Review abstract


Nature Geoscience 1, 297 - 304 (2008)
Published online: 27 April 2008 | doi:10.1038/ngeo186

The role of subglacial water in ice-sheet mass balance

Robin E. Bell1


In the coming decades, significant changes in the polar regions will increase the contribution of ice sheets to global sea-level rise. Under the ice streams and outlet glaciers that deliver ice to the oceans, water and deformable wet sediments lubricate the base, facilitating fast ice flow. The influence of subglacial water on fast ice flow depends on the geometry and capacity of the subglacial hydrologic system: water moving rapidly through a well-connected system of conduits or channels will have little impact on ice-sheet velocities, but water injected into a spatially dispersed subglacial system may reduce the effective pressure at the base of the ice sheet, and thereby trigger increased ice-sheet velocities. In Greenland, the form of the subglacial hydrologic system encountered by increasing surface melt water will determine the influence of changing atmospheric conditions on ice-sheet mass balance. In Antarctica, subglacial lakes have the capacity to both modulate velocities in ice streams and outlet glaciers and provide nucleation points for new fast ice-flow tributaries. Climate models of ice-sheet responses to global change remain incomplete without a parameterization of subglacial hydrodynamics and ice dynamics.

Top
  1. Lamont-Doherty Earth Observatory of Columbia University, 61 Rt. 9W, Palisades, 10964 New York, USA.
    e-mail: robinb@ldeo.columbia.edu


MORE ARTICLES LIKE THIS

These links to content published by NPG are automatically generated.

NEWS AND VIEWS

Cryosphere Fire and ice

Nature Geoscience News and Views (01 Feb 2008)

Glaciology Lubricating lakes

Nature News and Views (22 Feb 2007)

See all 17 matches for News And Views

Extra navigation

Subscribe to Nature Geoscience

Subscribe

natureproducts


ADVERTISEMENT