High Arctic Odyssey
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Meddelelser120.Pdf (2.493Mb)
MEDDELELSER NR. 120 IAN GJERTZ & BERIT MØRKVED Environmental Studies from Franz Josef Land, with Emphasis on Tikhaia Bay, Hooker Island '-,.J��!c �"'oo..--------' MikhalSkakuj NORSK POLARINSTITUTT OSLO 1992 ISBN 82-7666-043-6 lan Gjertz and Berit Mørkved Printed J uly 1992 Norsk Polarinstitutt Cover picture: Postboks 158 Iceberg of Franz Josef Land N-1330 Oslo Lufthavn (Ian Gjertz) Norway INTRODUCTION The Russian high Arctic archipelago Franz Josef Land has long been closed to foreign scientists. The political changes which occurred in the former Soviet Union in the last part of the 1980s resulted in the opening of this area to foreigners. Director Gennady Matishov of Murmansk Marine Biological Institute deserves much of the credit for this. In 1990 an international cooperation was established between the Murmansk Marine Biological Institute (MMBI); the Arctic Ecology Group of the Institute of Oceanology, Gdansk; and the Norwegian Polar Research Institute, Oslo. The purpose of this cooperation is to develope scientific cooperation in the Arctic thorugh joint expeditions, the establishment of a high Arctic scientific station, and the exchange of scientific information. So far the results of this cooperation are two scientific cruises with the RV "Pomor", a vessel belonging to the MMBI. The cruises have been named Sov Nor-Poll and Sov-Nor-Po12. A third cruise is planned for August-September 1992. In addition the MMBI has undertaken to establish a scientific station at Tikhaia Bay on Hooker Island. This is the site of a former Soviet meteorological base from 1929-1958, and some of the buildings are now being restored by MMBI. -
Novaya Zemlya Archipelago (Russian Arctic)
This is a repository copy of First records of testate amoebae from the Novaya Zemlya archipelago (Russian Arctic). White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/127196/ Version: Accepted Version Article: Mazei, Yuri, Tsyganov, Andrey N, Chernyshov, Viktor et al. (2 more authors) (2018) First records of testate amoebae from the Novaya Zemlya archipelago (Russian Arctic). Polar Biology. ISSN 0722-4060 https://doi.org/10.1007/s00300-018-2273-x Reuse Items deposited in White Rose Research Online are protected by copyright, with all rights reserved unless indicated otherwise. They may be downloaded and/or printed for private study, or other acts as permitted by national copyright laws. The publisher or other rights holders may allow further reproduction and re-use of the full text version. This is indicated by the licence information on the White Rose Research Online record for the item. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ 1 First records of testate amoebae from the Novaya Zemlya archipelago (Russian Arctic) 2 Yuri A. Mazei1,2, Andrey N. Tsyganov1, Viktor A. Chernyshov1, Alexander A. Ivanovsky2, Richard J. 3 Payne1,3* 4 1. Penza State University, Krasnaya str., 40, Penza 440026, Russia. 5 2. Lomonosov Moscow State University, Leninskiye Gory, 1, Moscow 119991, Russia. 6 3. University of York, Heslington, York YO10 5DD, United Kingdom. -
Arctic Floating University-2018: Terrae Novae”
Expedition Project “Arctic Floating University-2018: Terrae Novae” Dates: July 10-29, 2018 Duration: 20 days Organizers: Northern (Arctic) Federal University named after M.V. Lomonosov, ROSHYDROMET. Route: Arkhangelsk – Solovetsky Islands – Russkaya Gavan’ (Novaya Zemlya) – Malye Oranskiye Islands – Cape Zhelaniya – Murmantsa Bay (Gemskerk Island) – Ledyanaya Gavan’ – Varnek (Vaigach Island) – Matveev Island – Cape Menshikov – Propashchaya Bay – Bugrino (Kolguyev Island) – Arkhangelsk. I - IV -hydrological sections Expected Number of Participants: 58 (students, post-graduate students, research fellows from Russian and foreign scientific and educational institutions). Partners: Russian Geographical Society, Russian Arctic National Park, Lomonosov Moscow State University, University of Geneva, University of Lausanne, Federal Polytechnic School of Lausanne. Expedition Aims: • acquiring new knowledge about the state and changes in the ecosystem of the coastal areas of Novaya Zemlya archipelago; • training of young specialists in the Arctic-focused specialties: hydrometeorology, ecology, arctic biology, geography, ethnopolitology, international law etc.; • development of scientific and educational cooperation with the Arctic Council countries in the framework of high-latitude Arctic expeditions; • promotion of the Russian scientific, historical, cultural and natural heritage and polar specialties, promotion of the Russian Arctic concept at the national and international level. RESEARCH PROGRAM: assessment of man-made pollution of the local -
