Articles | Volume 9, issue 3
The Cryosphere, 9, 1169–1181, 2015
The Cryosphere, 9, 1169–1181, 2015

Research article 04 Jun 2015

Research article | 04 Jun 2015

Evolution of ice-shelf channels in Antarctic ice shelves

R. Drews


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 Reinhard Drews on behalf of the Authors (11 May 2015)  Author's response    Manuscript
ED: Publish as is (11 May 2015) by Eric Larour
Short summary
Floating ice shelves extend the continental ice of Antarctica seawards and mediate ice-ocean interactions. Many ice shelves are incised with channels where basal melting is enhanced. With data and modeling it is shown how the channel geometry depends on basal melting and along-flow advection (also for channels which are not freely floating), and how channel formation imprints the general flow pattern. This opens up the opportunity to map the channel formation from surface velocities only.