Abstract
Abstract. Interdecadal variability in the salinity of the Baltic Sea is dominated by a 30-year cycle with a peak-to-peak amplitude of around 0.4 g kg−1 at the surface. Such changes may have substantial consequences for the ecosystem, since species are adapted to a suitable salinity range and may experience habitat shifts. It is therefore important to understand the drivers of such changes. We use both analysis of empirical data and a numerical model reconstruction for the period of 1850–2008 to explain these interdecadal changes. The model explains 93 % and 52 % of the variance in the observed interdecadal salinity changes at the surface and the bottom, respectively, at an oceanographic station at Gotland Deep. It is known that the 30-year periodicity coincides with a variability in river runoff. Periods of enhanced runoff are followed by lower salinities. We demonstrate, however, that the drop in mean salinity cannot be understood as a simple dilution of the Baltic Sea water by freshwater. Rather, the 30-year periodicity in river runoff occurs synchronously with a substantial variation in salt water import across Darss Sill. Fewer strong inflow events occur in periods of enhanced river runoff. This reduction in the import of high-salinity water is the main reason for the freshening of the water below the permanent halocline. In the bottom waters, the variation in salinity is larger than at the surface. As a consequence, the surface layer salinity variation is caused by a combination of both effects: a direct dilution by river water and a reduced upward diffusion of salt as a consequence of reduced inflow activity. Our findings suggest that the direct dilution effect is responsible for 27 % of the salinity variations only. It remains unclear whether the covariation in river runoff and inflow activity are only a coincidental correlation during the historical period or whether a mechanistic link exists between the two quantities, e.g. whether both are caused by the same atmospheric patterns.
Highlights
The Baltic Sea is a brackish sea with pronounced salinity gradients, both in the horizontal and in the vertical
We demonstrate that the use of (a) wavelet coherence analyses and (b) a new dataset on barotropic inflow variability suggests that the direct influence of runoff on salinity is limited, while barotropic inflow variability contributes to the interdecadal fluctuations
For the decade 1910–1920, we find wavelet coherence above 0.95 when Atlantic Multidecadal Oscillation (AMO) and bottom salinity are in anti-phase, at a period around 20 years
Summary
The Baltic Sea is a brackish sea with pronounced salinity gradients, both in the horizontal and in the vertical. The brackish salinities in the Baltic Sea are the consequence of (i) a positive freshwater balance due to river runoff and net precipitation, (ii) an import of saline water across the shallow Drogden Sill and Darss Sill, and (iii) mixing processes inside the Baltic Sea. Changes in any of these controlling factors may affect the Baltic Sea salinity. Major ecological consequences may result from this, since the ecosystem of the Baltic Sea is adapted to the brackish salinities and their horizontal gradient. A change in Baltic Sea salinity means a regional shift in this isohaline with corresponding spatial shifts in habitats. Since a freshening of the Baltic Sea is expected in future climate due to enhanced precipitation in the catchment, these
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