Centuries of intense surface melt on Larsen C Ice Shelf

Bevan, Suzanne L.; Luckman, Adrian; Hubbard, Bryn; Kulessa, Bernd; Ashmore, David; Kuipers Munneke, Peter; O'Leary, Martin; Booth, Adam; Sevestre, Heidi; McGrath, Daniel

doi:https://doi.org/10.5194/tc-11-2743-2017

Articles | Volume 11, issue 6

https://doi.org/10.5194/tc-11-2743-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/tc-11-2743-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 11, issue 6

Research article

|

05 Dec 2017

Research article |

| 05 Dec 2017

Centuries of intense surface melt on Larsen C Ice Shelf

Suzanne L. Bevan, Adrian Luckman, Bryn Hubbard, Bernd Kulessa, David Ashmore, Peter Kuipers Munneke, Martin O'Leary, Adam Booth, Heidi Sevestre, and Daniel McGrath

Download

Final revised paper (published on 05 Dec 2017)
Preprint (discussion started on 30 May 2017)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

- Printer-friendly version

- Supplement

RC1: 'mapping past melt in space and time', Anonymous Referee #1, 25 Jun 2017
- AC1: 'Author response to Review 1', Suzanne Bevan, 28 Sep 2017
RC2: 'Review of Bevan et al., Centuries of surface melt on Larsen C ice shelf', Elizabeth Thomas, 11 Sep 2017
- AC2: 'Author response to Review 2', Suzanne Bevan, 28 Sep 2017

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Suzanne Bevan on behalf of the Authors (09 Oct 2017) Author's response Manuscript

ED: Publish as is (01 Nov 2017) by G. Hilmar Gudmundsson

Short summary

Five 90 m boreholes drilled into an Antarctic Peninsula ice shelf show units of ice that are denser than expected and must have formed from refrozen surface melt which has been buried and transported downstream. We used surface flow speeds and snow accumulation rates to work out where and when these units formed. Results show that, as well as recent surface melt, a period of strong melt occurred during the 18th century. Surface melt is thought to be a factor in causing recent ice-shelf break-up.