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1

Basharat, Salma. "Proactive Emergency Preparedness in the Barents Sea." Thesis, Norges teknisk-naturvitenskapelige universitet, Institutt for produksjons- og kvalitetsteknikk, 2012. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-18401.

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Today rise in oil and gas demand, energy crisis, issues concerning energy security and increase in oil prices in the world provoke further exploration and production of oil and gas. The Arctic Sea is the last frontier of abundant hydrocarbon reserves. Having effective regulations, innovative technologies and adequate safety norms, the world has still seen some major accidents such as Gulf of Mexico accident. Knowing that offshore petroleum industry is moving further north in Arctic poses additional challenges due to harsh climatic conditions and remoteness from existing oil and gas infrastruct
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2

Navarro-Rodríguez, Alba. "Reconstruction of recent and palaeo sea ice conditions in the Barents Sea." Thesis, University of Plymouth, 2014. http://hdl.handle.net/10026.1/3085.

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IP25 is a highly branched isoprenoid alkene derived from certain Arctic sea ice diatoms that, when detected in marine sediments, has been used as a proxy for past Arctic sea ice over the last decade. In the current study, the structure of this biomarker was determined following large-scale extraction from sediment material collected from the Canadian Arctic. After purification, the structure of IP25 was confirmed by NMR spectroscopy as being the same as that of a laboratory standard. The purified IP25 was subsequently used to obtain a quantitative (GC-MS) instrumental response factor that coul
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3

McLaughlin, Philip G. "Signal processing for the 1992 barents sea tomography experiment." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 1993. http://handle.dtic.mil/100.2/ADA278580.

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Thesis (M.S. in Engineering Acoustics and M.S. in Electrical Engineering) Naval Postgraduate School, December 1993.<br>Thesis advisor(s): Miller, James H. ; Chiu, Ching-Sang. "December 1993." Includes bibliographical references (p. 61-62). Also available online.
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4

Yndestad, Harald. "The Lunar Nodal Cycle Influence on the Barents Sea." Doctoral thesis, Norwegian University of Science and Technology, Faculty of Social Sciences and Technology Management, 2004. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-384.

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<p>The Barents Sea contains one of the most productive marine areas in the world. For centuries, Northeast Arctic cod and Norwegian spring spawning herring have been of vital importance for the Norwegian fish export industry and hence economic growth in Norway. It has been common knowledge that the biomass of different Barents Sea species experiences both shortand long-term fluctuations. These fluctuations have been explained by changes in herring cycles and cod cycles, or by the introduction of new fishing equipment, and more. Norwegian marine research began in earnest at the beginning of the
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5

Liu, Zhaolong. "Petroleum System Analysis in Skrugard Area, SW Barents Sea." Thesis, Norges teknisk-naturvitenskapelige universitet, Institutt for petroleumsteknologi og anvendt geofysikk, 2013. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-22770.

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In 2011, Skrugard discovery (well 7220/8-1) made an explorational breakthrough in the south- western Barents Sea. Earlier this year, Havis discovery (well 7220/7-1) was found in the same area. Both two discoveries are in the production license PL 532. However, there are many dry wells (7219/9-1, 7219/8-1S) in the same area before these two discoveries. The objective of this master thesis is to figure out why there found commercial hydrocarbon in Skrugard and Havis rather than other areas close to them, furthermore contribute to a better understanding of the petroleum system in the south-wester
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6

McLaughlin, Fiona Ann. "The Canada basin, 1989-1995, upstream events and far-field effects of the Barents Sea branch." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp03/NQ48224.pdf.

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7

Elliott, John M. "Simulation of acoustic multipath arrival structure in the Barents Sea." Thesis, Monterey, California. Naval Postgraduate School, 1992. http://hdl.handle.net/10945/24036.

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8

Siegert, Martin John. "Numerical modelling studies of the Svalbard-Barents Sea Ice Sheet." Thesis, University of Cambridge, 1993. https://www.repository.cam.ac.uk/handle/1810/273251.

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9

Palmlöv, Erik. "Seismic stratigraphy and tectonics of the Loppa High, western Barents Sea." Doctoral thesis, Stockholms universitet, Naturvetenskapliga fakulteten, 1995. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-81976.

