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The Cryosphere An interactive open-access journal of the European Geosciences Union
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TC | Volume 13, issue 7
The Cryosphere, 13, 1801–1817, 2019
https://doi.org/10.5194/tc-13-1801-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
The Cryosphere, 13, 1801–1817, 2019
https://doi.org/10.5194/tc-13-1801-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 08 Jul 2019

Research article | 08 Jul 2019

Antarctic ice shelf thickness change from multimission lidar mapping

Tyler C. Sutterley et al.

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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 Tyler Sutterley on behalf of the Authors (22 Feb 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (25 Feb 2019) by Kenichi Matsuoka
RR by Laurence Padman (19 Mar 2019)
RR by Anonymous Referee #1 (26 Mar 2019)
ED: Publish subject to minor revisions (review by editor) (06 May 2019) by Kenichi Matsuoka
AR by Tyler Sutterley on behalf of the Authors (22 May 2019)  Author's response    Manuscript
ED: Publish subject to technical corrections (04 Jun 2019) by Kenichi Matsuoka
Publications Copernicus
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Short summary
Most of the Antarctic ice sheet is fringed by ice shelves, floating extensions of ice that help to modulate the flow of the glaciers that float into them. We use airborne laser altimetry data to measure changes in ice thickness of ice shelves around West Antarctica and the Antarctic Peninsula. Each of our target ice shelves is susceptible to short-term changes in ice thickness. The method developed here provides a framework for processing NASA ICESat-2 data over ice shelves.
Most of the Antarctic ice sheet is fringed by ice shelves, floating extensions of ice that help...
Citation