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...
Published in: | Global Biogeochemical Cycles |
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Main Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2002
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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 |