Articles | Volume 12, issue 4
https://doi.org/10.5194/tc-12-1347-2018
https://doi.org/10.5194/tc-12-1347-2018
Research article
 | 
13 Apr 2018
Research article |  | 13 Apr 2018

Recent dynamic changes on Fleming Glacier after the disintegration of Wordie Ice Shelf, Antarctic Peninsula

Peter Friedl, Thorsten C. Seehaus, Anja Wendt, Matthias H. Braun, and Kathrin Höppner

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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 Peter Friedl on behalf of the Authors (14 Dec 2017)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (22 Dec 2017) by Bert Wouters
RR by Anonymous Referee #1 (08 Jan 2018)
RR by Anonymous Referee #3 (23 Jan 2018)
ED: Reconsider after major revisions (23 Jan 2018) by Bert Wouters
AR by Peter Friedl on behalf of the Authors (22 Feb 2018)  Author's response   Manuscript 
ED: Publish subject to technical corrections (10 Mar 2018) by Bert Wouters
AR by Peter Friedl on behalf of the Authors (13 Mar 2018)  Manuscript 
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Short summary
Fleming Glacier is the biggest tributary glacier of the former Wordie Ice Shelf. Radar satellite data and airborne ice elevation measurements show that the glacier accelerated by ~27 % between 2008–2011 and that ice thinning increased by ~70 %. This was likely a response to a two-phase ungrounding of the glacier tongue between 2008 and 2011, which was mainly triggered by increased basal melt during two strong upwelling events of warm circumpolar deep water.