Quantifying the effect of vegetation dynamics on the climate of the Last Glacial Maximum
The importance of the biogeophysical atmosphere-vegetation feedback in comparison with the radiative effect of lower atmospheric CO<sub>2</sub> concentrations and the presence of ice sheets at the last glacial maximum (LGM) is investigated with the climate system model CLIMBER-2. Equilib...
| Main Authors: | , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2005-01-01
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| Series: | Climate of the Past |
| Online Access: | http://www.clim-past.net/1/1/2005/cp-1-1-2005.pdf |