Articles | Volume 11, issue 11
Geosci. Model Dev., 11, 4657–4675, 2018
https://doi.org/10.5194/gmd-11-4657-2018
Geosci. Model Dev., 11, 4657–4675, 2018
https://doi.org/10.5194/gmd-11-4657-2018

Development and technical paper 22 Nov 2018

Development and technical paper | 22 Nov 2018

Application of HadCM3@Bristolv1.0 simulations of paleoclimate as forcing for an ice-sheet model, ANICE2.1: set-up and benchmark experiments

Constantijn J. Berends et al.

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
AR by Tijn Berends on behalf of the Authors (27 Sep 2018)  Author's response    Manuscript
ED: Publish subject to minor revisions (review by editor) (18 Oct 2018) by Steven Phipps
AR by Tijn Berends on behalf of the Authors (23 Oct 2018)  Author's response    Manuscript
ED: Publish as is (08 Nov 2018) by Steven Phipps
Download
Short summary
We have devised a novel way to couple a climate model to an ice-sheet model. Usually, climate models are too slow to simulate more than a few centuries, whereas our new model set-up can simulate a full 120 000-year ice age in about 12 h. This makes it possible to look at the interactions between global climate and ice sheets on long timescales, something which is relevant for both research into past climate and future projections.