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10

Heinicke, Susanne. "Paleobathymetric reconstruction in the Hammerfest and Tromsø basins, southwestern Barents Sea." Thesis, Norges teknisk-naturvitenskapelige universitet, Institutt for geologi og bergteknikk, 2012. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-20381.

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Seismic interpretation of 13 lines has been conducted in the Hammerfest and Tromsø basin areas in the southwestern Barents Sea. Based on interpretations, a 3D Geomodel comprising 10 layers has been constructed. Depth conversion of the Geomodel was accomplished after building of the herein required velocity model. Paleobathymetric reconstruction was performed for 9 time intervals from Top Oxfordian/Late Jurassic until Intra Sotbakken/Base Pliocene utilizing SINTEF´s basin modeling tool SEMI Paleowater. The restoration method is based on the information about depositional geometries from seismic
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11

Emblidge, John Mark. "A feasibility study of ocean acoustic tomography in the Barents Sea." Thesis, Monterey, California. Naval Postgraduate School, 1991. http://hdl.handle.net/10945/28211.

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12

Seidenglanz, Anne <1985&gt. "Impact of reduced sea ice conditions in the Barents-Kara seas on wintertime atmospheric circulation in the Euro-Atlantic sector." Doctoral thesis, Università Ca' Foscari Venezia, 2019. http://hdl.handle.net/10579/15580.

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The sea ice cover in the Arctic Ocean has experienced an ongoing loss in volume and extent in the last decades with recognised consequences for the northern hemisphere atmospheric circulation. According to climate model projections, this loss is going to continue. Sea ice is an important component of the global climate system as its presence strongly affects the air-sea interaction (via changes in the fluxes of radiative energy, sensible heat, latent heat and momentum) and thus both the atmosphere and ocean. The Barents/Kara (B/K) Seas is the part of the Arctic Ocean experiencing the largest i
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13

Stensland, Hege. "Sedimentology and Diagenesis of the Triassic Snadd Formation in the Barents Sea." Thesis, Norges teknisk-naturvitenskapelige universitet, Institutt for geologi og bergteknikk, 2012. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-20117.

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A palaeodepositional model and an analysis of the diagenetic evolution of the Upper Triassic Snadd Formation in the Barents Sea are here presented. Attention has especially been given to the pedogenic structures dominating the sediments. The interpretations are based on core logging and thin section analyses including three shallow, stratigraphic wells from the south- western Barents Sea area. The data from the Nordkapp Basin represent a sediment succession of only a few meter thicknesses, and the main interpretation is therefore based on data from the Bjarmeland Platform core, which covers th
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14

Harris, Carolyn Louise. "Water mass distribution and Polar Front structure in the Southwestern Barents Sea." Thesis, Massachusetts Institute of Technology, 1996. http://hdl.handle.net/1721.1/54421.

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Thesis (M.S.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, and Woods Hole Oceanographic Institution, 1996.<br>Includes bibliographic references (leaves 63-66). Includes bibliographical references (leaves 63-66).<br>by Carolyn Louise Harris.<br>M.S.
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15

Matteo, Bazzaro. "Past and active biogeochemical processes in the Kveithola trough (NW Barents Sea)." Doctoral thesis, Università di Siena, 2019. http://hdl.handle.net/11365/1089134.

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The Arctic Ocean plays a key role in sequestrating the carbon dioxide (the greenhouse gas mainly responsible of global climate change) from the atmosphere. However, the melting of sea ice and the release of the huge amounts of methane stored in Arctic marine sediments and permafrost have uncertain feedbacks on the Arctic marine carbon cycle. Therefore, in order to refine the future climate modelling, it is of primary importance to promote regional studies on carbon dynamics in the Arctic areas. In following this approach, studies on the interaction of carbon with chemical elements like nitroge
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16

Moro, Ylenia <1994&gt. "Life traits in the nekton assemblage: a comparison between effects of Climate Change on Adriatic Sea and Barents Sea." Master's Degree Thesis, Università Ca' Foscari Venezia, 2022. http://hdl.handle.net/10579/21622.

