Articles | Volume 14, issue 6
Research article
30 Jun 2020
Research article |  | 30 Jun 2020

Large-scale englacial folding and deep-ice stratigraphy within the West Antarctic Ice Sheet

Neil Ross, Hugh Corr, and Martin Siegert


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to revisions (further review by editor and referees) (05 Feb 2020) by Joseph MacGregor
AR by Svenja Lange on behalf of the Authors (14 May 2020)  Author's response
ED: Publish as is (18 May 2020) by Joseph MacGregor
Short summary
Using airborne ice-penetrating radar we investigated the physical properties and structure of the West Antarctic Ice Sheet. Ice deep beneath the Institute Ice Stream has prominent layers with physical properties distinct from those around them and which are heavily folded like geological layers. In turn, these folds influence the present-day flow of the ice sheet, with implications for how computer models are used to simulate ice sheet flow and behaviour in a warming world.