Modelling the advection and diffusion of eggs and larvae of Northeast Arctic Greenland halibut

In later years there has been considerable uncertainty on the recruitment of the northeast Arctic stock of Greenland halibut (Reinhardtius hyppoglossoides). The abundance of several year classes originally considered very low at 0-3 years age, are now considered higher than expected at the age of 6...

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Main Authors: Ådlandsvik, Bjørn, Gundersen, Agnes C., Nedreaas, Kjell Harald, Stene, Anne, Albert, Ole Thomas
Format: Report
Language:English
Published: ICES 1999
Subjects:
Online Access:http://hdl.handle.net/11250/100189
id ftimr:oai:imr.brage.unit.no:11250/100189
record_format openpolar
spelling ftimr:oai:imr.brage.unit.no:11250/100189 2023-05-15T14:56:10+02:00 Modelling the advection and diffusion of eggs and larvae of Northeast Arctic Greenland halibut Ådlandsvik, Bjørn Gundersen, Agnes C. Nedreaas, Kjell Harald Stene, Anne Albert, Ole Thomas 1999 2129284 bytes application/pdf http://hdl.handle.net/11250/100189 eng eng ICES ICES CM documents 1999/K:03 http://hdl.handle.net/11250/100189 20 s. greenland halibut blåkveite halibut kveite VDP::Agriculture and fishery disciplines: 900::Fisheries science: 920::Resource biology: 921 Working paper 1999 ftimr 2021-09-23T20:15:31Z In later years there has been considerable uncertainty on the recruitment of the northeast Arctic stock of Greenland halibut (Reinhardtius hyppoglossoides). The abundance of several year classes originally considered very low at 0-3 years age, are now considered higher than expected at the age of 6 or more. A possible explanation, raised earlier, is more northeasterly than expected distribution of the young fish by active migration and/or drift of eggs and Iarvae. The present work considers the transport and dispersion of eggs and larvae of Greenland halibut by numerical nod el ling. Current fields from a 3D baroclinic hydrodynarnic model are fed in to a Lagrangian particle tracking model. The particles arc released into the current at the spawning field along the shelf slope from Vesterålen to Bjørnøya (69-75"N). Vertically, the particles can follow a predefined depth-by-age curve or be kept, at a fixed depth, This model system is used for different years to examine changes in the drift pattern. Report Arctic Bjørnøya Bjørnøya Greenland Vesterålen Institute for Marine Research: Brage IMR Arctic Bjørnøya ENVELOPE(-67.250,-67.250,-68.151,-68.151) Greenland Vesterålen ENVELOPE(14.939,14.939,68.754,68.754)
institution Open Polar
collection Institute for Marine Research: Brage IMR
op_collection_id ftimr
language English
topic greenland halibut
blåkveite
halibut
kveite
VDP::Agriculture and fishery disciplines: 900::Fisheries science: 920::Resource biology: 921
spellingShingle greenland halibut
blåkveite
halibut
kveite
VDP::Agriculture and fishery disciplines: 900::Fisheries science: 920::Resource biology: 921
Ådlandsvik, Bjørn
Gundersen, Agnes C.
Nedreaas, Kjell Harald
Stene, Anne
Albert, Ole Thomas
Modelling the advection and diffusion of eggs and larvae of Northeast Arctic Greenland halibut
topic_facet greenland halibut
blåkveite
halibut
kveite
VDP::Agriculture and fishery disciplines: 900::Fisheries science: 920::Resource biology: 921
description In later years there has been considerable uncertainty on the recruitment of the northeast Arctic stock of Greenland halibut (Reinhardtius hyppoglossoides). The abundance of several year classes originally considered very low at 0-3 years age, are now considered higher than expected at the age of 6 or more. A possible explanation, raised earlier, is more northeasterly than expected distribution of the young fish by active migration and/or drift of eggs and Iarvae. The present work considers the transport and dispersion of eggs and larvae of Greenland halibut by numerical nod el ling. Current fields from a 3D baroclinic hydrodynarnic model are fed in to a Lagrangian particle tracking model. The particles arc released into the current at the spawning field along the shelf slope from Vesterålen to Bjørnøya (69-75"N). Vertically, the particles can follow a predefined depth-by-age curve or be kept, at a fixed depth, This model system is used for different years to examine changes in the drift pattern.
format Report
author Ådlandsvik, Bjørn
Gundersen, Agnes C.
Nedreaas, Kjell Harald
Stene, Anne
Albert, Ole Thomas
author_facet Ådlandsvik, Bjørn
Gundersen, Agnes C.
Nedreaas, Kjell Harald
Stene, Anne
Albert, Ole Thomas
author_sort Ådlandsvik, Bjørn
title Modelling the advection and diffusion of eggs and larvae of Northeast Arctic Greenland halibut
title_short Modelling the advection and diffusion of eggs and larvae of Northeast Arctic Greenland halibut
title_full Modelling the advection and diffusion of eggs and larvae of Northeast Arctic Greenland halibut
title_fullStr Modelling the advection and diffusion of eggs and larvae of Northeast Arctic Greenland halibut
title_full_unstemmed Modelling the advection and diffusion of eggs and larvae of Northeast Arctic Greenland halibut
title_sort modelling the advection and diffusion of eggs and larvae of northeast arctic greenland halibut
publisher ICES
publishDate 1999
url http://hdl.handle.net/11250/100189
long_lat ENVELOPE(-67.250,-67.250,-68.151,-68.151)
ENVELOPE(14.939,14.939,68.754,68.754)
geographic Arctic
Bjørnøya
Greenland
Vesterålen
geographic_facet Arctic
Bjørnøya
Greenland
Vesterålen
genre Arctic
Bjørnøya
Bjørnøya
Greenland
Vesterålen
genre_facet Arctic
Bjørnøya
Bjørnøya
Greenland
Vesterålen
op_source 20 s.
op_relation ICES CM documents
1999/K:03
http://hdl.handle.net/11250/100189
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