When will it happen? When will a sudden loss of polar ice cause sea levels to rise rapidly, not by millimetres but by metres? That’s the multi-trillion dollar question that should be keeping the world’s policymakers up at night, but alas, they are otherwise engaged.
Not so polar scientists. The focus of their attention has long been on continental ice on Greenland and West Antarctica, the part of Antarctica south of the Pacific Ocean and South America. Now it’s shifted to the Antarctic coast directly south of Tasmania.
A riveting Antarctic Antarctic Program science and policy seminar in Hobart last week highlighted abrupt events in south polar regions, including loss of “permanent” coastal ice shelves and two dramatic crashes in sea ice cover in 2016 and 2023.
Due south of Hobart are the towering ice cliffs forming the face of Ninnis Glacier, one of the main outlets for the ice of Wilkes Basin, an extensive depression in underlying rocks descending over 2000 m below sea level.
Early this century the ice of East Antarctica (the main part of the continent south of Australia and Africa) was considered by scientists to be a very long-term melting risk because of its isolation and altitude, with the greater risk coming from smaller West Antarctica, whose bedrock is mostly below sea level.
That remains the case today, but exceptional ocean heating is changing calculations. A landmark study of the 150-year ocean temperature record published in 2022 found that ocean heating passed a point of no return 12 years ago, and that extreme temperatures – ocean heatwaves – are the new normal.
This extreme heat is no surprise to science. It simply reflects the increasing rate at which carbon compounds are pouring into the air and the consequent heating of the lower atmosphere. Well over 90 per cent of that heat energy finds its way into the ocean.
Abrupt change is an abnormally rapid shift in climate or environmental conditions, like the sea level and ocean circulation shifts at the end of the last ice age around 11,000 years ago. This century has seen rapid sea ice decline and melting Greenland ice, a rise in Arctic methane release, and extreme weather events happening more often and with growing intensity.
All are related to that massive increase in ocean heat, which is where Wilkes Basin comes into the picture.
At various points around the Antarctic coast, warming Southern Ocean waters can penetrate under the ice sheet margin. Drawn by gravity into submarine basins in the continent’s interior, that water can cause the ice above it to float. If that were to happen to ice in Wilkes Basin, global sea levels would rise by three to four metres.
For many years such a mind-boggling scenario has focused on the West Antarctic coast including Thwaites Glacier, dubbed the doomsday glacier on account of its vulnerability to warming seas and its potential impact on sea levels.
More recently Aurora Basin to the south of Australia’s Casey station was the subject of coastal and ice sheet studies, driven by that same potential for sea water penetrating underneath large coastal glaciers to open up the interior to melting from below.
Now Ninnis and neighbouring Mertz Glaciers, over 1500 km east of Casey, are getting attention. They are named after Belgrave Ninnis and Xavier Mertz, who died during Douglas Mawson’s famous, fateful sledge journey in 1912. But this corner of the continent has been little explored since then.
It’s generally agreed that the tipping point for Thwaites Glacier, beyond which complete ice sheet loss is inevitable, is just a decade or so away, but we know much less about East Antarctic glaciers, least of all about those in Wilkes Basin. And the clock is ticking.
This troubles scientists like Philip Boyd, Sonya Fiddes, Poul Christoffersen, Tas van Ommen, Paul Spence and Steve Rintoul, all speakers at that Hobart seminar. But they lack the resources to get the answers they need – tools that aren’t readily available and don’t come cheap when they are, like a research ship and retrievable submersible drones.
The fuel crisis has brought some Australian politicians and commentators close to hysteria about the cost of our renewable energy rollout. “There is no benefit, only huge costs… generational pain but no gain,” wrote Chris Kenny in The Australian at the weekend.
How many of these people have given a moment’s thought to what it’s like to lose home, livelihood and heritage to rising seas, as is happening now for coastal and island dwellers as close to home as Torres Strait?
Their sea level rise is measured in millimetres. Multiply that impact by a thousand, and you’ll begin to understand those scientists’ state of mind.