Arctic Expedition Cruise
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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. -
Studying Changes of Ice Coasts in the European Arctic
Geo-Mar Lett (2005) 25: 153–166 DOI 10.1007/s00367-004-0197-7 ORIGINAL Aleksey I. Sharov Studying changes of ice coasts in the European Arctic Received: 22 September 2003 / Accepted: 2 August 2004 / Published online: 18 December 2004 Ó Springer-Verlag 2004 Abstract The present extent of European ice coasts, their recently been receiving closer scientific attention since spatial changes in the past 50 years and the velocities of their dynamic environment and interesting natural scen- ice flow in marginal parts of tidewater glaciers were ery is proving highly sensitive to climatic changes determined and mapped at a regional scale using space- (Koryakin 1988; Hanson and Hooke 2000). Seaward ice borne image data, both optical and radar. The methods cliffs rising 2–50 m and sometimes even 100 m above sea of satellite photogrammetry and radar interferometry level stand at the forefront of glaciomarine interactions provided efficient solutions to the integral estimation of and represent a unique object for comprehensive envi- ice-coast dynamics in the Franz Josef Land, Novaya ronmental research at the ‘‘cutting edge’’ of several sci- Zemlya and Svalbard archipelagos. Studies revealed entific disciplines such as oceanography, glaciology and significant degradation of the ice coasts (À7.7% by coastal geomorphology. Paleogeographers consider the length) compared to the situation represented in the present glaciomarine settings along ice cliffs as being available maps. The results obtained in the laboratory analogous to those in the Ice Age and find them useful for were verified during several field campaigns. retrospective reconstructions (Korsun and Hald 1998). Glacier ice is destroyed relatively fast, even in cold water, and ice shores are thus among the most varied elements of the arctic coastline. -
Pamphlet to Accompany Scientific Investigations Map 3131
Bedrock Geologic Map of the Seward Peninsula, Alaska, and Accompanying Conodont Data By Alison B. Till, Julie A. Dumoulin, Melanie B. Werdon, and Heather A. Bleick Pamphlet to accompany Scientific Investigations Map 3131 View of Salmon Lake and the eastern Kigluaik Mountains, central Seward Peninsula 2011 U.S. Department of the Interior U.S. Geological Survey Contents Introduction ....................................................................................................................................................1 Sources of data ....................................................................................................................................1 Components of the map and accompanying materials .................................................................1 Geologic Summary ........................................................................................................................................1 Major geologic components ..............................................................................................................1 York terrane ..................................................................................................................................2 Grantley Harbor Fault Zone and contact between the York terrane and the Nome Complex ..........................................................................................................................3 Nome Complex ............................................................................................................................3 -
Sources and Pathways 4.1
