As they seep and calve into the sea, melting glaciers and ice sheets are raising global water levels at unprecedented rates. To predict and prepare for future sea-level rise, scientists need a better understanding of how fast glaciers melt and what influences their flow.  Now, a study by MIT scientists offers a new picture of glacier flow, based on microscopic deformation in the ice. The results show that a glacier’s flow depends strongly on how microscopic defects move through the ice.

“This study really shows the effect of microscale processes on macroscale behavior,” says Meghana Ranganathan who led the study as a MIT graduate student and is now a NOAA Climate & Global Change Postdoctoral Fellow in the School of Earth and Atmospheric Sciences. “These mechanisms happen at the scale of water molecules and ultimately can affect the stability of the West Antarctic Ice Sheet.” (This also appeared at Mirage News and Phys.org.)