The Holocene climate evolution in the high-latitude Southern Hemisphere simulated by a coupled atmosphere-sea ice-ocean-vegetation model

The Holocene climate is simulated in a 9000-yr-long transient experiment performed with the ECBilt-CLIO-VECODE coupled atmosphere-sea ice-ocean-vegetation model. This experiment is forced with annually varying orbital parameters and atmospheric concentrations of CO

Bibliographic Details
Published in:The Holocene
Main Authors: Goosse, H., Fichefet, T., Masson-Delmotte, V., Koc, N., Renssen, H.
Format: Article in Journal/Newspaper
Language:English
Published: 2005
Subjects:
Online Access:https://research.vu.nl/en/publications/fc12780f-2801-4a2b-b10e-4b17eccee12a
https://doi.org/10.1191/0959683605hl869ra
https://hdl.handle.net/1871.1/fc12780f-2801-4a2b-b10e-4b17eccee12a
Description
Summary:The Holocene climate is simulated in a 9000-yr-long transient experiment performed with the ECBilt-CLIO-VECODE coupled atmosphere-sea ice-ocean-vegetation model. This experiment is forced with annually varying orbital parameters and atmospheric concentrations of CO