Articles | Volume 10, issue 4
https://doi.org/10.5194/tc-10-1883-2016
https://doi.org/10.5194/tc-10-1883-2016
Research article
 | 
25 Aug 2016
Research article |  | 25 Aug 2016

Persistence and variability of ice-stream grounding lines on retrograde bed slopes

Alexander A. Robel, Christian Schoof, and Eli Tziperman

Download

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
AR by Alexander Robel on behalf of the Authors (23 May 2016)  Author's response   Manuscript 
ED: Reconsider after major revisions (13 Jun 2016) by Robert Bingham
AR by Alexander Robel on behalf of the Authors (13 Jun 2016)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (23 Jun 2016) by Robert Bingham
RR by Anonymous Referee #1 (11 Jul 2016)
ED: Publish subject to minor revisions (Editor review) (11 Jul 2016) by Robert Bingham
AR by Alexander Robel on behalf of the Authors (20 Jul 2016)  Author's response   Manuscript 
ED: Publish subject to minor revisions (Editor review) (08 Aug 2016) by Robert Bingham
AR by Alexander Robel on behalf of the Authors (08 Aug 2016)  Author's response   Manuscript 
ED: Publish as is (09 Aug 2016) by Robert Bingham
AR by Alexander Robel on behalf of the Authors (09 Aug 2016)
Download
Short summary
Portions of the Antarctic Ice Sheet edge that rest on upward-sloping beds have the potential to collapse irreversibly and raise global sea level. Using a numerical model, we show that changes in the slipperiness of sediments beneath fast-flowing ice streams can cause them to persist on upward-sloping beds for hundreds to thousands of years before reversing direction. This type of behavior is important to consider as a possibility when interpreting observations of ongoing ice sheet change.