, global sea level would rise by at least 3.5 metres in the coming centuries.

“Working with international partners allowed us to gather important data in an area where the floating ice shelf is often more than 300 metres thick,” GNS Science marine geophysicist Fabio Caratori Tontini says.

“GNS Science contributed not just our expertise, but our dynamic gravimeter, which measures the earth’s gravitational force from a moving aeroplane.

Working with international partners allowed us to gather important data in an area where the floating ice shelf is often more than 300 metres thick,” GNS Science marine geophysicist Fabio Caratori Tontini says

"Working with international partners allowed us to gather important data in an area where the floating ice shelf is often more than 300 metres thick,” GNS Science marine geophysicist Fabio Caratori Tontini says. Image: Robin Bell, Lamont-Doherty Earth Observatory

“This instrument makes measurements that allow us to model the shape of the sea floor under the ice – which is essential for understanding how the ocean circulates and how the ice melts.”

“We could see that a previously unmapped geological boundary was making the seafloor on the East Antarctic side much deeper than the West, and that affects the way the ocean water circulates under the ice shelf,” explained Kirsty Tinto, the Lamont-Doherty Earth Observatory research scientist who led all three field expeditions and is lead author of the study.

“This research will help scientists develop new ways of monitoring the health of Antarctic ice sheets,” GNS Science’s Environment and Climate theme leader Richard Levy says.

“We can use this research to help determine where to place instruments to observe ocean currents that circulate beneath the ice shelf.

“These observations can then guide computer models to predict how the Ross Ice Shelf and the West Antarctic Ice Sheet will change as our climate warms.

“Some studies suggest that collapse of the ice sheets can be avoided if we reduce greenhouse gas emissions and keep warming under 1.5 degrees centigrade above pre-industrial levels.

“This is the primary goal of New Zealand’s Zero Carbon Bill which is currently under consideration in Parliament.

“We need to know how Antarctica will respond to this relatively small amount of warming, and the ROSETTA team’s research is a big step forward.”