The influence of the ocean circulation state on ocean carbon storage and CO<sub>2</sub> drawdown potential in an Earth system model
During the four most recent glacial cycles, atmospheric CO<sub>2</sub> during glacial maxima has been lowered by about 90–100 ppm with respect to interglacials. There is widespread consensus that most of this carbon was partitioned in the ocean. It is, however, still debated which pro...
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2018-03-01
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| Series: | Biogeosciences |
| Online Access: | https://www.biogeosciences.net/15/1367/2018/bg-15-1367-2018.pdf |