Systematic study of the impact of fresh water fluxes on the glacial carbon cycle
During glacial periods, atmospheric CO<sub>2</sub> concentration increases and decreases by around 15 ppm. At the same time, the climate changes gradually in Antarctica. Such climate changes can be simulated in models when the AMOC (Atlantic Meridional Oceanic Circulation...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2012-03-01
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| Series: | Climate of the Past |
| Online Access: | http://www.clim-past.net/8/589/2012/cp-8-589-2012.pdf |