Littérature scientifique sur le sujet « Barents-Kara »
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Articles de revues sur le sujet "Barents-Kara"
Suslova, Anna A., Alina V. Mordasova, Antonina V. Stoupakova, Rinar M. Gilaev, Yury A. Gatovsky, Nataliya I. Korobova, Arsen R. Gumerov, Timur R. Sakhabo et Tatyana O. Kolesnikova. « Structure and petroleum prospects of the northern part of the Barents-Kara Sea region ». Georesursy 25, no 2 (30 juin 2023) : 47–63. http://dx.doi.org/10.18599/grs.2023.2.4.
Texte intégralBakanev, S. V., et V. A. Pavlov. « Comparative Analysis of Morphometric and Reproductive Parameters of Snow Crab (<i>Chionoecetes opilio</i>) of the Kara and Barents Seas ». Океанология 63, no 5 (1 septembre 2023) : 762–72. http://dx.doi.org/10.31857/s0030157423050039.
Texte intégralYang, Xiao-Yi, et Xiaojun Yuan. « The Early Winter Sea Ice Variability under the Recent Arctic Climate Shift ». Journal of Climate 27, no 13 (juillet 2014) : 5092–110. http://dx.doi.org/10.1175/jcli-d-13-00536.1.
Texte intégralBelchansky, Gennady I., Ilia N. Mordvintsev, Gregory K. Ovchinnikov et David C. Douglas. « Assessing trends in Arctic sea-ice distribution in the Barents and Kara seas using the Kosmos–Okean satellite series ». Polar Record 31, no 177 (avril 1995) : 129–34. http://dx.doi.org/10.1017/s0032247400013620.
Texte intégralKlitzke, P., J. I. Faleide, M. Scheck-Wenderoth et J. Sippel. « A lithosphere-scale structural model of the Barents Sea and Kara Sea region ». Solid Earth Discussions 6, no 2 (10 juillet 2014) : 1579–624. http://dx.doi.org/10.5194/sed-6-1579-2014.
Texte intégralStoupakova, Antonina V., Maria A. Bolshakova, Anna A. Suslova, Alina V. Mordasova, Konstantin O. Osipov, Svetlana O. Kovalevskaya, Tatiana O. Kolesnikova et al. « Generation potential, distribution area and maturity of the Barents-Kara Sea source rocks ». Georesursy 23, no 2 (25 mai 2021) : 6–25. http://dx.doi.org/10.18599/grs.2021.2.1.
Texte intégralMordasova, Alina V., Antonina V. Stoupakova, Anna A. Suslova, Daria K. Ershova et Svetlana A. Sidorenko. « Conditions of formation and forecast of natural reservoirs in clinoform complex of the Lower Cretaceous of the Barents-Kara shelf ». Georesursy 21, no 2 (mai 2019) : 63–79. http://dx.doi.org/10.18599/grs.2019.2.63-79.
Texte intégralPodporin, S. A., et A. V. Kholoptsev. « Current trends of dangerous winds frequency variation in the western sector of the Russian Arctic in winter-spring period ». Vestnik Gosudarstvennogo universiteta morskogo i rechnogo flota imeni admirala S. O. Makarova 15, no 2 (26 juillet 2023) : 215–25. http://dx.doi.org/10.21821/2309-5180-2023-15-2-215-225.
Texte intégralYang, Huidi, Jian Rao, Haohan Chen, Qian Lu et Jingjia Luo. « Lagged Linkage between the Kara–Barents Sea Ice and Early Summer Rainfall in Eastern China in Chinese CMIP6 Models ». Remote Sensing 15, no 8 (17 avril 2023) : 2111. http://dx.doi.org/10.3390/rs15082111.
Texte intégralKlitzke, P., J. I. Faleide, M. Scheck-Wenderoth et J. Sippel. « A lithosphere-scale structural model of the Barents Sea and Kara Sea region ». Solid Earth 6, no 1 (12 février 2015) : 153–72. http://dx.doi.org/10.5194/se-6-153-2015.
Texte intégralThèses sur le sujet "Barents-Kara"
Van, Aalderen Victor. « Modéliser l'évolution du climat global et de la calotte eurasienne pendant la dernière déglaciation ». Electronic Thesis or Diss., université Paris-Saclay, 2023. http://www.theses.fr/2023UPASJ029.
