Russia and the Arctic: the New Great Game 1 Dr Mark a Smith
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Northern Sea Route Cargo Flows and Infrastructure- Present State And
Northern Sea Route Cargo Flows and Infrastructure – Present State and Future Potential By Claes Lykke Ragner FNI Report 13/2000 FRIDTJOF NANSENS INSTITUTT THE FRIDTJOF NANSEN INSTITUTE Tittel/Title Sider/Pages Northern Sea Route Cargo Flows and Infrastructure – Present 124 State and Future Potential Publikasjonstype/Publication Type Nummer/Number FNI Report 13/2000 Forfatter(e)/Author(s) ISBN Claes Lykke Ragner 82-7613-400-9 Program/Programme ISSN 0801-2431 Prosjekt/Project Sammendrag/Abstract The report assesses the Northern Sea Route’s commercial potential and economic importance, both as a transit route between Europe and Asia, and as an export route for oil, gas and other natural resources in the Russian Arctic. First, it conducts a survey of past and present Northern Sea Route (NSR) cargo flows. Then follow discussions of the route’s commercial potential as a transit route, as well as of its economic importance and relevance for each of the Russian Arctic regions. These discussions are summarized by estimates of what types and volumes of NSR cargoes that can realistically be expected in the period 2000-2015. This is then followed by a survey of the status quo of the NSR infrastructure (above all the ice-breakers, ice-class cargo vessels and ports), with estimates of its future capacity. Based on the estimated future NSR cargo potential, future NSR infrastructure requirements are calculated and compared with the estimated capacity in order to identify the main, future infrastructure bottlenecks for NSR operations. The information presented in the report is mainly compiled from data and research results that were published through the International Northern Sea Route Programme (INSROP) 1993-99, but considerable updates have been made using recent information, statistics and analyses from various sources. -
Bathymetry and Deep-Water Exchange Across the Central Lomonosov Ridge at 88–891N
ARTICLE IN PRESS Deep-Sea Research I 54 (2007) 1197–1208 www.elsevier.com/locate/dsri Bathymetry and deep-water exchange across the central Lomonosov Ridge at 88–891N Go¨ran Bjo¨rka,Ã, Martin Jakobssonb, Bert Rudelsc, James H. Swiftd, Leif Andersone, Dennis A. Darbyf, Jan Backmanb, Bernard Coakleyg, Peter Winsorh, Leonid Polyaki, Margo Edwardsj aGo¨teborg University, Earth Sciences Center, Box 460, SE-405 30 Go¨teborg, Sweden bDepartment of Geology and Geochemistry, Stockholm University, Stockholm, Sweden cFinnish Institute for Marine Research, Helsinki, Finland dScripps Institution of Oceanography, University of California San Diego, La Jolla, CA, USA eDepartment of Chemistry, Go¨teborg University, Go¨teborg, Sweden fDepartment of Ocean, Earth, & Atmospheric Sciences, Old Dominion University, Norfolk, USA gDepartment of Geology and Geophysics, University of Alaska, Fairbanks, USA hPhysical Oceanography Department, Woods Hole Oceanographic Institution, Woods Hole, MA, USA iByrd Polar Research Center, Ohio State University, Columbus, OH, USA jHawaii Institute of Geophysics and Planetology, University of Hawaii, HI, USA Received 23 October 2006; received in revised form 9 May 2007; accepted 18 May 2007 Available online 2 June 2007 Abstract Seafloor mapping of the central Lomonosov Ridge using a multibeam echo-sounder during the Beringia/Healy–Oden Trans-Arctic Expedition (HOTRAX) 2005 shows that a channel across the ridge has a substantially shallower sill depth than the 2500 m indicated in present bathymetric maps. The multibeam survey along the ridge crest shows a maximum sill depth of about 1870 m. A previously hypothesized exchange of deep water from the Amundsen Basin to the Makarov Basin in this area is not confirmed. -
Main Themes Identified for 5Th International Arctic Forum The