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Global warming and global environmental changes are impacting marine ecosystems and altering species distributions and interactions. In ecology, trait-based approaches are useful and efficient in order to understand what determine species distributions and the relationship with the environment. Fishes’ life-histories and traits distributions can also be used to predict future responses to environmental changes. This thesis is going to analyse life traits histories of the nekton communities of North Adriatic Sea, between 1945 and 2019 to perform temporal distribution analysis, between 2016 and
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17

Barton, Benjamin I. "Climate change in the Barents Sea : ice-ocean interactions, water mass formation and variability." Thesis, Brest, 2019. http://www.theses.fr/2019BRES0053.

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L’étendue hivernale de la banquise en mer de Barents n’a cessé de diminuer, et un certain nombre d’études suggèrent que cette diminution pourrait coïncider avec des hivers très froids en Europe et Asie. L’eau Atlantique (AW) transportée vers la mer de Barents, se réchauffe. En mer de Barents, l’AW se transforme en Barents Sea Water (BSW), plus froide et moins salée. Etudier cette dernière nous permet d’en savoir plus sur l’influence de la saisonnalité de la banquise Arctique sur la stratification et la circulation de l’océan.Tout d’abord, nous utilisons des observations satellites pour localis
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18

Pierce, David D. "Range-dependent passive source localization using data from the Barents Sea tomography experiment." Diss., Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 1996. http://handle.dtic.mil/100.2/ADA313862.

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Dissertation (Ph.D. in Engineering Acoustics) Naval Postgraduate School, June 1996.<br>Dissertation advisor(s): Ching-Sang Chiu, Charles W. Therrien. "June 1996." Includes bibliographical references. Also available online.
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19

Marello, Laura. "Basin Architecture and Lithospheric Structure of the Barents Sea Region from Geophysical Modelling." Doctoral thesis, Norges teknisk-naturvitenskapelige universitet, Institutt for petroleumsteknologi og anvendt geofysikk, 2012. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-17309.

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This thesis provided a new understanding of the lithospheric structural setting and anomalies observed in the greater Barents Sea. The Barents Sea has been focus of attention for geological and economical reason since the 70ies-80ies. The crustal and lithospheric evolution of this area has been poorly understood and relatively challenging because it involved a large number of different processes. During its evolution, plate aggregation and orogenesis have been alternated with episodic rifting and magmatic events. The final result is the present day continental shelf area formed by a heterogene
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20

Snow, Tasha. "Timing of Svalbard/Barents Sea Ice Sheet Decay during the Last Glacial Termination." Scholar Commons, 2014. https://scholarcommons.usf.edu/etd/5313.

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The Arctic and North Atlantic underwent significant climactic changes since the Last Glacial Maximum (25,000 years before present (1950 AD); ka BP), but offsets in the timing of events between the two regions are poorly constrained due to age model uncertainties that arise from changing radiocarbon reservoir ages. Here, we use a relatively high-resolution, multi-proxy stable isotope and sedimentologic dataset from Eastern Fram Strait (ODP Leg 162 Site 986) marine sediments to constrain the timing of Svalbard/Barents Sea Ice Sheet decay and infer deglacial reservoir ages over the last 30 ka. We
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21

RUI, LEONARDO. "Integrated analysis of glacial sediment input and ocean circulation in NW Barents Sea." Doctoral thesis, Università degli Studi di Trieste, 2018. http://hdl.handle.net/11368/2922568.

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The Arctic Ocean is one of the most climatically sensitive areas, being the crossway of global ocean circulation (Charles et al., 1994; Thiede and Myhre, 1996; Knies et al., 1999; Hald et al., 2004). The West Spitsbergen continental margin is characterized by the presence of the West Spitsbergen Current, a warm Atlantic Water that flows northwards along the continental margin. This Atlantic Water is the major heat advection toward the Arctic, mixing with the cold and partially sea-ice covered Polar Water; thanks to the West Spitsbergen Current, the Polar Water is driven into the northern hemis
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22

Musco, M. E. "Palaeo-ice stream dynamics in the North-western Barents Sea depicted from clay mineral analyses." Doctoral thesis, Università di Siena, 2019. http://hdl.handle.net/11365/1074888.

