Study finds Antarctica’s glacial border migrates for miles with the tide

The grounding line of the southern Ronne Ice Shelf in Antarctica can shift up to 15 km with changing tides, new analysis shows. The research, published today in The Cryosphere, examines the key region where land-based Antarctic ice spills over into the surrounding ocean. Observing and understanding the dynamics of this region can help scientists predict Antarctica’s response to climate change, and so how much global sea levels will rise.

“We typically think of ice sheet change as being very slow, taking place over decades, centuries or even millennia. But our findings highlight that there are some processes operating over minutes to hours that may have significant impacts,” says Bryony Freer, lead author and glaciologist at the British Antarctic Survey and the Centre for Satellite Data in Environmental Science at the University of Leeds.

The location of Antarctica’s grounding line—the boundary between the land-based section of the ice sheet and the floating ice shelf—helps control ice stability. During a rising tide, extra buoyancy lifts more of the ice shelf off the seabed and the grounding line temporarily moves inland. It returns to its seaward position at low tide.

Earlier measurements of such grounding line movement were restricted to small regions over short timescales. In the new study, the researchers monitored a large chunk of the Ronne Ice Shelf grounding line (220 km) for nearly five years.

Using lasers bounced off the ice from the orbiting satellite ICESat-2, the team could measure to within a few centimeters the height of the ice surface and how it rose and sank with daily tides. They used this information to calculate the changing position of the grounding line.

The 15 km shift in the grounding line position between high and low tide described in the new paper is the one of the largest observed anywhere in Antarctica. It shows the grounding line can move at more than 30 km per hour, flushing ocean water several kilometers further inland under the ice sheet.

This exposure to sea water could help the ice melt more quickly from below. In less stable Antarctic regions, such as the Thwaites Glacier, this process is known to have driven long-term historic grounding line retreat.

Grounding line movement depends on the tidal range, the shape of the seafloor and the strength of the ice. The new study found the grounding line in some regions moved inland much faster during a rising tide than it later returned as the tide dropped—a particularly exciting finding, according to the researchers. This is because it suggests that sea water may become trapped under the ice as the grounding line readvances and so takes longer to be flushed out, perhaps increasing the rate at which the ice sheet melts from below.

“It’s vital that we improve both our observations and modeling of these tidal processes, to better understand how they operate and work out the likely implications for long-term ice sheet change,” Freer says.

The researchers recommend that any future satellite-derived measurements of grounding line position should be timestamped to the nearest hour, along with tide height and phase. They also want to repeat the analysis across more of Antarctica.

Helen Amanda Fricker, ICESat-2 Science Team Leader and Professor at the Scripps Institution of Oceanography in California, and paper co-author, says, “This work showcases how the unprecedented sampling in both space and time of ICESat-2 can reveal new information about dynamic features on ice shelves. It is critical that we continue these measurements with future missions.”