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Journal articles on the topic 'The Norwegian Sea'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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1

Drife, J. O. "Norwegian sea." BMJ 339, aug05 3 (2009): b3136. http://dx.doi.org/10.1136/bmj.b3136.

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2

Maureen Pilkington. "Toward the Norwegian Sea." Antioch Review 76, no. 2 (2018): 245. http://dx.doi.org/10.7723/antiochreview.76.2.0245.

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3

Risebrobakken, Bjørg, Mari F. Jensen, Helene R. Langehaug, et al. "Buoyancy forcing: a key driver of northern North Atlantic sea surface temperature variability across multiple timescales." Climate of the Past 19, no. 5 (2023): 1101–23. http://dx.doi.org/10.5194/cp-19-1101-2023.

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Abstract. Analyses of observational data (from year 1870 AD) show that sea surface temperature (SST) anomalies along the pathway of Atlantic Water transport in the North Atlantic, the Norwegian Sea and the Iceland Sea are spatially coherent at multidecadal timescales. Spatially coherent SST anomalies are also observed over hundreds of thousands of years during parts of the Pliocene (5.23–5.03, 4.63–4.43, and 4.33–4.03 Ma). However, when investigating CMIP6 (Coupled Model Intercomparison Project 6) SSP126 (Shared Socioeconomic Pathway) future scenario runs (next century) and other Pliocene time

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Brunstad, Harald, Felix Gradstein, Jan Erik Lie, et al. "Stratigraphic Guide to the Rogaland Group, Norwegian North Sea." Newsletters on Stratigraphy 46, no. 2 (2013): 137–286. http://dx.doi.org/10.1127/0078-0421/2013/0032.

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5

Iakovleva, D. A., and I. L. Bashmachnikov. "The role of Regional Atmospheric Circulation in Interannual Variability of the Ocean Heat Advection in the Nordic Seas." Известия Российской академии наук. Физика атмосферы и океана 59, no. 5 (2023): 539–48. http://dx.doi.org/10.31857/s0002351523050127.

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More than 90% of oceanic heat enters the Arctic Ocean with the Norwegian Current. In this paper we examine the mechanisms of variability of the oceanic heat flux in the Norwegian Current (across the Svinoy section in the southern Norwegian Sea) in 1993–2019. GLORYS oceanic reanalysis with a spatial resolution of 1/12° is used. It is found that the variability of oceanic heat flux is associated with that of water transport, which, in turn, is associated with variability of the sea level gradient across the Norwegian Current. It is shown that an increase in water transport of the Norwegian Curre

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Svendsen, Kristoffer. "The Impact of Choice-of-Law Rules in Cross-Border Pollution Damage Caused by Petroleum Spills from Offshore Rigs and Installations: The Case of the Barents Sea." Yearbook of Polar Law Online 8, no. 1 (2017): 163–86. http://dx.doi.org/10.1163/22116427_008010010.

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The article examines the impact of choice-of-law rules in cross-border pollution damage caused by petroleum spills from offshore rigs and installations in the Barents Sea. Norway and Russia share the Barents Sea, and the ocean currents go from West to East. Therefore, the article examines the impact of an oil spill from a Norwegian licensee on the Norwegian side of the Barents Sea on a Russian party harmed by the spill on the Russian side of the Barents Sea. The article shows the procedural hurdles a Russian harmed party would need to jump in order to access Norwegian courts. The question of v

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Laberg, Jan Sverre, Tore O. Vorren, and Stig-Morten Knutsen. "The Lofoten Drift, Norwegian Sea." Geological Society, London, Memoirs 22, no. 1 (2002): 57–64. http://dx.doi.org/10.1144/gsl.mem.2002.022.01.05.

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8

Rich, Vera. "Pollution fears for Norwegian Sea." Nature 338, no. 6216 (1989): 529. http://dx.doi.org/10.1038/338529b0.

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9

Sundvor, Eirik, Olav Eldholm, Tadeusz P. Gladczenko, and Sverre Planke. "Norwegian-Greenland Sea thermal field." Geological Society, London, Special Publications 167, no. 1 (2000): 397–410. http://dx.doi.org/10.1144/gsl.sp.2000.167.01.15.

