Arctic Geopolitics, Media and Power
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AAR Chapter 2
Go back to opening screen 9 Chapter 2 Physical/Geographical Characteristics of the Arctic –––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––– Contents 2.2.1. Climate boundaries 2.1. Introduction . 9 On the basis of temperature, the Arctic is defined as the area 2.2. Definitions of the Arctic region . 9 2.2.1. Climate boundaries . 9 north of the 10°C July isotherm, i.e., north of the region 2.2.2. Vegetation boundaries . 9 which has a mean July temperature of 10°C (Figure 2·1) 2.2.3. Marine boundary . 10 (Linell and Tedrow 1981, Stonehouse 1989, Woo and Gre- 2.2.4. Geographical coverage of the AMAP assessment . 10 gor 1992). This isotherm encloses the Arctic Ocean, Green- 2.3. Climate and meteorology . 10 2.3.1. Climate . 10 land, Svalbard, most of Iceland and the northern coasts and 2.3.2. Atmospheric circulation . 11 islands of Russia, Canada and Alaska (Stonehouse 1989, 2.3.3. Meteorological conditions . 11 European Climate Support Network and National Meteoro- 2.3.3.1. Air temperature . 11 2.3.3.2. Ocean temperature . 12 logical Services 1995). In the Atlantic Ocean west of Nor- 2.3.3.3. Precipitation . 12 way, the heat transport of the North Atlantic Current (Gulf 2.3.3.4. Cloud cover . 13 Stream extension) deflects this isotherm northward so that 2.3.3.5. Fog . 13 2.3.3.6. Wind . 13 only the northernmost parts of Scandinavia are included. 2.4. Physical/geographical description of the terrestrial Arctic 13 Cold water and air from the Arctic Ocean Basin in turn 2.4.1. -
Norwegian Arctic Expansionism, Victoria Island (Russia) and the Bratvaag Expedition IAN GJERTZ1 and BERIT MØRKVED2
ARCTIC VOL. 51, NO. 4 (DECEMBER 1998) P. 330– 335 Norwegian Arctic Expansionism, Victoria Island (Russia) and the Bratvaag Expedition IAN GJERTZ1 and BERIT MØRKVED2 (Received 6 October 1997; accepted in revised form 22 March 1998) ABSTRACT. Victoria Island (Ostrov Viktoriya in Russian) is the westernmost island of the Russian Arctic. The legal status of this island and neighbouring Franz Josef Land was unclear in 1929 and 1930. At that time Norwegian interests attempted, through a secret campaign, to annex Victoria Island and gain a foothold on parts of Franz Josef Land. We describe the events leading up to the Norwegian annexation, which was later abandoned for political reasons. Key words: Franz Josef Land, Victoria Island, Norwegian claim, acquisition of sovereignty RÉSUMÉ. L’île Victoria (en russe Ostrov Viktoriya) est l’île la plus occidentale de l’Arctique russe. En 1929 et 1930, le statut légal de cette île et de l’archipel François-Joseph voisin n’était pas bien défini. À cette époque, les intérêts norvégiens tentaient, par le biais d’une campagne secrète, d’annexer l’île Victoria et d’établir une emprise sur des zones de l’archipel François- Joseph. On décrit les événements menant à l’annexion norvégienne, annexion qui fut délaissée par la suite pour des raisons politiques. Mots clés: archipel François-Joseph, île Victoria, revendication norvégienne, acquisition de la souveraineté Traduit pour la revue Arctic par Nésida Loyer. INTRODUCTION One of the bases for claiming these polar areas was that Norwegians either had discovered them or had vital eco- Norway has a long tradition in Arctic exploration, fishing, nomic interests in them as the most important commercial sealing, and hunting. -
After the Ice – the Arctic and European Security
