Laptev Sea System
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
Consensus Statement
Arctic Climate Forum Consensus Statement 2020-2021 Arctic Winter Seasonal Climate Outlook (along with a summary of 2020 Arctic Summer Season) CONTEXT Arctic temperatures continue to warm at more than twice the global mean. Annual surface air temperatures over the last 5 years (2016–2020) in the Arctic (60°–85°N) have been the highest in the time series of observations for 1936-20201. Though the extent of winter sea-ice approached the median of the last 40 years, both the extent and the volume of Arctic sea-ice present in September 2020 were the second lowest since 1979 (with 2012 holding minimum records)2. To support Arctic decision makers in this changing climate, the recently established Arctic Climate Forum (ACF) convened by the Arctic Regional Climate Centre Network (ArcRCC-Network) under the auspices of the World Meteorological Organization (WMO) provides consensus climate outlook statements in May prior to summer thawing and sea-ice break-up, and in October before the winter freezing and the return of sea-ice. The role of the ArcRCC-Network is to foster collaborative regional climate services amongst Arctic meteorological and ice services to synthesize observations, historical trends, forecast models and fill gaps with regional expertise to produce consensus climate statements. These statements include a review of the major climate features of the previous season, and outlooks for the upcoming season for temperature, precipitation and sea-ice. The elements of the consensus statements are presented and discussed at the Arctic Climate Forum (ACF) sessions with both providers and users of climate information in the Arctic twice a year in May and October, the later typically held online. -
Recent Declines in Warming and Vegetation Greening Trends Over Pan-Arctic Tundra
Remote Sens. 2013, 5, 4229-4254; doi:10.3390/rs5094229 OPEN ACCESS Remote Sensing ISSN 2072-4292 www.mdpi.com/journal/remotesensing Article Recent Declines in Warming and Vegetation Greening Trends over Pan-Arctic Tundra Uma S. Bhatt 1,*, Donald A. Walker 2, Martha K. Raynolds 2, Peter A. Bieniek 1,3, Howard E. Epstein 4, Josefino C. Comiso 5, Jorge E. Pinzon 6, Compton J. Tucker 6 and Igor V. Polyakov 3 1 Geophysical Institute, Department of Atmospheric Sciences, College of Natural Science and Mathematics, University of Alaska Fairbanks, 903 Koyukuk Dr., Fairbanks, AK 99775, USA; E-Mail: [email protected] 2 Institute of Arctic Biology, Department of Biology and Wildlife, College of Natural Science and Mathematics, University of Alaska, Fairbanks, P.O. Box 757000, Fairbanks, AK 99775, USA; E-Mails: [email protected] (D.A.W.); [email protected] (M.K.R.) 3 International Arctic Research Center, Department of Atmospheric Sciences, College of Natural Science and Mathematics, 930 Koyukuk Dr., Fairbanks, AK 99775, USA; E-Mail: [email protected] 4 Department of Environmental Sciences, University of Virginia, 291 McCormick Rd., Charlottesville, VA 22904, USA; E-Mail: [email protected] 5 Cryospheric Sciences Branch, NASA Goddard Space Flight Center, Code 614.1, Greenbelt, MD 20771, USA; E-Mail: [email protected] 6 Biospheric Science Branch, NASA Goddard Space Flight Center, Code 614.1, Greenbelt, MD 20771, USA; E-Mails: [email protected] (J.E.P.); [email protected] (C.J.T.) * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +1-907-474-2662; Fax: +1-907-474-2473. -
Underground Nuclear Explosion (Western Yakutia) from TEM Data