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10

Laberg, J. S., H. B. Amundsen, and T. A. Rydningen. "The Andøya Canyon, Norwegian Sea." Geological Society, London, Memoirs 46, no. 1 (2016): 409–10. http://dx.doi.org/10.1144/m46.80.

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11

Mork, Kjell Arne, Øystein Skagseth, and Henrik Søiland. "Recent Warming and Freshening of the Norwegian Sea Observed by Argo Data." Journal of Climate 32, no. 12 (2019): 3695–705. http://dx.doi.org/10.1175/jcli-d-18-0591.1.

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Abstract Climate variability in the Norwegian Sea, comprising the Norwegian and Lofoten Basins, was investigated based upon monthly estimates of ocean heat and freshwater contents using data from Argo floats during 2002–18. Both local air–sea exchange and advective processes were examined and quantified for monthly to interannual time scales. In the recent years, 2011–18, the Norwegian Sea experienced a decoupling of the temperature and salinity, with a simultaneous warming and freshening trend. This was mainly explained by two different processes; reduced ocean heat loss to the atmosphere and

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12

Bachem, Paul E., Bjørg Risebrobakken, Stijn De Schepper, and Erin L. McClymont. "Highly variable Pliocene sea surface conditions in the Norwegian Sea." Climate of the Past 13, no. 9 (2017): 1153–68. http://dx.doi.org/10.5194/cp-13-1153-2017.

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Abstract. The Pliocene was a time of global warmth with small sporadic glaciations, which transitioned towards the larger-scale Pleistocene glacial–interglacial variability. Here, we present high-resolution records of sea surface temperature (SST) and ice-rafted debris (IRD) in the Norwegian Sea from 5.32 to 3.14 Ma, providing evidence that the Pliocene surface conditions of the Norwegian Sea underwent a series of transitions in response to orbital forcing and gateway changes. Average SSTs are 2 °C above the regional Holocene mean, with notable variability on millennial to orbital timescales.

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13

Larsen, Eiliv, and Hans Petter Sejrup. "Weichselian land-sea interactions: Western Norway-Norwegian sea." Quaternary Science Reviews 9, no. 1 (1990): 85–97. http://dx.doi.org/10.1016/0277-3791(90)90006-v.

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14

Haakenstad, Hilde, Øyvind Breivik, Birgitte R. Furevik, Magnar Reistad, Patrik Bohlinger, and Ole Johan Aarnes. "NORA3: A Nonhydrostatic High-Resolution Hindcast of the North Sea, the Norwegian Sea, and the Barents Sea." Journal of Applied Meteorology and Climatology 60, no. 10 (2021): 1443–64. http://dx.doi.org/10.1175/jamc-d-21-0029.1.

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AbstractThe 3-km Norwegian Reanalysis (NORA3) is a 15-yr mesoscale-permitting atmospheric hindcast of the North Sea, the Norwegian Sea, and the Barents Sea. With a horizontal resolution of 3 km, the nonhydrostatic numerical weather prediction model HARMONIE–AROME runs explicitly resolved deep convection and yields hindcast fields that realistically downscale the ERA5 reanalysis. The wind field is much improved relative to its host analysis, in particular in mountainous areas and along the improved grid-resolving coastlines. NORA3 also performs much better than the earlier hydrostatic 10-km Nor

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15

Miettinen, Arto, Dmitry Divine, Nalan Koç, Fred Godtliebsen, and Ian R. Hall. "Multicentennial Variability of the Sea Surface Temperature Gradient across the Subpolar North Atlantic over the Last 2.8 kyr*,+." Journal of Climate 25, no. 12 (2012): 4205–19. http://dx.doi.org/10.1175/jcli-d-11-00581.1.

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Abstract A 2800-yr-long August sea surface temperature (aSST) record based on fossil diatom assemblages is generated from a marine sediment core from the northern subpolar North Atlantic. The record is compared with the aSST record from the Norwegian Sea to explore the variability of the aSST gradient between these areas during the late Holocene. The aSST records demonstrate the opposite climate tendencies toward a persistent warming in the core site in the subpolar North Atlantic and cooling in the Norwegian Sea. At the multicentennial scale of aSST variability of 600–900 yr, the records are

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16

Konik, A. A., O. A. Atadzhanova, and E. V. Sentyabov. "Analysis of mesoscale frontal zones of the Norwegian Sea based on satellite observations and reanalysis data in May 2011–2020." Fundamental and Applied Hydrophysics 17, no. 1 (2024): 52–62. http://dx.doi.org/10.59887/2073-6673.2024.17(1)-4.

