A number of floating ice shelves in Antarctica are at risk of disappearing entirely in the next 200 years, as global warming reduces their snow cover. Their collapse would enhance the discharge of ice into the oceans and increase the rate at which sea-level rises. A rapid reduction of greenhouse gas emissions could save a number of these ice shelves, researchers at Utrecht University and the British Antarctic Survey say in a new paper published today in the Journal of Glaciology.
Back in 1995 and 2002, two floating ice shelves in the north of the Antarctic Peninsula (Larsen A and B) suddenly collapsed – each event occurred in a matter of weeks.
Dr Peter Kuipers Munneke, the paper’s lead author, said: “This was a spectacular event, especially when you imagine the size of these ice shelves, which are several hundreds of metres thick, and have been in place for over 10,000 years.”
The team of researchers suspected that the disappearance of the snow layer on top of the ice shelves could be an important precursor for shelf collapse. Their calculations confirm this hypothesis, and show that many more ice shelves could disappear in the next 200 years.
The scientists believed the snow layer plays an important role in regulating the effect of meltwater lakes on the ice shelves.
As long as the snow layer is sufficiently thick and cold, all meltwater can sink into the snow and refreeze. But in a warmer climate, the amount of meltwater increases, and the snow layers become thinner.
As a result, meltwater can no longer refreeze and forms large lakes on the surface of the ice shelves. The water drains through cracks and faults, causing them to widen until they become so wide and deep that the entire ice shelf disintegrates.
After their collapse, ice shelves can no longer provide resistance to the flow of the glaciers previously feeding them. As a result, the glacier flow accelerates significantly, contributing to an increase in sea-level rise.
The researchers performed calculations that show how this process may evolve over the next 200 years, using two different climate scenarios.
Dr Kuipers Munneke said: “If we continue to burn fossil fuels at the current rate, almost all ice shelves in the Antarctic Peninsula will be under threat of collapse in the next 200 years. Only the two largest ones seem to be safe. Even in the much colder eastern part of Antarctica, some ice shelves could disintegrate. If we manage to keep global warming below the European Union target of 2oC, more than half of the ice shelves could be saved, compared to no action taken on emissions reductions.”
The study received financial support from the European Union’s four-year ice2sea project.
Prof. David Vaughan said “We’ve been observing ice-shelf retreat around the Antarctic Peninsula since the early 1990s, but for the first time this model provides a strong basis for the prediction of future changes, which is a major step forward in understanding future sea-level changes.”
Notes to editors
“Firn air depletion as a precursor of Antarctic ice-shelf Collapse” Peter Kuipers Munneke1, Stefan R.M. Ligtenberg1, Michiel van den Broeke1, David G. Vaughan2,Journal of Glaciology, 60 (220), (2014), 10.3189/2014JoG13J183.
1 Affiliated with Utrecht University, Institute for Marine and Atmospheric research Utrecht (IMAU)
2 Affiliated to the British Antarctic Survey, Natural Environment Research Council (www.antarctica.ac.uk)
Ice2sea brings together the EU’s scientific and operational expertise from 24 leading institutions across Europe and beyond. Improved projections of the contribution of ice to sea-level rise produced by this major programme funded by the European Commission’s Framework 7 Programme (grant agreement 226375) informed the fifth IPCC report. In 2007, the fourth Intergovernmental Panel on Climate Change (IPCC) report highlighted ice-sheets as the most significant remaining uncertainty in projections of sea-level rise. www.ice2sea.eu.
To request an interview with Dr Peter Kuipers Munneke or for more information call Monica van der Garde, Press Officer at the Faculty of Science, Utrecht University: email firstname.lastname@example.org; tel +31 6 13 66 14 38.
To request an interview with Professor David Vaughan or for more information on ice2sea and BAS contact Linda Capper, British Antarctic Survey: email@example.com, tel +44 (0)223 221 448.
Copies of the paper are available open access from JoG at: