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Regional Maps of Locations Mentioned in Global Review of The
Regional Maps of Locations Mentioned in Global Review of the Conservation Status of Monodontid Stocks These maps provide the locations of the geographic features mentioned in the Global Review of the Conservation Status of Monodontid Stocks. Figure 1. Locations associated with beluga stocks of the Okhotsk Sea (beluga stocks 1-5). Numbered locations are: (1) Amur River, (2) Ul- bansky Bay, (3) Tugursky Bay, (4) Udskaya Bay, (5) Nikolaya Bay, (6) Ulban River, (7) Big Shantar Island, (8) Uda River, (9) Torom River. Figure 2. Locations associated with beluga stocks of the Bering Sea and Gulf of Alaska (beluga stocks 6-9). Numbered locations are: (1) Anadyr River Estuary, (2) Anadyr River, (3) Anadyr City, (4) Kresta Bay, (5) Cape Navarin, (6) Yakutat Bay, (7) Knik Arm, (8) Turnagain Arm, (9) Anchorage, (10) Nushagak Bay, (11) Kvichak Bay, (12) Yukon River, (13) Kuskokwim River, (14) Saint Matthew Island, (15) Round Island, (16) St. Lawrence Island. Figure 3. Locations associated with beluga stocks of the Chukchi and Beaufort Seas, Canadian Arctic and West Greenland (beluga stocks 10-12 and 19). Numbered locations are: (1) St. Lawrence Island, (2) Kotzebue Sound, (3) Kasegaluk Lagoon, (4) Point Lay, (5) Wain- wright, (6) Mackenzie River, (7) Somerset Island, (8) Radstock Bay, (9) Maxwell Bay, (10) Croker Bay, (11) Devon Island, (12) Cunning- ham Inlet, (13) Creswell Bay, (14) Mary River Mine, (15) Elwin Bay, (16) Coningham Bay, (17) Prince of Wales Island, (18) Qeqertarsuat- siaat, (19) Nuuk, (20) Maniitsoq, (21) Godthåb Fjord, (22) Uummannaq, (23) Upernavik. Figure 4. Locations associated with beluga stocks of subarctic eastern Canada, Hudson Bay, Ungava Bay, Cumberland Sound and St. -
Data Structure
Data structure – Water The aim of this document is to provide a short and clear description of parameters (data items) that are to be reported in the data collection forms of the Global Monitoring Plan (GMP) data collection campaigns 2013–2014. The data itself should be reported by means of MS Excel sheets as suggested in the document UNEP/POPS/COP.6/INF/31, chapter 2.3, p. 22. Aggregated data can also be reported via on-line forms available in the GMP data warehouse (GMP DWH). Structure of the database and associated code lists are based on following documents, recommendations and expert opinions as adopted by the Stockholm Convention COP6 in 2013: · Guidance on the Global Monitoring Plan for Persistent Organic Pollutants UNEP/POPS/COP.6/INF/31 (version January 2013) · Conclusions of the Meeting of the Global Coordination Group and Regional Organization Groups for the Global Monitoring Plan for POPs, held in Geneva, 10–12 October 2012 · Conclusions of the Meeting of the expert group on data handling under the global monitoring plan for persistent organic pollutants, held in Brno, Czech Republic, 13-15 June 2012 The individual reported data component is inserted as: · free text or number (e.g. Site name, Monitoring programme, Value) · a defined item selected from a particular code list (e.g., Country, Chemical – group, Sampling). All code lists (i.e., allowed values for individual parameters) are enclosed in this document, either in a particular section (e.g., Region, Method) or listed separately in the annexes below (Country, Chemical – group, Parameter) for your reference. -
PDF Version Assessing the Efficiency of Gazprom Neft's Contribution
GAZPROM NEFT Gazprom Neft at a glance Sustainable development management Health and safety Commissioning Environmental safety of the Sports Complex Employee development in Yamalo-Nenets Social policy Autonomous Okrug Appendices Expanding partnership with the Yamalo-Nenets Autonomous Okrug Gazprom Neft and the Government The area of the Ice Centre totals 5,400 of the Yamalo-Nenets Autonomous square metres. The Centre will host Okrug signed a supplementary ice-hockey, figure-skating, and other agreement on partnership winter-sports training sessions in social and economic projects. and competitions. The parties will continue their cooperation to ensure The Polyarny Sports Complex will further economic development allow local residents to swim, Modern sports centres of the region, and improve quality play futsal, basketball, volleyball are an essential of life there. The agreement also and tennis, do aerobics and dance all part of development provides