Remote Antarctic Ice Forms From Beneath Glaciers
An international team of scientists working in the most remote parts of Antarctica have discovered that masses of ice form underneath the ice sheet instead of on top, according to a study published Thursday in the journal Science.
Liquid water locked deep under Antarctica’s coat of ice regularly thaws, and then refreezes to the bottom, creating as much as half the thickness of the ice in some places, the researchers said.
“We usually think of ice sheets like cakes — one layer at a time added from the top,” said geophysicist Robin Bell of Columbia University’s Lamont-Doherty Earth Observatory, the study’s co-author.
“This is like someone injected a layer of frosting at the bottom — a really thick layer,” he said.
The findings contradict common perceptions of glacial formation, and could reshape scientists’ understanding of how the ice sheet expands and moves, the researchers said.
Ice sheets are well known to grow from the top as snow falls and accumulates annual layers over thousands of years. However, until recently scientists have known little about the processes going on far below.
In 2006, the researchers found that lakes of liquid water underlie widespread parts of Antarctica. In 2008-2009, they mounted an expedition using geophysical instruments to create 3-D images of the Gamburtsev Mountains, a range larger than the European Alps that lies buried under as much as two miles of ice.
The expedition also made detailed images of the overlying ice and subglacial water.
“Water has always been known to be important to ice sheet dynamics, but mostly as a lubricant,” Bell said.
“As ice sheets change, we want to predict how they will change. Our results show that models must include water beneath.”
The Antarctic ice sheet holds enough fresh water to raise ocean levels 200 feet, and if even a small part of it were to melt it could put major coastal cities under water.
The scientists found that refrozen ice makes up 24% of the ice sheet base around Dome A, a 13,800-foot-high plateau that forms the high point of the East Antarctic ice sheet, which is roughly the size of the continental United States.
In some places, more than half the ice thickness appears to have originated from the bottom, not the top. Here, rates of refreezing are greater than surface accumulation rates.
The researchers suggest that such refreezing has been going on since East Antarctica became encased in a large ice sheet some 32 million years ago.
However, they may never know for sure, since the ice is always moving from the deep interior toward the coast, such that ice formed millions of years ago is long gone. Furthermore, deeply buried ice may melt because overlying layers insulate the base, hemming in heat created there by friction, or radiating naturally from underlying rock.
When the ice melts, refreezing may take place in a number of ways, the researchers said.
If it collects along mountain ridges and heads of valleys, where the ice is thinner, low temperatures penetrating from the surface may refreeze it. In other cases, water gets squeezed up valley walls, and changes pressure rapidly.
In the depths, water remains liquid even when it is below the normal freezing point due to high pressure. However, once moved up to an area of less pressure, such supercooled water can freeze almost instantly.
“When we first saw these structures in the field, we thought they looked like beehives and were worried they were an error in the data,” Bell said.
“As they were seen on many lines, it became clear that they were real. We did not think that water moving through ancient river valleys beneath more than one mile of ice would change the basic structure of the ice sheet.”
Because the ice is in motion, understanding how it forms and deforms at the base is vital to understanding how the sheets will move, the researchers said.
“It’s an extremely important observation for us because this is potentially lifting the very oldest ice off the bed,” said Jeff Severinghaus, a geologist at Scripps Institution of Oceanography in San Diego, who was not involved in the study.
It could either mean older ice is better preserved ““ or, it could “make it harder to interpret the record, if it’s shuffled like a deck of cards,” he said.
From November 2008 to January 2009, the researchers conducted fieldwork around a large part of Dome A. Using aircraft equipped with ice penetrating radars, laser ranging systems, gravity meters and magnetometers, they flew low-altitude transects back and forth over the ice to create 3-D images of what lay beneath.
The goal was to understand how the mountains arose, and to study the connections between the peaks, the ice sheet and subglacial lakes. They were also searching for likely spots where future coring may retrieve the oldest ice.
The work took place near the Southern Pole of Inaccessibility, the point farthest away from any ocean, and much harder to reach than the South Pole itself. They lived in isolated field camps, enduring high winds and temperatures as low as minus 40 degrees Celsius.
“Understanding these interactions is critical for the search for the oldest ice and also to better comprehend subglacial environments and ice sheet dynamics,” said Fausto Ferraccioli, a scientist with the British Antarctic Survey who also helped lead the project.
“Incorporating these processes into models will enable more accurate predictions of ice sheet response to global warming and its impact on future sea-level rise.”
The researchers now will investigate how the refreezing process acts along the margins of ice sheets, where the most visible change is occurring in Antarctica.
Based on their data, a Chinese team also hopes to drill deep into Dome A in the next few years to remove cores that would trace long-ago climate shifts.
They hope to find ice more than a million years old.
The study, part of a six-nation study of the invisible Gamburtsev Mountains, appears in this week’s early online edition of the journal Science. A summary can be viewed at http://www.sciencemag.org/content/early/2011/03/02/science.1200109.abstract.
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