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Map of snow and ice with lines.
Photo Credit: NASA
This satellite image shows a portion of a new map of Antarctic’s ice edge. Where ice extends beyond the edge of the continent, the map shows the grounding line, the point where the ice sheet separates from land and begins to float on the ocean. The red line is the new analysis, while the previous best estimate is shown in gray.

Traced from space

New map redefines Antarctic grounding line, a key step in sea-level rise research

An international team of scientists used high-resolution satellite imagery to trace the most accurate map to date of Antarctica’s grounding line — a key step in helping determine how much of the continent’s ice is contributing to sea-level rise.

Researchers connected more than 3.5 million geographic points around the continent to trace a 53,610-kilometer boundary where ice separates from the land.

The map is a product of the Antarctic Surface Accumulation and Ice Discharge (ASAID) project External Non-U.S. government site.

Led by Robert Bindschadler of NASA’s Goddard Space Flight Center External U.S. government site, the researchers used data and images from multiple sources. These included images from the Landsat 7 satellite and the LIMA satellite mosaic of Antarctica External U.S. government site, precise elevation data from ICESat External U.S. government site, and grounding line estimates from earlier studies.

Map of Antarctica
Photo Credit: NASA
Map of Antarctica shows new grounding line.

“This project has been a major achievement to come from the International Polar Year External U.S. government site,” said Bindschadler in a press release from NASA. “This project included young scientists, it was an international effort, and it produced freely available data — all from satellites.”

The data from ASAID will help resolve the mass balance of Antarctica — how much ice is lost to the ocean versus how much snow accumulates in the interior. It’s likely the continent is experiencing a negative mass balance, meaning more ice is flowing into the ocean than accumulating on the continent.

How much ice is making it into the sea has been a tough question to answer. Previously, researchers calculated the speed of outflow from 33 of Antarctica’s outlet glaciers, including 25 of the 30 largest glaciers. But that accounts for just half of what is lost, as outlet glaciers make up only 5 percent of the coastline.

The rest of the coastline might lose ice through icebergs that calve off from outlet glaciers or over land cliffs. Sometimes ice flows gently from glaciers that extend far into the ocean as floating ice shelves or skinnier ice tongues. In other cases, the ice never reaches the ocean at all.

Earlier mapping efforts had included rocky outcrops and sometimes icebergs as part of the ice sheet perimeter, but elevation data and interpretation based on more detailed satellite imagery enabled the researchers to identify the ice perimeter more accurately.

“ASAID doesn’t just show the location of the ice edge; it provides the elevation all along that line. That’s a key step in measuring mass balance because it tells you the ice thickness near the grounding line,” said Ted Scambos of the National Snow and Ice Data Center (NSIDC) External Non-U.S. government site in Boulder, Colo., where the data will be archived.

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Curator: Peter Rejcek, Antarctic Support Contract | NSF Official: Winifred Reuning, Division of Polar Programs