Available online at www.sciencedirect.com Russian Geology and Geophysics 53 (2012) 185–193 www.elsevier.com/locate/rgg The geoelectric structure at the site of “Crystal” underground nuclear explosion (Western Yakutia) from TEM data N.O. Kozhevnikov a,*, E.Yu. Antonov a, S.Yu. Artamonova b, A.E. Plotnikov c a A.A. Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia b V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia c LUCH R&D Company for Geophysical Instruments, ul. Geologicheskaya 49, Novosibirsk, 630010, Russia Received 25 May 2010; accepted 7 October 2010 Abstract The resistivity pattern at the site of the “Crystal” underground nuclear explosion (Daldyn–Alakit district of Yakutia) of 1974 which led to an accident has been imaged using TEM data. The local background pattern corresponds to a three- or four-layer earth with a conductor at the base. The uppermost layer, with a resistivity of tens to hundreds of ohm ⋅ m, has its bottom at 190–260 m asl and consists of perennially frozen Late Cambrian carbonates. The resistivity structure of shallow subsurface at the blast epicenter remained unperturbed though being subject to mechanic and thermal effects. The bottom of the second layer is at 20 to 190 m below the sealevel and its resistivity is 7–10 ohm ⋅ m. It is composed of frost-bound and unfrozen cold rocks that belong to a Late Cambrian water-bearing sequence (an aquifer). -
Sediment Transport to the Laptev Sea-Hydrology and Geochemistry of the Lena River
Sediment transport to the Laptev Sea-hydrology and geochemistry of the Lena River V. RACHOLD, A. ALABYAN, H.-W. HUBBERTEN, V. N. KOROTAEV and A. A, ZAITSEV Rachold, V., Alabyan, A., Hubberten, H.-W., Korotaev, V. N. & Zaitsev, A. A. 1996: Sediment transport to the Laptev Sea-hydrology and geochemistry of the Lena River. Polar Research 15(2), 183-196. This study focuses on the fluvial sediment input to the Laptev Sea and concentrates on the hydrology of the Lena basin and the geochemistry of the suspended particulate material. The paper presents data on annual water discharge, sediment transport and seasonal variations of sediment transport. The data are based on daily measurements of hydrometeorological stations and additional analyses of the SPM concentrations carried out during expeditions from 1975 to 1981. Samples of the SPM collected during an expedition in 1994 were analysed for major, trace, and rare earth elements by ICP-OES and ICP-MS. Approximately 700 h3freshwater and 27 x lo6 tons of sediment per year are supplied to the Laptev Sea by Siberian rivers, mainly by the Lena River. Due to the climatic situation of the drainage area, almost the entire material is transported between June and September. However, only a minor part of the sediments transported by the Lena River enters the Laptev Sea shelf through the main channels of the delta, while the rest is dispersed within the network of the Lena Delta. Because the Lena River drains a large basin of 2.5 x lo6 km2,the chemical composition of the SPM shows a very uniform composition. -
Information to Users
INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely afreet reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand corner and continuing from left to right in equal sections with small overlaps. Each original is also photographed in one exposure and is included in reduced form at the back of the book. Photographs included in the original manuscript have been reproduced xerographically in this copy. Higher quality 6" x 9" black and white photographic prints are available for any photographs or illustrations appearing in this copy for an additional charge. Contact UMI directly to order. University Microfilms International A Beil & Howell Information Company 300 North Zeeb Road. Ann Arbor. Ml 48106-1346 USA 313/761-4700 800/521-0600 Order Number 0211125 A need to know: The role of Air Force reconnaissance in war planning, 1045-1953 Farquhar, John Thomas, Ph.D. The Ohio State University, 1991 Copyright ©1001 by Farquhar, John Thomas. -
Paleozoic Rocks of Northern Chukotka Peninsula, Russian Far East: Implications for the Tectonicsof the Arctic Region
