Partner Series
Satellite Finds Hidden Upside-Down Canyon on Underside of Antarctic Ice
A view of the Dotson ice shelf, courtesy of the ESA satellite Sentinel-1. New research finds an under-ice canyon stretching the length of the shelf.
Credit: Copernicus Sentinel data (2017), processed by A. Hogg/CPOM

A mysterious world of upside-down canyons crisscrosses the underbelly of Antarctica's ice shelves.

Now, research finds that some of these crevasses may contribute to both the thinning of the shelves and sea-level rise. A single canyon in the Dotson ice shelf in West Antarctica is responsible for dumping 4.4 billion short tons (4 billion metric tons) of freshwater into the Southern Ocean, according to Noel Gourmelen, a remote-sensing researcher at The University of Edinburgh. [50 Amazing Facts About Antarctica]

These divots in the underside of the ice shelves are poorly understood, according to the European Space Agency (ESA). To learn more, Gourmelen and his colleagues have been using data from ESA's CryoSat and Copernicus Sentinel-1 satellites to peer into the invisible under-ice world of the Antarctic canyons.

The Dotson ice shelf appears flat from above, but its underside is a rugged landscape of melt.
The Dotson ice shelf appears flat from above, but its underside is a rugged landscape of melt.
Credit: N. Gourmelen

Both of these satellites use radar techniques to gauge ice-shelf thickness and dynamics. The team used the data to investigate the flow of the Dotson ice shelf, a 30-mile-wide (50 kilometers) expanse off the remote coast of Marie Byrd Land.

"We have found subtle changes in both surface elevation data from CryoSat and ice velocity from Sentinel-1, which shows that melting is not uniform, but has centered on a 5-km-wide [3 miles] channel that runs 60 km [37 miles] along the underside of the shelf," Gourmelen said in a statement.

This under-ice canyon is probably formed by relatively warm ocean water — 33.8 degrees Fahrenheit, or 1 degree Celsius — that circulates clockwise and upward due to the planet's rotation, Gourmelen said.

"Revisiting older satellite data, we think that this melt pattern has been taking place for at least the entire 25 years that Earth observation satellites have been recording changes in Antarctica," he said.

In that time, he said, the warm water has created an upside-down canyon in the bottom of the ice shelf that is up to 124 miles (200 km) deep and 9 miles (15 km) wide. The crevasse is deepening by about 22 feet (7 meters) each year, Gourmelen said.

"The strength of an ice shelf depends on how thick it is. Since shelves are already suffering from thinning, these deepening canyons mean that fractures are likely to develop and the grounded ice upstream will flow faster than would be the case otherwise," he said, referring to the land-based ice that is buttressed by the floating ice shelves. This land-based ice has a greater impact on overall sea-level rise because it's not already floating in the ocean. (When floating ice melts, it doesn't directly impact sea levels.)

The next goal, Gourmelen said, is to expand the same line of research to the rest of the ice shelves ringing Antarctica.

Original article on Live Science.