Temperature and salinity fluctuations in the Norwegian Sea in relation to wind

Hydrographic observations in the Svinøy section and results from the Princeton Ocean Modei are used to investigate the role the wind forcing has on temperature and salinity fluctuations in the Nonvegian Sea. In order to investigate the role the wind forcing has on observed fluctuations in the Norweg...

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Bibliographic Details
Main Authors: Mork, Kjell Arne, Asplin, Lars
Format: Report
Language:English
Published: ICES 1999
Subjects:
Online Access:http://hdl.handle.net/11250/105937
id ftimr:oai:imr.brage.unit.no:11250/105937
record_format openpolar
spelling ftimr:oai:imr.brage.unit.no:11250/105937 2023-05-15T16:50:38+02:00 Temperature and salinity fluctuations in the Norwegian Sea in relation to wind Mork, Kjell Arne Asplin, Lars 1999 application/pdf http://hdl.handle.net/11250/105937 eng eng ICES ICES CM Documents;1999/L:3 This report is not to be cited without prior reference to the authors http://hdl.handle.net/11250/105937 8 s. hydrography hydrografi temperature temperatur salinity salinitet VDP::Mathematics and natural science: 400::Zoology and botany: 480::Marine biology: 497 VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452 Working paper 1999 ftimr 2021-09-23T20:16:12Z Hydrographic observations in the Svinøy section and results from the Princeton Ocean Modei are used to investigate the role the wind forcing has on temperature and salinity fluctuations in the Nonvegian Sea. In order to investigate the role the wind forcing has on observed fluctuations in the Norwegian Sea the model is driven for two different air pressure regimes. A period from the 1960s with a relatively low NAO index is used for one regime while a period from the 1990s with a relatively high NAO index is used for the other regime. Wind data used in the model are from the Hindcast data base archive from the Norwegian Meteorological Institute. The period with high NAO index caused a freshening and cooling of the upper layers in the central Norwegian Sea relative to the period wiih low NAO index. Thls was caused by a reduced transport of Atlantic water over the Iceland-Faeroe Ridge and at the same time the transport through the Faeroe-Shetland increased. In the period with low NAO index the opposite case occured. Report Iceland Norwegian Sea Institute for Marine Research: Brage IMR Norwegian Sea Svinøy ENVELOPE(10.992,10.992,64.866,64.866)
institution Open Polar
collection Institute for Marine Research: Brage IMR
op_collection_id ftimr
language English
topic hydrography
hydrografi
temperature
temperatur
salinity
salinitet
VDP::Mathematics and natural science: 400::Zoology and botany: 480::Marine biology: 497
VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452
spellingShingle hydrography
hydrografi
temperature
temperatur
salinity
salinitet
VDP::Mathematics and natural science: 400::Zoology and botany: 480::Marine biology: 497
VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452
Mork, Kjell Arne
Asplin, Lars
Temperature and salinity fluctuations in the Norwegian Sea in relation to wind
topic_facet hydrography
hydrografi
temperature
temperatur
salinity
salinitet
VDP::Mathematics and natural science: 400::Zoology and botany: 480::Marine biology: 497
VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452
description Hydrographic observations in the Svinøy section and results from the Princeton Ocean Modei are used to investigate the role the wind forcing has on temperature and salinity fluctuations in the Nonvegian Sea. In order to investigate the role the wind forcing has on observed fluctuations in the Norwegian Sea the model is driven for two different air pressure regimes. A period from the 1960s with a relatively low NAO index is used for one regime while a period from the 1990s with a relatively high NAO index is used for the other regime. Wind data used in the model are from the Hindcast data base archive from the Norwegian Meteorological Institute. The period with high NAO index caused a freshening and cooling of the upper layers in the central Norwegian Sea relative to the period wiih low NAO index. Thls was caused by a reduced transport of Atlantic water over the Iceland-Faeroe Ridge and at the same time the transport through the Faeroe-Shetland increased. In the period with low NAO index the opposite case occured.
format Report
author Mork, Kjell Arne
Asplin, Lars
author_facet Mork, Kjell Arne
Asplin, Lars
author_sort Mork, Kjell Arne
title Temperature and salinity fluctuations in the Norwegian Sea in relation to wind
title_short Temperature and salinity fluctuations in the Norwegian Sea in relation to wind
title_full Temperature and salinity fluctuations in the Norwegian Sea in relation to wind
title_fullStr Temperature and salinity fluctuations in the Norwegian Sea in relation to wind
title_full_unstemmed Temperature and salinity fluctuations in the Norwegian Sea in relation to wind
title_sort temperature and salinity fluctuations in the norwegian sea in relation to wind
publisher ICES
publishDate 1999
url http://hdl.handle.net/11250/105937
long_lat ENVELOPE(10.992,10.992,64.866,64.866)
geographic Norwegian Sea
Svinøy
geographic_facet Norwegian Sea
Svinøy
genre Iceland
Norwegian Sea
genre_facet Iceland
Norwegian Sea
op_source 8 s.
op_relation ICES CM Documents;1999/L:3
This report is not to be cited without prior reference to the authors
http://hdl.handle.net/11250/105937
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