Influence of dynamic vegetation on climate change and terrestrial carbon storage in the Last Glacial Maximum
When the climate is reconstructed from paleoevidence, it shows that the Last Glacial Maximum (LGM, ca. 21 000 yr ago) is cold and dry compared to the present-day. Reconstruction also shows that compared to today, the vegetation of the LGM is less active and the distribution of vegetation was drastic...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2013-07-01
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| Series: | Climate of the Past |
| Online Access: | http://www.clim-past.net/9/1571/2013/cp-9-1571-2013.pdf |