Written by Kristen Kusek, Former Communications Director for 新澳门六合彩内幕信息CMS
The Thwaites Glacier in West Antarctica 鈥� about the size of Florida 鈥� has been an elephant in the room for scientists trying to make global sea level rise predictions. This massive ice stream is already in a phase of fast retreat (a 鈥渃ollapse鈥� when viewed on geological timescales) leading to widespread concern about exactly how much, or how fast, it may give up its ice to the ocean. The potential impact of Thwaites鈥� retreat is spine-chilling: a total loss of the glacier and surrounding icy basins could raise sea level from three to ten feet.
led by marine geophysicist Alastair Graham at the 新澳门六合彩内幕信息鈥檚 College of Marine Science (新澳门六合彩内幕信息CMS), adds cause for concern.
For the first time, scientists mapped in high-resolution a critical area of the seafloor in front of the glacier that gives them a window into how fast Thwaites retreated and moved in the past. The stunning imagery shows geologic features that are new to science, and also provides a kind of crystal ball to see into Thwaites鈥� future. In people and ice sheets alike, past behavior is key to understanding future behavior.
A 3D-rendered view of the multibeam bathymetry (seafloor shape) colored by depth, collected by R谩n across a seabed ridge, just in front of Thwaites Ice Shelf. (Credit: Alastair Graham/新澳门六合彩内幕信息).
The team documented more than 160 parallel ridges that were created, like a footprint, as the glacier鈥檚 leading edge retreated and bobbed up and down with the daily tides. 鈥淚t鈥檚 as if you are looking at a tide gauge on the seafloor,鈥� said Graham. 鈥淚t really blows my mind how beautiful the data are.鈥�
Beauty aside, what鈥檚 alarming is that the rate of Thwaites鈥� retreat that scientists have documented more recently are small compared to the fastest rates of change in its past, said Graham.
To understand Thwaites鈥� past retreat, the team analyzed the rib-like formations submerged 700 meters (just under half a mile) beneath the polar ocean and factored in the tidal cycle for the region, as predicted by computer models, to show that one rib must have been formed every single day.
At some point in the last 200 years, over a duration of less than six months, the front of glacier lost contact with a seabed ridge and retreated at a rate of more than 2.1 kilometers per year (1.3 miles per year) -- twice the rate documented using satellites between 2011 and 2019.
鈥淥ur results suggest that pulses of very rapid retreat have occurred at Thwaites Glacier in the last two centuries, and possibly as recently as the mid-20th Century,鈥� said Graham.
鈥淭hwaites is really holding on today by its fingernails, and we should expect to see big changes over small timescales in the future 鈥� even from one year to the next 鈥� once the glacier retreats beyond a shallow ridge in its bed,鈥� said marine geophysicist and study co-author, Robert Larter, from the British Antarctic Survey.
THOR scientists Alastair Graham (right) and Robert Larter (left) look on in awe at the crumbling ice face of the Thwaites Glacier margin, from the bridge deck of the R/V Nathaniel B. Palmer. (Credit: Frank Nitsche).
To collect the imagery and supporting geophysical data, the team, which included scientists from the United States, the United Kingdom, and Sweden, launched a state-of-the-art orange robotic vehicle loaded with imaging sensors called 鈥楻谩n鈥� from the R/V Nathaniel B. Palmer during an expedition in 2019. R谩n, operated by scientists at the University of Gothenburg in Sweden, embarked on a 20-hour mission that was as risky as it was serendipitous, Graham said. It mapped an area of the seabed in front of the glacier about the size of Houston 鈥� and did so in extreme conditions during an unusual summer notable for its lack of sea ice. This allowed scientists to access the glacier front for the first time in history.
Anna W氓hlin, a physical oceanographer from the University of Gothenburg who deployed R谩n at Thwaites, said, 鈥淭his was a pioneering study of the ocean floor, made possible by recent technological advancements in autonomous ocean mapping and a bold decision by the Wallenberg foundation to invest into this research infrastructure. The images Ran collected give us vital insights into the processes happening at the critical junction between the glacier and the ocean today.鈥�
R谩n, a Kongsberg HUGIN autonomous underwater vehicle, amongst sea ice in front of Thwaites Glacier, after a 20-hour mission mapping the seafloor. (Credit: Anna W氓hlin/University of Gothenburg).
鈥淚t was truly a once in a lifetime mission,鈥� said Graham, who said the team would like to sample the seabed sediments directly so they can more accurately date the ridge-like features. 鈥淏ut the ice closed in on us pretty quickly and we had to leave before we could do that on this expedition,鈥� he said.
While many questions remain, one thing鈥檚 for sure: It used to be that scientists thought of the Antarctic ice sheets as sluggish and slow to respond, but that鈥檚 simply not true, said Graham.
鈥淛ust a small kick to Thwaites could lead to a big response,鈥� he said.
Map of Thwaites Glacier shown in Landsat 8 satellite imagery collected in February 2019. The track of the mission of the autonomous underwater vehicle is shown in orange. Changes in grounding line positions of Thwaites Glacier in the recent past shown by colored lines. (Credit: Alastair Graham/新澳门六合彩内幕信息).
According to the United Nations, roughly 40 percent of the human population lives within 60 miles of the coast. 鈥淭his study is part of a cross-disciplinary collective effort to understand the Thwaites Glacier system better,鈥� said Tom Frazer, dean of the 新澳门六合彩内幕信息CMS, 鈥渁nd just because it鈥檚 out of sight, we can鈥檛 have Thwaites out of mind. This study is an important step forward in providing essential information to inform global planning efforts.鈥�
The study was supported by the National Science Foundation and the UK Natural Environment Research Council through the International Thwaites Glacier Collaboration (ITGC). The 2019 expedition was the first in a 5-year project dubbed THOR, which stands for Thwaites Offshore Research, and also included team members from a sister project called the Thwaites-Amundsen Regional Survey and Network Integrating Atmosphere-Ice-Ocean Processes, or TARSAN.
For more information, authored by Graham and the team.
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View more imagery from this historic expedition below.