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The Soviet Doctrine of the Closed Sea
The Soviet Doctrine of the Closed Sea JOSEPH J. DARBY* The Soviet Union's maritime borders include several enclosed and semi-enclosed seas. In order to strengthen its military defenses, Russian jurists, both Tsarist and Soviet, developed and offered to the community of nations the doctrine of the closed sea. According to this doctrine, which has never become part of customary inter- national law, the warships of all nonlittoral countries of certain designated peripheralseas would have no right to enter and navi- gate on those seas. Professor Darby analyzes the application of the doctrine to one of the most important of the peripheralseas on the borders of the USSR, namely the Black Sea, in light of recent history and contemporary developments in the Law of the Sea. SOVIET PUBLIC INTERNATIONAL LAW Writing in 1959, Gregorii Tunkin, who is generally recognized as the most authoritative spokesman of Soviet international law, stated that the international law position of a country is "determined by the basic principles of its foreign policy."' As far as it goes, this state- ment appears to be an accurate reflection of how the leaders of the Soviet Union perceive the nature and function of international law. International law is a means to be used by legal technicians to ad- vance the foreign policy goals of the Soviet state. Soviet legal schol- ars, whose writings are often obtuse and highly generalized, have al- ways been quite clear on this-no rule of international law is binding on the Soviet Union unless, through an unequivocal sovereign act, the Soviet Union has expressly and formally given its consent to be bound by it. -
Radioactivity in the Arctic Seas
IAEA-TECDOC-1075 XA9949696 Radioactivity in the Arctic Seas Report for the International Arctic Seas Assessment Project (IASAP) ffl INTERNATIONAL ATOMIC ENERGY AGENCA / Y / 1JrrziZr^AA 30-16 The originating Section of this publication in the IAEA was: Radiometrics Section International Atomic Energy Agency Marine Environment Laboratory B.P. 800 MC 98012 Monaco Cedex RADIOACTIVITY IN THE ARCTIC SEAS IAEA, VIENNA, 1999 IAEA-TECDOC-1075 ISSN 1011-4289 ©IAEA, 1999 Printe IAEe th AustriAn y i d b a April 1999 FOREWORD From 199 o 1993t e Internationa6th l Atomic Energy Agency's Marine Environment Laboratory (IAEA-MEL s engage IAEA'e wa ) th n di s International Arctic Seas Assessment Project (IASAP whicn i ) h emphasi bees ha sn place criticaa n do l revie f environmentawo l conditions in the Arctic Seas. IAEA-MEe Th L programme, organize framewore th n dIASAi e th f ko P included: (i) an oceanographic and an ecological description of the Arctic Seas; provisioe th (ii )centra a f no l database facilitIASAe th r yfo P programm collectione th r efo , synthesi interpretatiod san datf nmarino n ao e radioactivit Arctie th n yi c Seas; (iii) participation in official expeditions to the Kara Sea organized by the joint Russian- Norwegian Experts Group (1992, 1993 and 1994), the Russian Academy of Sciences (1994), and the Naval Research Laboratory and Norwegian Defence Research Establishment (1995); (iv) assistance wit d n laboratorsiti han u y based radiometric measurement f curreno s t radionuclide concentrations in the Kara Sea; (v) organization of analytical quality assurance intercalibration exercises among the participating laboratories; (vi) computer modellin e potentiath f o g l dispersa f radionuclideo l s released froe mth dumped f assessmeno wast d associatee ean th f o t d radiological consequencee th f o s disposals on local, regional and global scales; (vii) in situ and laboratory based assessment of distribution coefficients (Kd) and concentration factor sArctie (CFth r c)fo environment. -
For Classification and Construction of Ships (Rccs)
