Public Release: 

Ice sheets may melt rapidly in response to distant volcanoes

Study of ancient eruptions shows modern ice sheets could be vulnerable

The Earth Institute at Columbia University


IMAGE: Sediments deposited by ice sheet meltwater provide clues about ancient climates, as well as the future effects of global warming. view more 

Credit: Francesco Muschitiello

Volcanic eruptions have been known to cool the global climate, but they can also exacerbate the melting of ice sheets, according to a paper published today in Nature Communications.

Researchers who analyzed ice cores and meltwater deposits found that ancient eruptions caused immediate and significant melting of the ice sheet that covered much of northern Europe at the end of the last ice age, some 12,000 to 13,000 years ago.

"Over a time span of 1,000 years, we found that volcanic eruptions generally correspond with enhanced ice sheet melting within a year or so," says lead author Francesco Muschitiello, who completed the research as a postdoctoral fellow at Columbia University's Lamont-Doherty Earth Observatory.

These weren't volcanoes erupting on or near the ice sheet, but located a thousand miles away in some cases. The eruptions heaved huge clouds of ash into the sky, and when the ash fell on the ice sheet, its darker color made the ice absorb more solar heat than usual.

"We know that if you have darker ice, you decrease the reflectance and it melts more quickly. It's basic science," says Muschitiello. "But no one so far has been able to demonstrate this direct link between volcanism and ice melting when it comes to ancient climates."

The discovery comes from the cross-sections of deposits, called glacial varves, most of which had been collected in the 1980s and 1990s. Varves are the layered sediments that form when meltwater below an ice sheet routes large amounts of debris into lakes near the sheet's edge. Like the rings of a tree, the layers of a glacial varve tell the story of each year's conditions; a thicker layer indicates more melting, since there would have been a higher volume of water to carry the sediment.

The team also compared the varves to cores from the Greenland ice sheet, whose layers contain a record of ancient atmospheric conditions. Testing of those layers for sulfates revealed which years experienced explosive volcanic eruptions, which tend to release large amounts of ash. Matching up the ice layers with varve layers from the same time periods, the team found that years with explosive volcanic activity corresponded to thicker varve layers, indicating more melting of the northern European ice sheet.

Muschitiello and his colleagues studied a period ranging from 13,200 to 12,000 years ago, when the last ice age was transitioning into today's warm climate. They focused specifically on volcanic eruptions in the northern high latitudes--events similar to the 2010 eruptions of Iceland's Eyjafjallajökull volcano. Although that eruption was relatively minor, its large ash cloud shut down air traffic across most of Europe for about a week.

How much melting could an eruption like that cause? "It's difficult to put an exact number to it," says glaciologist and coauthor James Lea from the University of Liverpool. "It depends on many factors." Running thousands of model simulations, the team found that the amount of melting depends on the individual eruption, which season it occurs in, the snowpack conditions at the time, and the elevation of the ice sheet. "Change any one of these and you would get different amounts of melt," says Lea. In the worst scenarios, the model predicted that ash deposition would remove between 20 centimeters and almost one meter of ice from the surface of the highest parts of the ice sheet.

The model results should be taken with a pinch of salt, Muschitiello cautions, due to uncertainties about past conditions. However, because the team simulated a very broad range of potential conditions, he's confident that the ice sheet's real response lies somewhere within their range.

Michael Sigl, a paleoclimatologist from the Paul Scherrer Institute in Switzerland who wasn't involved in the new study, says the hypothesis that ash particles might counteract the cooling effects of volcanic eruptions is intriguing. But, he said, "coincidences in the timing of rapid ice-sheet melting events and eruption dates do not automatically imply causation, and there may be other scenarios that could be consistent with the presented data." Sigl's own work has found a link between eruption-induced ozone depletion and deglaciation in the Southern Hemisphere. Nevertheless, he says, the new study shows that more work is needed to understand the effects of aerosol emissions from volcanic eruptions.

The preliminary results suggest that "present day ice sheets are potentially very vulnerable to volcanic eruptions," says Muschitiello. They also point to a possible hole in the climate models that scientists use to make predictions about the future: Models currently don't simulate the ice sheets' response to changes in particulate deposition from the atmosphere in an interactive way.

Another intriguing implication is that previous research has suggested that melting ice sheets and glaciers could increase the frequency of volcanic eruptions in glaciated areas by lightening loads on earth's crust, allowing underlying magma to rise. If the link between volcanism and ice sheet melting is confirmed, it could indicate the presence of a so-called "positive feedback loop" in which eruptions exacerbate melting, and more melting causes more eruptions, and so on.

Muschitiello says the study "can give us hints about the mechanisms at play when you're expecting rapid climate change."


Muschitiello is now a research scientist at Uni Research and the Bjerknes Centre for Climate Research in Bergen, Norway. Other authors of the paper are Francesco Pausata at the University of Quebec in Montreal, Douglas Mair from the University of Liverpool, and Barbara Wohlfarth from Stockholm University.

The paper, "Enhanced ice sheet melting driven by volcanic eruptions during the last deglaciation," is available from the authors or After it is published, it will appear online at

Scientist contacts:

Francesco Muschitiello

Lamont-Doherty Earth Observatory is Columbia University's home for Earth science research. Its scientists develop fundamental knowledge about the origin, evolution and future of the natural world, from the planet's deepest interior to the outer reaches of its atmosphere, on every continent and in every ocean, providing a rational basis for the difficult choices facing humanity. | @LamontEarth

The Earth Institute, Columbia University mobilizes the sciences, education and public policy to achieve a sustainable earth.

Disclaimer: AAAS and EurekAlert! are not responsible for the accuracy of news releases posted to EurekAlert! by contributing institutions or for the use of any information through the EurekAlert system.