From: Editor, ENN
Published October 18, 2012 01:34 PM

Ice Sheets Coming and Going

There are many factors that can speed up or slow down climate caused changes in glaciers and ice sheets. Ice-sheet retreat can halt temporarily even during a long warming phases. A UK team led by Durham University has found that the geometry of channels beneath the ice can be a strong control on ice behavior, temporarily hiding the signals of ice retreat.


The findings, which provide the first simulation of past ice-sheet retreat and collapse over a ten thousand year period in Antarctica, shed new light on what makes ice stable or unstable and will help refine predictions of future ice extent and global sea-level rise, the researchers say.

The results of the new research from Durham University, the University of Sheffield, the University of Cambridge, and British Antarctic Survey are published this week in the journal Nature Geoscience.

Lead author, Dr Stewart Jamieson, a glaciologist at the Department of Geography, Durham University, said: "Our research shows that the physical shape of the channels is a more important factor in controlling ice stability than was previously realized. Channel width can have a major effect on ice flow, and determines how fast retreat, and therefore sea-level rise, can happen."



Marine-based ice streams are the fast flowing arteries of ice sheets, draining approximately 90 per cent of the ice that reaches the sea. They flow through large channels where the ice can move thousands of meters in a year. According to the scientists, the unpredictable nature of ice streams makes forecasting ice-sheet retreat extremely difficult. If ice streams speed up they can cause sea level to rise.

An ice stream is a region of an ice sheet that moves significantly faster than the surrounding ice. Ice streams are a type of glacier. They are significant features of the Antarctic where they account for 10% of the volume of the ice. They are up to 50 km wide, 2 km thick, can stretch for hundreds of kilometers, and account for most of the ice leaving the ice sheet.

The speed of an ice stream can be over 1,000 meters per year, an order of magnitude faster than the surrounding ice. The shear forces at the edge of the ice stream cause deformation and recrystallization of the ice, making it softer, and concentrating the deformation in narrow bands or shear margins. Crevasses form, particularly around the shear margins.

Satellite imagery from the last 20 years has led to advances in our knowledge of ice sheet stability and has shown that many ice streams are getting thinner and retreating because the ocean and climate are warming. The new research shows that ice behavior can successfully be simulated in places where ice streams meet the sea.



For further information see Ice Streams.

Glacier by Pete Bucktrout. image via British Antarctic Survey

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