The concentrations of total gaseous mercury (TGM) in air over the southern Baltic Sea and dissolved gaseous mercury (DGM) in the surface seawater were measured during summer and winter. The summer expedition was performed on 02-15 July 1997, and the winter expedition on 02-15 March 1998. Average TGM and DGM values obtained were 1.70 and 17.6 ng m-3 in the summer and 1.39 and 17.4 ng m-3 in the winter, respectively. Based on the TGM and DGM data, surface water saturation and air-water fluxes were calculated. The results indicate that the seawater was supersaturated with gaseous mercury during both seasons, with the highest values occurring in the summer. Flux estimates were made using the thin film gas-exchange model. The average Hg fluxes obtained for the summer and winter measurements were 38 and 20 ng m-2 d-1, respectively. The annual mercury flux from this area was estimated by a combination of the TGM and DGM data with monthly average water temperatures and wind velocities, resulting in an annual flux of 9.5 µg m-2 yr-1. This flux is of the same order of magnitude as the average wet deposition input of mercury in this area. This indicates that reemissions from the water surface need to be considered when making mass-balance estimates of mercury in the Baltic Sea as well as modelling calculations of long-range transboundary transport of mercury in northern Europe.
Medarbetare: John Munthe
Nyckelord: Gaseous mercury, Dissolved gaseous mercury
Författare: Ingvar Wängberg, Stefan Schmolke, Peter Schager, John Munthe, Ralf Ebinghaus, Åke Iverfeldt
Publicerad i: Atmospheric Environment, Vol 35/32, 5477-5483. 2001