Journal cover Journal topic
The Cryosphere An interactive open-access journal of the European Geosciences Union
The Cryosphere, 11, 451-467, 2017
http://www.the-cryosphere.net/11/451/2017/
doi:10.5194/tc-11-451-2017
© Author(s) 2017. This work is distributed
under the Creative Commons Attribution 3.0 License.
Research article
08 Feb 2017
Connected subglacial lake drainage beneath Thwaites Glacier, West Antarctica
Benjamin E. Smith et al.
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Interactive discussionStatus: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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RC1: 'Referee Comment', Anonymous Referee #1, 05 Sep 2016 Printer-friendly Version 
AC1: 'Authors' reply to referee 1.', Ben Smith, 05 Nov 2016 Printer-friendly Version 
 
RC2: 'Referee comments', Anonymous Referee #2, 30 Sep 2016 Printer-friendly Version 
AC2: 'Authors' response to Referee 2.', Ben Smith, 06 Nov 2016 Printer-friendly Version 
 
EC1: 'editor comment', Jonathan Bamber, 03 Oct 2016 Printer-friendly Version 
Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision
AR by Benjamin Smith on behalf of the Authors (24 Nov 2016)  Author's response  Manuscript
ED: Referee Nomination & Report Request started (01 Dec 2016) by Prof. Jonathan Bamber
ED: Publish as is (03 Jan 2017) by Prof. Jonathan Bamber
Publications Copernicus
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Short summary
In this paper we investigate elevation changes of Thwaites Glacier, West Antarctica, one of the main sources of excess ice discharge into the ocean. We find that in early 2013, four subglacial lakes separated by 100 km drained suddenly, discharging more than 3 km3 of water under the fastest part of the glacier in less than 6 months. Concurrent ice-speed measurements show only minor changes, suggesting that ice dynamics are not strongly sensitive to changes in water flow.
In this paper we investigate elevation changes of Thwaites Glacier, West Antarctica, one of the...
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