Earth Syst. Dynam., 8, 1107–1120, 2017 https://doi.org/10.5194/esd-8-1107-2017 © Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License. Structure and functioning of the acid–base system in the Baltic Sea Karol Kulinski´ 1, Bernd Schneider2, Beata Szymczycha1, and Marcin Stokowski1 1Institute of Oceanology, Polish Academy of Sciences, IO PAN, ul. Powstanców´ Warszawy 55, 81-712 Sopot, Poland 2Leibniz Institute for Baltic Sea Research Warnemünde, IOW, Seestrasse 15, 18119 Rostock, Germany Correspondence: Karol Kulinski´ (
[email protected]) Received: 6 April 2017 – Discussion started: 12 April 2017 Revised: 21 October 2017 – Accepted: 6 November 2017 – Published: 11 December 2017 Abstract. The marine acid–base system is relatively well understood for oceanic waters. Its structure and func- tioning is less obvious for the coastal and shelf seas due to a number of regionally specific anomalies. In this review article we collect and integrate existing knowledge of the acid–base system in the Baltic Sea. Hydro- graphical and biogeochemical characteristics of the Baltic Sea, as manifested in horizontal and vertical salinity gradients, permanent stratification of the water column, eutrophication, high organic-matter concentrations and high anthropogenic pressure, make the acid–base system complex. In this study, we summarize the general knowledge of the marine acid–base system as well as describe the peculiarities identified and reported for the Baltic Sea specifically. In this context we discuss issues such as dissociation constants in brackish water, differ- ent chemical alkalinity models including contributions by organic acid–base systems, long-term changes in total alkalinity, anomalies of borate alkalinity, and the acid–base effects of biomass production and mineralization.