91 research outputs found
Formation of heavy bottom water in the Barents Sea
Formation of heavy bottom water through rejection of brine
during ide freezing is a regular phenomenon in the Barents Sea,
particular on the Novaya Zemlya shelf, but also observed in
other shallow localities of the sea.
Water with temperature around -1°C and salinity above 34.95
is found moving eastwards on the southern side of the Novaya
Zemlya-Franz Josef Land Channel which communicates with the
Polar Sea. The relative high salinity is a result of admixture
from heavy water formed during the freezing process
Norwegian blue whiting investigation in April/May 1980.
An acoustic survey on the blue whiting stock was conducted from
8 April to 14 May 1980. The area west of the British Isles was
covered twice and then the area around the Farces and further up
to Shetland and the Norwegian coast covered once.
Blue whiting was recorded in the area around the Faroes and along
the slope continously south to the Porcupinebank, with densest
concentrations found off the Hebrides.
The hydrographical situation is presented and also the age and
length compositions, maturity conditions and the length-weight
relationships of the blue whiting in the area.
Higher contributions of young fish were found to represent the
blue whiting stock in the spawning area, than observed in recent
years. Acoustic abundance estimate gave a figure of 5.4 mill.tonnes
of blue whiting, which is 2,5 mill.tonnes lesser than the recalculated
figure of 1979
Formation of heavy bottom water in the Barents Sea
Formation of heavy bottom water through rejection of brine
during ide freezing is a regular phenomenon in the Barents Sea,
particular on the Novaya Zemlya shelf, but also observed in
other shallow localities of the sea.
Water with temperature around -1°C and salinity above 34.95
is found moving eastwards on the southern side of the Novaya
Zemlya-Franz Josef Land Channel which communicates with the
Polar Sea. The relative high salinity is a result of admixture
from heavy water formed during the freezing process
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