RULES FOR CLASSIFICATION AND CONSTRUCTION OF SHIPS (RCCS) Part 0 CLASSIFICATION 4 RCCS. Part 0 “Classification” 1 GENERAL PROVISIONS 1.1 The present Part of the Rules for the materials for the ships except for small craft Classification and Construction of Inland and used for non-for-profit purposes. The re- Combined (River-Sea) Navigation Ships (here quirements of the present Rules are applicable and in all other Parts — Rules) defines the to passenger ships, tankers, pushboats, tug- basic terms and definitions applicable for all boats, ice breakers and industrial ships of Parts of the Rules, general procedure of ship‘s overall length less than 20 m. class adjudication and composing of class The requirements of the present Rules are formula, as well as contains information on not applicable to small craft, pleasure ships, the documents issued by Russian River Regis- sports sailing ships, military and border- ter (hereinafter — River Register) and on the security ships, ships with nuclear power units, areas and seasons of operation of the ships floating drill rigs and other floating facilities. with the River Register class. However, the River Register develops and 1.2 When performing its classification and issues corresponding regulations and other survey activities the River Register is governed standards being part of the Rules for particu- by the requirements of applicable interna- lar types of ships (small craft used for com- tional agreements of Russian Federation, mercial purposes, pleasure and sports sailing Regulations on Classification and Survey of ships, ekranoplans etc.) and other floating Ships, as well as the Rules specified in Clause facilities (pontoon bridges etc.). -
DRAINAGE BASINS of the WHITE SEA, BARENTS SEA and KARA SEA Chapter 1
38 DRAINAGE BASINS OF THE WHITE SEA, BARENTS SEA AND KARA SEA Chapter 1 WHITE SEA, BARENTS SEA AND KARA SEA 39 41 OULANKA RIVER BASIN 42 TULOMA RIVER BASIN 44 JAKOBSELV RIVER BASIN 44 PAATSJOKI RIVER BASIN 45 LAKE INARI 47 NÄATAMÖ RIVER BASIN 47 TENO RIVER BASIN 49 YENISEY RIVER BASIN 51 OB RIVER BASIN Chapter 1 40 WHITE SEA, BARENT SEA AND KARA SEA This chapter deals with major transboundary rivers discharging into the White Sea, the Barents Sea and the Kara Sea and their major transboundary tributaries. It also includes lakes located within the basins of these seas. TRANSBOUNDARY WATERS IN THE BASINS OF THE BARENTS SEA, THE WHITE SEA AND THE KARA SEA Basin/sub-basin(s) Total area (km2) Recipient Riparian countries Lakes in the basin Oulanka …1 White Sea FI, RU … Kola Fjord > Tuloma 21,140 FI, RU … Barents Sea Jacobselv 400 Barents Sea NO, RU … Paatsjoki 18,403 Barents Sea FI, NO, RU Lake Inari Näätämö 2,962 Barents Sea FI, NO, RU … Teno 16,386 Barents Sea FI, NO … Yenisey 2,580,000 Kara Sea MN, RU … Lake Baikal > - Selenga 447,000 Angara > Yenisey > MN, RU Kara Sea Ob 2,972,493 Kara Sea CN, KZ, MN, RU - Irtysh 1,643,000 Ob CN, KZ, MN, RU - Tobol 426,000 Irtysh KZ, RU - Ishim 176,000 Irtysh KZ, RU 1 5,566 km2 to Lake Paanajärvi and 18,800 km2 to the White Sea. Chapter 1 WHITE SEA, BARENTS SEA AND KARA SEA 41 OULANKA RIVER BASIN1 Finland (upstream country) and the Russian Federation (downstream country) share the basin of the Oulanka River. -
Downloaded Daily to the Geodetic Survey Division in Ottawa, Where They Are Reviewed for Quality Control, Archived, and Uploaded to the International GPS Service
Arctic Coastal Dynamics Report of the 4th International Workshop VNIIOkeangeologia, St. Petersburg (Russia), 10-13 November 2003 Edited by Volker Rachold and Georgy Cherkashov Volker Rachold, Alfred Wegener Institute, Research Unit Potsdam, Telegrafenberg A43, 14473 Potsdam, Germany Georgy Cherkashov, VNIIOkeangeologia (Institute for Geology and Mineral Resources of the Ocean), Angliysky prospect 1, 190121 St. Petersburg, Russia Preface Arctic Coastal Dynamics (ACD) is a joint project of the International Arctic Sciences Committee (IASC) and the International Permafrost Association (IPA) and a regional project of IGBP-LOICZ (International Geosphere-Biosphere Programme – Land- Ocean Interactions in the Coastal Zone). Its overall objective is to improve our understanding of circum-Arctic coastal dynamics as a function of environmental forcing, coastal geology and cryology and morphodynamic behavior. The fourth IASC-sponsored ACD workshop was held in St. Petersburg, Russia, on November 10-13, 2003. Participants from Canada (7), Germany (7), Great Britain (2), the Netherlands (1), Norway (1), Russia (32), Ukraine (1) and the United States (8) attended. During the first part of the workshop, 63 papers dealing with regional and/or circum-Arctic coastal dynamics were presented. Based on the material presented, five thematic working groups were identified: (1) GIS working group to develop of a circum-Arctic coastal GIS system, (2) coastal permafrost working group to discuss processes involved in the transition of onshore to offshore permafrost, (3) biogeochemistry working group with the focus on transport and fate of eroded material (4) biodiversity working group to initiate planning of an Arctic Coastal Biodiversity research agenda, (5) environmental data working group to discuss coastal dynamics as a function of environmental forcing. -