REPORT — AUTUMN 2020 After the ice The Arctic and European security The authors in this discussion paper contribute in their personal capacities, and their views do not necessarily reflect those of the organisations they represent, nor of Friends of Europe and its board of trustees, members or partners. Reproduction on whole or in part is permitted, provided that full credit is given to Friends of Europe, and that any such reproduction, whether in whole or in part, is not sold unless incorporated in other works. The European Commission support for the production of this publication does not constitute an endorsement of the contents which reflects the views only of the authors, and the Commission cannot be held responsible for any use which may be made of the information contained therein. Co-funded by the Europe for Citizens Programme of the European Union Publisher: Geert Cami Director: Nathalie Furrer, Dharmendra Kanani Programme Manager: Raphaël Danglade Programme Assistant: Clara Casert Editor: Robert Arenella, Arnaud Bodet, Eleanor Doorley, Angela Pauly Design: Elza Lőw, Lucien Leyh © Friends of Europe - July 2019 Submarine and Polar Bears in the Arctic Submarine and Polar Bears in the Arctic This report is part of Friends of Europe’s Peace, Security and Defence programme. Written by Paul Taylor, it brings together the views of scholars, policymakers and senior defence and security stakeholders. Unless otherwise indicated, this report reflects the writer’s understanding of the views expressed by the interviewees. The author and the participants contributed in their personal capacities, and their views do not necessarily reflect those of the institutions they represent, or of Friends of Europe and its board of trustees, members or partners. -
UNIVERSITY of VAASA SCHOOL of MANAGEMENT Lisbet
UNIVERSITY OF VAASA SCHOOL OF MANAGEMENT Lisbet Frey WHO OWNS THE NORTH POLE? Analysis of the territorial claims made by the Arctic states over the Continental shelf in the Arctic Ocean. Public Law Master’s Thesis VAASA 2018 1 INDEX page LIST OF FIGURES 3 ABBREVIATIONS 4 ABSTRACT/ TIIVISTELMÄ 7 1. INTRODUCTION 9 1.1. General background and limitations 11 1.2. Method and Material 14 1.3. Geographical Limitations 19 2. MARITIME ZONES UNDER UNCLOS 23 2.1. Baselines 24 2.2. Internal Waters 35 2.3. Territorial Sea 35 2.4.Contiguous Zone 39 2.5. Exclusive Economic Zone (EEZ) 40 2.6. Continental Shelf 44 2.7. International Waters (High Seas) 50 2.8. The Area 51 2.9. Regime of Islands 53 3. GLOBAL OCEAN GOVERNANCE AND THE ARCTIC REGIME 56 3.1. The International Maritime Organisation (IMO) 56 3.2. The International Seabed Authority (ISA) 58 3.3. Commission on the Limits of the Continental Shelf (CLCS) 61 3.4. International Tribunal for Law of the Sea (ITLOS) 67 3.5. Dispute Settlement and Choice of Procedure 70 3.6. The Arctic Regime 72 3.7. The Arctic Five and the Ilulissat Declaration 72 3.8. The Arctic Council 74 3.9. The Relationship between the Arctic Five-Sates and the Arctic Council 79 2 4. TERRITORIAL CLAIMS AND THE ARCTIC FIVE-REGIME 82 4.1. The Russian Federation Territorial Claims – Background 85 4.2. Norway’s Territorial Claims 88 4.3. Kingdom of Denmark and Greenland Territorial Claims 90 4.4. Canada’s Territorial Claims 93 4.5. -
Of the Russian Arctic Islands in the Barents Sea
Polar Biology https://doi.org/10.1007/s00300-018-2425-z ORIGINAL PAPER Moths and butterfies (Insecta: Lepidoptera) of the Russian Arctic islands in the Barents Sea J. Kullberg1 · B. Yu. Filippov2 · V. M. Spitsyn2,3 · N. A. Zubrij2,3 · M. V. Kozlov4 Received: 28 April 2018 / Revised: 10 October 2018 / Accepted: 22 October 2018 © The Author(s) 2018 Abstract Faunistic data are scarce for the Lepidoptera from the Arctic islands of European Russia. New sampling and revision of the earlier fndings have revealed the occurrence of 60 species of moths and butterfies on Kolguev, Vaygach and Dolgij Islands and on the Novaya Zemlya archipelago. The faunas of Kolguev and Dolgij Islands (19 and 18 species, respectively) include typical moths of the northern taiga (Aethes deutschiana, Syricoris lacunana and Xanthorhoe designata), and the low num- bers of species discovered on these islands have resulted primarily from low collecting eforts. By contrast, the fauna of Vaygach Island (22 species) is relatively well known and includes several high Arctic species, such as Xestia aequaeva, X. liquidaria and X. lyngei. Nevertheless, Vaygach Island is depauperated even relative to the fauna of Amderma (29 species), which is located on the continent next to the Vaygach Island. The fauna of Novaya Zemlya totals 30 species, but only eight of these were collected from the Northern Island, mostly near Matochkin Shar strait. Noteworthy is the record of Plutella polaris from Novaya Zemlya: this species was recently re-discovered in Svalbard, where the type series was collected in 1873. Udea itysalis, described from North America, is reported here for the frst time from Europe. -