Chapter 4 Persistant toxic substances (PTS) sources and pathways 4.1. Introduction Chapter 4 4.1. Introduction 4.2. Assessment of distant sources: In general, the human environment is a combination Longrange atmospheric transport of the physical, chemical, biological, social and cultur- Due to the nature of atmospheric circulation, emission al factors that affect human health. It should be recog- sources located within the Northern Hemisphere, par- nized that exposure of humans to PTS can, to certain ticularly those in Europe and Asia, play a dominant extent, be dependant on each of these factors. The pre- role in the contamination of the Arctic. Given the spa- cise role differs depending on the contaminant con- tial distribution of PTS emission sources, and their cerned, however, with respect to human intake, the potential for ‘global’ transport, evaluation of long- chain consisting of ‘source – pathway – biological avail- range atmospheric transport of PTS to the Arctic ability’ applies to all contaminants. Leaving aside the region necessarily involves modeling on the hemi- biological aspect of the problem, this chapter focuses spheric/global scale using a multi-compartment on PTS sources, and their physical transport pathways. approach. To meet these requirements, appropriate modeling tools have been developed. Contaminant sources can be provisionally separated into three categories: Extensive efforts were made in the collection and • Distant sources: Located far from receptor sites in preparation of input data for modeling. This included the Arctic. Contaminants can reach receptor areas the required meteorological and geophysical informa- via air currents, riverine flow, and ocean currents. tion, and data on the physical and chemical properties During their transport, contaminants are affected by of both the selected substances and of their emissions. -
Sverdrup-Among-The-Tundra-People
AMONG THE TUNDRA PEOPLE by HARALD U. SVERDRUP TRANSLATED BY MOLLY SVERDRUP 1939 Copyright @ 1978 by Regents of the University of California. All rights reserved. No part of this book may be reproduced or utilized in any form or by any means, elec- tronic or mechanical, including photocopying, recording, or by any information storage and retrieval system, without permission in writing from the regents. Distributed by : Scripps Institution of Oceanography A-007 University of California, San Diego La Jolla, California 92093 Library of Congress # 78-60483 ISBN # 0-89626-004-6 ACKNOWLEDGMENTS We are indebted to Molly Sverdrup (Mrs. Leif J.) for this translation of Hos Tundra-Folket published by Gyldendal Norsk Forlag, Oslo, 1938. We are also indebted to the late Helen Raitt for recovering the manuscript from the archives of the Scripps Institution of Oceanography. The Norwegian Polar Institute loaned negatives from Sverdrup's travels among the Chukchi, for figures 1 through 4. Sverdrup's map of his route in the Chukchi country in 19 19/20 was copied from Hos Tundra-Folket. The map of the Chukchi National Okrug was prepared by Fred Crowe, based on the American Geographic Society's Map of the Arctic Region (1975). The map of Siberia was copied from Terence Armstrong's Russian Settlement in the North (1 965) with permission of the Cambridge University Press. Sam Hinton drew the picture of a reindeer on the cover. Martin W. Johnson identified individuals in some of the photographs. Marston C Sargent Elizabeth N. Shor Kittie C C Kuhns Editors The following individuals, most of whom were closely associated with Sverdrup, out of respect for him and wishing to assure preservation of this unusual account, met part of the cost of publication. -
Spanning the Bering Strait
National Park service shared beringian heritage Program U.s. Department of the interior Spanning the Bering Strait 20 years of collaborative research s U b s i s t e N c e h UN t e r i N c h UK o t K a , r U s s i a i N t r o DU c t i o N cean Arctic O N O R T H E L A Chu a e S T kchi Se n R A LASKA a SIBERIA er U C h v u B R i k R S otk S a e i a P v I A en r e m in i n USA r y s M l u l g o a a S K S ew la c ard Peninsu r k t e e r Riv n a n z uko i i Y e t R i v e r ering Sea la B u s n i CANADA n e P la u a ns k ni t Pe a ka N h las c A lf of Alaska m u a G K W E 0 250 500 Pacific Ocean miles S USA The Shared Beringian Heritage Program has been fortunate enough to have had a sustained source of funds to support 3 community based projects and research since its creation in 1991. Presidents George H.W. Bush and Mikhail Gorbachev expanded their cooperation in the field of environmental protection and the study of global change to create the Shared Beringian Heritage Program. -
