Articles | Volume 16, issue 4
https://doi.org/10.5194/os-16-847-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/os-16-847-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Current estimates of K1* and K2* appear inconsistent with measured CO2 system parameters in cold oceanic regions
Olivier Sulpis
CORRESPONDING AUTHOR
Department of Earth Sciences, Utrecht University, Utrecht, the
Netherlands
Department of Earth and Planetary Sciences, McGill University,
Montreal, Canada
Siv K. Lauvset
NORCE Norwegian Research Centre, Bjerknes Centre for Climate Research, Bergen, Norway
Mathilde Hagens
Soil Chemistry and Chemical Soil Quality, Wageningen University and
Research, Wageningen, the Netherlands
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- Random and systematic uncertainty in ship‐based seawater carbonate chemistry observations B. Carter et al. 10.1002/lno.12674
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- Recent developments in ionophore-based potentiometric electrochemical sensors for oceanic carbonate detection S. Toala et al. 10.1039/D3SD00232B
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Latest update: 13 Dec 2024
Short summary
As direct measurements of seawater carbonate system variables, such as pH, are difficult to obtain, scientists use equilibrium constants to compute them from known variables. Using a compilation of in situ data, we show that the set of equilibrium constants preferred by the community is not consistent with measurements in cold, polar waters, where human-made ocean acidification is spreading rapidly. Closing knowledge gaps regarding seawater carbon chemistry in polar regions should be a priority.
As direct measurements of seawater carbonate system variables, such as pH, are difficult to...