America's Arctic Moment
MARCH 2020 AMERICA’S ARCTIC MOMENT Great Power Competition in the Arctic to 2050 PRINCIPAL AUTHORS Heather A. Conley Matthew Melino CONTRIBUTING AUTHORS Nikos Tsafos Ian Williams A Report of the CSIS Europe Program AMERICA’S ARCTIC MOMENT / Great Power Competition in the Arctic to 2050 ABOUT CSIS The Center for Strategic and International Studies (CSIS) is a bipartisan, nonprofit policy research organization dedicated to advancing practical ideas to address the world’s greatest challenges. Thomas J. Pritzker was named chairman of the CSIS Board of Trustees in 2015, suc- ceeding former U.S. Senator Sam Nunn (D-GA). Founded in 1962, CSIS is led by John J. Hamre, who has served as president and chief executive officer since 2000. CSIS’s purpose is to define the future of national security. We are guided by a dis- tinct set of values—nonpartisanship, independent thought, innovative thinking, cross-disciplinary scholarship, integrity and professionalism, and talent develop- ment. CSIS’s values work in concert toward the goal of making real-world impact. CSIS scholars bring their policy expertise, judgment, and robust networks to their research, analysis, and recommendations. We organize conferences, publish, lecture, and make media appearances that aim to increase the knowledge, awareness, and salience of policy issues with relevant stakeholders and the interested public. CSIS has impact when our research helps to inform the decisionmaking of key pol- icymakers and the thinking of key influencers. We work toward a vision of a safer and more prosperous world. CSIS is ranked the number one think tank in the United States as well as the defense and national security center of excellence for 2016-2018 by the University of Penn- sylvania’s annual think tank report. -
Form and Flow of the Academy of Sciences Ice Cap, Severnaya Zemlya, Russian High Arctic J
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 107, NO. B4, 2076, 10.1029/2000JB000129, 2002 Form and flow of the Academy of Sciences Ice Cap, Severnaya Zemlya, Russian High Arctic J. A. Dowdeswell,1 R. P. Bassford,2 M. R. Gorman,1 M. Williams,3 A. F. Glazovsky,4 Y. Y. Macheret,4 A. P. Shepherd,5 Y. V. Vasilenko,6 L. M. Savatyuguin,7 H.-W. Hubberten,8 and H. Miller 8 Received 28 December 2000; revised 10 July 2001; accepted 14 July 2001; published 20 April 2002. 2 [ 1 ] The 5,575-km Acad emy of Sciences Ice Cap is the largest in the Russia n Arctic. A 100-M Hz airbo rne radar, digital Landsat imagery, and satelli te syntheti c apertu re radar (SAR) interfero metry are used to investig ate its form and flow, incl uding the propor tion of mass lost throu gh iceberg calvi ng. The ice cap was covered by a 10-km -space d grid of radar fli ght paths , and the centr al porti on was covered by a grid at 5-km inte rvals: a total of 1,657 km of radar data. Digit al elevation model s (DEM s) of ice surfa ce elevation, ice thickness, and bed elevat ion data sets wer e produce d (cell size 500 m). The DEMs wer e used in the selec tion o f a deep ice core dril l site. To tal ice cap volum e is 2,1 84 km3 ( 5.5 mm sea level equiva lent). The ice cap has a single dome reachi ng 749 m. -
The High Arctic Geopotential Stress Field and Its Implications for the Geodynamic 2 Evolution
