Carbon cycle, vegetation, and climate dynamics in the Holocene: Experiments with the CLIMBER-2 model

Multiple proxy data reveal that the early to middle Holocene (ca. 8-6 kyr B. P.) was warmer than the preindustrial period in most regions of the Northern Hemisphere. This warming is presumably explained by the higher summer insolation in the Northern Hemisphere, owing to changes in the orbital param...

Full description

Bibliographic Details
Published in:Global Biogeochemical Cycles
Main Authors: Brovkin, V., Bendtsen, J., Claussen, M., Ganopolski, A., Kubatzki, C., Petoukhov, V., Andreev, A.
Format: Article in Journal/Newspaper
Language:English
Published: 2002
Subjects:
Online Access:http://hdl.handle.net/11858/00-001M-0000-0013-A874-1
http://hdl.handle.net/11858/00-001M-0000-0013-A876-E