Main themes identified for 5th International Arctic Forum The business programme working group of the Organizing Committee of the 5th ‘Arctic: Territory of Dialogue’ International Arctic Forum held a meeting in Moscow chaired by Adviser to the Russian President Anton Kobyakov. The meeting was attended by representatives of agencies and institutions involved in organizing the event and creating its business programme. The main theme of the upcoming Forum is ‘The Arctic. An Ocean of Opportunities’. The business programme will consist of three sections: ‘Coastal Territories’, ‘The Open Ocean’, and ‘Sustainable Development’. The central event will be the plenary session attended by Russian President Vladimir Putin. “The programme of the 2019 International Arctic Forum will cover the full range of focuses for the development of the Arctic regions. Experts invited to take part in the Forum’s sessions and discussions will devote attention to both the current state of affairs and the immediate prospects for using these territories to develop industry, energy, construction, shipping, tourism, education, research, and other sectors. I am certain that the topics raised at this international discussion platform will provide an impetus for the further development of the Arctic and the full use of the enormous opportunities offered by this region”, Adviser to the Russian President Anton Kobyakov said. At the same time, Russian Presidential Aide Igor Levitin presented information about the need to invite representatives of the Indian government and business circles to take part in the Forum in order to discuss issues concerning the development of trade and economic relations on an international scale as part of the project to develop the North–South International Transport Corridor. -
Age and Origin of the Lomonosov Ridge: a Key Continental Fragment in Arctic Ocean Reconstructions
Geophysical Research Abstracts Vol. 17, EGU2015-10207-1, 2015 EGU General Assembly 2015 © Author(s) 2015. CC Attribution 3.0 License. Age and origin of the Lomonosov Ridge: a key continental fragment in Arctic Ocean reconstructions Christian Marcussen, Christian Knudsen, John R. Hopper, Thomas Funck, Jon R. Ineson, and Morten Bjerager Geological Survey of Denmark and Greenland (GEUS), Copenhagen, Denmark The Lomonosov Ridge is a trans-oceanic seafloor high that separates the Eurasia Basin from the Amerasia Basin. It extends for a distance of almost 1800 km across the Arctic Ocean from the Lincoln Shelf off Greenland and Canada to the East Siberian Shelf. Although known from the ACEX drilling expedition to be a sliver of continental crust, it remains an enigmatic feature and many details of its history are unknown. In the summer of 2012, GEUS recovered dredge samples from two locations along the flank of the ridge facing the Eurasian Basin. The samples comprise 100 kg and 200 kg of rocks and rock pieces ranging in size from 0.1 to 80 kg which were recovered from two different scarps associated with rotated continental fault blocks. A significant quantity of rocks with identical structures and isotopic fingerprints show that they formed at the same time and from the same geological material. This combined with the broken and angular nature of many of the pieces recovered indicates that the material is from in situ bedrock and does not represent dropstones brought to the area by drifting ice. Two main sedimentary rock types were recovered - an arkosic metasedimentary rock, and a quartz rich non-metamorphic sandstone. -
Joint Barents Transport Plan Proposals for Development of Transport Corridors for Further Studies
Joint Barents Transport Plan Proposals for development of transport corridors for further studies September 2013 Front page photos: Kjetil Iversen, Rune N. Larsen and Sindre Skrede/NRK Table of Contents Table Summary 7 1 Introduction 12 1.1 Background 12 1.2 Objectives and members of the Expert Group 13 1.3 Mandate and tasks 14 1.4 Scope 14 1.5 Methodology 2 Transport objectives 15 2.1 National objectives 15 2.2 Expert Group’s objective 16 3 Key studies, work and projects of strategic importance 17 3.1 Multilateral agreements and forums for cooperation 17 3.2 Multilateral projects 18 3.4 National plans and studies 21 4 Barents Region – demography, climate and main industries 23 4.1 Area and population 23 4.2 Climate and environment 24 4.3 Overview of resources and key industries 25 4.4 Ores and minerals 25 4.5 Metal industry 27 4.6 Seafood industry 28 4.7 Forest industry 30 4.8 Petroleum industry 32 4.9 Tourism industry 35 4.10 Overall transport flows 37 4.11 Transport hubs 38 5 Main border-crossing corridors in the Barents Region 40 5.1 Corridor: “The Bothnian Corridor”: Oulu – Haparanda/Tornio - Umeå 44 5.2 Corridor: Luleå – Narvik 49 5.3 Corridor: Vorkuta – Syktyvkar – Kotlas – Arkhangelsk - Vartius – Oulu 54 5.4 Corridor: “The Northern Maritime Corridor”: Arkhangelsk – Murmansk – The European Cont. 57 5.5 Corridor: “The Motorway of the Baltic Sea”: Luleå/Kemi/Oulu – The European Continent 65 5.6 Corridor: Petrozavodsk – Murmansk – Kirkenes 68 5.7 Corridor: Kemi – Salla – Kandalaksha 72 5.8 Corridor: Kemi – Rovaniemi – Kirkenes 76 -