Chapter 4. Oil and Gas Accidents – Prevention and Liquidation
Chapter 4. Oil and gas accidents – prevention and liquidation. In this chapter we take a theoretical approach towards accidents and incidents. This reason is twofold: In Soviet times, statistics were often used as political tools, and this makes it difficult to make a completely reliable analysis. To a certain extent, this legacy still applies to Russia today. We are therefore careful not to use too many official statistics. Secondly, there is still little offshore activity in Arctic waters, thus limiting the amount of empiric data available. Nonetheless, in this chapter we examine some accidents which occurred in the Arctic, such as the Usinsk oil spill in 1994 . This chapter also describes the emergency rescue routines in Murmansk oblast, together with regulations for emergency preparedness and response for the oil and gas sector. All the information presented in this chapter is accompanied by reference data, opinions from specialists, legal notes and illustrations. Several situations are examined using Murmansk oblast as an example. 4.1. Accidents and incidents: causes and consequences Here’s a thought… Oleg Mitvol, deputy director of the Russian federal service managing the oversight of natural resources (Rosprirodnadzor) said in an interview that spills of oil and other oil products take place every two weeks in Russia, RBC Daily Russian news agency reported in September 2005. According to RBC, Russian experts estimate that 3-7 per cent of all extracted oil is lost during extraction and transportation. The official numbers are much lower. 4,1,1 Accidents involving oil pipelines In 2003, according to data from Russia’s Ministry of Civil Defence, Emergencies and Disaster Relief, there were 48 accidents on main and intrafield pipelines which led to emergency situations (compared with 55 in 2002).1 However, other sources states that the number of accidents involving oil pipelines has increased by 20% over the course of several years. -
Quternary Geology and Landforming Processes
International Field Symposium on Quaternary Geology and Landforming Processes RUSSIAN ACADEMY OF SCIENCES KOLA SCIENCE CENTRE GEOLOGICAL INSTITUTE THE PERIBALTIC GROUP OF THE INQUA SUBCOMISSION ON GLACIATION FRIENDS OF BALTIC QUATERNARY QUTERNARY GEOLOGY AND LANDFORMING PROCESSES International Field Symposium Kola Peninsula, NW Russia, September 4-9, 2005 Proceedings of the International Field Symposium APATITY 2005 __________________________________________ Kola Peninsula, NW Russia, September 4-9, 2005 International Field Symposium on Quaternary Geology and Landforming Processes Published by decision of the Presidium of the Kola Science Centre Russian Academy of Sciences UDC 551.79+551.435 QUATERNARY GEOLOGY AND LANDFORMING PROCESSES Proceedings of the International Field Symposium, Kola Peninsula, NW Russia, September 4-9, 2005. – Apatity: Print. Kola Science Centre RAS, 2005. -77 p. Organizing Committee: Felix Mitrofanov – (Chair, Member of the Russian Academy of Sciences), Albertas Bitinas (Lithuania), Marina Efimova (Russia), Tiit Hang (Estonia), Clas Hattestrand (Sweden), Vasili Kolka (Russia), Olga Korsakova (Russia), Svetlana Nikolaeva (Russia), Irina Pavlovskaya (Belarus), Jan A. Piotrowski (Denmark), Vladimir Yevzerov (Russia), Elena Zakharchenko (Russia), Vitalijs Zelchs (Latvia), Dimitry Zozulja (Russia) Editorial handling: Vasili Kolka and Olga Korsakova Sponsored by: The International Union for Quaternary Research The Geological Institute of Kola Science Centre Russian Academy of Sciense © Geological Institute KSC RAS, 2005 ©Kola Science Centre Russian Academy of Sciences, 2005 2 _________________________________________ Kola Peninsula, NW Russia, September 4-9, 2005 International Field Symposium on Quaternary Geology and Landforming Processes CONTENTS SEDIMENT-LANDFORM ASSOCIATIONS AT THE SOUTHERN MARGIN OF THE SCANDINAVIAN ICE SHEET, SOUTH SWEDISH UPLAND Helena Alexanderson 8 LITHOLOGY AND PALAEOMAGNETIC RECORD OF LATE WEICHSELIAN VARVED CLAYS FROM NW RUSSIA Vladimir G. -
