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

Viewed

Total article views: 6,057 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,979 2,839 239 6,057 230 243
  • HTML: 2,979
  • PDF: 2,839
  • XML: 239
  • Total: 6,057
  • BibTeX: 230
  • EndNote: 243
Views and downloads (calculated since 16 Oct 2015)
Cumulative views and downloads (calculated since 16 Oct 2015)

Cited

Saved (preprint)

Latest update: 25 Dec 2024
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.