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The Arctic Ocean is one of the most climatically vulnerable areas on the planet, being a crossway of oceanic circulation. The study of high latitude continental margin sediments is useful for understanding past ice sheet dynamics history and its influence on climate changes. This PhD project focuses on the sedimentation history along the North-western Barents Sea continental margin from the Marine Isotope Stage (MIS) 3 to the Holocene. During the Last Glacial Maximum (LGM), around 21.000 years ago, this area was covered by the Svalbard-Barents Sea Ice sheet (SBSIS). The sedimentary record cont
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23

Baron-Taltre, Benjamin. "The Rise and Fall of the Maine Sea Urchin Industry: A Failure of Management and Institutions?" Fogler Library, University of Maine, 2005. http://www.library.umaine.edu/theses/pdf/Baron-TaltreBX2005.pdf.

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24

Klitzke, Peter [Verfasser], Magdalena [Akademischer Betreuer] Scheck-Wenderoth, and Jan Inge [Akademischer Betreuer] Faleide. "A 3D lithosphere-scale model of the Barents Sea and Kara Sea region / Peter Klitzke ; Magdalena Scheck-Wenderoth, Jan Inge Faleide." Aachen : Universitätsbibliothek der RWTH Aachen, 2020. http://d-nb.info/1231542152/34.

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25

Stott, Martin J. "The Arctic Ocean's interaction with wind-driven coastal polynyas and the Barents Sea polar front." Thesis, Keele University, 2005. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.412988.

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26

Travan, Gaia. "Interactions between salt tectonics and crustal tectonics in the Mediterranean and in the Barents sea." Electronic Thesis or Diss., Université de Lille (2022-....), 2022. http://www.theses.fr/2022ULILR050.

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À l'échelle des temps géologiques, le comportement du sel peut être approché d'un fluide newtonien (comportement visqueux) par rapport au comportement fragile des roches environnantes. La tectonique crustale, extensive et compressive, joue souvent un rôle fondamental dans l'évolution des structures salines et devient la principale cause de déformation dans de nombreuses zones d'étude. Le but de cette thèse est d'analyser le calendrier et les mécanismes de la tectonique salifère dans trois zones d'étude caractérisées par différents âges du sel et l'influence croissante de la tectonique crustale
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27

Wagner, Lara Suzanne. "Investigations of Upper Mantle Structure using Broadband Seismology." Diss., Tucson, Arizona : University of Arizona, 2005. http://etd.library.arizona.edu/etd/GetFileServlet?file=file:///data1/pdf/etd/azu%5Fetd%5F1204%5F1%5Fm.pdf&type=application/pdf.

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28

Oziel, Laurent. "Variabilité de la mer de Barents et son impact sur le phytoplancton." Thesis, Paris 6, 2015. http://www.theses.fr/2015PA066483/document.

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La mer de Barents possède un écosystème particulièrement riche. Elle est affectée par le changement climatique actuel, comme le reste de l'Arctique. L'effet le plus visible et le plus connu est la réduction spectaculaire de la banquise. On examine dans cette thèse les répercussions de ces changements sur l'hydrologie et le phytoplancton en mer de Barents. Pour cela, on s'appuie sur la création d'une base de données historiques comprenant les paramètres hydrologiques et bio-géochimiques. Un modèle 3D bio-géochimique spécifique à l'écosystème arctique est aussi utilisé quand les observations son
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29

Mykyta, John L. "Prediction of the beamformed acoustic ray arrival structure for the 1992 Barents Sea coastal tomography test." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 1993. http://handle.dtic.mil/100.2/ADA276741.

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Thesis (M.S. in Physical Oceanography) Naval Postgraduate School, December 1993.<br>Thesis advisor(s): Chiu, Ching-Sang ; Miller, James H. Cover title: Prediction of the plane wave beamformed acoustic arrival ... "December 1993." Bibliography: p. 36-37. Also available online.
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30

Porten, Hege Walderhaug. "Petrography, diagenesis and reservoir quality of the Triassic Fruholmen, Snadd and Kobbe formations, southern Barents Sea." Thesis, Norges teknisk-naturvitenskapelige universitet, Institutt for geologi og bergteknikk, 2012. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-20107.