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The aim of this study is to compare the horizontal temperature gradients calculated based on satellite observations and reanalysis data in the area of mesoscale frontal zones’ surface manifestations, both for the entire Norwegian Sea and during the onset of pelagic fish spawning migrations in May from 2011 to 2020. Using monthly average temperature data from MODIS/Aqua, GHRSST OSTIA, and CMEMS GLORYS12v1, the fields of monthly and decade-long horizontal gradients on the surface of the Norwegian Sea were derived. A comparison was made between the decade-long temperature gradient estimates and t

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17

Christakos, Konstantinos, George Varlas, Ioannis Cheliotis, Christos Spyrou, Ole Johan Aarnes, and Birgitte Rugaard Furevik. "Characterization of Wind-Sea- and Swell-Induced Wave Energy along the Norwegian Coast." Atmosphere 11, no. 2 (2020): 166. http://dx.doi.org/10.3390/atmos11020166.

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The necessity to reduce C O 2 emissions in combination with the rising energy demand worldwide makes the extensive use of renewable energy sources increasingly important. To that end, countries with long coastlines, such as Norway, can exploit ocean wave energy to produce large amounts of power. In order to facilitate these efforts as well as to provide quantitative data on the wave energy potential of a specific area, it is essential to analyze the weather and climatic conditions detecting any variabilities. The complex physical processes and the atmosphere-wave synergetic effects make the in

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18

Ibrekk, Hans Olav, Jarle Molvær, and Bjørn Faafeng. "Nutrient Loading to Norwegian Coastal Waters and Its Contribution to the Pollution of the North Sea." Water Science and Technology 24, no. 10 (1991): 239–49. http://dx.doi.org/10.2166/wst.1991.0297.

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The North Sea Declaration aims at reducing the load of nutrients to the North Sea by the order of 50 per cent between 1985 and 1995. This paper gives an overview of the nutrient loading to the Norwegian coastal waters, and an estimate of how much of this loading reaches the local Skagerrak coast and the North Sea. The average annual nutrient load to coastal waters from land-based sources along the Norwegian North Sea coastline (from the Swedish border to 62°N) is approximately 3,600 tons of phosphorus and 70,000 tons of nitrogen. Municipal wastewater is the main source of phosphorus (44 per ce

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19

Verdenius, Jacob G., and Michael A. Kaminski. "Hyperammina grosserugosa, nom. nov., a replacement name for Hyperammina rugosa Verdenius and Van Hinte 1983." Micropaleontology 66, no. 6 (2020): 572. http://dx.doi.org/10.47894/mpal.66.6.07.

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In 1983 one of us (JGV) in collaboration with J. Van Hinte described the new foraminiferal species Hyperammina rugosa from the Oligocene of DSDP Hole 345 in the Norwegian Sea. It was also reported from the Eocene at Site 346, Lower Miocene at Site 348, and the Oligocene-Miocene at Site 348 (Verdenius and Van Hinte 1983). The species Hyperammina rugosa was subsequently reported throughout the North Sea, Norwegian Sea, and Barents Sea region (Kaminski and Gradstein 2005). The species has been reported more recently from the Miocene of the Fram Strait region and the Central Arctic Ocean by Kamins

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20

Morozov, E. G., D. I. Frey, N. A. Diansky, and V. V. Fomin. "Bottom circulation in the Norwegian Sea." Russian Journal of Earth Sciences 19, no. 2 (2019): 1–6. http://dx.doi.org/10.2205/2019es000655.

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21

Kjell, Utne, Huse Geir, Ottersen Geir, et al. "Horizontal distribution and overlap of planktivorous fish stocks in the Norwegian Sea during summers 1995–2006." Marine Biology Research 8, no. 5-6 (2012): 420–41. https://doi.org/10.1080/17451000.2011.640937.

