The long-term stability of the massive ice sheets of Antarctica, which have the potential to raise sea levels by hundreds of meters, has been called into question with the discovery of fast-moving rivers of water sliding beneath their base.
Scientists analyzing satellite data were astonished to discover the size of the vast lakes and river systems flowing beneath the Antarctic ice sheets, which may lubricate the movement of these glaciers as they flow into the surrounding sea.
A foraging Emperor penguin preens on snow-covered sea ice in Antarctica, in this December 9, 2006 file photo. Lasers beamed from space have detected big sloshing lakes of water underneath Antarctic ice. The discovery raises fresh questions about the speed at which sea levels might rise in a warmer world due to the rate at which parts of the ice sheets slide from the land into the ocean. REUTERS/Deborah Zabarenko
The discovery raises fresh questions about the speed at which sea levels might rise in a warmer world due to the rate at which parts of the ice sheets slide from the land into the ocean, scientists said at the American Association for the Advancement of Science in San Francisco.
"We've found that there are substantial subglacial lakes under ice that's moving a couple of meters per day. It's really ripping along. It's the fast-moving ice that determines how the ice sheet responds to climate change on a short timescale," said Robert Bindschadler, a Nasa scientist at the Goddard Space Flight Centre in Maryland, one of the study's co-authors.
"We aren't yet able to predict what these ice streams are going to do. We're still learning about the controlling processes. Water is critical, because it's essentially the grease on the wheel. But we don't know the details yet," Dr Bindschadler said. "Until now, we've had just a few glimpses into what's going on down there. This is the most complete picture to date about what's going on," he said.
The findings, to be published in the journal Science, came from satellite surveillance of the surface elevation of the ice sheets, which found that they rise or lower depending on the amount of water flowing between the base of the ice sheet and the rock beneath.
The scientists identified many regions of the ice sheet either rose or deflated between 2003 and 2006 as a result of water movements below. Water would be capable of this because it is highly pressurized under the weight of the overlying ice, they said.
Glaciologists have known for some time that water exists under the Antarctic ice sheets - which can be hundreds of meters thick - but they were surprised to find how much water is involved and the speed at which it moves from one subglacial reservoir to another, said Helen Fricker at the Scripps Institution of Oceanography in San Diego.
"We didn't realize that the water under these ice streams was moving in such large quantities, and on such short time scales. We thought these changes took place over years and decades, but we are seeing large changes over months. The detected motions are astonishing in magnitude, dynamic nature and spatial extent," Dr Fricker said.
The West Antarctic ice sheet is the second biggest on the continent, and the rate at which ice flows from it to the Ross ice shelf, and then ultimately into the sea, is critical in assessing the likely impact of climate change on global sea levels.
The study provides evidence that subglacial water is stored in a linked system of reservoirs underneath the ice and can move quickly into and out of those reservoirs. This activity may play a major role in controlling the rate at which ice moves off the continent, Dr Fricker said.
"The links between ice stream activity and the climate are not well understood. To predict how the ice sheets might respond to global warming, this new information is vital as it gives us a more complete picture of what is happening under the ice," she said.
The study was conductedusing the Icesat satellite. It carries a laser altimeter instrument to detect changes as small as 1.5 centimeters in the elevation of the ice sheet's surface, from an orbit of 400 miles above the earth. "From 600 kilometers up in space, we were able to see small portions of the ice sheet rise and sink," Dr Bindschadler said.
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