Multiple regimes of air-sea carbon partitioning identified from constant-alkalinity buffer factors
Numerical studies have indicated that the steady-state ocean-atmosphere partitioning of carbon will change profoundly as emissions continue. In particular, the globally averaged Revelle buffer factor will first increase and then decrease at higher emissions. Furthermore, atmospheric carbon will init...
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| Aineistotyyppi: | Artikkeli |
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American Geophysical Union (AGU)
2018
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| Linkit: | http://hdl.handle.net/1721.1/118341 https://orcid.org/0000-0002-3102-0341 |