Articles | Volume 15, issue 1
The Cryosphere, 15, 113–132, 2021
The Cryosphere, 15, 113–132, 2021

Research article 07 Jan 2021

Research article | 07 Jan 2021

Drivers of Pine Island Glacier speed-up between 1996 and 2016

Jan De Rydt et al.


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to revisions (further review by editor and referees) (31 Oct 2020) by Andreas Vieli
AR by Jan De Rydt on behalf of the Authors (11 Nov 2020)  Author's response    Manuscript
ED: Publish as is (22 Nov 2020) by Andreas Vieli
Short summary
We used satellite observations and numerical simulations of Pine Island Glacier, West Antarctica, between 1996 and 2016 to show that the recent increase in its flow speed can only be reproduced by computer models if stringent assumptions are made about the material properties of the ice and its underlying bed. These assumptions are not commonly adopted in ice flow modelling, and our results therefore have implications for future simulations of Antarctic ice flow and sea level projections.