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Petrographic composition, diagenesis and reservoir quality of the Upper Triassic fluvial to marginal marine Fruholmen Formation, the Middle and Upper Triassic estuarine and coastal plain Snadd Formation, and the Middle Triassic estuarine Kobbe Formation have been examined in wells 7131/4-1 and 7222/11-1 located on the western Bjarmeland Platform and on the eastern Finnmark Platform in the southern Barents Sea. Twenty-nine thin-sections from the Fruholmen Formation, sixty-eight from the Snadd Formation and eleven from the Kobbe Formation were studied with a petrographic microscope, forty were p
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31

Auset, Marthe. "Sedimentology and Diagenesis of Upper Triassic Sandstones, with Emphasis on the Snadd-Fruholmen Transition, Barents Sea." Thesis, Norges teknisk-naturvitenskapelige universitet, Institutt for geologi og bergteknikk, 2012. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-20110.

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Triassic and Jurassic sediments from two cores in the Nordkapp Basin, Barents Sea, were analyzed by sedimentological, petrographic, SEM and XRD methods. The objective of the study was to gain better understanding of the depositional environments of the Upper Triassic-Jurassic, Snadd-, Fruholmen- and St&#248; formations with emphasis a mineralogical shift in the transition between the Snadd and Fruholmen formations, and try to relate the differences to depositional environment, climatic changes and diagenesis.The studied sediments of the Snadd and Fruholmen formations represent a transition fro
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32

CARIDI, FRANCESCA. "Influence of environmental patterns on the benthic faunal structure in the Kveithola Trough, NW Barents Sea." Doctoral thesis, Università Politecnica delle Marche, 2020. http://hdl.handle.net/11566/274551.

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Per la prima volta, abbiamo documentato la struttura della comunità bentonica artica nel Kveithola Trough (NW Mare di Barents), per migliorare i gaps conoscitivi esistenti. Il Kveithola è caratterizzato da particolari condizioni morfo-deposizionali e idrografiche che permettono di distinguere tre aree principali (esterna, interna e il canale settentrionale). Nell'area esterna, l’elevato idrodinamismo contrasta l'accumulo di materia organica e la bassa biodisponibilità di carbonio organico nei sedimenti supporta una comunità con bassa richiesta di ossigeno. L’area interna e il canale settentrio
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33

Johnson, Joseph C. "Turbulent heat flux measurements over the Greenland, Norwegian and Barents Seas." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 1995. http://handle.dtic.mil/100.2/ADA294129.

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Thesis (M.S. in Meteorology and Physical Oceanography) Naval Postgraduate School, March 1995.<br>Thesis advisor(s): Peter S. Guest, Roland W. Garwood. "March 1995." Bibliography: p. 81-82. Also available online.
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34

Wertholz, Nina J. C. "Förvaltningsplanen för Barents hav och havsområdena utanför Lofoten : Värden och utmaningar utifrån personer inom förvaltningen." Thesis, Södertörn University College, School of Life Sciences, 2009. http://urn.kb.se/resolve?urn=urn:nbn:se:sh:diva-3370.

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<p>Ekosystembaserad förvaltning bygger på en helhetlig syn på ekosystemen och dess förhållande till mänsklig aktivitet. Förvaltningsplanen för Barents hav utanför Norge är ett de längst framskridna försöken till implementering av denna förvaltningsmodell. Lång väg återstår dock för att uppnå de målsättningar som satts och särskilt gäller detta miljömålet för biologisk mångfald. Trots att fiskeri utpekats som den största påverkningsfaktorn på biologisk mångfald har det varit lite fokus på fiskeriernas negativa konsekvenser i arbetet med förvaltningsplanen. Den här uppsatsen försöker ge en bild
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35

Pfirman, S. L. "Modern sedimentation in the Northern Barents Sea : input, dipersal and deposition of suspended sediments from glacial meltwater." Thesis, Massachusetts Institute of Technology, 1985. http://hdl.handle.net/1721.1/54946.

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Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric and Planetary Sciences, 1985.<br>Microfiche copy available in Archives and Science.<br>Includes bibliographies.<br>by Stephanie Louise Pfirman.<br>Ph.D.
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36

Javid, Sanaz. "Petrography and petrophysical well log interpretation for evaluation of sandstone reservoir quality in the Skalle well (Barents Sea)." Thesis, Norges teknisk-naturvitenskapelige universitet, Institutt for geologi og bergteknikk, 2013. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-23137.