Texte intégralThe marine West Antarctic ice sheet is characterized by being largely in contact with the ocean. The latest observations reveal an acceleration in its mass loss over the last few decades, mainly due to increased melting under floating ice shelves. However, its future evolution remains highly uncertain, due to our poor understanding of the physical processes at play between the ice sheet and the ocean.The last deglaciation (21 ka-11 ka) is one of the most recent major climatic changes in our history. This period is marked by an increase in global atmospheric temperatures and the melting of the North American and Eurasian ice sheets. The study of the Barents-Kara Ice Sheet (BKIS), which covered the Barents and Kara Seas during the Last Glacial Maximum (LGM, 21 ka) and was an integral part of the Eurasian Ice Sheet, is of particular interest because of its common features with present-day West Antarctica. Identifying the mechanisms responsible for its retreat allows to provide information to better understand the West Antarctic behavior within under present and future climatic conditions.The impact of climate on the evolution of a marine ice sheet depends on two main processes: The surface mass balance, depending on atmospheric temperatures and precipitation, and melting under floating ice, related to oceanic temperatures and salinity. In order to identify the mechanisms triggering the BKIS retreat, I used the GRISLI2.0 ice-sheet model to analyse the ice-sheet response to climate perturbations at the LGM. This study highlighted the key role of atmospheric temperatures in triggering the melting of the ice sheet via surface melting, while ocean temperatures had only a limited impact despite a large part of BKIS being in contact with the ocean. I also identified that the total retreat of BKIS could be attributed to a mechanical instability at the grounding line, caused by a decrease in ice thickness resulting from an increase in surface melting.In order to better understand the impact of ice sheets on the global climate, I have also carried out the first transient simulation of the last deglaciation with the IPSL-CM5A2 model, modifying the geometry of the ice sheets provided by the GLAC-1D reconstruction at some key periods. The simulations show a warming trend in line with the reconstructions, particularly during MWP1A, which was characterised by an abrupt rise in atmospheric temperatures. Using sensitivity experiments, I have shown that changes in the ice sheet geometry have contributed to the increase in atmospheric temperatures via temperature-altitude feedbacks and the albedo effect. Moreover, I have shown that ocean dynamics have been significantly altered by freshwater fluxes from the melting ice sheets. This has led to a weakening of the strength of the Atlantic Meridional Overturning Circulation and a reduction of its deepening, resulting in a warming slowdown, mainly located in the North Atlantic Ocean. In addition, the IPSL-CM5A2 experiments all simulate a shutdown of the Antarctic bottom water circulation at the onset of MWP1A, leading to a significant cooling of about 100 years in the Amundsen Sea, followed by a restart of this circulation.This work is contributing to a better understanding of the complex mechanisms governing the dynamics of the ice sheets and their interaction with the climate, while also providing a basis for anticipating the consequences of current and future climate change, particularly in West Antarctica
Seidenglanz, Anne <1985>. « 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.
Texte intégralKlitzke, Peter [Verfasser], Magdalena [Akademischer Betreuer] Scheck-Wenderoth et 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.
Texte intégralAnselme, Brice. « Contribution de l'imagerie satellitaire visible, proche infrarouge et infrarouge thermique, à l'étude des mers arctiques eurasiatiques ». Phd thesis, Paris 4, 1997. https://tel.archives-ouvertes.fr/tel-00955324.
Texte intégralThe overall objective of our work was to improve the knowledge of the arctic marine environment. Using satellite remote sensing operating in the visible, near infrared and thermal infrared, we studied oceanic surface structures over the Barents and Kara seas, as well as in the southern part of the Barents sea. In situ measurements obtained from oceanographic campaigns allowed us to validate the algorithms we used for image processing and helped us in analyzing the images. We studied both biological and physical oceanic structures. Concerning primary production, we showed in which areas and when phytoplanktonic bloom start to develop. We also emphasized the areas where thermal and hydrological fronts appear, sea ice drift and its relationship to surface currents, as well as the transport of sediments and associated pollutants by rivers and their outflow distribution patterns into the sea. The final goal of our work was to outline which areas of the eurasiatic arctic seas are the most sensitive and exposed if a pollution should occur. We finally concluded that two areas were particularly vulnerable: the marginal sea ice zone in the northern Barents sea that supports large part of the phytoplanktonic ecosystem, source of the food chain. Due to the intensity and very short timing of the phytoplanktonic bloom in that area, a pollution could have serious consequences there. Important exchange of water masses and ice, potentially contaminated, occur in the southeastern part of the Barents sea, which constitute a large refuge for marine mammals and migratory birds. Concerns about oil and natural gas exploitation should lead future investigations to focus on monitoring of both areas
Livres sur le sujet "Barents-Kara"
Knies, Jochen. Spätquartäre Paläoumweltbedingungen am nördlichen Kontinentalrand des Barents-und Kara-See : Eine Multi-Parameter-Analyse = Late Quaternary paleoenvironment along the northern Barents and Kara seas continental margin : a multi parameter analysis. Bremerhaven : Alfred-Wegener-Institut für Polar- und Meeresforschung, 1999.
