The Skagerrak and Kattegat form a transition zone between the Baltic a
nd the North Sea. Both areas are subject to increased nutrient loads.
In this paper a non-parametric method is used to calculate the changes
in nutrient and oxygen concentrations in the area. The period chosen
was 1971 to 1990 and the parameters were dissolved inorganic nitrogen,
phosphorus, silicate, total nitrogen and total phosphorus together wi
th oxygen and oxygen saturation. Data have been sorted after salinity
and the analyses have been carried out for different water masses and
subareas. The results demonstrate that both surface and deep water in
the Kattegat show increasing trends during winter for all nutrients ex
cept silicate. During summer there is an increase in total nitrogen an
d total phosphorus while silicate shows a decrease. In the Skagerrak t
he picture is more variable; in the eastern part, however, there is a
clear increase for all inorganic nutrients during winter in the coasta
l water. Oxygen shows a declining trend in most areas.