5 
[s 
GAUSS 385 
. af 
% 
ä 
be 
Zir 
ir 
ix 
no 
40 
50 
60 
70 
80 
sa 
A 
x 
Profil 11 
J 
2 
m“ 
ea 
A 
Chlorophyll 
10 
Profil 9 
30 
40 
RX 
3 
70 
40 
.50- 
60- 
70 
-80- 
32 
10} 
E 30° 
E 40- 
oO 
® 50- 
50: 
8C 
Profil 7 
Proul 5 
Profil 4 
} 
5 
Longitude [°W/E] 
3 
= 1 
caused by upwelling of nutrient-rich water from deeper layers, between the English 
soast and the Dogger Bank. In the northern German Bight and off Jutland, the lowest 
axygen saturation values recorded, about 75-80 %, were measured near the bottom. 
These values are good for the season. Because of the thicker surface layer in the