Abstract
Variation in seawater pH is just one response to the increased CO2concentration in the atmosphere due to anthropogenic activities. The decrease in pH has a significant effect on the carbonate chemistry of the ocean and causes a decrease in the calcium carbonate saturation state (Ω). Ten years of experimental pH measurements at the ESTOC station show a progressive reduction on pH in the ocean (-0.0017 ± 0.0002 year–1) and its effects on its carbonate chemistry. The calcium carbonate saturation state decreases by 0.018 ± 0.006 unit year–1for calcite and 0.012 ± 0.004 unit year–1for aragonite. The direct consequences of the pH decrease are a decrease in the buffer capacity (-1.99 ± 0.25 µmol kg–1year–1) and an increase in the Revelle factor (0.02 ± 0.002 year–1) of the surface seawater.
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Acknowledgments
This work has been supported by the European Commission, through the MAST III program, the CANIGO project (MAS3-CT96-0060), by the Ministerio de Ciencia y Tecnología, Proyecto FLUCAN (2002-01548) and by the European Project CARBOOCEAN 2005–2009, CN 511176-2. The authors thank all the participants in the ESTOC work during these 10 years, in special Dr. O. Llinás and M.J. Rueda from the ICCM-Gobierno de Canarias in charge of keeping the station work, Dr. E.F. González-Dávila for the statistical data treatment and the SeaS Canarias-Departamento de Biología ULPGC-Viceconsejería de Pesca (G.A.C) by to provide us the AVHRR image in Fig. 5.1. We thank Frank J. Millero for his helpful discussion and comments which improved the manuscript.
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Santana-Casiano, J.M., González-Dávila, M. (2011). pH Decrease and Effects on the Chemistry of Seawater. In: Duarte, P., Santana-Casiano, J. (eds) Oceans and the Atmospheric Carbon Content. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-9821-4_5
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