Seiches in the Semiclosed Seas of the Continental Shelf
International Journal of Oceanography & Aquaculture MEDWIN PUBLISHERS ISSN: 2577-4050 Committed to Create Value for Researchers Seiches in the Semiclosed Seas of the Continental Shelf Inzhebeikin Yu I* Research Article Russian Academy of Sciences, Russia Volume 4 Issue 3 Received Date: September 18, 2020 *Corresponding author: Published Date: October 23, 2020 Center, Rostov-on-Don, Russia, Email: [email protected] Inzhebeikin Yu I, Russian Academy of Sciences, Southern Scientific DOI: 10.23880/ijoac-16000199 Abstract Seiche movements in two small areas of semi-closed seas on the Continental Shelf (the White Sea and the Sea of Azov) with very different morphometric characteristics are considered in this paper. In addition, tidal movements are highly developed in the White sea, while in the Azov sea tides are virtually absent. We’ve used morphometric characteristics of the seas, including the ones recently obtained by the Azov Sea, as well as methods of numerical hydrodynamic simulation based on the theory of shallow water, and spectral analysis of the observation data of the sea level fluctuations. Keywords: Continental Shelf; Semi-Closed Seas; White Sea; Sea Of Azov; Seiche; Numerical Hydrodynamic Simulation; Spectral Analysis; Flood Introduction located in the Northern and South-Western boundaries of the European part of Russia respectively (Figure 1). In August 2006, on the Dolzhanskaya spit of the Azov sea, the water level rose sharply, people and cars washed away in the sea, the spit broke in several places. At the same time there was no storm warning. In June 2010 on the Yeisk spit of the same sea of Azov at full calm across the sea suddenly appeared powerful current washed away children, wandering on the spit knee-deep in water. -
Council CNL(05)32 Supplementary Returns by the Russian Federation
Agenda items 6.2, 6.4(a), 6.7, 6.8(a), 7 For information Council CNL(05)32 Supplementary Returns by the Russian Federation CNL(05)32 Supplementary Returns by the Russian Federation Comment on Application of the Decision Structure for Management of Atlantic Salmon Fisheries in Russia in 2004 The Decision Structure continued to be applied for management of fisheries on 38 White Sea rivers and 37 Barents Sea rivers on the Kola Peninsula. For each river the Polar Research Institute provides advice on the abundance of spawning stock, conservation limit, and catch options. On the basis of this advice the Science and Fisheries Council makes management decisions concerning catch limits in each fishery: commercial, catch-and-retain, catch-and- release, on a river-by-river basis. Murmanrybvod (Control and Enforcement authority) details fishing regime for each river including time of fishing, fishing gears, sites, catch limit for each site. Users then base their operations on these decisions. The application of the Decision Structure was expanded in 2004 to include a number of rivers in the Archangel region, Nenets okrug, Komi Republic and Karelia. Specifically, the Decision Structure was applied to decide on management measures for the salmon fishery on the rivers Pechora, Severnaya Dvina, Onega (Archangel) and Keret (Karelian Republic). No suggestions have been made on how the Decision Structure could be improved as it requires the use of practically the same information as was provided by the control schemes and monitoring programs conducted in Russia and used previously to inform management decisions concerning salmon fisheries. Russian managers find it useful. -
Alexander P. Lisitsyn Liudmila L. Demina Editors the White Sea
The Handbook of Environmental Chemistry 82 Series Editors: Damià Barceló · Andrey G. Kostianoy Alexander P. Lisitsyn Liudmila L. Demina Editors Sedimentation Processes in the White Sea The White Sea Environment Part II The Handbook of Environmental Chemistry Founding Editor: Otto Hutzinger Editors-in-Chief: Damia Barcelo´ • Andrey G. Kostianoy Volume 82 Advisory Editors: Jacob de Boer, Philippe Garrigues, Ji-Dong Gu, Kevin C. Jones, Thomas P. Knepper, Alice Newton, Donald L. Sparks More information about this series at http://www.springer.com/series/698 Sedimentation Processes in the White Sea The White Sea Environment Part II Volume Editors: Alexander P. Lisitsyn Á Liudmila L. Demina With contributions by T. N. Alexсeeva Á D. F. Budko Á O. M. Dara Á L. L. Demina Á