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The Norwegian Sea harbours several large pelagic fish stocks, which use the area for feeding during the summer. The period 1995–2006 had some of the highest biomass of pelagic fish feeding in the Norwegian Sea on record. Here we address the horizontal distribution and overlap between herring, blue whiting and mackerel in this period during the summers using a combination of acoustic, trawl and LIDAR data. A newly developed temperature atlas for the Norwegian Sea is used to present the horizontal fish distributions in relation to temperature. The centre of gravity of the herring distribution ch

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22

Krylova, E. M., A. V. Gebruk, D. A. Portnova, C. Todt, and H. Haflidason. "New species of the genus Isorropodon (Bivalvia: Vesicomyidae: Pliocardiinae) from cold methane seeps at Nyegga (Norwegian Sea, Vøring Plateau, Storrega Slide)." Journal of the Marine Biological Association of the United Kingdom 91, no. 5 (2011): 1135–44. http://dx.doi.org/10.1017/s002531541100004x.

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A new species of vesicomyid bivalve (Isorropodon nyeggaensis sp. nov.) is described based on shell morphology, from the Nyegga cold methane seep area on the Norwegian continental margin. This is the first description of vesicomyids from the Norwegian Sea and the northernmost record of recent representatives of the family Vesicomyidae. A dispersion of the genus into the Norwegian Sea basin from the north-eastern Atlantic is suggested. A brief description of other macrofauna from methane seep sites at Nyegga is also given.

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23

Larsen, Eiliv, Hans Petter Sejrup, Sigfus J. Johnsen, and Karen Luise Knudsen. "Do Greenland Ice Cores Reflect NW European Interglacial Climate Variations?" Quaternary Research 43, no. 2 (1995): 125–32. http://dx.doi.org/10.1006/qres.1995.1014.

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AbstractThe climatic evolution during the Eemian and the Holocene in western Europe is compared with the sea-surface conditions in the Norwegian Sea and with the oxygen-isotope-derived paleotemperature signal in the GRIP and Renland ice cores from Greenland. The records show a warm phase (ca. 3000 yr long) early in the Eemian (substage 5e). This suggests that the Greenland ice sheet, in general, recorded the climate in the region during this time. Rapid fluctuations during late stage 6 and late substage 5e in the GRIP ice core apparently are not recorded in the climatic proxies from western Eu

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24

Hjøllo, Solfrid Sætre, Geir Huse, Morten D. Skogen, and Webjørn Melle. "Modelling secondary production in the Norwegian Sea with a fully coupled physical/primary production/individual-based Calanus finmarchicus model system." Marine Biology Research 8, no. 5-6 (2012): 508–26. https://doi.org/10.1080/17451000.2011.642805.

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The copepod Calanus finmarchicus is the dominant species of the meso-zooplankton in the Norwegian Sea, and constitutes an important link between the phytoplankton and the higher trophic levels in the Norwegian Sea food chain. An individual-based model for C. finmarchicus, based on super-individuals and evolving traits for behaviour, stages, etc., is two-way coupled to the NORWegian ECOlogical Model system (NORWECOM). One year of modelled C. finmarchicus spatial distribution, production and biomass are found to represent observations reasonably well. High C. finmarchicus abundance is found alon

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25

Breili, Kristian. "Evolution of sea-level trends along the Norwegian coast from 1960 to 2100." Ocean Dynamics 72, no. 2 (2022): 115–36. http://dx.doi.org/10.1007/s10236-021-01492-7.

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AbstractA first national analysis of the evolution of sea-level rates along the Norwegian coast for the period 1960–2100 has been accomplished by exploring tide-gauge records, relative sea-level projections, and detection techniques for acceleration. Firstly, sea-level rates for the two study periods 1960–2020 and 1991–2020 were estimated. Along the Norwegian coast, relative sea-level rates show significant spatial variation due to glacial isostatic adjustment. Moreover, the coastal average sea-level rate for the period 1991–2020 is significantly higher than for the period 1960–2020. Accelerat

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26

Witte, Ursula, and Gerhard Graf. "Metabolism of deep-sea sponges in the Greenland-Norwegian Sea." Journal of Experimental Marine Biology and Ecology 198, no. 2 (1996): 223–35. http://dx.doi.org/10.1016/0022-0981(96)00006-8.

