Results 191 to 200 of about 38,290 (237)
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2021
A review of the published data on the distribution of biomass of zooplankton and its main groups: mesozooplankton, meroplankton, crustacean macrozooplankton and gelatinous macrozooplankton in the Barents Sea is presented. The factors that determine the amplitude and direction of interannual changes in the abundance of zooplankton are considered.
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A review of the published data on the distribution of biomass of zooplankton and its main groups: mesozooplankton, meroplankton, crustacean macrozooplankton and gelatinous macrozooplankton in the Barents Sea is presented. The factors that determine the amplitude and direction of interannual changes in the abundance of zooplankton are considered.
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Barents Sea Ecosystem overview
2023The Barents Sea is a shelf area of approximately 1.4 million km2, which borders to the Norwegian Sea in the west and the Arctic Ocean in the north, and is part of the continental shelf area surrounding the Arctic Ocean. The Barents Sea is bounded by the continental slope between Norway and Spitsbergen in the west, the continental slope towards the ...
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Sea Ice Distribution in the Barents Sea
Volume 8: Polar and Arctic Sciences and Technology; Petroleum Technology, 2016This paper provides a statistical description of the sea ice occurrence in the Barents Sea, using yearly maximum sea ice data for the last 36 years from the European Centre for Medium-Range Weather Forecasts (ECMWF). A set of four distribution functions have been estimated with the maximum likelihood method. The distribution functions used were Extreme
Sindre M. Fritzner, Trond Sagerup
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Governing the Barents Sea Region
2020Drawing on the chapters dealing with the ecological, economic, and sociocultural systems of the Barents Sea Region, this chapter identifies key issues of governance arising in the region and makes use of our approach to informed decisionmaking for sustainability to guide thinking about options for addressing these issues.
Alexander N. Vylegzhanin +2 more
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2021
Аннотация на английском языке: Based on the analysis of retrospective and recent materials, the species richness of the bottom fauna and the long-term variability of the quantitative characteristics of zoobenthos of the Barents Sea are considered. The role of key taxa in the formation of benthic biomass and its trophic structure is indicated.
N.V. Denisenko, S.G. Denisenko
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Аннотация на английском языке: Based on the analysis of retrospective and recent materials, the species richness of the bottom fauna and the long-term variability of the quantitative characteristics of zoobenthos of the Barents Sea are considered. The role of key taxa in the formation of benthic biomass and its trophic structure is indicated.
N.V. Denisenko, S.G. Denisenko
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Proceedings, 2014
The CO2 storage atlas of the Barents Sea has been prepared by the Norwegian Petroleum Directorate at the request of the Ministry of Petroleum and Energy (Halland et al. 2013). The main objectives have been to identify the safe and effective areas for long-term storage of CO2 and to avoid possible negative interference with ongoing and future petroleum ...
J.M. Mujezinovic, I.T. Gjeldvik
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The CO2 storage atlas of the Barents Sea has been prepared by the Norwegian Petroleum Directorate at the request of the Ministry of Petroleum and Energy (Halland et al. 2013). The main objectives have been to identify the safe and effective areas for long-term storage of CO2 and to avoid possible negative interference with ongoing and future petroleum ...
J.M. Mujezinovic, I.T. Gjeldvik
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Barents Sea ecoregion – fisheries overview
2019The commercial fisheries in the Barents Sea Ecoregion target few stocks. The largest pelagic fishery targets capelin (cap.27.1-2) using midwater trawl. The largest demersal fisheries target cod (cod.27.1-2), haddock (had.27.1-2), and other gadoids; predominantly using trawls, gillnets, longlines, and handlines.
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Glaciotectonic Features, Southeastern Barents Sea
1997Seismic and borehole data show that Quaternary deposits in the southeastern Barents Sea (Fig. 1) overlie the Mesosoic bedrock with a prominent erosional unconformity, known from the western Barents Sea as the Upper Regional Unconformity (URU) [Solheim and Kristoffersen, 1984].The Quaternary sequence is subdivided into three seismic and lithologic units:
Valery Gataullin, Leonid Polyak
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Geology of Barents Sea: ABSTRACT
AAPG Bulletin, 1984The Barents Sea is situated on the continental shelf between Norway, the Spitsbergen Islands, and Novaya Zemlya. The main structural framework of the area was formed during the Caledonian and Hercynian orogenies, whereas the western parts were reactivated by the Kimmerian and Alpine orogenies.
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Subglacial Channels, Southern Barents Sea
1997Seismic reflection records from the southern Barents Sea have revealed a system of deep (20–50 m, locally reaching 200 m) and narrow (2–5 km) linear channels cut into the Mesozoic bedrock, and covered by Quaternary sediments. These channels are particularly abundant near the Kola Peninsula, where they are roughly subparallel to the coastline (Figs. 1–2)
Valery Gataullin, Leonid Polyak
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