MARITIME ACTIVITY in the HIGH NORTH – CURRENT and ESTIMATED LEVEL up to 2025 MARPART Project Report 1
MARITIME ACTIVITY IN THE HIGH NORTH – CURRENT AND ESTIMATED LEVEL UP TO 2025 MARPART Project Report 1 Authors: Odd Jarl Borch, Natalia Andreassen, Nataly Marchenko, Valur Ingimundarson, Halla Gunnarsdóttir, Iurii Iudin, Sergey Petrov, Uffe Jacobsen and Birita í Dali List of authors Odd Jarl Borch Project Leader, Nord University, Norway Natalia Andreassen Nord University, Norway Nataly Marchenko The University Centre in Svalbard, Norway Valur Ingimundarson University of Iceland Halla Gunnarsdóttir University of Iceland Iurii Iudin Murmansk State Technical University, Russia Sergey Petrov Murmansk State Technical University, Russia Uffe Jakobsen University of Copenhagen, Denmark Birita í Dali University of Greenland 1 Partners MARPART Work Package 1 “Maritime Activity and Risk” 2 THE MARPART RESEARCH CONSORTIUM The management, organization and governance of cross-border collaboration within maritime safety and security operations in the High North The key purpose of this research consortium is to assess the risk of the increased maritime activity in the High North and the challenges this increase may represent for the preparedness institutions in this region. We focus on cross-institutional and cross-country partnerships between preparedness institutions and companies. We elaborate on the operational crisis management of joint emergency operations including several parts of the preparedness system and resources from several countries. The project goals are: • To increase understanding of the future demands for preparedness systems in the High North including both search and rescue, oil spill recovery, fire fighting and salvage, as well as capacities fighting terror or other forms of destructive action. • To study partnerships and coordination challenges related to cross-border, multi-task emergency cooperation • To contribute with organizational tools for crisis management Project characteristics: Financial support: -Norwegian Ministry of Foreign Affairs, -the Nordland county Administration -University partners. -
Argus Nefte Transport
Argus Nefte Transport Oil transportation logistics in the former Soviet Union Volume XVI, 5, May 2017 Primorsk loads first 100,000t diesel cargo Russia’s main outlet for 10ppm diesel exports, the Baltic port of Primorsk, shipped a 100,000t cargo for the first time this month. The diesel was loaded on 4 May on the 113,300t Dong-A Thetis, owned by the South Korean shipping company Dong-A Tanker. The 100,000t cargo of Rosneft product was sold to trading company Vitol for delivery to the Amsterdam-Rotter- dam-Antwerp region, a market participant says. The Dong-A Thetis was loaded at Russian pipeline crude exports berth 3 or 4 — which can handle crude and diesel following a recent upgrade, and mn b/d can accommodate 90,000-150,000t vessels with 15.5m draught. 6.0 Transit crude Russian crude It remains unclear whether larger loadings at Primorsk will become a regular 5.0 occurrence. “Smaller 50,000-60,000t cargoes are more popular and the terminal 4.0 does not always have the opportunity to stockpile larger quantities of diesel for 3.0 export,” a source familiar with operations at the outlet says. But the loading is significant considering the planned 10mn t/yr capacity 2.0 addition to the 15mn t/yr Sever diesel pipeline by 2018. Expansion to 25mn t/yr 1.0 will enable Transneft to divert more diesel to its pipeline system from ports in 0.0 Apr Jul Oct Jan Apr the Baltic states, in particular from the pipeline to the Latvian port of Ventspils. -
The Antarctic Sun, January 16, 2005
