Greenland’s ice sheet is melting at a scale “off the charts” compared with the previous four centuries, warns a new study.
Researchers say that if the Greenland ice sheet melting continues at “unprecedented rates” – which they attribute to warmer summers – it could accelerate the already fast pace of sea level rise.
Surface melting across Greenland’s mile-thick ice sheet began increasing in the mid-19th Century and then ramped up dramatically during the 20th and early 21st Centuries – and shows no signs of abating, according to the study.
Scientists say their findings, published in the journal Nature, provide new evidence of the impacts of climate change on Arctic melting and global sea level rise.
Study lead author Dr Luke Trusel, a glaciologist at Rowan University in the United States, said: “Melting of the Greenland Ice Sheet has gone into overdrive.
“As a result, Greenland melt is adding to sea level more than any time during the last three-and-a-half centuries, if not thousands of years.
“And increasing melt began around the same time as we started altering the atmosphere in the mid-1800s.”
Co-author Dr Sarah Das, a glaciologist at Woods Hole Oceanographic Institution (WHOI), said: “From a historical perspective, today’s melt rates are off the charts, and this study provides the evidence to prove this.
“We found a 50 per cent increase in total ice sheet meltwater runoff versus the start of the industrial era, and a 30 per cent increase since the 20th Century alone.”
Ice loss from Greenland is one of the key drivers of global sea level rise, according to the study.
Icebergs calving into the ocean from the edge of glaciers represent one component of water re-entering the ocean and raising sea levels.
But more than half of the ice-sheet water entering the ocean comes from runoff from melted snow and glacial ice atop the ice sheet.
Dr Trusel said: “Rather than increasing steadily as climate warms, Greenland will melt increasingly more and more for every degree of warming.
“The melting and sea level rise we’ve observed already will be dwarfed by what may be expected in the future as climate continues to warm.”
To determine how intensely Greenland ice has melted in past centuries, the research team used a drill the size of a traffic light pole to extract ice cores from the ice sheet itself and an adjacent coastal ice cap, at sites more than 6,000 feet above sea level.
The scientists drilled at these elevations to ensure the cores would contain records of past melt intensity, allowing them to extend their records back into the 17th Century.
During warm summer days in Greenland, melting occurs across much of the ice sheet surface.
At lower elevations, where melting is the most intense, meltwater runs off the ice sheet and contributes to sea level rise, but no record of the melt remains.
But at higher elevations the summer meltwater quickly refreezes from contact with the below-freezing snowpack sitting underneath, preventing it from escaping the ice sheet in the form of runoff.
Instead, it forms distinct icy bands that stack up in layers of densely packed ice over time.
Scientists then measured physical and chemical properties along the cores to determine the thickness and age of the melt layers.
Dark bands running horizontally across the cores, like ticks on a ruler, enabled the scientists to visually chronicle the strength of melting at the surface from year to year.
Thicker melt layers represented years of higher melting, while thinner sections indicated years with less melting.
Combining results from multiple ice cores with observations of melting from satellites and sophisticated climate models, the scientists were able to show that the thickness of the annual melt layers they observed clearly tracked not only how much melting was occurring at the coring sites, but also much more broadly across Greenland.
The research team said ice core records provide “critical” historical context because satellite measurements – which scientists rely on today to understand melting rates in response to changing climate – have only been around since the late 1970s.
Study co-author Matt Osman, a graduate student, said: “We have had a sense that there’s been a great deal of melting in recent decades, but we previously had no basis for comparison with melt rates going further back in time.
“By sampling ice, we were able to extend the satellite data by a factor of 10 and get a clearer picture of just how extremely unusual melting has been in recent decades compared to the past.”
Dr Trusel said: “To be able to answer what might happen to Greenland next, we need to understand how Greenland has already responded to climate change.
“What our ice cores show is that Greenland is now at a state where it’s much more sensitive to further increases in temperature than it was even 50 years ago.”
An interesting aspect of the findings, according to Dr Das, was how little additional warming it now takes to cause huge “spikes” in ice sheet melting.
She said: “Even a very small change in temperature caused an exponential increase in melting in recent years”
Dr Trusel added: “Warming means more today than it did in the past.”
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