A new bed elevation model for the Weddell Sea  sector of the West Antarctic Ice Sheet

Jeofry, Hafeez; Ross, Neil; Corr, Hugh F. J.; Li, Jilu; Morlighem, Mathieu; Gogineni, Prasad; Siegert, Martin J.

doi:https://doi.org/10.5194/essd-10-711-2018

Articles | Volume 10, issue 2

https://doi.org/10.5194/essd-10-711-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/essd-10-711-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 10, issue 2

Review article

|

09 Apr 2018

Review article |

| 09 Apr 2018

A new bed elevation model for the Weddell Sea sector of the West Antarctic Ice Sheet

Hafeez Jeofry, Neil Ross, Hugh F. J. Corr, Jilu Li, Mathieu Morlighem, Prasad Gogineni, and Martin J. Siegert

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Final revised paper (published on 09 Apr 2018)
Preprint (discussion started on 26 Oct 2017)

Interactive discussion

Status: closed

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

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RC1: 'Reviewer Comments', Anonymous Referee #1, 20 Nov 2017
RC2: 'Review of “A new bed elevation model for the Weddell Sea sector of the West Antarctic Ice Sheet” by H. Jeofry et al.', Anonymous Referee #2, 02 Dec 2017
AC1: 'Response to Reviewers’ comments on manuscript #essd-2017-90', Muhammad Jeofry, 30 Jan 2018

Post-review adjustments

AA: Author's adjustment | EA: Editor approval

AA by Muhammad Jeofry on behalf of the Authors (28 Mar 2018) Author's adjustment Manuscript

EA: Adjustments approved (03 Apr 2018) by Reinhard Drews

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Short summary

Accurately characterizing the complexities of the ice-sheet dynamic specifically close to the grounding line across the Weddell Sea (WS) sector in the ice-sheet models provides challenges to the scientific community. Our main objective is to comprehend these complexities, adding accuracy to the projection of future ice-sheet dynamics. Therefore, we have developed a new bed elevation digital elevation model across the WS sector, which will be of value to ice-sheet modelling experiments.