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27

Ahlgren, Gunnel, Lies Van Nieuwerburgh, Ingrid Wänstrand, Marianne Pedersén, Merike Boberg, and Pauli Snoeijs. "Imbalance of fatty acids in the base of the Baltic Sea food web a mesocosm study." Canadian Journal of Fisheries and Aquatic Sciences 62, no. 10 (2005): 2240–53. http://dx.doi.org/10.1139/f05-140.

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A reproductive disturbance in Baltic Sea Atlantic salmon (Salmo salar), the M74 syndrome, has been reported since early 1970s and has occasionally caused up to 90% mortality for newborn fry. Previous research has revealed that the M74 syndrome may be due to reduced levels of the vitamin thiamin, the carotenoid astaxanthin, and elevated ratios of ω3/ω6 fatty acids in salmon eggs. Using mesocosm experiments, we compared the quantity (µg·L1) and quality (mg·g1 C) of fatty acids in microalgae and copepods in the southern Baltic Sea where the M74 syndrome is common with those in a habitat in the

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28

Ersland, Geir Atle. "The Notau harbour and the Kontor in Bergen." AmS-Skrifter, no. 27 (January 6, 2020): 237–44. http://dx.doi.org/10.31265/ams-skrifter.v0i27.276.

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The Hanseatic Kontor in Bergen was one of the main hubs of trade in the North Sea region. This paper explores a possibility suggested in a late sixteenth-century manuscript that the Norwegian Kontor for some time was also located at Notau, a place south of Bergen. It is argued that this written source might refer to the years 1427–33 when the Hanseatic merchants withdrew from Bergen because of an on-going war between King Erik and northern German princes. Notau is mentioned several times in sources from the fifteenth century and most of these references are related to Hanseatic activity. Howev

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29

Heath, Michael R., Peter R. Boyle, Astthor Gislason, et al. "Comparative ecology of over-wintering Calanus finmarchicus in the northern North Atlantic, and implications for life-cycle patterns." ICES Journal of Marine Science 61, no. 4 (2004): 698–708. http://dx.doi.org/10.1016/j.icesjms.2004.03.013.

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Abstract Data from plankton net and Optical Plankton Counter sampling during 12 winter cruises between 1994 and 2002 have been used to derive a multi-annual composite 3-D distribution of the abundance of over-wintering Calanus finmarchicus in a swath across the North Atlantic from Labrador to Norway. Dense concentrations occurred in the Labrador Sea, northern Irminger Basin, northern Iceland Basin, eastern Norwegian Sea, Faroe–Shetland Channel, and in the Norwegian Trench of the North Sea. A model of buoyancy regulation in C. finmarchicus was used to derive the lipid content implied by the in

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30

Ibrahim, Ahmed, Are Olsen, Siv Lauvset, and Francisco Rey. "Seasonal Variations of the Surface Nutrients and Hydrography in the Norwegian Sea." International Journal of Environmental Science and Development 5, no. 5 (2014): 496–505. http://dx.doi.org/10.7763/ijesd.2014.v5.534.

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31

Olsen, Erik, and Jens Christian Holst. "A note on common minke whale (Balaenoptera acutorostrata) diets in the Norwegian Sea and the North Sea." J. Cetacean Res. Manage. 3, no. 2 (2023): 179–83. http://dx.doi.org/10.47536/jcrm.v3i2.888.

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Visual observations and quantitative samples of forestomach contents were made of minke whales caught in the Norwegian Sea (15 visual observations in 1999, 8 in 2000 and 1 stomach sample) and North Sea (15 visual observations and 7 stomach samples, all from 1999). Prey species were identified, and from the forestomach samples, each prey’s relative contribution by weight to the diet was calculated. In the Norwegian Sea, the diet was dominated by Norwegian spring-spawning herring (100%). This was consistent with the large and dominant abundance of herring in the area. Observations and forestomac

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32

Kolstad, Erik W., and Marius Årthun. "Seasonal Prediction from Arctic Sea Surface Temperatures: Opportunities and Pitfalls." Journal of Climate 31, no. 20 (2018): 8197–210. http://dx.doi.org/10.1175/jcli-d-18-0016.1.