Satellite Ice Extent, Sea Surface Temperature, and Atmospheric 2 Methane Trends in the Barents and Kara Seas
The Cryosphere Discuss., https://doi.org/10.5194/tc-2018-237 Manuscript under review for journal The Cryosphere Discussion started: 22 November 2018 c Author(s) 2018. CC BY 4.0 License. 1 Satellite ice extent, sea surface temperature, and atmospheric 2 methane trends in the Barents and Kara Seas 1 2 3 2 4 3 Ira Leifer , F. Robert Chen , Thomas McClimans , Frank Muller Karger , Leonid Yurganov 1 4 Bubbleology Research International, Inc., Solvang, CA, USA 2 5 University of Southern Florida, USA 3 6 SINTEF Ocean, Trondheim, Norway 4 7 University of Maryland, Baltimore, USA 8 Correspondence to: Ira Leifer ([email protected]) 9 10 Abstract. Over a decade (2003-2015) of satellite data of sea-ice extent, sea surface temperature (SST), and methane 11 (CH4) concentrations in lower troposphere over 10 focus areas within the Barents and Kara Seas (BKS) were 12 analyzed for anomalies and trends relative to the Barents Sea. Large positive CH4 anomalies were discovered around 13 Franz Josef Land (FJL) and offshore west Novaya Zemlya in early fall. Far smaller CH4 enhancement was found 14 around Svalbard, downstream and north of known seabed seepage. SST increased in all focus areas at rates from 15 0.0018 to 0.15 °C yr-1, CH4 growth spanned 3.06 to 3.49 ppb yr-1. 16 The strongest SST increase was observed each year in the southeast Barents Sea in June due to strengthening of 17 the warm Murman Current (MC), and in the south Kara Sea in September. The southeast Barents Sea, the south 18 Kara Sea and coastal areas around FJL exhibited the strongest CH4 growth over the observation period. -
With Nansen in the North; a Record of the Fram Expedition in 1893-96
with-nXT^sen Ulllii I Hi nil I li "'III"!!!!!!!! Lieut JOHANSi; i*ll III Hi!; :1 III I iiil |i;iii'i'iiiiiiii i; \Ki THE LIBRARY OF THE UNIVERSITY OF CALIFORNIA LOS ANGELES WITH NANSEN IN THE NORTH [LANCASTER. K lOHANSEN. {Frontis/iiece. WITH NANSEN IN THE NORTH A Record of the Fram Expedition in 1893-96 BY HJALMAR JOHANSEN lieutenant in the norwegian army Translated from the Norwegian BY H. L. BR.EKSTAD LONDON WARD, LOCK AND CO LIMITED NEW YORK AND MELBOURNE 1899 — ijr Contents CHAPTER I TAGE The Equipment of the Expedition— Its Start—The Voyage along the Coast—Farewell to Norway I CHAI'TER II The First Ice — Arrival at Khabarova—Meeting with Trontheim Arrival of the Dogs— Life among the Samoyedes— Christofersen Leaves us—Excursion on Yalmal—The last Human Beings we saw lo CHAPTER III A Heavy Sea—Sverdrup Island—A Reindeer Hunt—The First Bear —A Stiff Pull—Firing with Kerosene 20 CHAPTER IV Death among the Dogs — Taimur Island — Cape Butterless — The Northernmost Point of the Old World—A Walrus Hunt—To the North 28 CHAPTER V Open Water—Unwelcome Guests—Fast in the Ice—Warping—The Northern Lights 34 CHAPTER VI First Day of Rest— Surprised by Bears—The Dogs are let Loose- Ice Pressure—A Hunt in the Dark 4° CHAPTER VII More Bears—The Power of Baking Powder— "Johansen's Friend"— V Electric Light— Shooting Competition ...•• 5° V 1212604 vi COXTENTS CHAPTER VIII PAGE Foot-races on the Ice—More about the Dogs—The Northern Lights- Adulterated Beer—Ice Pressure—Peder Attacked by a Bear . -
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. -
Exceptional Retreat of Novaya Zemlya's Marine