1 The High Arctic geopotential stress field and its implications for the geodynamic 2 evolution 3 Christian Schiffer1*, Christian Tegner2, Andrew J. Schaeffer3, Victoria Pease4, Søren B. 4 Nielsen2 5 1Department of Earth Sciences, Durham University, Durham DH1 3LE, UK 6 2Centre of Earth System Petrology, Department of Geoscience, Aarhus University, 8000 7 Aarhus, Denmark 8 3Department of Earth and Environmental Sciences, University of Ottawa, 120 9 University, Ottawa ON Canada, K1N 6N5 10 4Department of Geological Sciences, Stockholm University, 106 91, Sweden 11 *Corresponding Author (email: [email protected]) 12 13 14 Abstract 15 We use new models of crustal structure and the depth of the lithosphere-asthenosphere 16 boundary to calculate geopotential energy and its corresponding geopotential stress field for 17 the High Arctic. Palaeo-stress indicators such as dykes and rifts of known age are used to 18 compare the present-day and palaeo stress field. When both stress fields coincide, a 19 minimum age for the configuration of the lithospheric stress field may be defined. We 20 identify three regions in which this is observed. In North Greenland and the eastern 21 Amerasia Basin the stress field is likely the same as during the late Cretaceous. In western 22 Siberia, the stress field is similar to that of the Triassic. The stress directions on the eastern 23 Russian Arctic shelf and the Amerasia Basin are similar to that of the Cretaceous. The 24 persistent misfit of the present stress field and Early Cretaceous dyke swarms associated 25 with the High Arctic Large Igneous Province indicates a short-lived transient change of the 26 stress field at the time of dyke emplacement. -
Status of the Endangered Ivory Gull, Pagophila Eburnea, in Greenland
Published in "Polar Biology 32(9): 1275-1286, 2009" which should be cited to refer to this work. Status of the endangered ivory gull, Pagophila eburnea, in Greenland Olivier Gilg · David Boertmann · Flemming Merkel · Adrian Aebischer · Brigitte Sabard Abstract The ivory gull, a rare high-Arctic species whose >2,000 pairs) since all colonies have not yet been discov- main habitat throughout the year is sea ice, is currently ered and since only 50% or less of the breeding birds are listed in Greenland as ‘Vulnerable’, and as ‘Endangered’ in usually present in the colonies at the time the censuses take Canada, where the population declined by 80% in 20 years. place. Although this estimate is four to eight times higher Despite this great concern, the status of the species in than that previously arrived at, the species seems to be Greenland has been largely unknown as it breeds in remote declining in the south of its Greenland breeding range, areas and in colonies for which population data has rarely, while in North Greenland the trends are unclear and unpre- if at all, been collected. Combining bibliographical dictable, calling for increased monitoring eVorts. research, land surveys, aerial surveys and satellite tracking, we were able to identify 35 breeding sites, including 20 Keywords Pagophila eburnea · Greenland · new ones, in North and East Greenland. Most colonies are Endangered species · Satellite tracking · Climate change · found in North Greenland and the largest are located on Sea-ice islands and lowlands. The current best estimate for the size of the Greenland population is approx. 1,800 breeding birds, but the real Wgure is probably >4,000 adult birds (i.e. -
A Grand Tour of the Ocean Basins by Declan G
Transforms and fracture zones are introduced, also abandoned basins, convergent boundaries, and marginal basins. Instructors can easily change the sequence of stops to suit their courses using the Google Earth desktop app or by editing the KML file.Because large placemark balloons tend to obscure the Google Earth terrain behind them, you are advised to keep Google Earth and this PDF document open in separate windows, preferably on separate monitors or devices. Fig. 0 caption acknowledges all data and imagery sources. A Grand Tour of the Ocean Basins by Declan G. De Paor, [email protected] Welcome to the Grand Tour of the Ocean Basins! Use this document in association with the Google Earth tour which you can download from http://geode.net/GTOB/GTOB.kml Ocean floor ages are from http://nachon.free.fr/GE, based on Müller et al. (2008). See earthbyte.org/Resources/agegrid2008.html. Plate boundaries are from Laurel Goodell’s SERC web page: http://serc.carleton.edu/sp/library/google_earth/examples/ 49004.html based on Bird (2003) and programmed by Thomas Chust. Colors and line sizes were changed to improve visibility for persons with color vision deficiency, and I added other minor adjustments. The Tour Stops are arranged in a teaching sequence, Fig. 0. Plate Tectonics on Google Earth. ©2017 Google starting with continental rifting and incipient ocean basin Inc. Data SIO, NOAA, US Navy, NGA, USGS, GEBCO, formation in East Africa and the Red Sea and ending with NSF, LDEO, NOAA. Image Landsat/Copernicus, IBCAO, the oldest surviving fragments of oceanic crust. PGC, LDEO-Columbia. -
