Irreversible ocean warming threatens the Filchner-Ronne Ice Shelf
How the ocean’s heat is threatening the ice shelves. Credit: Alfred-Wegener-Institut/Martin Kuensting CC-BY 4.0
By the second half of this century, rising air temperatures above the Weddell Sea could set off a self-amplifying meltwater feedback cycle under the Filchner-Ronne Ice Shelf, ultimately causing the second-largest ice shelf in the Antarctic to shrink dramatically. Climate researchers at the Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research (AWI) recently made this prediction in a new study, which can be found in the latest issue of the Journal of Climate, released today. In the study, the researchers use an ice-ocean model created in Bremerhaven to decode the oceanographic and physical processes that could lead to an irreversible inflow of warm water under the ice shelf – a development that has already been observed in the Amundsen Sea.
When it comes to the fate of the great Antarctic ice shelves, the sea ice surrounding them is of central importance. For example, in the southern Weddell Sea so much sea ice forms during the autumn and winter months that the amount of salt released in the process turns the water around and below the 450,000 km2 Filchner-Ronne Ice Shelf into a massive protective sheath. So far, this barrier of extremely salty water, with an average temperature of ca. minus 2 degrees Celsius, has protected the shelf from the inflow of water masses that are 0.8 degrees warm, which the Weddell Gyre transports along the edge of the continental shelf (see graphic).
New simulations from climate researchers at the AWI now indicate that this cold-water barrier could be permanently lost in the course of the next few decades. The reason: rising air temperatures over the Weddell Sea, which could cause less sea ice to form. “We can already see the first signs of this trend today. First of all, less sea ice is forming in the region, and secondly, oceanographic recordings from the continental shelf break confirm that the warm water masses are already moving closer and closer to the ice shelf in pulses,” says Dr Hartmut Hellmer, an oceanographer at the AWI and first author of the study.
These comparatively small-scale changes may mark the beginning of a fundamental and irrevocable transformation in the southern Weddell Sea. The researchers expect the effects to become noticeable by 2070. “Our simulations show that there will be no turning back once the warm water masses find their way under the ice shelf, since their heat will accelerate the melting at its base. In turn, the resulting meltwater will produce an intensified overturning, which will suck even more warm water from the Weddell Gyre under the ice. As such, according to our calculations, the hope that the ocean would someday run out of heat won’t pan out in the long run,” Hellmer explains.
As a result of the dramatic melting on its underside, the shelf’s grounding line will shift further south and the ice will gradually lose direct contact with the seafloor. To date, frictional contact with the seafloor has helped to slow down the ice flow. Once this natural brake is gone, the draining of ice from the Antarctic Ice Sheet will quicken. “The meltwater feedback cycle under the ice shelf will only slow down once the shelf has collapsed, or no more glacial ice flows in from inland to take its place. So we’re talking about processes that will continue over several centuries,” says co-author and AWI model designer Dr Ralph Timmermann.