Why we may be able to save the Greenland ice sheet

Why we may be able to save the Greenland ice sheet
Sea ice is affected by water temperature while the Greenland ice sheet responds to atmospheric temperature rises. Credit: Dr Teodóra Pados

Studies of ice melt in the Arctic suggest that world may have a fighting chance of preventing huge sea level changes that would result from the dramatic collapse of the vast ice sheets that cover Greenland, but that more work is needed to understand the wider effects.

Greenland has more than two trillion tonnes of water locked up in an enormous blanket of ice that smothers 80% of its land. If it were to disappear, it would cause sea levels around the world to increase by an average of seven metres, leaving many low-lying coastlines and islands submerged.

And as rising temperatures in the Arctic have led to the sea ice that covers much of the region's ocean to retreat even further, scientists have been nervously studying Greenland's melting ice sheet to see how it is being affected.

They fear that without the insulating effect of the sea ice – along with its ability to reflect the summer sunlight – Greenland may suffer accelerated levels of melting in the coming decades. Indeed, with currently at their warmest in more than 11,000 years, there are concerns that the world may have already committed itself to the melting in Greenland over the coming decades.

Now, research that uses sophisticated computer models to simulate the relationship between the Arctic and the ice sheet in Greenland is suggesting that this may not be the case.

Researchers working on the Ice2Ice project have shown that changes in the sea ice and on Greenland's ice sheet appear to occur largely independently of each other. Sea ice is prone to temperature changes in the layers of water in the ocean beneath it while most of Greenland responds to atmospheric temperature rises.

The finding indicates that while the Arctic sea ice appears to be diminishing, Greenland's ice sheet could remain for centuries to come. It suggests that efforts to cut greenhouse gas emissions and limit global temperature increases to below 2°C above pre-industrial levels, as set out in the Paris Agreement on , may allow the world to prevent the sort of melting that would lead to catastrophic rises.

"It means we do not need to worry about any secondary effects from the loss of sea ice on ... (surface) melting in Greenland that is occurring due to the greenhouse effect," explained Professor Jens Hesselbjerg Christensen, a researcher of climate physics at the Niels Bohr Institute in Copenhagen, Denmark and one of the lead coordinators of the Ice2Ice project.

"Yet, the loss of sea ice in the Arctic is still alarming because it has a major impact on the ecosystems in the region."


The Ice2Ice project reconstructed how Arctic sea ice and Greenland's ice sheets have responded to climate changes in the past by analysing ice cores from Greenland and sediment cores from the bottom of the Arctic Ocean. They used this information to build a simulation of what may happen if the world continues to warm.

"We ran an experiment where we had 15°C of , which is very high, to cause all of the sea ice to disappear," said Prof. Hesselbjerg Christensen. "Even so, the response in Greenland only seemed to be driven by the overall enhanced greenhouse effect. It stays steady for hundreds of years and we were not able to see much of an impact from the loss of the sea ice." He said the ice sheet started to change its shape after several hundred years.

While simulating such extreme warming might seem to be unrealistic, some parts of the Arctic are already experiencing abrupt changes in temperature at a local level that could mimic this in the coming decades.

"If you look around Svalbard (on the boundary of the Arctic Ocean), we have seen very large over the last 40 years – something in the order of 2°C per decade," said Prof. Hesselbjerg Christensen. "If that goes on for 100 years, then the warming (locally) would be very strong."

While global temperatures are estimated to have increased by around 1°C compared to those in pre-industrial times, this is an average increase around the world. Some areas will experience greater warming – like the Arctic – while others will not.

This has led many to consider the Arctic to be a kind of canary in the coalmine for what may lie in store as the world continues to warm up. The Stockholm Resilience Centre in Sweden recently identified 19 regime shifts that it considers to be markers of how climate change is transforming the Arctic.

It found that there is already evidence of 15 of these regime shifts taking place in the Arctic as the warming climate causes irreversible changes in the vegetation on land and ecosystems in the ocean.

"The Arctic is the forerunner for climate change around the world as it has, in general, been warming twice as fast as the global average," said Professor Garry Peterson, an environmental scientist at the Stockholm Resilience Centre. "There is growing concern about how the loss of sea ice is changing global weather patterns."


One recent paper published last year in Nature found evidence that the loss of Arctic sea ice might impact precipitation patterns around the world, driving an increase in droughts and fires in places like California, which this year has seen devastating blazes tear through its towns and countryside.

"One of the problems we have is that the Arctic is still not really very well understood," said Prof. Peterson. "There is relatively little monitoring going on in the Arctic compared to other parts of the world. So we are likely to see some more surprises as the Arctic continues to change."

Most of our knowledge about the changes currently taking place in the Arctic come from satellite imaging that show reductions in summer sea ice over the past 40 years. Unfortunately, to really understand whether these are due to humanity's influence on the climate or natural variations in the environment needs data that goes back further into the past.

The IceDynamO project is attempting to build up a high-resolution reconstruction of the sea ice cover in the Arctic Ocean off the coast of the northeast Greenland . Using information stored in the sediment at the bottom of the ocean, researchers on the project are piecing together how the sea ice varied over the last few millennia and how the ocean and atmospheric conditions may have influenced that.

"If we can see what happened in the last 2,000 years, we can see what the natural variations have been in the sea ice before humans started to influence it," said Dr. Teodóra Pados, a geoscientist at Aarhus University in Denmark, who is the lead researcher on the project. "We need to understand what the natural variation of sea ice has been in the recent past and what caused that."

Although the project only started earlier this year, the results should help to inform scientists' attempts to construct models for how the Arctic is likely to change in the coming years. The fate of the region could have profound implications not just for those living there but elsewhere in the world too.

"The (variability in) sea ice influences large-scale climate phenomena that have impacts elsewhere in the world," said Dr. Pados. 'A recent study showed that it can influence the weather in the mid latitudes of Europe, for example, and it is also know to influence the deep water conveyor belt that transports water around the whole world. (The system) is very complex and we still don't know what the full effects will be if we lose the sea ice."

Citation: Why we may be able to save the Greenland ice sheet (2018, December 10) retrieved 20 June 2024 from https://phys.org/news/2018-12-greenland-ice-sheet.html
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