TECTONICS, VOL. 18, NO. 6, PAGES 977-1003 DECEMBER 1999 Paleozoic rocks of northern Chukotka Peninsula, Russian Far East: Implications for the tectonicsof the Arctic region BorisA. Natal'in,1 Jeffrey M. Amato,2 Jaime Toro, 3,4 and James E. Wright5 Abstract. Paleozoicrocks exposedacross the northernflank of Alaskablock the essentialelement involved in the openingof the the mid-Cretaceousto Late CretaceousKoolen metamorphic Canada basin. domemake up two structurallysuperimposed tectonic units: (1) weaklydeformed Ordovician to Lower Devonianshallow marine 1. Introduction carbonatesof the Chegitununit which formed on a stableshelf and (2) strongly deformed and metamorphosedDevonian to Interestin stratigraphicand tectoniccorrelations between the Lower Carboniferousphyllites, limestones, and an&site tuffs of RussianFar East and Alaska recentlyhas beenrevived as the re- the Tanatapunit. Trace elementgeochemistry, Nd isotopicdata, sult of collaborationbetween North Americanand Russiangeol- and texturalevidence suggest that the Tanataptuffs are differen- ogists.This paperpresents the resultsof one suchstudy from the tiatedcalc-alkaline volcanic rocks possibly derived from a mag- ChegitunRiver valley, Russia,where field work was carriedout matic arc. We interpretthe associatedsedimentary facies as in- to establishthe stratigraphic,structural, and metamorphicrela- dicativeof depositionin a basinal setting,probably a back arc tionshipsin the northernpart of the ChukotkaPeninsula (Figure basin. Orthogneissesin the core of the Koolen dome yielded a -
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.). -
Mikhail Gorbachev's Speech in Murmansk at the Ceremonial Meeting on the Occasion of the Presentation of the Order of Lenin and the Gold Star to the City of Murmansk
MIKHAIL GORBACHEV'S SPEECH IN MURMANSK AT THE CEREMONIAL MEETING ON THE OCCASION OF THE PRESENTATION OF THE ORDER OF LENIN AND THE GOLD STAR TO THE CITY OF MURMANSK Murmansk, 1 Oct. 1987 Indeed, the international situation is still complicated. The dangers to which we have no right to turn a blind eye remain. There has been some change, however, or, at least, change is starting. Certainly, judging the situation only from the speeches made by top Western leaders, including their "programme" statements, everything would seem to be as it was before: the same anti-Soviet attacks, the same demands that we show our commitment to peace by renouncing our order and principles, the same confrontational language: "totalitarianism", "communist expansion", and so on. Within a few days, however, these speeches are often forgotten, and, at any rate, the theses contained in them do not figure during businesslike political negotiations and contacts. This is a very interesting point, an interesting phenomenon. It confirms that we are dealing with yesterday's rhetoric, while real- life processes have been set into motion. This means that something is indeed changing. One of the elements of the change is that it is now difficult to convince people that our foreign policy, our initiatives, our nuclear-free world programme are mere "propaganda". A new, democratic philosophy of international relations, of world politics is breaking through. The new mode of thinking with its humane, universal criteria and values is penetrating diverse strata. Its strength lies in the fact that it accords with people's common sense. -
Migratory Movements of Peregrine Falcons Falco Peregrinus, Breeding on the Yamal Peninsula, Russia
Ornis Hungarica 2018. 26(2): 222–231. DOI: 10.1515/orhu-2018-0030 Migratory movements of Peregrine Falcons Falco peregrinus, breeding on the Yamal Peninsula, Russia Vasiliy SOKOLOV1, Aleksandr SOKOLOV2 & Andrew DIXON3* Received: October 30, 2018 – Revised: November 11, 2018 – Accepted: December 21, 2018 This is a contribution submitted to the Proceedings of the World Conference on the Peregrine Falcon in Buda- pest in September 2017. Sokolov, V., Sokolov, A. & Dixon, A. 2018. Migratory movements of Peregrine Falcons Falco peregrinus, breeding on the Yamal Peninsula, Russia. – Ornis Hungarica 26(2): 222–231. DOI: 10.1515/orhu-2018-0030 Abstract We describe the migration pathways of 12 Peregrine Falcons Falco peregrinus cali dus breeding on the Yamal Peninsula, Russia. Overall, we tracked 30 complete (17 autumn and 13 spring) and 5 incomplete seasonal migration routes. Winter ranges extended from the Atlantic coast of southern Portugal in the west to Kish Island in the Arabian Gulf in the east, and from Krasnodar in southern Russia in the north to South Sudan. Eight birds were tracked to their wintering sites, with migration pathways ranging from 3,557 km to 8,114 km, taking 14 to 61 days to complete. Birds spent an average of 190 days in their winter ranges (range 136 to 212 days, N = 14), and departure on spring migration took place in April. The home ranges used by win- tering Peregrines were varied including coastal habitats, agricultural landscapes, savannah, desert and an urban city. Departure from breeding areas took place in September with birds returning in May. Peregrines exhibited a high degree of fidelity to their winter ranges, with four birds tracked over three successive migrations until the 2012 breeding season. -