for the development year round. The 7,000-square-metre on Yamal. Sports of energy infrastructure and roads complex also includes a versatile facilities such as Polyarny in the Tazovsky district. gym and a weight room, an aerobics are becoming centres that studio, and a six-lane swimming pool. attract local residents The company implemented several and open up new opportunities major infrastructure projects The company has previously opened for talented children. Together in the Yamalo-Nenets Autonomous such sports facilities in Noyabrsk, with the Avangard Ice Centre, Okrug, designed to promote Myuravlenko, and Tarko-Sale. which we built nearby an attractive urban environment, Construction of the multifunctional in cooperation with regional and develop sport for children Yamal-Arena Sports Complex authorities, it marks and the general public, as part in Salekhard is continuing the completion of sports of the “Home Towns” Programme. -
Zeszyt 10. Morza I Oceany
Uwaga: Niniejsza publikacja została opracowana według stanu na 2008 rok i nie jest aktualizowana. Zamieszczony na stronie internetowej Komisji Standaryzacji Nazw Geograficznych poza Granica- mi Rzeczypospolitej Polskiej plik PDF jest jedynie zapisem cyfrowym wydrukowanej publikacji. Wykaz zalecanych przez Komisję polskich nazw geograficznych świata (Urzędowy wykaz polskich nazw geograficznych świata), wraz z aktualizowaną na bieżąco listą zmian w tym wykazie, zamieszczo- ny jest na stronie internetowej pod adresem: http://ksng.gugik.gov.pl/wpngs.php. KOMISJA STANDARYZACJI NAZW GEOGRAFICZNYCH POZA GRANICAMI RZECZYPOSPOLITEJ POLSKIEJ przy Głównym Geodecie Kraju NAZEWNICTWO GEOGRAFICZNE ŚWIATA Zeszyt 10 Morza i oceany GŁÓWNY URZĄD GEODEZJI I KARTOGRAFII Warszawa 2008 KOMISJA STANDARYZACJI NAZW GEOGRAFICZNYCH POZA GRANICAMI RZECZYPOSPOLITEJ POLSKIEJ przy Głównym Geodecie Kraju Waldemar Rudnicki (przewodniczący), Andrzej Markowski (zastępca przewodniczącego), Maciej Zych (zastępca przewodniczącego), Katarzyna Przyszewska (sekretarz); członkowie: Stanisław Alexandrowicz, Andrzej Czerny, Janusz Danecki, Janusz Gołaski, Romuald Huszcza, Sabina Kacieszczenko, Dariusz Kalisiewicz, Artur Karp, Zbigniew Obidowski, Jerzy Ostrowski, Jarosław Pietrow, Jerzy Pietruszka, Andrzej Pisowicz, Ewa Wolnicz-Pawłowska, Bogusław R. Zagórski Opracowanie Kazimierz Furmańczyk Recenzent Maciej Zych Komitet Redakcyjny Andrzej Czerny, Joanna Januszek, Sabina Kacieszczenko, Dariusz Kalisiewicz, Jerzy Ostrowski, Waldemar Rudnicki, Maciej Zych Redaktor prowadzący Maciej -
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. -
2.5.2. Alternative Construction Sites in Other Antarctic Areas
Draft Comprehensive Environmental Evaluation 2.5.2. Alternative construction sites in other Antarctic areas Other BAS placement options in other Antarctic regions were further analised, taking into consideration scientific, environmental, logistic and other aspects. However, no alternative site for BAS placement was reported to meet all the criteria to a greater extent than that at Mount Vechernyaya location selected. 2.5.3. Zero alternative (no construction) As a zero alternative option, renovation and continuation of use of the Mount Vechernyaya field base infrastructure was subject to analysis. However, continued use of the residential premises and other RAE field base infrastructure turns out to become increasingly problematic due to their deterioration and incompliance to the Antarctic environmental protection requirements. Therefore, the zero alternative option seems to be only a temporary postponement of own station construction. Unavailability of existing facilities hampers substantially the development of scientific research, increasing the number of staff involved in BAE, making the field season longer and thus jeopardising the proper implementation of the National Program in its entirety. The up-to-date station construction would benefit to friendlier environment for living and working of polar explorers and contribute to reduced impact on the environment. Research Station at Mount Vechernyaya 39 Draft Comprehensive Environmental Evaluation 3. Initial Environmental Evaluation 3.1. General geographic description and relief The natural complex known as Mount Vechernyaya is located at the western part of Enderby Land, Tala Hills (eastern part), at the coastal area of the Alasheeva Gulf, Cosmonaut Sea. It incorporates a series of rocky ridges with a dominant mountain, the Mount Vecherniaya (272.0 m), and several lower ridges, breaking through the Antarctic ice sheet on the Cosmonauts Sea shore. -
