dc.contributor.author | Ådlandsvik, Bjørn | |
dc.date.accessioned | 2012-08-17T11:04:29Z | |
dc.date.available | 2012-08-17T11:04:29Z | |
dc.date.issued | 1989 | |
dc.identifier.citation | This report is not to be cited without prior reference to the author | no_NO |
dc.identifier.uri | http://hdl.handle.net/11250/104581 | |
dc.description.abstract | Results from a wind-driven homogeneous numerical current model for the Barents
Sea are presented. The wind-driven fluctuations in the volume flux through the section
between Fugløya and the Bear Island are computed for the period 1970-86. This time
series shows a remarkable coincidence with measured temperature anomalies in the Kola
section.
Reasons for and implications of this connection are discussed. In warm periods there
is often low pressure over the central Barents Sea giving an increased Atlantic inflow. In
colder periods the opposite effect occurs.
It is also suggested that these wind-driven fiuctuations in the current may infiuence
the transport of fish larvae. The east-west distribution of 0-group Arcto-Norwegian cod
is discussed. | no_NO |
dc.language.iso | eng | no_NO |
dc.publisher | ICES | no_NO |
dc.relation.ispartofseries | ICES CM Documents;1989/C:18 | |
dc.subject | currents | no_NO |
dc.subject | strømforhold | no_NO |
dc.subject | environmental impact | no_NO |
dc.subject | miljøpåvirkning | no_NO |
dc.title | Wind-driven variations in the Atlantic inflow to the Barents Sea | no_NO |
dc.type | Working paper | no_NO |
dc.subject.nsi | VDP::Mathematics and natural science: 400::Zoology and botany: 480::Marine biology: 497 | no_NO |
dc.subject.nsi | VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452 | no_NO |
dc.source.pagenumber | 14 s. | no_NO |