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Arctic sea ice extent and sea surface temperature (SST) anomalies have been shown to be skillful predictors of weather anomalies in the midlatitudes on the seasonal time scale. In particular, below-normal sea ice extent in the Barents Sea in fall has sometimes preceded cold winters in parts of Eurasia. Here we explore the potential for predicting seasonal surface air temperature (SAT) anomalies in Europe from seasonal SST anomalies in the Nordic seas throughout the year. First, we show that fall SST anomalies not just in the Barents Sea but also in the Norwegian Sea have the potential to predi

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33

Bakken, Torkild, and Toril Loennechen Moen. "New records of scalpellids: Are scalpellids (Cirripedia: Scalpellidae) in the Nordic Seas confined to specific oceanographical regimes?" Fauna norvegica 24 (September 27, 2024): 1–6. http://dx.doi.org/10.5324/fn.v24i0.5942.

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Records of cirriped species in the family Scalpellidae from the Nordic Seas are scarce. New records of the four species Amigdoscalpellum hispidum (G. O. Sars, 1890), Ornatoscalpellum stroemi (M. Sars, 1859) Tarasovium cornutum (G.O. Sars, 1879) and Weltnerium nymphocola (Hoek, 1883) from the eastern part of the Norwegian Sea are reported. The record of W. nymphocola is the first from the Norwegian coastline, found on the shelf slope, and the rarely found T. cornutum was found in a depth representing the lower depth range for this species. Based on new data from the Norwegian Sea and from the l

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34

Østerhus, Svein. "The Norwegian Sea one hundred years after." IOP Conference Series: Earth and Environmental Science 6, no. 3 (2009): 032021. http://dx.doi.org/10.1088/1755-1307/6/3/032021.

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35

Dickson, Bob, and Svein Østerhus. "One hundred years in the Norwegian Sea." Norsk Geografisk Tidsskrift - Norwegian Journal of Geography 61, no. 2 (2007): 56–75. http://dx.doi.org/10.1080/00291950701409256.

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36

Swift, James H., and Klaus Peter Koltermann. "The origin of Norwegian Sea Deep Water." Journal of Geophysical Research 93, no. C4 (1988): 3563. http://dx.doi.org/10.1029/jc093ic04p03563.

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37

Gislefoss, Jorunn S., Reidar Nydal, Dag Slagstad, Eloni Sonninen, and Kim Holmén. "Carbon time series in the Norwegian sea." Deep Sea Research Part I: Oceanographic Research Papers 45, no. 2-3 (1998): 433–60. http://dx.doi.org/10.1016/s0967-0637(97)00093-9.

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38

Meinecke, G., and G. Wefer. "Seasonal pteropod sedimentation in the Norwegian Sea." Palaeogeography, Palaeoclimatology, Palaeoecology 79, no. 1-2 (1990): 129–47. http://dx.doi.org/10.1016/0031-0182(90)90109-k.

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39

Blindheim, Johan. "Arctic intermediate water in the Norwegian sea." Deep Sea Research Part A. Oceanographic Research Papers 37, no. 9 (1990): 1475–89. http://dx.doi.org/10.1016/0198-0149(90)90138-l.

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40

Bryne, Helge, and Eilif Dahl. "Oil Rig Disaster in the North Sea." Prehospital and Disaster Medicine 1, S1 (1985): 357–59. http://dx.doi.org/10.1017/s1049023x00045131.

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Since oil was found under the North Sea in the mid 1960's, oil production now plays an important part in Norwegian economy. A major oil field isEkofisk, between Norway and Britain (Figure 1). TheAlexander Kielland, one of the rigs atEkofisk, was a mobile platform of the pentagon type, floating on 5 columns, 150 nautical miles of f the Norwegian coast. It was developed and built as a drilling rig, but was used as an accommodation platform since delivery in July 1976. OnMarch27,1980, theAlexander Kiellandrig lay at anchor on theEkofisk field, close to the production platform EDDA.

