Measuring the location and width of the Antarctic grounding zone using CryoSat-2

Dawson, Geoffrey J.; Bamber, Jonathan L.

doi:https://doi.org/10.5194/tc-14-2071-2020

Articles | Volume 14, issue 6

https://doi.org/10.5194/tc-14-2071-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/tc-14-2071-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 14, issue 6

Research article

|

25 Jun 2020

Research article |

| 25 Jun 2020

Measuring the location and width of the Antarctic grounding zone using CryoSat-2

Geoffrey J. Dawson and Jonathan L. Bamber

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Final revised paper (published on 25 Jun 2020)
Preprint (discussion started on 08 Oct 2019)

Interactive discussion

Status: closed

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

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- Supplement

RC1: 'Review of Antarctic grounding zone characteristics from CryoSat-2 Paper', Anonymous Referee #1, 31 Oct 2019
- AC1: 'Response to reviewers', Geoffrey Dawson, 17 Apr 2020
RC2: 'Review of "Antarctic grounding zone characteristics from CryoSat-2"', Anonymous Referee #2, 26 Nov 2019
- AC2: 'Response to reviewers', Geoffrey Dawson, 17 Apr 2020
RC3: 'Review: Antarctic grounding zone characteristics from CryoSat-2 Geoffrey J. Dawson and Jonathan L. Bamber', Anonymous Referee #3, 04 Jan 2020
- AC3: 'Response to reviewers', Geoffrey Dawson, 17 Apr 2020
RC4: 'Review of TCD manuscript “Antarctic grounding zone characteristics from CryoSat-2” submitted by Dawson and Bamber', Anonymous Referee #4, 23 Mar 2020
- AC4: 'Response to reviewers', Geoffrey Dawson, 17 Apr 2020

Peer-review completion

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

ED: Publish subject to revisions (further review by editor and referees) (14 May 2020) by Kerim Nisancioglu

AR by Geoffrey Dawson on behalf of the Authors (14 May 2020) Author's response Manuscript

ED: Publish subject to technical corrections (15 May 2020) by Kerim Nisancioglu

Short summary

The grounding zone is where grounded ice begins to float and is the boundary at which the ocean has the most significant influence on the inland ice sheet. Here, we present the results of mapping the grounding zone of Antarctic ice shelves from CryoSat-2 radar altimetry. We found good agreement with previous methods that mapped the grounding zone. We also managed to map areas of Support Force Glacier and the Doake Ice Rumples (Filchner–Ronne Ice Shelf), which were previously incompletely mapped.