A key area of ice in west Antarctica may already be unstable enough to cause global sea levels to rise by three metres of ocean rise, scientists said on Monday.
The study follows research published last year, led by Nasa glaciologist Eric Rignot, warning that ice in the Antarctic had gone into a state of irreversible retreat, that the melting was considered “unstoppable” and could raise sea level by 1.2 metres.
This time, researchers at Germany’s Potsdam Institute for Climate Impact Research pointed to the long-term impacts of the crucial Amundsen Sea sector of west Antarctica, which they said “has most likely been destabilized”.
They used computer models to project the effects of 60 more years of melting at the current rate.
This “would drive the west Antarctic ice sheet past a critical threshold beyond which a complete, long-term disintegration would occur.”
In other words, “the entire marine ice sheet will discharge into the ocean, causing a global sea level rise of about three meters,” the authors wrote.
“If the destabilisation has begun, a three-meter increase in sea level over the next several centuries to millennia may be unavoidable.”
Even just a few decades of ocean warming can unleash a melting spree that lasts for hundreds to thousands of years.
“Once the ice masses get perturbed, which is what is happening today, they respond in a non-linear way: there is a relatively sudden breakdown of stability after a long period during which little change can be found,” said lead author Johannes Feldmann.
The authors noted that Antarctica’s situation presents the largest uncertainty in sea level projections for the coming centuries, and that studying the vast region poses many challenges.
And indeed, just days before the PNAS study was released, another scientific paper used Nasa satellite data form 2003 to 2008 to show that Antarctic ice had gained mass, and had packed on enough to exceed the amount lost in other areas.