Extract from The Guardian
Study finds that a global temperature increase of 3C would cause ice
shelves to disappear, triggering sea-level rise that would continue for
thousands of years
A British Antarctic Survey photo released on 25 March 2008 shows of a
chunk of ice that has started to break away from the Antarctic ice
shelf.
Photograph: Jim Elliott/AFP/Getty Images
A team of researchers has found that steep cuts to emissions during
the next decade are the only way to avoid a catastrophic collapse of
Antarctic ice sheets and associated sea-level rise that will continue
for thousands of years.
The study, published in the journal Nature on Wednesday, found that should the global temperature increase to around 3C (5.4F) above the pre-industrial era then the ice shelves that hold back the giant continental ice sheets would be lost over the next few centuries.
This would trigger a collapse that would go on for thousands of years, raising sea levels by 0.6 metres to 3 metres by the year 2300 depending on how high manmade greenhouse gas emissions remain. Our descendants living in the year 5000 will continue to suffer the consequences of today’s fossil fuel burning, as sea levels continue to rise up to nine metres above current levels.
However, the results leave a narrow opening through which humanity can slip. If temperatures remain within 2C, the collapse of the shelves will stabilise and the sheets will remain mostly intact. Sea-level rise from Antarctica would remain within 23cm by 2300.
To achieve this, the authors said the world will have to follow the Intergovernmental Panel on Climate Change’s (IPCC) lowest emissions scenario. This requires global emissions to peak around 2020 and decline to zero by 2100.
In preparation for the climate conference in Paris next month, 150 governments representing 90% of emissions have submitted pledges to cut and curb them. However, these still chart a pathway to a world well above 2C – one analysis suggested they lead to 2.7C of warming, not enough to avoid the runaway decline of the Antarctic ice.
The new study “ultimately confirm[s] the suspicions of earlier glaciologists that the fate of ice shelves largely determines whether Antarctica contributes less than 1 metre or up to 9 metres to long-term sea-level rise,” wrote the California Institute of Technology scientist Alexander Robel in an accompanying comment piece in Nature.
Hilmar Gudmundsson, a scientist at the British Antarctic Survey, said the changes between 2100 and 2300 were “large and alarming” although the degree of uncertainty was still high.
In 2014 Professor Eric Rignot, a senior researcher at Nasa, made the dramatic finding that the West Antarctic ice sheet and its 4 metres worth of sea-level rise had already started slipping away. He said the paper’s assertion that the loss of this ice sheet could be stopped was “hardly believable” because the projections lacked reliable modelling of ocean circulation and iceberg calving. He said the loss of the West Antarctic sheet was “inevitable”; the only thing humans could control was how fast it goes.
“Whether we control our emissions or not will only matter in terms of how fast we get there. I find it disheartening that we are still talking about 2C above pre-industrial as a ‘reasonable’ target when we already passed the threshold for a large share of the ice sheets,” he said.
“It is counterproductive to give the impression that we have to figure out a way out of carbon soon, when we really need to do this yesterday,” he said.
The global sea level has risen roughly 20cm over the last century and is already causing problems for communities in low-lying areas. Only a little of this has so far been caused by melting ice; most comes from the expansion of oceans as they warm. But Golledge and his colleagues warned that this would change in the future if Antarctica’s ice sheets began falling into the sea.
Antarctica’s two ice sheets, east and west, cover an area the size of the contiguous US and Mexico combined and would raise the seas 60 metres if lost completely, according to the US National Snow and Ice Data Centre.
The friction of floating ice shelves against the deeply buried rock of the coast slows the flow of ice from the interior. Removing the ice shelves is like taking the chocks from a truck sitting on a slope. Without them, the loss of the giant ice sheets will trigger an “unstoppable” event that will last for thousands of years, said Golledge’s team. Some buttressing shelves have already been lost and others are weakening. Another study this week warned that all may be lost by the end of the century.
At the UN climate summit in Paris, much of the talk will be about the steps that can be taken over the next decade to strengthen each country’s emissions cuts. Professor Andrew Shepherd, the director of the Nerc Centre for Polar Observation and Modelling said the new research added urgency to Paris.
