Sheet, stream, and shelf flow as progressive ice-bed uncoupling:  Byrd Glacier, Antarctica and Jakobshavn Isbrae, Greenland

Hughes, T.; Sargent, A.; Fastook, J.; Purdon, K.; Li, J.; Yan, J.-B.; Gogineni, S.

doi:https://doi.org/10.5194/tc-10-193-2016

Articles | Volume 10, issue 1

https://doi.org/10.5194/tc-10-193-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue:

Interactions between climate change and the Cryosphere: SVALI,...

https://doi.org/10.5194/tc-10-193-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 10, issue 1

Research article

|

21 Jan 2016

Research article |

| 21 Jan 2016

Sheet, stream, and shelf flow as progressive ice-bed uncoupling: Byrd Glacier, Antarctica and Jakobshavn Isbrae, Greenland

T. Hughes, A. Sargent, J. Fastook, K. Purdon, J. Li, J.-B. Yan, and S. Gogineni

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Final revised paper (published on 21 Jan 2016)
Preprint (discussion started on 17 Aug 2015)

Interactive discussion

Status: closed

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

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RC C1516: 'A novel method, but I would have called it "model emulation" instead of "holistic"', Anonymous Referee #1, 31 Aug 2015
- SC C1625: 'Reply to anonymous referee #1 for tc-2015-63.', Terence Hughes, 15 Sep 2015
RC C1617: 'A much improved revision', Anonymous Referee #2, 14 Sep 2015
- AC C1627: 'Reply to comments by anonymous referee #2 on tc-2015-63', Terence Hughes, 15 Sep 2015

Peer-review completion

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

AR by Terence Hughes on behalf of the Authors (16 Nov 2015) Author's response Manuscript

ED: Publish as is (27 Nov 2015) by Frank Pattyn

AR by Terence Hughes on behalf of the Authors (02 Dec 2015)

Short summary

The Antarctic and Greenland ice sheets are drained primarily by fast ice streams that end as ice shelves if they become afloat. Smooth transitions from slow sheet flow to fast stream flow to confined shelf flow are obtained and applied to Byrd Glacier in Antarctica after two upstream subglacial lakes suddenly drained in 2006, and to Jakobshavn Isbrae in Greenland after a confined ice shelf suddenly disintegrated in 2002. Byrd Glacier quickly stabilized, but Jakobshavn Isbrae remains unstable.