Abstract
Early measurements of pCO2 in the surface waters of the Baltic Sea clearly pointed to biological production as the major controlling factor underlying the seasonality of the pCO2. However the temporal resolution of the measurements was too low to allow reasonable quantitative conclusions regarding biological production. This problem was overcome in 2003, when a fully automated measurement system that continuously recorded the surface-water pCO2 was deployed on a cargo ship. The ship commuted at regular intervals of 2–3 days between the southwest Baltic Sea (Lübeck) and the western Gulf of Finland (Helsinki) and thus traversed the entire Baltic Proper. Between 2003 and 2015, pCO2 data for 1600 transects were obtained. Investigations of CO2 accumulation in deep water also started in 2003, in conjunction with IOW’s long-term observation program. The measurements were confined to a central station in the eastern Gotland Basin and were made four to five times per year. The vertical resolution of the data with respect to total CO2 and the accompanying variables, such as nutrient and oxygen/H2S concentrations, was 25 m.
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References
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Schneider, B., Müller, J.D. (2018). The Database. In: Biogeochemical Transformations in the Baltic Sea. Springer Oceanography. Springer, Cham. https://doi.org/10.1007/978-3-319-61699-5_4
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DOI: https://doi.org/10.1007/978-3-319-61699-5_4
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