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41

Nøttestad, Leif, Justine Diaz, Hector Penã, Henrik Søiland, Geir Huse, and Anders Fernö. "Feeding strategy of mackerel in the Norwegian Sea relative to currents, temperature, and prey." ICES Journal of Marine Science 73, no. 4 (2015): 1127–37. http://dx.doi.org/10.1093/icesjms/fsv239.

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Abstract High abundance of Northeast Atlantic mackerel (Scomber scombrus L.), combined with limited food resources, may now force mackerel to enter new and productive regions in the northern Norwegian Sea. However, it is not known how mackerel exploit the spatially varying feeding resources, and their vertical distribution and swimming behaviour are also largely unknown. During an ecosystem survey in the Norwegian Sea during the summer feeding season, swimming direction, and speed of mackerel schools were recorded with high-frequency omnidirectional sonar in four different regions relative to

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42

Andersson, C., F. S. R. Pausata, E. Jansen, B. Risebrobakken, and R. J. Telford. "Holocene trends in the foraminifer record from the Norwegian Sea and the North Atlantic Ocean." Climate of the Past 6, no. 2 (2010): 179–93. http://dx.doi.org/10.5194/cp-6-179-2010.

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Abstract. The early to mid-Holocene thermal optimum is a well-known feature in a wide variety of paleoclimate archives from the Northern Hemisphere. Reconstructed summer temperature anomalies from across northern Europe show a clear maximum around 6000 years before present (6 ka). For the marine realm, Holocene trends in sea-surface temperature reconstructions for the North Atlantic and Norwegian Sea do not exhibit a consistent pattern of early to mid-Holocene warmth. Sea-surface temperature records based on alkenones and diatoms generally show the existence of a warm early to mid-Holocene opt

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Andersson, C., F. S. R. Pausata, E. Jansen, B. Risebrobakken, and R. J. Telford. "Holocene trends in the foraminifer record from the Norwegian Sea and the North Atlantic Ocean." Climate of the Past Discussions 5, no. 4 (2009): 2081–113. http://dx.doi.org/10.5194/cpd-5-2081-2009.

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Abstract. The early to mid-Holocene thermal optimum is a well-known feature in a wide variety of paleoclimate archives from the Northern Hemisphere. Reconstructed summer temperature anomalies from across northern Europe show a clear maximum around 6 ka. For the marine realm, Holocene trends in sea-surface temperature reconstructions for the North Atlantic and Norwegian Sea do not exhibit a consistent pattern of early to mid-Holocene warmth. Sea-surface temperature records based on alkenones and diatoms generally show the existence of a warm early to mid-Holocene optimum. In contrast, several f

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Ly, Johan Marius, Rune Bergstrøm, Ole Kristian Bjerkemo, and Synnøve Lunde. "To Cooperate or Not? Why Working Together is Essential in the Arctic." International Oil Spill Conference Proceedings 2017, no. 1 (2017): 1146–65. http://dx.doi.org/10.7901/2169-3358-2017.1.1146.

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Abstract The Norwegian Arctic covers Svalbard, Bear Island, Jan Mayen and the Barents Sea. 80% of all shipping activities in the Arctic are within Norwegian territorial waters and the Exclusive Economic Zone. To reduce the risk for accidents, the Norwegian authorities have established several preventive measures. Among these are ship reporting systems, traffic separation schemes in international waters and surveillance capabilities. If an accident has occurred and an oil spill response operation must be organized - resources, equipment, vessels and manpower from Norwegian and neighboring state

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Glover, Kevin A., Øystein Skaala, Morten Limborg, Cecilie Kvamme, and Else Torstensen. "Microsatellite DNA reveals population genetic differentiation among sprat (Sprattus sprattus) sampled throughout the Northeast Atlantic, including Norwegian fjords." ICES Journal of Marine Science 68, no. 10 (2011): 2145–51. http://dx.doi.org/10.1093/icesjms/fsr153.

