Glaciology: Greenland's glacial basics
VAW Glaciology Group, ETH Zürich, 8092 Zürich, Switzerland
Abstract
Sliding of the Greenland ice sheet is affected by the production of surface meltwater. A new theory shows that whether the result is a long-term speed-up or slow-down of ice motion depends on the variability in melt input.
*Correspondence e-mail: luethi@vaw.baug.ethz.ch
Link: http://www.nature.com/nature/journal/v468/n7325/full/468776a.html
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