Articles | Volume 11, issue 1
https://doi.org/10.5194/tc-11-381-2017
https://doi.org/10.5194/tc-11-381-2017
Research article
 | 
02 Feb 2017
Research article |  | 02 Feb 2017

Antarctic subglacial lakes drain through sediment-floored canals: theory and model testing on real and idealized domains

Sasha P. Carter, Helen A. Fricker, and Matthew R. Siegfried

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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 Sasha Carter on behalf of the Authors (03 Aug 2016)  Author's response   Manuscript 
ED: Publish subject to minor revisions (Editor review) (07 Oct 2016) by Robert Bingham
AR by Sasha Carter on behalf of the Authors (18 Oct 2016)  Author's response   Manuscript 
ED: Publish as is (26 Oct 2016) by Robert Bingham
AR by Sasha Carter on behalf of the Authors (02 Nov 2016)
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Short summary
We use a new process-scale model for the drainage of active subglacial lakes in Antarctica that considers channel incision into the soft sedimentary bed. Compared to models with ice-incised channels, our model better reproduces magnitudes and recurrence intervals of active subglacial lake fill–drain cycles derived from satellite altimetry observations.