Ocean Sci., 16, 767–780, 2020 https://doi.org/10.5194/os-16-767-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Ventilation of the northern Baltic Sea Thomas Neumann1, Herbert Siegel1, Matthias Moros1, Monika Gerth1, Madline Kniebusch1, and Daniel Heydebreck1,ė 1Leibniz Institute for Baltic Sea Research Warnemünde, Rostock 18119 Warnemünde Seestr. 15, Germany ėpreviously published under the name Daniel Neumann Correspondence: Thomas Neumann (
[email protected]) Received: 9 May 2019 – Discussion started: 17 July 2019 Revised: 14 May 2020 – Accepted: 19 May 2020 – Published: 3 July 2020 Abstract. The Baltic Sea is a semi-enclosed, brackish wa- Matthäus, 2008), and as a result, the surface salinity ranges ter sea in northern Europe. The deep basins of the central from 14 gkg−1 (south) to 2.5 gkg−1 (north). Due to its hy- Baltic Sea regularly show hypoxic conditions. In contrast, the drographic conditions, an estuarine-like circulation is estab- northern parts of the Baltic Sea, the Bothnian Sea and Both- lished and a strong and permanent vertical density stratifica- nian Bay, are well oxygenated. Lateral inflows or a ventila- tion occurs. These hydrographic conditions set the prerequi- tion due to convection are possible mechanisms for high oxy- sites for vulnerability to hypoxia and anoxia below the pyc- gen concentrations in the deep water of the northern Baltic nocline. In general, a ventilation is only possible by lateral Sea. intrusions of oxygenated water of a sufficiently high den- In March 2017, conductivity–temperature–depth (CTD) sity which allows this water to enter depths below the pyc- profiles and bottle samples, ice core samples, and brine were nocline.