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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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 |
_version_ |
1766369893889867776 |