Global climate and the atmospheric partial pressure of carbon dioxide are correlated over recent glacial cycles, with lower partial pressure of carbon dioxide during ice ages, but the causes of the changes in the partial pressure of carbon dioxide are unknown. Here the authors review the evidence in support of the hypothesis that the Southern Ocean is an important driver of glacial/interglacial changes in the partial pressure of carbon dioxide.
- Daniel M. Sigman
- Mathis P. Hain
- Gerald H. Haug
