Articles | Volume 9, issue 2
https://doi.org/10.5194/gmd-9-647-2016
https://doi.org/10.5194/gmd-9-647-2016
Model description paper
 | 
17 Feb 2016
Model description paper |  | 17 Feb 2016

Glacial–interglacial changes in H218O, HDO and deuterium excess – results from the fully coupled ECHAM5/MPI-OM Earth system model

M. Werner, B. Haese, X. Xu, X. Zhang, M. Butzin, and G. Lohmann

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 Martin Werner on behalf of the Authors (22 Dec 2015)  Author's response   Manuscript 
ED: Publish as is (15 Jan 2016) by Didier Roche
AR by Martin Werner on behalf of the Authors (25 Jan 2016)
Download
Short summary
This paper presents the first results of a new isotope-enabled GCM set-up, based on the ECHAM5/MPI-OM fully coupled atmosphere-ocean model. Results of two equilibrium simulations under pre-industrial and Last Glacial Maximum conditions reveal a good to very good agreement with many delta O-18 and delta D observational records, and a remarkable improvement for the modelling of the deuterium excess signal in Antarctic ice cores.