Published during the austral summer at McMurdo Station, Antarctica, for the United States Antarctic Program January 16, 2005 Bye plane Russians retrieve their plane By Kristan Hutchison Sun staff Russia sent a big plane to pick up the little one this week. Artur Chilingarov, Deputy chairman of the Russian State Duma, returned to Antarctica to retrieve the biplane he had left there three years ago. He came with a group of mechanics and media on an Ilyushin 76 cargo plane, under the auspices of the Russian polar program. “We were sorry we couldn’t return the same year,” Chilingarov said through an interpreter. Chilingarov had been aboard the Antonov 3T biplane when it originally flew from Patriot Hills to South Pole in January 2002. After landing at the Pole, the biplane had a problem when the pilot tried to restart it and had to be left behind. Chilingarov was waiting at Pegasus ice runway when the biplane landed Tuesday after its 6 1/2 hour flight from the Pole. A strong tailwind helped the plane during the flight, allowing it to complete the journey without refueling. The Antonov 3T biplane landed at McMurdo the same way it originally had at the South Pole, show- ing off first by circling the runway and tipping its wings Photo by Kristan Hutchison / The Antarctic Sun at the small cluster of watchers below. Politician and polar explorer Artur Chilingarov, center, welcomes the pilot of the After celebratory hugs and photos, the Russian Antonov 3T biplane after its flight from South Pole to McMurdo Station while Michael See Biplane on page 10 Orkin, from the independent Russian station NTV, films the moment. -
Geographic Names
Commentary THE FLOOR OF THE ARCTICOCEAN: GEOGRAPHIC NAMES M. A. Beall, F. Edvalson2, K. Hunkins3, A. Molloyl, and N. Ostenso4 HE NAMING OF OCEAN FLOOR features in the Arctic seems to have been done Twithout thought to standardization in geographic nomenclature. W. K. Lyon, Director of the Arctic Sciences and Technology Division of the US.Navy Electronics Laboratory, called a meeting of the authors of the present paper to arbitrate the naming of these features in the hope that it would help to stem the proliferation of new namesand to standardize the names of the major features. The decisions of the meeting which was held in San Diego on 10 and 11 January 1966 were based on the following criteria: 1. Consistency with the Undersea terms and definitions proposed by the Advisory Committee on Undersea Features to the U.S. Board on Geo- graphicNames (Washington, D.C.: 1964) andLimits of Oceans and Seas, InternationalHydrographic Bureau Special PublicationNo. 23 (Monte Carlo: 1953) 2. Common usage 3. Priority of discovery or naming 4. Association withestablished geographic features 5. Minimizing ambiguity Fifty-four major features were discussed. Table 1 lists the names considered, the final suggested name, the approximate location, and the status of the name with the U.S. Board on Geographic Names and the International Hydrographic Bureau. The final suggested names represent the majority decision of the authors but it should be noted that in certain cases there was not complete unanimity. For the most part, however, it it felt that the accepted names should raise little controversy. The authors will endeavour to use the final suggested namesin future publications, and it is hoped that other investigatorswill find them suitable for their use. -
Redacted for Privacy Abstract Approved: John V
AN ABSTRACT OF THE THESIS OF MIAH ALLAN BEAL for the Doctor of Philosophy (Name) (Degree) in Oceanography presented on August 12.1968 (Major) (Date) Title:Batymety and_Strictuof_thp..4rctic_Ocean Redacted for Privacy Abstract approved: John V. The history of the explordtion of the Central Arctic Ocean is reviewed.It has been only within the last 15 years that any signifi- cant number of depth-sounding data have been collected.The present study uses seven million echo soundings collected by U. S. Navy nuclear submarines along nearly 40, 000 km of track to construct, for the first time, a reasonably complete picture of the physiography of the basin of the Arctic Ocean.The use of nuclear submarines as under-ice survey ships is discussed. The physiography of the entire Arctic basin and of each of the major features in the basin are described, illustrated and named. The dominant ocean floor features are three mountain ranges, generally paralleling each other and the 40°E. 140°W. meridian. From the Pacific- side of the Arctic basin toward the