The Cryosphere, 11, 2149–2174, 2017 https://doi.org/10.5194/tc-11-2149-2017 © Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License. Exceptional retreat of Novaya Zemlya’s marine-terminating outlet glaciers between 2000 and 2013 J. Rachel Carr1, Heather Bell2, Rebecca Killick3, and Tom Holt4 1School of Geography, Politics and Sociology, Newcastle University, Newcastle-upon-Tyne, NE1 7RU, UK 2Department of Geography, Durham University, Durham, DH13TQ, UK 3Department of Mathematics & Statistics, Lancaster University, Lancaster, LA1 4YF, UK 4Centre for Glaciology, Department of Geography and Earth Sciences, Aberystwyth University, Aberystwyth, SY23 4RQ, UK Correspondence to: J. Rachel Carr ([email protected]) Received: 7 March 2017 – Discussion started: 15 May 2017 Revised: 20 July 2017 – Accepted: 24 July 2017 – Published: 8 September 2017 Abstract. Novaya Zemlya (NVZ) has experienced rapid ice al., 2013). This ice loss is predicted to continue during loss and accelerated marine-terminating glacier retreat dur- the 21st century (Meier et al., 2007; Radic´ et al., 2014), ing the past 2 decades. However, it is unknown whether and changes are expected to be particularly marked in the this retreat is exceptional longer term and/or whether it has Arctic, where warming of up to 8 ◦C is forecast (IPCC, persisted since 2010. Investigating this is vital, as dynamic 2013). Outside of the Greenland Ice Sheet, the Russian high thinning may contribute substantially to ice loss from NVZ, Arctic (RHA) accounts for approximately 20 % of Arctic but is not currently included in sea level rise predictions. glacier ice (Dowdeswell and Williams, 1997; Radic´ et al., Here, we use remotely sensed data to assess controls on NVZ 2014) and is, therefore, a major ice reservoir. -
Foreign Military Studies Office
community.apan.org/wg/tradoc-g2/fmso/ PENDING PUBLIC RELEASE/APPROVAL - QUESTIONS: 757-501-6236 Foreign Military Studies Office Volume 9 Issue #10 OEWATCH October 2019 FOREIGN NEWS & PERSPECTIVES OF THE OPERATIONAL ENVIRONMENT EURASIA 28 New Chinese Aircraft Carrier to Carry 50 Percent More 3 Sinking the Armata? Fighters AFRICA 4 Where is Strelkov Aiming? 30 China and Kazakhstan Upgrade Ties 59 Urban Deployment Reveals South African Military Deficiencies 5 Northern and Eastern Military Districts Get S-300V4 Air 32 China and Russia Sign Heavy Helicopter Deal 60 South Africa’s Xenophobic Violence: Foreigners as Scapegoats Defense Systems 34 China Reports the Launch of Unmanned ‘Mini-Aegis-Class for Failing Economy 7 Russian Ground Forces’ Air Defense: A Look At Russia’s Destroyer’ 61 Somalia’s Newest Military Commander Also Its Youngest Threat-Based Military 35 Contrasting Chinese and Foreign Media Accounts on 62 African Union Raises Concerns Over Foreign Military Bases in 8 The Modernization of Russian Coastal Defense Missiles Xinjiang Africa 10 Mines Seen as Key Capabilities for Russian Naval and Coastal 37 Papuans Hope for Independence, but is it Possible? 63 Regional Rivalries Heat Up as AMISOM Leaves Somalia Defense 39 Another Counter-Terrorism Operation in Palu, Indonesia 64 China’s Investment in African Aviation 12 Russia Developing On-Orbit Fueling Technologies 40 India to Create New Chief of Defence Staff Position 65 International Connections to Guinea-Bissau Drug Trafficking 13 Public Protests and “Hybrid War” 66 Borno Governor -
Cruise 54Th of the Research Vessel Akademik Mstislav Keldysh in the Kara Sea M
ISSN 00014370, Oceanology, 2010, Vol. 50, No. 5, pp. 637–642. © Pleiades Publishing, Inc., 2010. Original Russian Text © M.V. Flint, 2010, published in Okeanologiya, 2010, Vol. 50, No. 5, pp. 677–682. Cruise 54th of the Research Vessel Akademik Mstislav Keldysh in the Kara Sea M. V. Flint Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia Email: [email protected] Received December 10, 2009 DOI: 10.1134/S0001437010050012 The modern state of the Arctic Basin and the vari ered characteristic of the vast region located east of ability of this basin are determined to a great extent by Novaya Zemlya. the processes on the shelf and continental slope of the The key role of the Kara Sea in the Arctic ecosys Arctic marginal seas. Annually, the volume of tem is in the fact that it accepts the greatest freshwater 5000 km3 of the rivers’ runoff is transported to the shelf runoff of the rivers in the entire Arctic Basin. Its and continental slope. The rivers’ runoff determines annual volume reaches 1200–1300 km3/yr, 90% of the significant freshening of the Arctic surface waters. which is the runoff of the Ob and Yenisei rivers. The It influences the formation of the seasonal stratifica river runoff into the Kara Sea is more than half of the tion and the circulation pattern in the upper layer of entire runoff of the Siberian Arctic and more than the continental seas. The runoff of the rivers transports onethird of the total freshwater runoff into the Arctic enormous volumes of allochtonous nutrients, sus Basin. -
