Diverse landscapes beneath Pine Island Glacier influence ice flow

Bingham, Robert G.; Vaughan, David G.; King, Edward C.; Davies, Damon; Cornford, Stephen L.; Smith, Andrew M.; Arthern, Robert J.; Brisbourne, Alex M.; De Rydt, Jan; Graham, Alastair G. C.; Spagnolo, Matteo; Marsh, Oliver J.; Shean, David E.. 2017 Diverse landscapes beneath Pine Island Glacier influence ice flow. Nature Communications, 8 (1), 1618. 9, pp.

Before downloading, please read NORA policies.
Bingham.pdf - Published Version
Available under License Creative Commons Attribution 4.0.

Download (4MB) | Preview


The retreating Pine Island Glacier (PIG), West Antarctica, presently contributes ~5–10% of global sea-level rise. PIG’s retreat rate has increased in recent decades with associated thinning migrating upstream into tributaries feeding the main glacier trunk. To project future change requires modelling that includes robust parameterisation of basal traction, the resistance to ice flow at the bed. However, most ice-sheet models estimate basal traction from satellite-derived surface velocity, without a priori knowledge of the key processes from which it is derived, namely friction at the ice-bed interface and form drag, and the resistance to ice flow that arises as ice deforms to negotiate bed topography. Here, we present high-resolution maps, acquired using ice-penetrating radar, of the bed topography across parts of PIG. Contrary to lower-resolution data currently used for ice-sheet models, these data show a contrasting topography across the ice-bed interface. We show that these diverse subglacial landscapes have an impact on ice flow, and present a challenge for modelling ice-sheet evolution and projecting global sea-level rise from ice-sheet loss.

Item Type: Publication - Article
Digital Object Identifier (DOI):
ISSN: 2041-1723
Date made live: 23 Nov 2017 12:23 +0 (UTC)

Actions (login required)

View Item View Item

Document Downloads

Downloads for past 30 days

Downloads per month over past year

More statistics for this item...