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: C. E. Turner, P. J. Brown, K. I. C. Oliver, E. L. McDonagh
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2022
Subjects:
G
Online Access:https://doi.org/10.5194/os-18-523-2022
https://doaj.org/article/7529d0cbc8fb482c86b84fc9f937d039