Researchers found that melting on the island passed a tipping point 20 years ago.
The glaciers and ice caps that dot the edges of the Greenland coast are not likely to recover from the melting they are experiencing now, and some of it will be permanently lost by 2100, a study has found.
Researchers found that melting on the island passed a tipping point 20 years ago. The smallest glaciers and ice caps on the coast are no longer able to regrow lost ice.
The new study suggests that the melting of Greenland's coastal ice will raise global sea level by about 1.5 inches by 2100.
The findings reveal why the parts of Greenland ice are melting so quickly - the deep snow layer that normally captures coastal meltwater was filled to capacity in 1997.
That layer of snow and meltwater has since frozen solid, so that all new meltwater flows over it and out to sea.
It is bad news, but not immediate cause for panic, said Ohio State University glaciologist Ian Howat.
The findings apply to the comparatively small amount of ice along the coast only, he explained - not the Greenland Ice Sheet, which is the second largest ice cache in the world.
"These peripheral glaciers and ice caps can be thought of as colonies of ice that are in rapid decline, many of which will likely disappear in the near future," said Howat, associate professor at Ohio State.
Were all of Greenland's coastal ice to melt away at once, global sea level would rise a few inches. For comparison, were the whole Greenland Ice Sheet to melt away at once, global sea level would rise 24 feet.
The problem lies between fresh surface snow and the ice, in a layer of older snow called the firn. Normally, meltwater drains through gaps in the firn down to the ice surface, where the bottom layer re-freezes.
When the firn around Greenland's edges became fully saturated 20 years ago, it froze through from bottom to top.
Since then, there have not been any gaps to capture meltwater, and the ice has not been able to grow.
At the time, researchers could not have known, because they lacked three things: a high-resolution topographic model of the glaciers, a detailed map of glacier boundaries, and a high resolution numerical model of drainage processes.
Howat provided the first two with his Greenland Ice Mapping Project Digital Elevation Model, which offers 30-metre resolution over the entire Greenland surface.
Then his colleagues were able to use that data to boost the resolution of their numerical model and get a better idea of where and how the ice caps and glaciers were losing mass.
They found that, for the last 20 years, mass loss has been exactly equal to the amount of meltwater runoff lost to sea.
Simulations showed that a frozen firn was the most likely cause.
The Greenland Ice Sheet is subject to the same danger, Howat said, but to a much lesser degree than the isolated bits of ice on its edges.
The real value of the study is that provides "more evidence of rapid change and how it happens," he added.
The study was published in the journal Nature Communications.
(This article has not been edited by DNA's editorial team and is auto-generated from an agency feed.)
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