Personnel - Conflict of Interest: Clements, William” of the Philip Buchen Files at the Gerald R
The original documents are located in Box 37, folder “Personnel - Conflict of Interest: Clements, William” of the Philip Buchen Files at the Gerald R. Ford Presidential Library. Copyright Notice The copyright law of the United States (Title 17, United States Code) governs the making of photocopies or other reproductions of copyrighted material. Gerald R. Ford donated to the United States of America his copyrights in all of his unpublished writings in National Archives collections. Works prepared by U.S. Government employees as part of their official duties are in the public domain. The copyrights to materials written by other individuals or organizations are presumed to remain with them. If you think any of the information displayed in the PDF is subject to a valid copyright claim, please contact the Gerald R. Ford Presidential Library. Digitized from Box 37 of the Philip Buchen Files at the Gerald R. Ford Presidential Library MEMORANDUM NATIONAL SECURITY COUNCIL ADMINISTRATIVELY June 10, 1975 CONFIDENTIAL MEMORANDUM FOR GENERAL SCOWCROFT FROM: Mr. Clift ~......-- SUBJECT: Status of NSSM 214: "Implications of US Participation in Siberian Development" Attached is a copy of the interagency response to NSSM 214. All agencies except Defense have concurred with the principal conclusions of the response, though several have suggested minor revisions. With regard to Defense, we understand that someone at a high level (we think Deputy Secretary Clements) objected to the conclusions of the study and thereby caused the delay in the Defense response. Subsequently his objections have been overcome and the response is now on its way back through Defense channels for official concurrence. -
1 Influence of Sea Ice Anomalies on Antarctic Precipitation Using
https://doi.org/10.5194/tc-2019-69 Preprint. Discussion started: 12 June 2019 c Author(s) 2019. CC BY 4.0 License. Influence of Sea Ice Anomalies on Antarctic Precipitation Using Source Attribution Hailong Wang1*, Jeremy Fyke2,3, Jan Lenaerts4, Jesse Nusbaumer5,6, Hansi Singh1, David Noone7, and Philip Rasch1 (1) Pacific Northwest National Laboratory, Richland, WA 5 (2) Los Alamos National Laboratory, Los Alamos, NM (3) Associated Engineering, Vernon, British Columbia, Canada (4) Department of Atmospheric and Oceanic Sciences, University of Colorado at Boulder, Boulder, CO (5) NASA Goddard Institute for Space Studies, New York, NY (6) Center for Climate Systems Research, Columbia University, New York, NY 10 (7) Oregon State University, Corvallis, OR *Correspondence to: [email protected] 1 https://doi.org/10.5194/tc-2019-69 Preprint. Discussion started: 12 June 2019 c Author(s) 2019. CC BY 4.0 License. Abstract We conduct sensitivity experiments using a climate model that has an explicit water source tagging capability forced by prescribed composites of sea ice concentrations (SIC) and corresponding SSTs to understand the impact of sea ice anomalies on regional evaporation, moisture transport, and source– 5 receptor relationships for precipitation over Antarctica. Surface sensible heat fluxes, evaporation, and column-integrated water vapor are larger over Southern Ocean (SO) areas with lower SIC, but changes in Antarctic precipitation and its source attribution with SICs reflect a strong spatial variability. Among the tagged source regions, the Southern Ocean (south of 50°S) contributes the most (40%) to the Antarctic total precipitation, followed by more northerly ocean basins, most notably the S. -
Years of Sustainable Development
Years of Sustainable 20 Development NOVATEK Sustainability Report for 2014 CONTENTS Letter from the Chief Executive Officer 3 Preserving Cultural Heritage 52 Sports 52 Report and Reporting Process 6 Volunteering 53 NOVATEK`s Social Reporting Development 6 NOVATEK-Veteran Program 53 Principles for Defining Report Content 6 Report Boundary 8 Employment Practices 55 NOVATEK Group’s Structure Changes 8 Personnel 55 Corporate Technical Competency Assessment System 58 Company Profile 10 Personnel Training and Development 58 The Company’s Scope and Key Lines of Business 10 Trade Union Relations 59 Geography 10 Social Policy 59 The Company’s Structure as at 31 December 2014 13 Our Business Model 14 Procurement Practices 