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

Mork, Kjell Arne; Asplin, Lars
Working paper
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CM_1999_L_03.pdf (323.9Kb)
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http://hdl.handle.net/11250/105937
Utgivelsesdato
1999
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  • ICES CM documents authored by IMR scientists (1949-2011) [3138]
Originalversjon
This report is not to be cited without prior reference to the authors  
Sammendrag
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.
Utgiver
ICES
Serie
ICES CM Documents;1999/L:3

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