Trouver le texte intégralBakken, Vidar. Seabird colony databases of the Barents sea region and the Kara sea : Vidar Bakken, editor. 2e éd. Tromsø, Norway : Norsk polarinstitutt, 2002.
Trouver le texte intégralBiological Atlas of the Arctic Seas 2000 : Plankton of the Barents and Kara Seas, International Ocean Atlas Series, V.2, 2000. [S.l : s.n., 2001.
Trouver le texte intégralChapitres de livres sur le sujet "Barents-Kara"
Zenkovich, V., et Y. Shuysky. « USSR--White, Barents, and Kara Seas ». Dans The GeoJournal Library, 41–46. Dordrecht : Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-2999-9_7.
Texte intégralPredovsky, A. A., et V. V. Lyubtsov. « The Kara-Barents Sea Shelf and Its Provinces ». Dans Social and Environmental Impacts in the North : Methods in Evaluation of Socio-Economic and Environmental Consequences of Mining and Energy Production in the Arctic and Sub-Arctic, 25–34. Dordrecht : Springer Netherlands, 2003. http://dx.doi.org/10.1007/978-94-007-1054-2_3.
Texte intégralSpesivtsev, V. I. « The Cryolithozone of the Shelf of Barents and Kara Sea ». Dans Permafrost Response on Economic Development, Environmental Security and Natural Resources, 105–34. Dordrecht : Springer Netherlands, 2001. http://dx.doi.org/10.1007/978-94-010-0684-2_9.
Texte intégralPoplavsky, E. I., A. M. Kuznetsova, A. S. Dosaev et Yu I. Troitskaya. « Trends in Barents and Kara Sea Areas from Reanalysis Data ». Dans Springer Geology, 73–77. Cham : Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-16575-7_8.
Texte intégralBukatov, A. A., E. A. Pavlenko et N. M. Solovei. « Estimation of Waters Vertical Structure in the Barents and Kara Seas ». Dans Processes in GeoMedia - Volume II, 41–53. Cham : Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-53521-6_7.
Texte intégralGlukhovets, D. I., E. A. Aglova, V. A. Artemiev, O. V. Glitko, V. A. Glukhov, D. N. Deryagin, S. K. Klimenko, M. A. Pavlova et I. V. Sahling. « Results of Hydrooptical Field Studies in the Barents and Kara Seas in September 2022 ». Dans Springer Proceedings in Earth and Environmental Sciences, 439–45. Cham : Springer Nature Switzerland, 2023. http://dx.doi.org/10.1007/978-3-031-47851-2_53.
Texte intégralGrosswald, Mikhail G. « Extent and Melting History of the Late Weichselian Ice Sheet, the Barents-Kara Continental Margin ». Dans Ice in the Climate System, 1–20. Berlin, Heidelberg : Springer Berlin Heidelberg, 1993. http://dx.doi.org/10.1007/978-3-642-85016-5_1.
Texte intégralSivintsev, Yurii V. « An Appraisal of the Radiation Hazard of Radioactive Waste Discharges in the Kara and Barents Seas ». Dans Assessing the Risks of Nuclear and Chemical Contamination in the former Soviet Union, 85–100. Dordrecht : Springer Netherlands, 1996. http://dx.doi.org/10.1007/978-94-009-1645-6_9.
Texte intégralShevchenko, V. P., A. P. Lisitzin, R. Stein, V. V. Serova, A. B. Isaeva et N. V. Politova. « The Composition of the Coarse Fraction of Aerosols in the Marine Boundary Layer over the Laptev, Kara and Barents Seas ». Dans Land-Ocean Systems in the Siberian Arctic, 53–58. Berlin, Heidelberg : Springer Berlin Heidelberg, 1999. http://dx.doi.org/10.1007/978-3-642-60134-7_6.
Texte intégralFonnum, F., S. Hoibråten, P. Thoresen et O. Andreas Nedregård. « The NATO/CCMS/NACC Pilot Study on Cross-Border Radioactive Contamination Emanating from Defense-Related Installations in the Barents and the Kara Sea ». Dans Nuclear Submarine Decommissioning and Related Problems, 331–34. Dordrecht : Springer Netherlands, 1996. http://dx.doi.org/10.1007/978-94-009-1758-3_40.
