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August 12, 2013

Studying glacial sliding related to rising sea levels

Researchers at Iowa State University (ISU) use cross-polarized lenses to examine thin, horizontal sections of ice. Here, the black colors tell them when they're looking down an axis of the ice grains and helps them to understand deformation in the ice.

Lucas Zoet, a postdoctoral research associate, and Neal Iverson, a professor of geological and atmospheric sciences, are using the newly constructed ISU sliding simulator, developed with support from the National Science Foundation (NSF), to study glacier sliding.

Data collected by the researchers show that resistance to glacier sliding--the drag that the bed exerts on the ice--can decrease in response to increasing sliding speed. This decrease in drag with increasing speed, although predicted by some theoreticians as long as 45 years ago, is the opposite of what is usually assumed in mathematical models of the flow of ice sheets. These are the first empirical results demonstrating that as ice slides at an increasing speed--perhaps in response to changing weather or climate--the bed can become slipperier, which could promote still faster glacier flow.

Understanding how glaciers slide across their beds could help researchers predict how glaciers will react to climate change, and how this will contribute to rising sea levels.

NSF funded both the construction and operation of the sliding simulator through grants ANT 06-18747 and EAR 10-23586. (Date of Image: 2013)

Credit: Lucas Zoet


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