Migration behaviour of herring along the cold front in the Norwegian Sea in April 1997

The behaviour of Norwegian spring spawning herring when migrating to the feeding areas in the Norwegian Sea in April was mapped by an acoustic survey in 1997. The distribution of herring was recorded by conventional echo integration, and the swimming behaviour of selected herring schools was recorde...

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Main Authors: Misund, Ole Arve, Fernö, Anders, Guenette, Sylvie, Mackinson, Steven, Melle, Webjørn, Nøttestad, Leif, Slotte, Aril
Format: Report
Language:English
Published: ICES 1997
Subjects:
Online Access:http://hdl.handle.net/11250/105703
id ftimr:oai:imr.brage.unit.no:11250/105703
record_format openpolar
spelling ftimr:oai:imr.brage.unit.no:11250/105703 2024-09-15T18:26:47+00:00 Migration behaviour of herring along the cold front in the Norwegian Sea in April 1997 Misund, Ole Arve Fernö, Anders Guenette, Sylvie Mackinson, Steven Melle, Webjørn Nøttestad, Leif Slotte, Aril 1997 application/pdf http://hdl.handle.net/11250/105703 eng eng ICES ICES CM Documents;1997/EE:12 This report is not to be cited without prior reference to the authors http://hdl.handle.net/11250/105703 14 s. fish behaviour fiskeatferd migration patterns vandringsmønster distribution utbredelse herring sild VDP::Mathematics and natural science: 400::Zoology and botany: 480::Ethology: 485 VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452 Working paper 1997 ftimr 2024-07-31T03:37:25Z The behaviour of Norwegian spring spawning herring when migrating to the feeding areas in the Norwegian Sea in April was mapped by an acoustic survey in 1997. The distribution of herring was recorded by conventional echo integration, and the swimming behaviour of selected herring schools was recorded by a high-resolution sonar. Individual schools were tracked for up to o ne ho ur. The herring were recorded in an area between 66° and 68° north, 2° east to 3° 30' west. The western part of the area was influenced by the southbound, cold East Icelandic current which induced a termal front within the area. Schools far east of the front had a western migration direction, while schools closer to the front had a southern migration direction. The migration behaviour of the herring schools seemed to be influenced by the temperature distribution in the front. The herring were recorded in large dense schools at 200 - 400 m during daytime. At night the schools rose to surface and scattered or remained as distinct schools. Report Norwegian Sea Institute for Marine Research: Brage IMR
institution Open Polar
collection Institute for Marine Research: Brage IMR
op_collection_id ftimr
language English
topic fish behaviour
fiskeatferd
migration patterns
vandringsmønster
distribution
utbredelse
herring
sild
VDP::Mathematics and natural science: 400::Zoology and botany: 480::Ethology: 485
VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452
spellingShingle fish behaviour
fiskeatferd
migration patterns
vandringsmønster
distribution
utbredelse
herring
sild
VDP::Mathematics and natural science: 400::Zoology and botany: 480::Ethology: 485
VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452
Misund, Ole Arve
Fernö, Anders
Guenette, Sylvie
Mackinson, Steven
Melle, Webjørn
Nøttestad, Leif
Slotte, Aril
Migration behaviour of herring along the cold front in the Norwegian Sea in April 1997
topic_facet fish behaviour
fiskeatferd
migration patterns
vandringsmønster
distribution
utbredelse
herring
sild
VDP::Mathematics and natural science: 400::Zoology and botany: 480::Ethology: 485
VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452
description The behaviour of Norwegian spring spawning herring when migrating to the feeding areas in the Norwegian Sea in April was mapped by an acoustic survey in 1997. The distribution of herring was recorded by conventional echo integration, and the swimming behaviour of selected herring schools was recorded by a high-resolution sonar. Individual schools were tracked for up to o ne ho ur. The herring were recorded in an area between 66° and 68° north, 2° east to 3° 30' west. The western part of the area was influenced by the southbound, cold East Icelandic current which induced a termal front within the area. Schools far east of the front had a western migration direction, while schools closer to the front had a southern migration direction. The migration behaviour of the herring schools seemed to be influenced by the temperature distribution in the front. The herring were recorded in large dense schools at 200 - 400 m during daytime. At night the schools rose to surface and scattered or remained as distinct schools.
format Report
author Misund, Ole Arve
Fernö, Anders
Guenette, Sylvie
Mackinson, Steven
Melle, Webjørn
Nøttestad, Leif
Slotte, Aril
author_facet Misund, Ole Arve
Fernö, Anders
Guenette, Sylvie
Mackinson, Steven
Melle, Webjørn
Nøttestad, Leif
Slotte, Aril
author_sort Misund, Ole Arve
title Migration behaviour of herring along the cold front in the Norwegian Sea in April 1997
title_short Migration behaviour of herring along the cold front in the Norwegian Sea in April 1997
title_full Migration behaviour of herring along the cold front in the Norwegian Sea in April 1997
title_fullStr Migration behaviour of herring along the cold front in the Norwegian Sea in April 1997
title_full_unstemmed Migration behaviour of herring along the cold front in the Norwegian Sea in April 1997
title_sort migration behaviour of herring along the cold front in the norwegian sea in april 1997
publisher ICES
publishDate 1997
url http://hdl.handle.net/11250/105703
genre Norwegian Sea
genre_facet Norwegian Sea
op_source 14 s.
op_relation ICES CM Documents;1997/EE:12
This report is not to be cited without prior reference to the authors
http://hdl.handle.net/11250/105703
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