Texte intégralActes de conférences sur le sujet "Barents-Kara"
Mironcheva, E., P. Safronova, P. Golynchik, M. Ogarkova, A. Stoupakova, E. Henriksen et B. Rafaelsen. « Barents-Kara Region Palaeozoic-Mesozoic Hydrocarbon Complexes ». Dans 69th EAGE Conference and Exhibition incorporating SPE EUROPEC 2007. European Association of Geoscientists & Engineers, 2007. http://dx.doi.org/10.3997/2214-4609.201401825.
Texte intégralFomina, E., T. Kirillova - Pokrovskaya et S. Pavlov. « The Structure of the Barents - Kara Continental Margin ». Dans Saint Petersburg 2018. Netherlands : EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201800303.
Texte intégralShilin, Mikhail, Mikhail Shilin, Denis Alexeev, Denis Alexeev, Vladimir Zhigulski, Vladimir Zhigulski, Kirill Petrov et al. « HIERARCHICAL REGIONALIZATION SYSTEM FOR BARENTS AND KARA SEAS IN CONNECTION WITH THE MULTI-LEVEL ENVIRONMENTAL MONITORING OF HYDRO-TECHNICAL MACRO-PROJECTS ». Dans Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b937049d462.28996151.
Texte intégralShilin, Mikhail, Mikhail Shilin, Denis Alexeev, Denis Alexeev, Vladimir Zhigulski, Vladimir Zhigulski, Kirill Petrov et al. « HIERARCHICAL REGIONALIZATION SYSTEM FOR BARENTS AND KARA SEAS IN CONNECTION WITH THE MULTI-LEVEL ENVIRONMENTAL MONITORING OF HYDRO-TECHNICAL MACRO-PROJECTS ». Dans Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.21610/conferencearticle_58b43157e4a1d.
Texte intégralVergun, Alexey, Alisa Baranskaya, Nataliya Belova Belova, Anatoly Kamalov, Osip Kokin, Dmitry Kuznetsov, Nataliya Shabanova et Stanislav Ogorodov. « Coastal Dynamics Monitoring at the Barents and Kara Seas ». Dans SPE Arctic and Extreme Environments Technical Conference and Exhibition. Society of Petroleum Engineers, 2013. http://dx.doi.org/10.2118/166927-ms.
Texte intégralLiu, Jianfei, Guoqing Feng, Huilong Ren, Wenjia Hu et Yuwei Sun. « Design Optimization of Ship’s Bow Sailing in Kara Sea and Barents Sea ». Dans ASME 2019 38th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2019. http://dx.doi.org/10.1115/omae2019-95586.
Texte intégralVergun, Alexey, Alisa Baranskaya, Nataliya Belova Belova, Anatoly Kamalov, Osip Kokin, Dmitry Kuznetsov, Nataliya Shabanova et Stanislav Ogorodov. « Coastal Dynamics Monitoring at the Barents and Kara Seas (Russian) ». Dans SPE Arctic and Extreme Environments Technical Conference and Exhibition. Society of Petroleum Engineers, 2013. http://dx.doi.org/10.2118/166927-ru.
Texte intégralKunitsyn, A. V., et V. B. Piip. « Geology Aspects of Barents-Kara Region Based on Deep Seismic Sounding ». Dans Saint Petersburg 2008. Netherlands : EAGE Publications BV, 2008. http://dx.doi.org/10.3997/2214-4609.20146908.
Texte intégralNikishin, V. A., N. A. Malyshev, A. A. Valiuscheva, D. Y. Golovanov, L. N. Kleschina, V. A. Nikitina, A. M. Nikishin, G. V. Ulianov et D. E. Cherepanov. « The Geological Aspects of Evolution the North Kara Basin and East Barents Megabasin ». Dans 7th EAGE Saint Petersburg International Conference and Exhibition. Netherlands : EAGE Publications BV, 2016. http://dx.doi.org/10.3997/2214-4609.201600176.
Texte intégralVelikhov, Evgeny Pavlovich, Vyacheslav Petrovich Kuznetsov, Vladimir Ivanovich Makarov, Vladimir Vladimirovich Mikhailichenko, Stanislav Alexandrovich Lavkovskiy et Ivan Fedorovich Glumov. « What’s Going on in the Russian Arctic ». Dans SNAME 9th International Conference and Exhibition on Performance of Ships and Structures in Ice. SNAME, 2010. http://dx.doi.org/10.5957/icetech-2010-186.
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