I. V. Dotsenko Á Y. A. Fedorov Á A. A. Klyuvitkin Á A. I. Kochenkova Á M. D. Kravchishina Á A. P. Lisitsyn Á I. A. Nemirovskaya Á Y. A. Novichkova Á A. N. Novigatsky Á A. E. Ovsepyan Á N. V. Politova Á Y. I. Polyakova Á A. E. Rybalko Á V. A. Savitskiy Á L. R. Semyonova Á V. P. Shevchenko Á M. Y. Tokarev Á A. Yu. Lein Á V. A. Zhuravlyov Á A. A. Zimovets Editors Alexander P. Lisitsyn Liudmila L. Demina Shirshov Inst. of Oceanology Shirshov Inst. of Oceanology Russian Academy of Sciences Russian Academy of Sciences Moscow, Russia Moscow, Russia ISSN 1867-979X ISSN 1616-864X (electronic) The Handbook of Environmental Chemistry ISBN 978-3-030-05110-5 ISBN 978-3-030-05111-2 (eBook) https://doi.org/10.1007/978-3-030-05111-2 Library of Congress Control Number: 2018964918 © Springer Nature Switzerland AG 2018 This work is subject to copyright. -
Finnish Botanists on the Kola Peninsula (Russia) up to 1918
Memoranda Soc. Soc. Fauna Fauna Flora Flora Fennica Fennica 89, 89: 2013 75–104. • Uotila 2013 75 Finnish botanists on the Kola Peninsula (Russia) up to 1918 Pertti Uotila Uotila, P., Finnish Museum of Natural History (Botany), P.O.Box 7, FI-00014 University of Helsinki, Finland. E-mail: [email protected] Finnish botanists actively studied the flora of Karelia (Karelian Republic) and the Kola Peninsula (Murmansk Region) when Finland was a Grand Duchy of Russia in 1809–1918. J. Fellman’s ex- peditions in 1829 were the first notable botanical expeditions to the area. Geologically and floristi- cally the area was similar to Finland, and exploring the area was considered to be a national duty for Finnish biologists. Almost 40 Finnish scientists who travelled on the Kola Peninsula collected significant amounts of herbarium specimens from there. The specimens are mostly in H, but du- plicates were distributed widely. The collectors include M. Aschan, W. M. Axelson (Linnaniemi), V. Borg (Kivilinna), M. Brenner, V. F. Brotherus, R. Envald, J. Fellman, N. I. Fellman, C. W. Fontell, E. af Hällström, H. Hollmén, P. A. Karsten, A. Osw. Kihlman (Kairamo), F. W. Klingstedt, H. Lindberg, J. Lindén, A. J. Malmberg (Mela), J. Montell, F. Nylander, J. A. Palmén, V. Pesola, P. A. Rantaniemi, J. Sahlberg, and G. Selin. A short description is given of the biographies of the most important collectors with notes on their itineraries. Details of the collections from the Kola Peninsula are mostly taken from the vascular-plant specimens kept in the Finnish main herbaria and entered in the Floristic database Kastikka of the Finnish Museum of Natural History. -
The Position of the Dialect of Varzuga in the Russian Dialect Landscape
MARGJE POST The Position of the Dialect of Varzuga in the Russian Dialect Landscape Until recently, few researchers had studied the archaic Russian dialects of the Kola Peninsula. In 2001 and 2004, slavists from the University of Tromsø carried out dialectological field work on the Ter Coast of Kola Peninsula. On our first expedition we were joined by colleagues from Moscow. In 2004, the universities of Tromsø and Bochum received funding from NFR (Norway) and DAAD (Germany) to set up a coopera- tion project for the study of the endangered Russian dialects around the White Sea. This autumn, dr. Christian Sappok from Bochum University combined his visit to Tromsø with a joint field work expedition to the villages of Varzuga and Kuzomen' on the Ter Coast. Our studies have so far resulted in a Master's thesis (Pétursdóttir 2003) and a range of short articles, part of which has been published in this journal (vols. 4, 5 and the present volume). In due course I hope to finish my PhD dissertation about the dialect of the village of Varzuga. In the present article I will discuss the position of the Varzuga dia- lect in the Russian dialect landscape. Comparisons between dialects tell us how a dialect relates to other dialects: how isolated it is, and which dialects it is most closely related to. Areal linguistic studies also give in- formation about the historical ties of the dialect and its speakers to other regions and about their cultural background. The people of Varzuga and the other villages around the White Coast lived relatively isolated from the rest of the Russian world, and their closeness to the sea, their contact with different cultures and the poor conditions for agriculture led to the development of a distinct coastal, Pomor culture.