Atlantic, they are: The Alpha Cordillera; The Lomonosov Ridge; andThe Nansen Cordillera. The Alpha Cordillera is the widest of the three mountain ranges. It abuts the continental slopes off the Canadian Archipelago and off Asia across more than550of longitude on each slope.Its minimum width of about 300 km is located midway between North America and Asia.In cross section, the Alpha Cordillera is a broad arch rising about two km, above the floor of the basin.The arch is marked by volcanoes and regions of "high fractured plateau, and by scarps500to 1000 meters high.The small number of data from seismology, heat flow, magnetics and gravity studies are reviewed.The Alpha Cordillera is interpreted to be an inactive mid-ocean ridge which has undergone some subsidence. -
Quaternary Stratigraphy of the Northwind Ridge, Arctic Ocean
Quaternary Stratigraphy of the Northwind Ridge, Arctic Ocean THESIS Presented in Partial Fulfillment of the Requirements for the Degree Master of Science in the Graduate School of The Ohio State University By Kevin Allen Crawford B.S. Graduate Program in Geological Sciences The Ohio State University 2010 Master's Examination Committee: Peter-Noel Webb, Advisor Leonid Polyak Lawrence A. Krissek Copyright by Kevin A Crawford 2010 Abstract The Arctic Ocean plays an important role in modulating the world‘s climate. Changes in sea-ice albedo and the export of freshwater into the North Atlantic could have serious repercussions to the climate patterns far beyond the Arctic. To understand fully the impacts of the retreating sea-ice cover and the warming Arctic Ocean we need to look into the past for clues. Paleoenvironments of the Arctic Ocean can be reconstructed by using sea-floor sediment constituents, such as paleobiological and mineral components as well as chemical and paleomagnetic parameters. Three cores raised from the Northwind Ridge, north of the Alaskan continental margin, were chosen to investigate sedimentary patterns and related paleoenvironments in the western Arctic Ocean across a time frame from the Holocene to estimated early Pleistocene. These cores show a range of sedimentation rates decreasing from south to north, thus allowing a development of a relatively high-resolution Upper Quaternary stratigraphy at the southern part of the ridge and a lower-resolution, yet longer stratigraphy for its northern part. In addition to this long stratigraphic coverage, the northern core has well-preserved calcareous microfauna, which provides new insights into paleoceanographic environments. -
On Thin Ice? (Mis)Interpreting Russian Policy in the High North Roderick Kefferpütz
No. 205/February 2010 On Thin Ice? (Mis)interpreting Russian Policy in the High North Roderick Kefferpütz limate change in the Arctic is expected to make the ice cap dwindling to a record-low minimum extent the region a lot busier as new strategic of 4.3 million square km in September 2007.2 resources become available. The Russian C These developments open up an array of intractable Federation is a key player in this context, having put challenges, including threats to biodiversity and the forth a comprehensive Arctic strategy. Russian policy traditional way of life of autochthon communities in towards the so-called High North, however, is the Arctic region. Of particular danger to global oftentimes not seen in its entirety and has received a environmental stability, however, is the threat to low- plethora of criticism in the Western media and foreign lying coastal regions posed by rising sea levels. This policy community. This paper aims to contribute to a would not only have immense political, environmental better understanding of Russian actions in the High and social consequences; the economic effects would North by providing a succinct overview of Russian also be tremendous. According to Allianz financial policies in the region and identifying the fundamental services, a rise of half a metre by the middle of this rationale behind them. The paper concludes that century could put at risk more than 28 trillion dollars’ Russia’s Arctic policy is not only a lot more nuanced worth of assets in the world’s largest coastal cities.3 In but also not very different from the policies conducted addition, increasing temperatures in this volatile region by other riparian states.