DISTRIBUTION, MIGRATION AND ABUNDANCE OF NORWEGIAN SPRING SPAWNING HERRING IN RELATION TO THE TEMPERATURE AND ZOOPLANKTON BIOMASS IN THE NORWEGIAN SEA AS RECORDED BY COORDINATED SURVEYS IN SPRING AND SUMMER 1996
Oa. Misund et al., DISTRIBUTION, MIGRATION AND ABUNDANCE OF NORWEGIAN SPRING SPAWNING HERRING IN RELATION TO THE TEMPERATURE AND ZOOPLANKTON BIOMASS IN THE NORWEGIAN SEA AS RECORDED BY COORDINATED SURVEYS IN SPRING AND SUMMER 1996, Sarsia, 83, 1998, pp. 117-127
The distribution and migration of Norwegian spring spawning herring (C
lupea harengus) in the Norwegian Sea in spring and summer 1996 were ma
pped during 13 coordinated surveys carried out by Faroese, Icelandic,
Norwegian and Russian research vessels. After spawning at the banks of
the Norwegian Coast in February-March, most of the spent herring migr
ated out in the Norwegian Sea through a corridor between 67 degrees N
and 68 degrees N. In May, 4 and 5 year old herring, which form the you
nger part of the spawning stock, were distributed in small schools or
scattered layers at 25-100 m depth over large areas of the central Nor
wegian Sea. Older and larger herring formed large schools, generally a
t 250-400 m depth near the cold front along the eastern part of the Ic
elandic Exclusive Economic Zone (EEZ). The total abundance of herring
in the Norwegian Sea was estimated to be about 47 billion individuals
or about 8 million tonnes. In June, the older and larger herring had m
igrated northwards into the Jan Mayen zone, while the younger herring
remained in the southern and central Norwegian Sea. In July, the young
er herring had migrated back to the area off Vesteralen, northern Norw
ay. In July/August, the larger herring were found in small schools nea
r the surface in the northern Norwegian Sea. Relationships between the
temperature distribution, zooplankton abundance and herring distribut
ion and migration are considered. In May, the lowest zooplankton bioma
ss was observed in the central and southern Norwegian Sea. At that tim
e, there were high zooplankton concentrations in the westernmost part
of the Norwegian Sea, within the domain of the East Icelandic Current.
The herring did not enter this body of cold water with temperatures o
f 1-2 degrees C in the uppermost 300 m, but migrated to the north and
north-east in search of food.