Browsing Havforskningsinstituttet by Subject "currents"
Now showing items 1-20 of 36
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Arctic intermediate water in the Norwegian Sea
(ICES CM Documents;1986/C:14, Working paper, 1986)Two types of intermediate water propagate into the Norwegian Sea from the Iceland and Greenland seas. North Icelandic Winter water flows along the slope cf the Faroe-Iceland Ridge towards the Faroes . The distribution ... -
Deepwater flowthrough as a temperature stabilizer in rearing of halibut (Hippoglossus hippoglossus) fry
(ICES CM Documents;1987/F:16, Working paper, 1987)Through the period of yolk sac absorption, halibut larvae were kept in plastic bags in plastic basins with flowthrough of deepwater. When maintaining sufficient flowthrough, in this period the temperature in the bags ... -
Density driven currents in the Barents Sea calculated by a numerical model
(ICES CM Documents;1989/C:20, Working paper, 1989)A baroclinic, 3-D model is described. It is adapted to a Barents Sea situation in order to simulate the currents in this area. The model is of a so-called level type which contains fixed, but permeable levels. It also ... -
Drift of capelin larvae - a population sink?
(ICES CM Documents;1988/H:54, Working paper, 1988) -
Effects of near-bottom currents on the distribution of olfactory stimuli (smell) from baits
(ICES CM Documents;1983/B:3, Working paper, 1983) -
Episodic formation of intermediate water along the Greenland Sea Arctic Front
(ICES CM Documents;1995/Mini:6, Working paper, 1995)During CTD and plankton surveys in the Nordic Seas in November 1991 - 1994, a CTD section has been worked across the Arctic Front between the Lofoten and Greenland Basins. Along this front Isopycnic surfaces slope down ... -
Evidence for effects on the North Sea ecosystem due to varying oceanic inflow over the last 100 years
(ICES CM Documents;2002/Q:8, Working paper, 2002)Oceanic inflow is estimated to contribute more than 90% of the nutrient input into the North Sea (NSTF, 1993). Variability in the volume, chemical properties, biological content and source of the inflowing water is thus ... -
Features of the Barents Sea circulation
(Fisken og havet, Research report, 2001)During the period 1970-1996, a number of current measurements were carried out in the Barents Sea by different institutions. The observations include measurements from fixed mooring buoys and data from drifting satellite ... -
Field experiences with a new miniature vector averaging current meter
(ICES CM Documents;1991/C:20, Working paper, 1991)For several years Inst. of Marine Research Bergen has been developing miniaturized modular current meters. Thanks to major improvements in electronic component technology in recent years, a physically small current meter ... -
Formation of nutrient rich bottom water in the eastern parth of the Barents Sea
(ICES CM Documents;1997/R:1, Working paper, 1997)During yearly routine observations of hydrography, nutrients and plankton in the Barents Sea we have observed a distinct anomaly in the distribution of the nutrients silicate and nitrate in near bottom water in an area ... -
Kystmodellen NorKyst-800 – en strømmodell for hele norskekysten
(Havforskningsnytt;Nr. 8 - 2011, Working paper, 2011)Kystmodellen NorKyst-800 er en beregningsmodell som simulerer bl.a. strøm, saltholdighet og temperatur med 800 meters romlig oppløsning og med høy oppløsning i tid for hele norskekysten. NorKyst-800 er utviklet på ... -
Northern North Sea circulation during early fall
(ICES CM Documents;1988/C:32, Working paper, 1988)During the fall of 1987 the Autumn Circulation Experiment (ACE) was carried out in the northern North Sea. The transversal flow of mixed Scottish coastal and Atlantic water from northeast of Scottland towards Norway was ... -
Ocean pathways in the Arctic
(ICES CM Documents;1997/R:8, Working paper, 1997)Introduction: The Arctic Monitoring and Assessment Programme (AMAP), established in 1991, was given the responsibility to monitor the levels and assess the effects of selected anthropogenic pollutants in all compartments ... -
Outflow of Skagerrak water to the North Sea during summer 1984
(ICES CM Documents;1985/C:21, Working paper, 1985)This paper describes a situation from summer 1984 where low salinity water from the Skagerrak was flowing west and north and covered a significant part of the northern North Sea Plateau. This unusually Skagerrak water ... -
Report of the ICES-EuroGOOS planning group on the North sea pilot project NORSEPP (PGNSP)
(ICES CM documents, Working paper, 2005)There had been limited intersessional work but members provided updated information on NORSEPP relevant activities and products, including a modelled 50-years time-series (1955–2004) of modelled water fluxes in the North ... -
Report of the ICES/IOC/IMO Study Group on Ballast Water and Sediments [Llandudno, UK, 12- 13 April, 1999]
(ICES CM Documents;1999/ACME:2, Working paper, 1999) -
Report of the Working Group on Oceanic Hydrography [13- 15 March, 1999, Murmansk, Russia]
(ICES CM Documents;1999/C:8, Working paper, 1999) -
Report of the Working Group on Oceanic Hydrography [Brest, France, 27 -29 April, 1983]
(ICES CM Documents;1983/C:3, Working paper, 1983) -
Report of the Working Group on Oceanic Hydrography [Texel, The Netherlands, 21- 23 April, 1997]
(ICES CM Documents;1997/C:3, Working paper, 1997)