64 Share Capital 15 Key Approaches 64 Membership in Trade Associations 16 Supply Chain Management 64 Awards 16 Import Substitution Policy 64 Key Performance Indicators 16 Occupational Health and Safety 66 Sustainability Strategy 18 Occupational Health and Safety Goals and Objectives 66 Special Assessment of Working Conditions 66 Stakeholder Engagement 21 Operational Control 66 Basics of Stakeholder Engagement 21 Fire Safety 68 Stakeholder Engagement Matrix 23 Accidents and Incidents 68 Corporate Governance 29 Contractor Engagement 68 Corporate Governance Principles 29 Workplace Injury Rate 68 Corporate Governance Structure 29 OHS Training 68 BoD and Management Board Remuneration Packages 34 Environmental Protection 70 Internal Control and Audit 35 Environmental Vision 70 Risk Management 36 Environmental Monitoring and Industrial -
Subject of the Russian Federation)
How to use the Atlas The Atlas has two map sections The Main Section shows the location of Russia’s intact forest landscapes. The Thematic Section shows their tree species composition in two different ways. The legend is placed at the beginning of each set of maps. If you are looking for an area near a town or village Go to the Index on page 153 and find the alphabetical list of settlements by English name. The Cyrillic name is also given along with the map page number and coordinates (latitude and longitude) where it can be found. Capitals of regions and districts (raiony) are listed along with many other settlements, but only in the vicinity of intact forest landscapes. The reader should not expect to see a city like Moscow listed. Villages that are insufficiently known or very small are not listed and appear on the map only as nameless dots. If you are looking for an administrative region Go to the Index on page 185 and find the list of administrative regions. The numbers refer to the map on the inside back cover. Having found the region on this map, the reader will know which index map to use to search further. If you are looking for the big picture Go to the overview map on page 35. This map shows all of Russia’s Intact Forest Landscapes, along with the borders and Roman numerals of the five index maps. If you are looking for a certain part of Russia Find the appropriate index map. These show the borders of the detailed maps for different parts of the country. -
Pleistocene-Holocene Palaeoenvironmental
Irina D. Streletskaya1*, Еvgeny А. Gusev3,4, Alexander A. Vasiliev2, Gleb E. Oblogov2, Anatoly N. Molodkov5 1Lomonosov Moscow State University, Department of Geography, 119991, Moscow, Leninskie Gory 1, Russia, e-mail: [email protected] *Corresponding author 2Earth Cryosphere Institute SB RAS, 625000, Tyumen, p/o box 1230, Russia; e-mail: [email protected], [email protected] 3VNIIOkeangeologia, 190121 St. Petersburg Angliyskii pr. 1, Russia; e-mail: [email protected] GEOGRAPHY 4St. Petersburg State University, 199034, St. Petersburg, Universitetskaya nab. 7–9, Russia 60 5Research Laboratory of Geochronology of the Quaternary Period, Institute of Geology, Tallinn Technical University, Estonia, 5, Ehitjate Street. 19086 Tallinn. Estonia; e-mail: [email protected] PLEISTOCENE-HOLOCENE PALAEOENVIRONMENTAL RECORDS FROM PERMAFROST SEQUENCES AT THE KARA SEA COAST (NW SIBERIA, RUSSIA) ABSTRACT. The Kara Sea coasts were INTRODUCTION studied using comprehensive stratigraphic Accumulation of Late Pleistocene sediments and geocryological methods. The paper in climatic conditions similar or colder than presents the new analytical studies of present ones, and wide distribution of ground ice and Quaternary deposits of polygonal ground ice exclude the presence Western Taymyr and presents the results of of large ice sheet in the north of West Siberia spore and pollen, foraminifera, grain-size, [Svendsen at al., 2004]. There is evidence of mineralogical, geochemical, oxygen isotopic, marine conditions in the lower Yenisey River and other analyses. Several stratigraphic- during the entire MIS5, which excludes the geocryological transects from Yenisey and glaciation around 90 kBP [Gusev and Molodkov, Gydan Bays enable us to refine the stratigraphy 2012]. Such contradictions in currently existing and palaeogeographical reconstruction of the models of development of northern West environments and freezing of Late Pleistocene- Siberia in the Middle-Late Pleistocene indicate Holocene sediments. -
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.