In a first ever estimate of its kind, researchers have used a high-resolution, large-scale computer model to forecast the ice loss that may occur from the West Antarctic Ice Sheet over the course of next 200 years and the resulting increase in sea-levels.
Published in The Cryosphere, the results of the estimates paint the most clear picture till date of West Antarctica’s future than was previously possible.
Global warming is having huge impact on the climate across the world and even the polar regions are not exempted. West Antarctica is one of the fastest warming regions on Earth and its ice sheet has been stage to dramatic thinning in recent years. The West Antarctic Ice Sheet (WAIS) is out of balance because it is losing significant amounts of ice to the ocean, with the losses not being offset by snowfall.
The lost ice, drained by the ice sheet’s several ice streams, amounts to a significant contribution to sea-level rise, which is expected to increase in the future.
Stephen Cornford, a research assistant at the University of Bristol, UK and lead-author of the study, co-author Dan Martin from the Lawrence Berkeley National Laboratory in California, US, and a team of researchers from around the world have used their model to estimate how much of sea-level increase would WAIS contribute to over the next couple of centuries. Their high-resolution, computationally demanding simulations capture future changes in West Antarctica with increased accuracy compared to previous models.
The results reflect uncertainty in future greenhouse gas emissions, snowfall and ocean circulation, but the choice of a high-resolution model allowed the researchers to reduce the numerical error that often plagues ice-flow models.
“We expect future change in the West Antarctic Ice Sheet to be dominated by thinning in the Amundsen Sea Embayment, just as it is today, until at least the 22nd century. But other regions of West Antarctica could thin to a similar extent if the ocean warms sufficiently,” explains Cornford.
In their most extreme simulation, where the ice shelves progressively disintegrate over the next century, most of the major ice streams retreat by hundreds of kilometres. The WAIS as a whole would contribute some 80,000 cubic kilometres of lost ice to sea-level rise by 2100 and 200,000 cubic kilometres by 2200. This corresponds to a 20 cm increase in global sea level by the end of this century – sufficient to fill the Caspian Sea – and close to 50 cm by 2200. While these amounts would be enough to threaten low-lying cities and countries, the researchers point out this is an extreme scenario.
“There are many climate processes lying between the direct consequences of greenhouse-gas emissions and the regional ocean warming used as forcing in the modelling reported in The Cryosphere, many of which are poorly understood,” explains co-author Tony Payne, a professor at the University of Bristol. “It would therefore be premature to attach a likelihood to any particular retreat scenario; however it is useful to quantify the magnitude of sea-level rise in some of these more extreme cases.”
Cornford notes that though the fourth and fifth assessment reports by the IPCC’s [Intergovernmental Panel on Climate Change] did provide details about the acceleration of West Antarctic ice streams in response to ocean warming, they didn’t provide a satisfactory analysis of the situation.
Researchers say that the unique aspect of their research is the use of high-resolution ice-sheet model over a larger area and longer time-scale than previously attempted.
“Much like a higher-resolution digital camera transforms a blur into a flock of birds, higher resolution in a computer model often helps to capture details of the physics involved which may be crucial to the broad picture,” says Martin.
The researchers wanted to find out how the ice sheet would respond to both modest and extreme future warming. “We subjected an ice dynamics model to a range of ocean and atmospheric changes, ranging from no change at all, through the future changes projected by state-of-the-art ocean and atmosphere models, to extreme changes intended to study the upper reaches of future sea-level rise,” explains Cornford.
“The research involved many different steps as the results of global climate models were fed into regional models of the Antarctic atmosphere and ocean, whose results were in turn used to force the ice-sheet model in this study,” Payne adds.
This comprehensive high-resolution study is a significant improvement from previous calculations, which were lower in resolution or scale, allowing researchers to make more accurate predictions about West Antarctica’s future.