Articles | Volume 14, issue 3
https://doi.org/10.5194/tc-14-985-2020
https://doi.org/10.5194/tc-14-985-2020
Research article
 | 
16 Mar 2020
Research article |  | 16 Mar 2020

Twenty-first century ocean forcing of the Greenland ice sheet for modelling of sea level contribution

Donald A. Slater, Denis Felikson, Fiamma Straneo, Heiko Goelzer, Christopher M. Little, Mathieu Morlighem, Xavier Fettweis, and Sophie Nowicki

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (20 Jan 2020) by Robin Smith
AR by Donald Slater on behalf of the Authors (24 Jan 2020)  Author's response   Manuscript 
ED: Publish as is (31 Jan 2020) by Robin Smith
AR by Donald Slater on behalf of the Authors (31 Jan 2020)  Manuscript 
Download
Short summary
Changes in the ocean around Greenland play an important role in determining how much the ice sheet will contribute to global sea level over the coming century. However, capturing these links in models is very challenging. This paper presents a strategy enabling an ensemble of ice sheet models to feel the effect of the ocean for the first time and should therefore result in a significant improvement in projections of the Greenland ice sheet's contribution to future sea level change.