The Evolution of Knowledge About the Arctic and Its Climate
Cambridge University Press 0521814189 - The Arctic Climate System Mark C. Serreze and Roger G. Barry Excerpt More information 1 The evolution of knowledge about the Arctic and its climate Overview The land of the midnight sun has enchanted humankind for centuries. Rarely does a visitor to this unique and storied region leave without impressions that last a lifetime. Whether it is images of immense glaciers, the shifting pack ice under steel grey skies, or bountiful wildlife grazing treeless, windswept tundra, the Arctic, even today, evokes images of a largely wild and untamed place. For many, the Arctic is as much a feeling as it is a region. Those with even a passing knowledge of the Arctic are familiar with the spirit of adventure – humans against nature – that drove some of the early exploration of the region. But the history of Arctic exploration and discovery is much more than Peary’s glorified, albeit doubtful conquest of the pole. The expeditions of Bering, Franklin, Frobisher, Hudson, Nansen, Nares, Sverdrup, Wegener and others variously reflected nationalism, the shifting economic significance of the region, and scientific inquiry. Many of the geographic place names in the Arctic honor these explorers (Figure 1.1). To appreciate our present understanding of the Arctic, we need to step back and review some of this rich history over the past four or five centuries, recognizing, of course, that there have been indigenous populations in the Arctic for many thousands of years. 1 © Cambridge University Press www.cambridge.org Cambridge University Press 0521814189 - The Arctic Climate System Mark C. Serreze and Roger G. -
The Historical and Legal Background of Canada's Arctic Claims
THE HISTORICAL AND LEGAL BACKGROUND OF CANADA’S ARCTIC CLAIMS ii © The estate of Gordon W. Smith, 2016 Centre on Foreign Policy and Federalism St. Jerome’s University 290 Westmount Road N. Waterloo, ON, N2L 3G3 www.sju.ca/cfpf All rights reserved. This ebook may not be reproduced without prior written consent of the copyright holder. LIBRARY AND ARCHIVES CANADA CATALOGUING IN PUBLICATION Smith, Gordon W., 1918-2000, author The Historical and Legal Background of Canada’s Arctic Claims ; foreword by P. Whitney Lackenbauer (Centre on Foreign Policy and Federalism Monograph Series ; no.1) Issued in electronic format. ISBN: 978-0-9684896-2-8 (pdf) 1. Canada, Northern—International status—History. 2. Jurisdiction, Territorial— Canada, Northern—History. 3. Sovereignty—History. 4. Canada, Northern— History. 5. Canada—Foreign relations—1867-1918. 6. Canada—Foreign relations—1918-1945. I. Lackenbauer, P. Whitney, editor II. Centre on Foreign Policy and Federalism, issuing body III. Title. IV. Series: Centre on Foreign Policy and Federalism Monograph Series ; no.1 Page designer and typesetting by P. Whitney Lackenbauer Cover design by Daniel Heidt Distributed by the Centre on Foreign Policy and Federalism Please consider the environment before printing this e-book THE HISTORICAL AND LEGAL BACKGROUND OF CANADA’S ARCTIC CLAIMS Gordon W. Smith Foreword by P. Whitney Lackenbauer Centre on Foreign Policy and Federalism Monograph Series 2016 iv Dr. Gordon W. Smith (1918-2000) Foreword FOREWORD Dr. Gordon W. Smith (1918-2000) dedicated most of his working life to the study of Arctic sovereignty issues. Born in Alberta in 1918, Gordon excelled in school and became “enthralled” with the history of Arctic exploration.