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 -
The Importance of Protection 57 60 1
Arctic Ocean B e a u Utqiagvik f o r t Wrangel 4 (Point Barrow) S e a Island 62 49 52 3 61 1 2 Pacific Walrus Haulout 21. Dezhnev Bay 42. Tyulen’e Ozero Bay 58 The Importance of Protection 57 60 1. Cape Blossom 22. Anastasia Bay 43. Srednyaya Bay 56 59 23. Bogoslava Island 44. Somneniye Chukchi Sea 2. Somnitelnaya Spit 55 24. Cape Tiomney 45. Olutorskaya Spit The Walrus Islands State Game Sanctuary (WISGS) was established 51 3. Davidova Spit 54 25. Cape Sery-Anana 46. Lekalo Spit in 1960 to protect Pacific walrus haulout sites on seven small craggy 4. Gavai 39 53 5. Kolyuchyn Island 26. Verkhoturova Island 47. Cape Vankarem 47 27. Cape Golenishcheva 48. Cape Onmyn islands in northern Bristol Bay: Round Island, Summit Island, Crooked 48 6. Belyaka Spit 7. Strait of Neskenpil’gyn Lagoon 28. Cape Semionova 49. Ayon Island Island, High Island, Black Rock, and The Twins. Chukotka, Russia 5 7 30 50 29. Little Diomede Island 50. Cape Serdtse-Kamen’ t S o u 8. Unlisted 6 i e n u d a e b 30. Kotzebue Sound 51. Ryrkaipii r z t 9. Cape Inkigur 9 t 10 o The sanctuary includes the surrounding waters that support a diverse S K 31. King Island 52. Cape Shelagsky 10. Cape Dezhnev 16 12 11 group of marine mammals, seabirds, and other marine wildlife. 15 32. Gambell 53. Cape Lisburne g 29 11. Big Diomede Island 17 n Alaska, USA i 31 A b a r 33. Savoonga 54. -
Reconstruction of Paleoclimate of Russian Arctic in the Late Pleistocene–Holocene on the Basis of Isotope Study of Ice Wedges I.D
Kriosfera Zemli, 2015, vol. XIX, No. 2, pp. 86–94 http://www.izdatgeo.ru RECONSTRUCTION OF PALEOCLIMATE OF RUSSIAN ARCTIC IN THE LATE PLEISTOCENE–HOLOCENE ON THE BASIS OF ISOTOPE STUDY OF ICE WEDGES I.D. Streletskaya1, A.A. Vasiliev2,3, G.E. Oblogov2, I.V. Tokarev4 1 Lomonosov Moscow State University, Department of Geography, 1 Leninskie Gory, Moscow, 119991, Russia; [email protected] 2 Earth Cryosphere Institute, SB RAS, 86 Malygina str., Tyumen, 625000, Russia; [email protected], [email protected] 3 Tyumen State Oil and Gas University, 38 Volodarskogo str., Tyumen, 625000, Russia 4 Resources Center “Geomodel” of Saint-Petersburg State University, 1 Ulyanovskaya str., St. Petersburg, 198504, Russia The results of paleoclimate reconstructions for the Russian Arctic on the basis of the isotope composition (δ18O) of ice wedges have been presented with the attendant analysis of all available data on isotope composition of syngenetic ice wedges with determined geologic age. Spatial distributions of δ18O values in ice wedges and elementary ice veins have been plotted for the present time and for MIS 1, MIS 2, MIS 3, and MIS 4. Trend lines of spatial distribution of δ18O for different time periods are almost parallel. Based on the data on isotope composition of ice wedges of different age, winter paleotemperatures have been reconstructed for the Russian Arctic and their spatial distribution characterized. Paleoclimate, ice wedges, isotope composition, atmospheric transfer INTRODUCTION Over the last decades numerous papers on iso- Laptev Sea region [Derevyagin et al., 2010]. These tope composition of ice wedges and its relation to pa- data allow to expand this range and to adjust Vasil- leo-geographic conditions have been published chuk’s equations for the whole Russian Arctic. -
Download Itinerary
SHOKALSKIY | WRANGEL ISLAND: ACROSS THE TOP OF THE WORLD TRIP CODE ACHEATW DEPARTURE 02/08/2021 DURATION 15 Days LOCATIONS Not Available INTRODUCTION Undertake this incredible expedition across the Arctic Circle. Experience the beauty of the pristine Wrangel and Herald islands, a magnificent section of the North-East Siberian Coastline that few witness. Explore the incredible wilderness opportunities of the Bering Strait where a treasure trove of Arctic biodiversity and Eskimo history await. ITINERARY DAY 1: Anadyr All expedition members will arrive in Anadyr; depending on your time of arrival you may have the opportunity to explore Anadyr, before getting to know your fellow voyagers and expedition team on board the Spirit of Enderby. We will depart when everybody is on board. DAY 2: Anadyrskiy Bay At sea