The Baltic contrasts with the nearby North Sea, where oxygen concentrations
rarely fall to low levels, despite large inputs of nutrients. This is because the
North Sea is shallow and its waters exchange freely with those of the North
Atlantic providing a constant supply of oxygen-rich surface water to the North
Sea deeper waters.
234 Chapter Six
1958 1963 1968 1973 1980
Year
4
3
2
DIP ( 1
mmol l
N –1)
Germany Poland
Baltic Sea
Denmark
Gulf of Finland
BothnianFinland
Bay
Norway
Sweden
Skagerrak
Katte-
gat
Bothnian
Sea
1900 1920 1940 1960 1980
0.4
0.2
O^2 0
(mmol l
–1) O 2
HS–
Year
Fig. 6.30Oxygen and phosphorus concentrations in the Baltic Sea. Dark line through data is
a regression line and thin line marks zero O 2 concentration. DIP, dissolved inorganic
phosphorus. Data plots after Fonselius (1981) and Nehring (1981), with permission from
Elsevier Science.