image: The Helheim Glacier is a possible analog for the future behavior of the much larger glaciers on Antarctica. view more
Credit: Knut Christianson
AMHERST, Mass. - The world is currently on track to exceed three degrees Celsius of global warming, and new research led by the University of Massachusetts Amherst's Rob DeConto, co-director of the School of Earth & Sustainability, shows that such a scenario would drastically accelerate the pace of sea-level rise by 2100. If the rate of global warming continues on its current trajectory, we will reach a tipping point by 2060, past which these consequences would be "irreversible on multi-century timescales."
The new paper, published today in Nature, models the impact of several different warming scenarios on the Antarctic Ice Sheet, including the Paris Agreement target of two degrees Celsius of warming, an aspirational 1.5 degree scenario, and our current course which, if not altered, will yield three or more degrees of warming. If the more optimistic 1.5 and 2 degree Paris Agreement temperature targets are achieved, the Antarctic Ice Sheet would contribute between 6 and 11 centimeters of sea level rise by 2100. But if the current course toward 3 degrees is maintained, the model points to a major jump in melting. Unless ambitious action to rein in warming begins by 2060, no human intervention, including geoengineering, would be able to stop 17 to 21 centimeters of sea-level rise from Antarctic ice melt alone by 2100. The implications of exceeding Paris Agreement warming targets become even more stark on longer timescales. Antarctica contributes about 1 meter of sea level rise by 2300 if warming is limited to 2 degrees or less, but reaches globally catastrophic levels of 10 meters or more under a more extreme warming scenario with no mitigation of greenhouse-gas emissions.
DeConto and colleagues' research shows the very architecture of the Antarctic Ice Sheet itself plays a key role in ice loss. Ice flows slowly downhill, and the Antarctic Ice Sheet naturally creeps into the ocean, where it begins to melt. What keeps that ocean-bound ice flowing slowly is a ring of buttressing ice shelves, which float in the ocean but hold back the upstream glacial ice by scraping on shallow sea-floor features. Those buttressing ice shelves act both as dams that keep the sheet from sliding rapidly into the ocean, and as supports that keep the edges of the ice sheet from collapsing.
But as warming increases, the ice shelves thin and become more fragile. Meltwater on their surfaces can deepen crevasses and cause them to disintegrate entirely. This not only lets the ice sheet flow toward the warming ocean more quickly, it allows the exposed edges of the ice sheet to break off or "calve" into the ocean, adding to sea level rises. These processes of melting and ice shelf loss, followed by faster glacial flow and rapid calving are seen on Greenland today, but they haven't become widespread on the colder Antarctic ice sheet -- at least not yet. DeConto points out that "if the world continues to warm, the huge glaciers on Antarctica might begin behaving like their smaller counterparts on Greenland, which would be disastrous in terms of sea level rise." The authors of the study, which was supported by funding from the National Science Foundation and the NASA Sea Level Change Science Team, write that missing Paris Agreement temperature targets and allowing extensive loss of the buttressing ice shelves "represents a possible tipping point in Antarctica's future."
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Contact: Rob DeConto, deconto@geo.umass.edu
Daegan Miller, drmiller@umass.edu
Journal
Nature