today, there will be some briefings and lectures it is also a chance for some ‘birding’ cetacean watching and settling into ship life. Late this afternoon we plan to Zodiac cruise some spectacular bird cliffs in Preobrazheniya Bay. Copyright Chimu Adventures. All rights reserved 2020. Chimu Adventures PTY LTD SHOKALSKIY | WRANGEL ISLAND: ACROSS THE TOP OF THE WORLD TRIP CODE ACHEATW DAY 3: Yttygran and Gilmimyl Hot Springs DEPARTURE Yttygran Island is home to the monumental ancient aboriginal site known as Whale Bone Alley, where whale bones stretch along the beach for 02/08/2021 nearly half a kilometre. There are many meat pits used for storage and other remains of a busy DURATION whaling camp that united several aboriginal villages at a time. In one location, immense Bowhead Whale jawbones and ribs are placed 15 Days together in a stunning arch formation. -
EDB Eurasian Integration Yearbook 2011
Munich Personal RePEc Archive EDB Eurasian Integration Yearbook 2011 Vinokurov, Evgeny Euirasian Development Bank 2011 Online at https://mpra.ub.uni-muenchen.de/49178/ MPRA Paper No. 49178, posted 22 Aug 2013 07:48 UTC EDB EURASIAN I N T E G R A T I O N YEARBOOK 2011 Eurasian Integration Yearbook 2011 Annual publication of the Eurasian Development Bank УДК 339.7 ББК 65.012.3 Е 91 Eurasian Integration Yearbook 2011. – Almaty, 2011. – p. 352 ISBN 978–601–7151–21–8 Annual publication of the Eurasian Development Bank Edited by Evgeny Vinokurov The Eurasian Development Bank is an international financial institution established to promote economic growth and integration processes in Eurasia. The Bank was founded by the intergovernmental agreement signed in January 2006 by the Russian Federation and the Republic of Kazakhstan. In 2009–2010 Armenia, Tajikistan, Belarus became full members of the Bank. Electric power, water and energy, transportation infrastructure and high-tech and innovative industries are the key areas for Bank’s financing activity. As part of its mission the Bank carries out extensive research and analysis of contemporary development issues and trends in the region, with particular focus on Eurasian integration. The Bank also hosts regular conferences and round tables addressing various aspects of integration. In 2008, the Bank launched an annual EDB Eurasian Integration Yearbook (in English) and quarterly Journal of Eurasian Economic Integration (in Russian). Both publications are available online at: www.eabr.org. The Bank’s Strategy and Research Department publishes detailed Industry and Country Analytical Reports and plans to undertake a number of research projects. -
Laptev Sea System
Russian-German Cooperation: Laptev Sea System Edited by Heidemarie Kassens, Dieter Piepenburg, Jör Thiede, Leonid Timokhov, Hans-Wolfgang Hubberten and Sergey M. Priamikov Ber. Polarforsch. 176 (1995) ISSN 01 76 - 5027 Russian-German Cooperation: Laptev Sea System Edited by Heidemarie Kassens GEOMAR Research Center for Marine Geosciences, Kiel, Germany Dieter Piepenburg Institute for Polar Ecology, Kiel, Germany Jör Thiede GEOMAR Research Center for Marine Geosciences, Kiel. Germany Leonid Timokhov Arctic and Antarctic Research Institute, St. Petersburg, Russia Hans-Woifgang Hubberten Alfred-Wegener-Institute for Polar and Marine Research, Potsdam, Germany and Sergey M. Priamikov Arctic and Antarctic Research Institute, St. Petersburg, Russia TABLE OF CONTENTS Preface ....................................................................................................................................i Liste of Authors and Participants ..............................................................................V Modern Environment of the Laptev Sea .................................................................1 J. Afanasyeva, M. Larnakin and V. Tirnachev Investigations of Air-Sea Interactions Carried out During the Transdrift II Expedition ............................................................................................................3 V.P. Shevchenko , A.P. Lisitzin, V.M. Kuptzov, G./. Ivanov, V.N. Lukashin, J.M. Martin, V.Yu. ßusakovS.A. Safarova, V. V. Serova, ßvan Grieken and H. van Malderen The Composition of Aerosols