UMD-led Research Finds Warm Winds Could Strain Antarctic Ice Shelf
Brilliant blue pools of melt water can be seen collecting atop the Larsen C ice shelf on the Antarctic Peninsula in an image created by NASA’s Earth Observatory using Landsat data from the U.S. Geological Survey.
First, Antarctica’s Larsen A ice shelf broke up 1995. Then came the widely publicized 2002 collapse of Larsen B, which lost a Rhode Island-sized expanse. New University of Maryland-led research shows how warm autumn winds contribute to ice shelf surface melt, which could now be threatening Larsen C.
The findings, published yesterday in Geophysical Research Letters, show that the Larsen C ice shelf—the fourth-largest in Antarctica, and bigger than Maryland and Delaware combined at 17,100 square miles—experienced an unusual spike in late summer and early autumn surface melting in the years 2015–17. Its location just south of the former Larsen B on the Antarctic Peninsula, the northernmost part of Earth’s coldest continent, makes it particularly vulnerable to a changing global climate.
The study, spanning 1982 to 2017, quantifies how much of this additional melting can be ascribed to warm, dry air currents called foehn winds that originate high in the peninsula’s central mountain range.
The study further shows that the three-year spike in foehn-induced melting late in the melt season has begun to restructure the snowpack on the Larsen C ice shelf. If this pattern continues, it could significantly alter the density and stability of the Larsen C ice shelf, potentially putting it at further risk to suffer the same fate as the Larsen A and B shelves.
“Three years doesn't make a trend. But it’s definitely unusual that we are seeing enhanced foehn winds and associated melting in late summer and early autumn,” said Rajashree Tri Datta, a faculty assistant at UMD’s Earth System Science Interdisciplinary Center and the lead author of the research paper. “It’s unusual that we’re seeing increased foehn-induced melt in consecutive years—especially so late in the melt season, when the winds are stronger but the temperatures are usually cooling down. This is when we expect melting to end and the surface to be replenished with snow.”
Enhanced surface melting causes water to trickle into the underlying layers of firn—or uncompacted, porous snow—in the upper layers of the ice sheet. This water then refreezes, causing the normally porous, dry firn layers to become denser. Eventually, the firn layers can become too dense for water to enter, leading to a buildup of liquid water atop the ice shelf.
“With enhanced densification, the ice enters the next warm season with a very different structure. Our modeling results show that, with less open space for the surface water to filter into, runoff increases year after year,” said Datta, who also has an appointment at NASA’s Goddard Space Flight Center.
As foehn winds race down the colder eastern slopes of the Antarctic Peninsula’s central mountain range, they can raise air temperatures by as much as 30 degrees Fahrenheit, producing localized bursts of snowmelt. According to Datta, these winds exert their greatest effects at the bases of glacial valleys. Here, where the feet of the glaciers adjoin the Larsen C ice shelf, foehn winds stand to destabilize some of the most fragile and critical structures in the system.
“Because it’s a floating ice shelf, a breakup of Larsen C wouldn’t directly lead to a rise in global mean sea level,” Datta said. “However, the ice shelf does brace against the flow of the glaciers that feed it. So if Larsen C goes, some of these glaciers will be free to accelerate their rate of flow and melt, which will result in a rise in global sea level.”
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