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

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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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
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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.