Effects of climate on marine ecosystem

The spawning areas of the Arcto-Norwegian cod are located along the coast of mid and northern Norway, particulary in the Lofoten where up to 70% of the spawning occurs from mid March to early May. The larvae are carried northwards by the Norwegian Coastal Current to the nursery grounds in the Barent...

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Main Authors: Vikebø, Frode, Sundby, Svein, Ådlandsvik, Bjørn
Format: Report
Language:English
Published: ICES 2003
Subjects:
cod
Online Access:http://hdl.handle.net/11250/106501
id ftimr:oai:imr.brage.unit.no:11250/106501
record_format openpolar
spelling ftimr:oai:imr.brage.unit.no:11250/106501 2023-05-15T15:38:40+02:00 Effects of climate on marine ecosystem Vikebø, Frode Sundby, Svein Ådlandsvik, Bjørn 2003 application/pdf http://hdl.handle.net/11250/106501 eng eng ICES ICES CM Documents;2003/O:7 This report is not to be cited without prior reference to the authors http://hdl.handle.net/11250/106501 8 s. marine ecosystems marine økosystemer climate klima cod torsk spawning areas gyteplasser VDP::Mathematics and natural science: 400::Zoology and botany: 480::Marine biology: 497 VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452 VDP::Social science: 200::Library and information science: 320::Knowledge retrieval and organization: 323 Working paper 2003 ftimr 2021-09-23T20:16:16Z The spawning areas of the Arcto-Norwegian cod are located along the coast of mid and northern Norway, particulary in the Lofoten where up to 70% of the spawning occurs from mid March to early May. The larvae are carried northwards by the Norwegian Coastal Current to the nursery grounds in the Barents Sea. The year class strenght is largely determined during this period of pelagic free drift of 600-1200 km. Lateral spreading takes parts of the population out in the warmer Norwegian Atlantic Current and causes differences in the temperature experienced by the larvae. A three-dimensional baroclinic hydrodynamic model is set up for parts of the Norwegian Coast and the Barents Sea. Currents from this model move particles from the spawning grounds in the Vestfjord while keeping a record of the individual temperature histories. Temperature dependent growth is calculated using functional relationship know from ideal experiments. The model results are then compared to measurements. Report Barents Sea Lofoten Northern Norway Institute for Marine Research: Brage IMR Barents Sea Lofoten Norway Vestfjord ENVELOPE(-28.750,-28.750,70.500,70.500)
institution Open Polar
collection Institute for Marine Research: Brage IMR
op_collection_id ftimr
language English
topic marine ecosystems
marine økosystemer
climate
klima
cod
torsk
spawning areas
gyteplasser
VDP::Mathematics and natural science: 400::Zoology and botany: 480::Marine biology: 497
VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452
VDP::Social science: 200::Library and information science: 320::Knowledge retrieval and organization: 323
spellingShingle marine ecosystems
marine økosystemer
climate
klima
cod
torsk
spawning areas
gyteplasser
VDP::Mathematics and natural science: 400::Zoology and botany: 480::Marine biology: 497
VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452
VDP::Social science: 200::Library and information science: 320::Knowledge retrieval and organization: 323
Vikebø, Frode
Sundby, Svein
Ådlandsvik, Bjørn
Effects of climate on marine ecosystem
topic_facet marine ecosystems
marine økosystemer
climate
klima
cod
torsk
spawning areas
gyteplasser
VDP::Mathematics and natural science: 400::Zoology and botany: 480::Marine biology: 497
VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452
VDP::Social science: 200::Library and information science: 320::Knowledge retrieval and organization: 323
description The spawning areas of the Arcto-Norwegian cod are located along the coast of mid and northern Norway, particulary in the Lofoten where up to 70% of the spawning occurs from mid March to early May. The larvae are carried northwards by the Norwegian Coastal Current to the nursery grounds in the Barents Sea. The year class strenght is largely determined during this period of pelagic free drift of 600-1200 km. Lateral spreading takes parts of the population out in the warmer Norwegian Atlantic Current and causes differences in the temperature experienced by the larvae. A three-dimensional baroclinic hydrodynamic model is set up for parts of the Norwegian Coast and the Barents Sea. Currents from this model move particles from the spawning grounds in the Vestfjord while keeping a record of the individual temperature histories. Temperature dependent growth is calculated using functional relationship know from ideal experiments. The model results are then compared to measurements.
format Report
author Vikebø, Frode
Sundby, Svein
Ådlandsvik, Bjørn
author_facet Vikebø, Frode
Sundby, Svein
Ådlandsvik, Bjørn
author_sort Vikebø, Frode
title Effects of climate on marine ecosystem
title_short Effects of climate on marine ecosystem
title_full Effects of climate on marine ecosystem
title_fullStr Effects of climate on marine ecosystem
title_full_unstemmed Effects of climate on marine ecosystem
title_sort effects of climate on marine ecosystem
publisher ICES
publishDate 2003
url http://hdl.handle.net/11250/106501
long_lat ENVELOPE(-28.750,-28.750,70.500,70.500)
geographic Barents Sea
Lofoten
Norway
Vestfjord
geographic_facet Barents Sea
Lofoten
Norway
Vestfjord
genre Barents Sea
Lofoten
Northern Norway
genre_facet Barents Sea
Lofoten
Northern Norway
op_source 8 s.
op_relation ICES CM Documents;2003/O:7
This report is not to be cited without prior reference to the authors
http://hdl.handle.net/11250/106501
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