Decomposing oceanic temperature and salinity change using ocean carbon change

As the planet warms due to the accumulation of anthropogenic CO 2 in the atmosphere, the interaction of surface ocean carbonate chemistry and the radiative forcing of atmospheric CO 2 leads to the global ocean sequestering heat and carbon in a ratio that is nearly constant in time. This ratio has be...

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Bibliographic Details
Published in:Ocean Science
Main Authors: Turner, Charles E., Brown, Peter J., Oliver, Kevin I. C., McDonagh, Elaine L.
Format: Text
Language:English
Published: 2022
Subjects:
Online Access:https://doi.org/10.5194/os-18-523-2022
https://os.copernicus.org/articles/18/523/2022/