Blar i Brage IMR på emneord "temperatur"
Viser treff 21-27 av 27
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Report of the Marine Chemistry Working Group [ICES Headquarters, 28 February - 3 March, 2000]
(ICES CM Documents;2000/E:1, Working paper, 2000) -
Report of the Third ICES/GLOBEC Backward-Facing Workshop: Ocean climate of the NW Atlantic during the 1960s and 70s and consequences for gadoid populations [Woods Hole, USA, 4- 6 May, 1998]
(ICES CM Documents;1998/C:9, Working paper, 1998) -
Statistical modelling of temperature variability in the Barents Sea
(ICES CM Documents;1994/S:2, Working paper, 1994)During the latter years an effort has been made to find out more about the relations between environmental variation and recruitment, growth, distribution and migration of fish. The rationale has to a large degree been ... -
Temperature and salinity fluctuations in the Norwegian Sea in relation to wind
(ICES CM Documents;1999/L:3, Working paper, 1999)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 ... -
Temperature effect on growth and larval duration of plaice Pleuronectes platessa in three regions of the Northeast Atlantic
(Journal article; Peer reviewed, 2013-02-27)Transport models for planktonic fish eggs and larvae often use temperature to drive growth because temperature data are readily available. This pragmatic approach can be criticised as too simplistic as it ignores additional ... -
Water fluxes through the Barents Sea
(ICES CM Documents;1995/Mini:10, Working paper, 1995)The physical oceanographic conditions in the Barents Sea depend mainly on the variability in the Atlantic inflow from the Norwegian Sea and the inflow of Arctic water from the Kara Sea and the Arctic Ocean. The transport ... -
Wind generated fluctuations in water mass structure in the Nordic Seas
(ICES CM Documents;1999/L:24, Working paper, 1999)Hydroyaphic sections in the Nordic Seas which have been repeated during the 1990s are compared with observations from 1958 (IGY) in the Norwegian Sea and from 1965 in the Greenland Sea. The comparison shows that the water ...