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39 thin sections and petrophysical log data from the Skalle well in the Hammerfest Basin, in the southwestern part of the Barents Sea, have been studied to interpret lithology, and diagenesis and their effect on the reservoir quality, and to compare reservoir properties of the different reservoir units. Petrophysical log data have been calibrated for reservoir description in cases where core material is not available. The studied formations are comprised by the St&#248;, Fuglen, Hekkingen, Knurr, Kolje and the Lower Kolmule Formations. The Knurr and Kolje Formations have been identified and in
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37

Miraj, Muhammad Armaghan Faisal [Verfasser], Christophe [Gutachter] Pascal, and Adrian [Gutachter] Immenhauser. "Structural analysis of inversion features of the Barents Sea / Muhammad Armaghan Faisal Miraj ; Gutachter: Christophe Pascal, Adrian Immenhauser." Bochum : Ruhr-Universität Bochum, 2017. http://d-nb.info/1142001474/34.

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38

Bergstrand, Christoffer. "Geophysical characterization of fluid flow and hydrocarbon migration features in the SW Loppa High area, Norwegian Barents Sea." Thesis, Stockholms universitet, Institutionen för geologiska vetenskaper, 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-117990.

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39

Heber, Ryan Conover. "Evidence for Widespread, Low Saturation Gas Hydrate in the Barents and Norwegian Seas." The Ohio State University, 2020. http://rave.ohiolink.edu/etdc/view?acc_num=osu1587052616831745.

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40

Oziel, Laurent. "Variabilité de la mer de Barents et son impact sur le phytoplancton." Electronic Thesis or Diss., Paris 6, 2015. https://accesdistant.sorbonne-universite.fr/login?url=https://theses-intra.sorbonne-universite.fr/2015PA066483.pdf.

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La mer de Barents possède un écosystème particulièrement riche. Elle est affectée par le changement climatique actuel, comme le reste de l'Arctique. L'effet le plus visible et le plus connu est la réduction spectaculaire de la banquise. On examine dans cette thèse les répercussions de ces changements sur l'hydrologie et le phytoplancton en mer de Barents. Pour cela, on s'appuie sur la création d'une base de données historiques comprenant les paramètres hydrologiques et bio-géochimiques. Un modèle 3D bio-géochimique spécifique à l'écosystème arctique est aussi utilisé quand les observations son
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41

Llopart, Serra Jaume. "Storfjorden Trough Mouth Fan (Western Barents Sea): slope failures in polar continental margins; significance of stress changes and fluid migration induced by glacial cycles." Doctoral thesis, Universitat de Barcelona, 2016. http://hdl.handle.net/10803/401559.

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The development of two Arctic Trough Mouth Fans (TMFs), the Storfjorden and Kveithola TMFs, is investigated by means of sub-bottom and seismic reflection profiles, multibeam bathymetry and sediment samples allowing their detailed stratigraphic architecture to be defined. We find that the TMFs mainly consist of an alternation of rapidly deposited glacigenic debris flows during glacial maxima and a sequence of well-layered plumites and hemipelagic sediments, which were mainly deposited during the deglaciation phase of the adjacent glacial trough. We have identified eight units above regional ref
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42

Parsons, Arthur Rost. "On the Barents Sea Polar Front in summer and interpretations of the associated regional oceanography using an Arctic Ocean general circulation model." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 1995. http://handle.dtic.mil/100.2/ADA307933.

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Dissertation (Ph.D. in Physical Oceanography) Naval Postgraduate School, September 1995.<br>Dissertation supervisor(s): Robert H. Bourke, Albert J. Semtner. "September 1995." Bibliography: p. 171-178. Also available online.
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Svyatkovskiy, Alexey. "Upper Paleozoic Carbonate Buildups of the Timan-Pechora Basin, the Sverdrup Basin and the Barents Sea as Potential Reservoirs of the Arctic." Thesis, Norges teknisk-naturvitenskapelige universitet, Institutt for geologi og bergteknikk, 2014. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-25433.