“Ahead of COP [Conference of the Parties, the Paris summit], this new study is a useful reminder that future climate warming might trigger extreme and irreversible ice losses from Antarctica over centuries. But to reliably predict how things could change within the next century, we need to build and use a new class of ice sheet models that can capture the detailed response of each of the continent’s outlet glaciers,” he said.
The study, published in the journal Nature on Wednesday, found that should the global temperature increase to around 3C (5.4F) above the pre-industrial era then the ice shelves that hold back the giant continental ice sheets would be lost over the next few centuries.
This would trigger a collapse that would go on for thousands of years, raising sea levels by 0.6 metres to 3 metres by the year 2300 depending on how high manmade greenhouse gas emissions remain. Our descendants living in the year 5000 will continue to suffer the consequences of today’s fossil fuel burning, as sea levels continue to rise up to nine metres above current levels.
However, the results leave a narrow opening through which humanity can slip. If temperatures remain within 2C, the collapse of the shelves will stabilise and the sheets will remain mostly intact. Sea-level rise from Antarctica would remain within 23cm by 2300.
To achieve this, the authors said the world will have to follow the Intergovernmental Panel on Climate Change’s (IPCC) lowest emissions scenario. This requires global emissions to peak around 2020 and decline to zero by 2100.
In preparation for the climate conference in Paris next month, 150 governments representing 90% of emissions have submitted pledges to cut and curb them. However, these still chart a pathway to a world well above 2C – one analysis suggested they lead to 2.7C of warming, not enough to avoid the runaway decline of the Antarctic ice.
The new study “ultimately confirm[s] the suspicions of earlier glaciologists that the fate of ice shelves largely determines whether Antarctica contributes less than 1 metre or up to 9 metres to long-term sea-level rise,” wrote the California Institute of Technology scientist Alexander Robel in an accompanying comment piece in Nature.
Hilmar Gudmundsson, a scientist at the British Antarctic Survey, said the changes between 2100 and 2300 were “large and alarming” although the degree of uncertainty was still high.
In 2014 Professor Eric Rignot, a senior researcher at Nasa, made the dramatic finding that the West Antarctic ice sheet and its 4 metres worth of sea-level rise had already started slipping away. He said the paper’s assertion that the loss of this ice sheet could be stopped was “hardly believable” because the projections lacked reliable modelling of ocean circulation and iceberg calving. He said the loss of the West Antarctic sheet was “inevitable”; the only thing humans could control was how fast it goes.
“Whether we control our emissions or not will only matter in terms of how fast we get there. I find it disheartening that we are still talking about 2C above pre-industrial as a ‘reasonable’ target when we already passed the threshold for a large share of the ice sheets,” he said.
“It is counterproductive to give the impression that we have to figure out a way out of carbon soon, when we really need to do this yesterday,” he said.
The global sea level has risen roughly 20cm over the last century and is already causing problems for communities in low-lying areas. Only a little of this has so far been caused by melting ice; most comes from the expansion of oceans as they warm. But Golledge and his colleagues warned that this would change in the future if Antarctica’s ice sheets began falling into the sea.
Antarctica’s two ice sheets, east and west, cover an area the size of the contiguous US and Mexico combined and would raise the seas 60 metres if lost completely, according to the US National Snow and Ice Data Centre.
The friction of floating ice shelves against the deeply buried rock of the coast slows the flow of ice from the interior. Removing the ice shelves is like taking the chocks from a truck sitting on a slope. Without them, the loss of the giant ice sheets will trigger an “unstoppable” event that will last for thousands of years, said Golledge’s team. Some buttressing shelves have already been lost and others are weakening. Another study this week warned that all may be lost by the end of the century.
At the UN climate summit in Paris, much of the talk will be about the steps that can be taken over the next decade to strengthen each country’s emissions cuts. Professor Andrew Shepherd, the director of the Nerc Centre for Polar Observation and Modelling said the new research added urgency to Paris.
“Ahead of COP [Conference of the Parties, the Paris summit], this new study is a useful reminder that future climate warming might trigger extreme and irreversible ice losses from Antarctica over centuries. But to reliably predict how things could change within the next century, we need to build and use a new class of ice sheet models that can capture the detailed response of each of the continent’s outlet glaciers,” he said.
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