Social and Environmental Report 2015
SOCIAL AND ENVIRONMENTAL REPORT 2015 ALROSA* is a Russian Group of diamond mining companies that occupies a leading position in the industry and has the largest rough diamond reserves in the world. The Group accounts for one third of the reserves and more than a quarter of the production of the global rough diamonds market. The key areas of activity, comprising the focus of the major strategic efforts of the Group, are deposits exploration, mining, processing and sales of rough diamonds. The core activities of ALROSA Group are concentrated in two regions of the Russian Federation, namely the Republic of Sakha (Yakutia) and the Arkhangelsk Region, as well as on the African continent. The majority of ALROSA Group revenue comes from selling rough diamonds. Rough diamonds are sold under long-term agreements to Russian and foreign diamond cutting companies. The rough diamond segment accounts for about 90% of the total Group revenue. *For the purpose of this Report, ALROSA Group means PJSC ALROSA and its subsidiaries. INTRODUCTION ADDRESS BY THE PRESIDENT 2 4 6 OF PJSC ALROSA 6 OUR APPROACH ENVIRONMENTAL INDEPENDENT ABOUT THIS REPORT TO SUSTAINABLE RESPONSIBILITY AUDITOR’S 10 DEVELOPMENT 61 REPORT 27 ENVIRONMENTAL POLICY 112 IMPLEMENTATION INTEGRATION OF SUSTAINABLE 62 DEVELOPMENT GOALS IN ACTIVITIES OF THE COMPANY FUNDING OF ENVIRONMENTAL 28 PROTECTION ACTIVITIES 70 1 STAKEHOLDER ENGAGEMENT 31 ENVIRONMENTAL PROTECTION GOALS ABOUT ALROSA GROUP ACHIEVEMENT MANAGEMENT IN THE SPHERE 73 7 17 OF SUSTAINABLE DEVELOPMENT GENERAL INFORMATION 34 ANNEXES 18 115 ETHICS AND ANTI-CORRUPTION Annex 1. PRODUCTION CHAIN ACTIVITIES 40 SCOPE OF MATERIAL ASPECTS AND GEOGRAPHY 116 18 INNOVATIVE DEVELOPMENT Annex 2. -
The Evolutionary History of Sharp-And Blunt-Snouted Lenok (Brachymystax
BMC Evolutionary Biology BioMed Central Research article Open Access The evolutionary history of sharp- and blunt-snouted lenok (Brachymystax lenok (Pallas, 1773)) and its implications for the paleo-hydrological history of Siberia Elsa Froufe1,2, Sergey Alekseyev3, Paulo Alexandrino1,2 and Steven Weiss*4 Address: 1Centro de Investigação em Biodiversidade e Recursos Genéticos (CIBIO/UP), Campus Agrário de Vairão, 4485-661 Vairão, Portugal, 2Faculdade de Ciências, Universidade do Porto, Praça Gomes Teixeira, 4009-002 Porto, Portugal, 3N. K. Kolzov Institute of Developmental Biology (IDB), Russian Academy of Sciences, 117334, Moscow, Vavilova 26, Russia and 4Karl-Franzens Universität Graz, Institut für Zoologie, Universitätsplatz 2, A-8010 Graz, Austria Email: Elsa Froufe - [email protected]; Sergey Alekseyev - [email protected]; Paulo Alexandrino - [email protected]; Steven Weiss* - [email protected] * Corresponding author Published: 6 February 2008 Received: 4 August 2007 Accepted: 6 February 2008 BMC Evolutionary Biology 2008, 8:40 doi:10.1186/1471-2148-8-40 This article is available from: http://www.biomedcentral.com/1471-2148/8/40 © 2008 Froufe et al; licensee BioMed Central Ltd. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/2.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. Abstract Background: Broad-scale phylogeographic studies of freshwater organisms provide not only an invaluable framework for understanding the evolutionary history of species, but also a genetic imprint of the paleo- hydrological dynamics stemming from climatic change. Few such studies have been carried out in Siberia, a vast region over which the extent of Pleistocene glaciation is still disputed.