Fracture propagation to the base of the Greenland ice sheet during supraglacial lake drainage

Surface meltwater that reaches the base of an ice sheet creates a mechanism for the rapid response of ice flow to climate change. The process whereby such a pathway is created through thick, cold ice has not, however, been previously observed. We describe the rapid (<2 hours) drainage of a large...

Full description

Bibliographic Details
Published in:Science
Main Authors: Das, SB, Joughin, I, Behn, MD, Howat, IM, King, MA, Lizarralde, D, Bhatia, MP
Format: Article in Journal/Newspaper
Language:English
Published: Amer Assoc Advancement Science 2008
Subjects:
Earth Sciences
Physical Geography and Environmental Geoscience
Physical Geography and Environmental Geoscience not elsewhere classified
Greenland
Ice Sheet
Online Access:https://doi.org/10.1126/science.1153360
http://ecite.utas.edu.au/81951
Description
Summary:Surface meltwater that reaches the base of an ice sheet creates a mechanism for the rapid response of ice flow to climate change. The process whereby such a pathway is created through thick, cold ice has not, however, been previously observed. We describe the rapid (<2 hours) drainage of a large supraglacial lake down 980 meters through to the bed of the Greenland Ice Sheet initiated by water-driven fracture propagation evolving into moulin flow. Drainage coincided with increased seismicity, transient acceleration, ice-sheet uplift, and horizontal displacement. Subsidence and deceleration occurred over the subsequent 24 hours. The short-lived dynamic response suggests that an efficient drainage system dispersed the meltwater subglacially. The integrated effect of multiple lake drainages could explain the observed net regional summer ice speedup.

Similar Items