Articles | Volume 15, issue 7
https://doi.org/10.5194/tc-15-3443-2021
https://doi.org/10.5194/tc-15-3443-2021
Research article
 | 
23 Jul 2021
Research article |  | 23 Jul 2021

Downhole distributed acoustic seismic profiling at Skytrain Ice Rise, West Antarctica

Alex M. Brisbourne, Michael Kendall, Sofia-Katerina Kufner, Thomas S. Hudson, and Andrew M. Smith

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on tc-2021-1', Anonymous Referee #1, 01 Mar 2021
  • RC2: 'Comment on tc-2021-1', Huw Horgan, 15 Mar 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to revisions (further review by editor and referees) (08 May 2021) by Nanna Bjørnholt Karlsson
AR by Alex Brisbourne on behalf of the Authors (18 May 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to revisions (further review by editor and referees) (20 May 2021) by Nanna Bjørnholt Karlsson
AR by Alex Brisbourne on behalf of the Authors (01 Jun 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (03 Jun 2021) by Nanna Bjørnholt Karlsson
RR by Anonymous Referee #1 (10 Jun 2021)
ED: Publish subject to technical corrections (24 Jun 2021) by Nanna Bjørnholt Karlsson
AR by Alex Brisbourne on behalf of the Authors (28 Jun 2021)  Author's response   Manuscript 
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Short summary
How ice sheets flowed in the past is written into the structure and texture of the ice sheet itself. Measuring this structure and properties of the ice can help us understand the recent behaviour of the ice sheets. We use a relatively new technique, not previously attempted in Antarctica, to measure the seismic vibrations of a fibre optic cable down a borehole. We demonstrate the potential of this technique to unravel past ice flow and see hints of these complex signals from the ice flow itself.