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Abstract Glover, K. A., Skaala, Ø., Limborg, M., Kvamme, C., and Torstensen, E. Microsatellite DNA reveals population genetic differentiation among sprat (Sprattus sprattus) sampled throughout the Northeast Atlantic, including Norwegian fjords. – ICES Journal of Marine Science, 68: 2145–2151. Sprat (Sprattus sprattus), small pelagic shoaling fish, were sampled from the Celtic, North, and Baltic seas, and 10 Norwegian fjords. Significant overall genetic differentiation was observed among samples when analysed with eight microsatellite DNA loci (Global FST = 0.0065, p < 0.0001). The greatest

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Mazarovich, A. O., A. S. Abramova, K. O. Dobrolyubova, Yu A. Zaraiskaya, E. A. Moroz, and S. Yu Sokolov. "LANDSIDE HAZARD ON THE NORWEGIAN CONTINENTAL MARGIN." Bulletin of Kamchatka Regional Association «Educational-Scientific Center». Earth Sciences, no. 1(61) (2024): 42–56. http://dx.doi.org/10.31431/1816-5524-2024-1-61-42-56.

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Numerous landslides are located on the passive margin of Norway. According to the landslides number and the extent of their detachment zones, the margin can be divided into three segments (from south to north) — Scandinavian, Barents Sea and Svalbard. The fourth segment (Arctic) is the transition area located north of the Spitsbergen archipelago. In the Scandinavian segment, about forty large submarine landslide bodies have been identified on the continental slope and deeper. The Barents Sea segment is dominated by deep-sea fan deposits and relatively small landslides. No large landslides were

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Jensen, Preben. "Nematode assemblages in the deep-sea benthos of the Norwegian Sea." Deep Sea Research Part A. Oceanographic Research Papers 35, no. 7 (1988): 1173–84. http://dx.doi.org/10.1016/0198-0149(88)90008-8.

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Raj, Roshin P., Sourav Chatterjee, Laurent Bertino, Antonio Turiel, and Marcos Portabella. "The Arctic Front and its variability in the Norwegian Sea." Ocean Science 15, no. 6 (2019): 1729–44. http://dx.doi.org/10.5194/os-15-1729-2019.

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Abstract. The Arctic Front (AF) in the Norwegian Sea is an important biologically productive region which is well-known for its large feeding schools of pelagic fish. A suite of satellite data, a regional coupled ocean–sea ice data assimilation system (the TOPAZ reanalysis) and atmospheric reanalysis data are used to investigate the variability in the lateral and vertical structure of the AF. A method, known as “singularity analysis”, is applied on the satellite and reanalysis data for 2-D spatial analysis of the front, whereas for the vertical structure, a horizontal gradient method is used.

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Sentyabov, E. V. "Estimation of long-term changes in thermal conditions and distribution of Atlantic and Subarctic water in the XXI Century in the Norwegian Sea on area surveys data." Trudy VNIRO 192 (August 15, 2023): 162–71. http://dx.doi.org/10.36038/2307-3497-2023-192-162-171.

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Purpose of the work: assessing the spatial and temporal variability of thermal conditions in waters of various origins in the Norwegian Sea in the first decades of the 21st century. Materials: oceanographic data collected during the International Ecosystem Surveys in the Norwegian Sea in 2000–2021. Methods used: comparative data analysis, descriptive statistics methods, correlation analysis. Results: the “boxes”, temperature in which most fully describes the change in the temperature of the Atlantic and Subarctic waters of the Norwegian Sea, were identified. This is confirmed by the high corre

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Frolova, A. V., D. V. Pozdnyakov та E. A. Morozov. "Satellite Study of the <i>E. huxleyi Phenomenon</i> in the Barents, Norwegian, and Greenland Seas in 2003–2021: Temporal Dynamics of the Bloom Areal Extent, Inorganic Carbon Production and CО2 Partial Pressure in Surface Water". Fundamental and Applied Hydrophysics 16, № 1 (2023): 48–62. http://dx.doi.org/10.59887/fpg/rada-dxbz-35be.

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Based on satellite data, E. huxleyi bloom contouring, quantification of particulate inorganic carbon (PIC) production and increment of CO2 partial pressure, (pCO2) in surface water were performed. 18-year (2003–2021) time series of these variables are obtained for the Norwegian, Greenland and Barents seas. The bloom areas in the North Atlantic–Arctic water are the lowest in the Greenland Sea varying from 10×103 km2 to (20–40)×103 km2. In the Norwegian and Barents Seas they reach in some years (60–80)×103 km2 and (500–600)×103 km2, respectively. The total PIC content within E. huxleyi blooms ra

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