On a Revised Map of Kaiser Franz Josef Land, Based on Oberlieutenant Payer's Original Survey Author(S): Ralph Copeland Source: the Geographical Journal, Vol
On a Revised Map of Kaiser Franz Josef Land, Based on Oberlieutenant Payer's Original Survey Author(s): Ralph Copeland Source: The Geographical Journal, Vol. 10, No. 2 (Aug., 1897), pp. 180-191 Published by: geographicalj Stable URL: http://www.jstor.org/stable/1774601 Accessed: 27-06-2016 04:21 UTC Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at http://about.jstor.org/terms JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Wiley, The Royal Geographical Society (with the Institute of British Geographers) are collaborating with JSTOR to digitize, preserve and extend access to The Geographical Journal This content downloaded from 128.197.26.12 on Mon, 27 Jun 2016 04:21:08 UTC All use subject to http://about.jstor.org/terms 180 ON A REVISED MAP OF KAISER FRANZ JOSEF LAND, be used; but things turned out far otherwise, the Nansen sledges taken were seldom available, and the want of Samoyede sledges added greatly to the difficulties of transport. It was found that the north and south parts of the island, except for a belt along the western shore of Wijdo bay, were chiefly covered with immense accumulations of ice, while the central part was a region of boggy valleys and mountain ridges, with occasional more or less fertile slopes. -
Glacier Fluctuations During the Past 2000 Years
Quaternary Science Reviews 149 (2016) 61e90 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Invited review Glacier fluctuations during the past 2000 years * Olga N. Solomina a, , Raymond S. Bradley b, Vincent Jomelli c, Aslaug Geirsdottir d, Darrell S. Kaufman e, Johannes Koch f, Nicholas P. McKay e, Mariano Masiokas g, Gifford Miller h, Atle Nesje i, j, Kurt Nicolussi k, Lewis A. Owen l, Aaron E. Putnam m, n, Heinz Wanner o, Gregory Wiles p, Bao Yang q a Institute of Geography RAS, Staromonetny-29, 119017 Staromonetny, Moscow, Russia b Department of Geosciences, University of Massachusetts, Amherst, MA 01003, USA c Universite Paris 1 Pantheon-Sorbonne, CNRS Laboratoire de Geographie Physique, 92195 Meudon, France d Department of Earth Sciences, University of Iceland, Askja, Sturlugata 7, 101 Reykjavík, Iceland e School of Earth Sciences and Environmental Sustainability, Northern Arizona University, Flagstaff, AZ 86011, USA f Department of Geography, Brandon University, Brandon, MB R7A 6A9, Canada g Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales (IANIGLA), CCT CONICET Mendoza, CC 330 Mendoza, Argentina h INSTAAR and Geological Sciences, University of Colorado Boulder, USA i Department of Earth Science, University of Bergen, Allegaten 41, N-5007 Bergen, Norway j Uni Research Climate AS at Bjerknes Centre for Climate Research, Bergen, Norway k Institute of Geography, University of Innsbruck, Innrain 52, 6020 Innsbruck, Austria l Department of Geology, -
Russian Coal Mining in Svalbard
Russian Coal Mining in Svalbard An Examination of Sovereignty and Arctic Cooperation Group 25 Narin Zimbalista, Luna Persson, Zoe Svendsen & Julie Sejr Reventlow Characters: 141595 1 1. Introduction 4 Research Question 7 Supporting Questions 7 Research Design 7 2. Background Information 8 2.1 A Brief History of Svalbard 8 2.1.1 Mining as a Settlement Builder 9 2.1.2. Russian and Norwegian interests in Svalbard 10 2.2 Geopolitical Context in the Arctic 11 2.2.1 Russian conduct in the Arctic 12 2.2.2 Barents Sea Dispute 13 3. Literature Review 15 3.1 An overview of the Arctic conflict 15 3.2 Theoretical Considerations within the literature 17 3.3 Russia in the Arctic 18 3.4 Svalbard and the Russian Presence 19 3.5 Concluding Considerations 20 4. Theoretical Framework 22 4.1 Realism 22 4.1.1 Economic Nationalism 24 4.2 Constructivism 26 4.3 Main theoretical deductions 28 5. Methodology 31 5.1 Philosophy of Science 31 5.1.1 Realism 31 5.1.2 Constructivism 33 5.2 Methods 34 5.2.1 Content analysis 34 5.2.2 Documents as data 37 5.3 Results 39 5.3.1 - Thematic Coding Results 39 5.3.2 Summarizing Qualitative Content Analysis Results 42 6. Analysis 46 6.1 How is Russia utilizing coal mining in Svalbard to project influence? 46 6.2 How has the Svalbard Treaty and the UNCLOS constructed norms and rules that have affected the contemporary jurisdiction of Svalbard? 51 2 6.3 How can Realism and Constructivism offer insight to Russian and Norwegian behaviour in Svalbard? 55 7.