Articles | Volume 9, issue 11
https://doi.org/10.5194/gmd-9-3859-2016
https://doi.org/10.5194/gmd-9-3859-2016
Methods for assessment of models
 | 
01 Nov 2016
Methods for assessment of models |  | 01 Nov 2016

Transient simulations of the present and the last interglacial climate using the Community Climate System Model version 3: effects of orbital acceleration

Vidya Varma, Matthias Prange, and Michael Schulz

Viewed

Total article views: 3,778 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,378 1,271 129 3,778 167 165
  • HTML: 2,378
  • PDF: 1,271
  • XML: 129
  • Total: 3,778
  • BibTeX: 167
  • EndNote: 165
Views and downloads (calculated since 21 Jul 2015)
Cumulative views and downloads (calculated since 21 Jul 2015)

Cited

Latest update: 26 Apr 2024
Download
Short summary
We compare the results from simulations of the present and the last interglacial, with and without acceleration of the orbital forcing, using a comprehensive coupled climate model. In low latitudes, the simulation of long-term variations in interglacial surface climate is not significantly affected by the use of the acceleration technique and hence model–data comparison of surface variables is therefore not hampered but major repercussions of the orbital forcing are obvious below thermocline.