SciCombinator

Discover the most talked about and latest scientific content & concepts.

P Christoffersen, M Bougamont, A Hubbard, SH Doyle, S Grigsby and R Pettersson
Abstract
Supraglacial lakes on the Greenland Ice Sheet are expanding inland, but the impact on ice flow is equivocal because interior surface conditions may preclude the transfer of surface water to the bed. Here we use a well-constrained 3D model to demonstrate that supraglacial lakes in Greenland drain when tensile-stress perturbations propagate fractures in areas where fractures are normally absent or closed. These melt-induced perturbations escalate when lakes as far as 80‚ÄČkm apart form expansive networks and drain in rapid succession. The result is a tensile shock that establishes new surface-to-bed hydraulic pathways in areas where crevasses transiently open. We show evidence for open crevasses 135‚ÄČkm inland from the ice margin, which is much farther inland than previously considered possible. We hypothesise that inland expansion of lakes will deliver water and heat to isolated regions of the ice sheet’s interior where the impact on ice flow is potentially large.
Tweets*
212
Facebook likes*
1
Reddit*
0
News coverage*
27
Blogs*
4
SC clicks
0
Concepts
Glaciology, Water, Drainage, Fracture mechanics, Ice sheet, Lake, Greenland ice sheet, Glacier
MeSH headings
-
comments powered by Disqus

* Data courtesy of Altmetric.com