The importance of Öresund and the Drogden Sill for Baltic inflow

Based on high resolution current and salinity measurements from the Flinten and Drogden Channels, this paper assesses the relative importance of major Baltic inflows on ‘everydayʹ flow conditions of highly saline water (S>17 PSU) through the Öresund for a period of 43 months. During years with no major Baltic inflows, 1994–1996, it is found that the Öresund on average supplies 1.2 Peta-grams (Pg) of salt net/year to the Baltic, while inflow above 17 PSU is in the order of 2.3 to 4.0 Pg/year. Sixty percent of this inflow is in the salinity range 17–23 PSU; the remainder has a higher salinity. It is, thus, concluded that normal and regularly occurring flow in the Öresund plays a much larger role in supplying salt to the Baltic than is usually assumed.