The Baltic Sea is a semi-closed sea with a large net freshwater supply
and a strong permanent halocline at 60-70 m. Above the halocline the
salinity is low and rather homogeneous, and below the halocline there
is a pronounced vertical stratification. Long time series of the salin
ity in different depth intervals are shown for the three major sub-bas
ins, namely the Baltic proper, the Bothnian Sea and the Bothnian Bay.
These are compared with time series of the freshwater supply (runoff f
rom land), the estimated salt-water inflow and the estimated mixing ra
te. During the last decade, the salinity in the Baltic proper has decr
eased by approximately 1 psu in and below the halocline. Above the hal
ocline the decrease is about 0.4 psu. Over the same period, there was
an increased freshwater supply. How this increase may have diluted the
mixed layer and impeded the input of saltwater from the Kattegat is d
iscussed. It is argued that vertical mixing also has increased, thereb
y altering the vertical distribution of salt within the Baltic Sea. Co
pyright (C) 1996 Elsevier Science Ltd.