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The main objective of this work was to study the three Arctic Provinces: the Timan-Pechora Basin, the Sverdrup Basin and the Barents Sea, and make a comparison between them with a focus on the Paleozoic sediments and their potential as reservoirs based on published literature. The Upper Paleozoic carbonate reefal structures of the Timan-Pechora Basin have been proven as good reservoirs for hydrocarbon accumulation, while similar carbonate buildups of the Sverdrup Basin and the Barents Sea are still considered to be prospective. All the three provinces were at similar latitudes in Late Paleozo
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Henderson, Keith A. "An Ice Core Paleoclimate Study of Windy Dome, Franz Josef Land (Russia): Development of a Recent Climate History for the Barents Sea." The Ohio State University, 2002. http://rave.ohiolink.edu/etdc/view?acc_num=osu1392106069.

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Henderson, Keith Allen. "An ice core paleoclimate study of windy dome, Franz Josef Land (Russia) : development of a recent climate history for the Barents Sea /." The Ohio State University, 2002. http://rave.ohiolink.edu/etdc/view?acc_num=osu1486462067840906.

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Sattar, Nauman. "Mapping of Lower Cretaceous (Knurr Sandstone) turbidite lobes using Seismic Stratigraphy and prospectivity along the southern Loppa High Margin, Hammerfest Basin, Barents Sea, Norway." Thesis, Uppsala universitet, Geofysik, 2008. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-183699.

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The Hammerfest Basin was formed through downfaulting in Late Jurassic-Early Cretaceous times, allowing the deposition and preservation of Jurassic sediments which later were covered by thick Cretaceous sequences filling in the basin. This study has been conducted along the southern margin of the Loppa High to develop a complete sequence stratigraphic framework and to map Early Cretaceous Knurr Formation turbidite lobes along the slope of the High. Six seismic profiles have been selected for interpretation along the southern margin of the Loppa High on the basis of the availability of good qual
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Rodrigues, Duran Enmanuel Alexis Verfasser], Brian [Akademischer Betreuer] Horsfield, and Ralf [Akademischer Betreuer] [Littke. "Dynamics of petroleum generation, migration, accumulation and leakage : a 3D basin modelling study of the glacially influenced Southwestern Barents Sea / Enmanuel Alexis Rodrigues Duran. Gutachter: Brian Horsfield ; Ralf Littke." Berlin : Technische Universität Berlin, 2015. http://d-nb.info/1069159719/34.

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Sayago, Jhosnella [Verfasser], and Maria [Akademischer Betreuer] Mutti. "Late Paleozoic basin analysis of the Loppa High and Finnmark Platform in the Norwegian Barents Sea : integration of seismic attributes and seismic sequence stratigraphy / Jhosnella Sayago ; Betreuer: Maria Mutti." Potsdam : Universität Potsdam, 2014. http://d-nb.info/1218491280/34.

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Königstein, Stefan Verfasser], Stefan [Akademischer Betreuer] Gößling-Reisemann, Hans-Otto [Gutachter] [Pörtner, and Hauke [Gutachter] Reuter. "Modeling the impacts of ocean warming and acidification on marine fish and ecosystems in the Barents Sea / Stefan Königstein ; Gutachter: Hans-Otto Pörtner, Hauke Reuter ; Betreuer: Stefan Gößling-Reisemann." Bremen : Staats- und Universitätsbibliothek Bremen, 2017. http://d-nb.info/113760848X/34.

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Nickel, Julia Christine [Verfasser], Kai [Akademischer Betreuer] Mangelsdorf, Jens [Akademischer Betreuer] Kallmeyer, Primio Rolando [Akademischer Betreuer] Di, Brian [Akademischer Betreuer] Horsfield, and Jan [Akademischer Betreuer] Schwarzbauer. "Investigation of the activity and formation of cold seep systems in the SW Barents Sea / Julia Christine Nickel. Gutachter: Brian Horsfield ; Jan Schwarzbauer ; Jens Kallmeyer. Betreuer: Kai Mangelsdorf ; Jens Kallmeyer ; Rolando di Primio." Berlin : Technische Universität Berlin, 2014. http://d-nb.info/1066162123/34.

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