Research on Polar Bear Autumn Aggregations on Chukotka, 1989–2004
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Transit Passage in the Russian Arctic Straits
International Boundaries Research Unit MARITIME BRIEFING Volume 1 Number 7 Transit Passage in the Russian Arctic Straits William V. Dunlap Maritime Briefing Volume 1 Number 7 ISBN 1-897643-21-7 1996 Transit Passage in the Russian Arctic Straits by William V. Dunlap Edited by Peter Hocknell International Boundaries Research Unit Department of Geography University of Durham South Road Durham DH1 3LE UK Tel: UK + 44 (0) 191 334 1961 Fax: UK +44 (0) 191 334 1962 e-mail: [email protected] www: http://www-ibru.dur.ac.uk Preface The Russian Federation, continuing an initiative begun by the Soviet Union, is attempting to open the Northern Sea Route, the shipping route along the Arctic coast of Siberia from the Norwegian frontier through the Bering Strait, to international commerce. The goal of the effort is eventually to operate the route on a year-round basis, offering it to commercial shippers as an alternative, substantially shorter route from northern Europe to the Pacific Ocean in the hope of raising hard currency in exchange for pilotage, icebreaking, refuelling, and other services. Meanwhile, the international law of the sea has been developing at a rapid pace, creating, among other things, a right of transit passage that allows, subject to specified conditions, the relatively unrestricted passage of all foreign vessels - commercial and military - through straits used for international navigation. In addition, transit passage permits submerged transit by submarines and overflight by aircraft, practices with implications for the national security of states bordering straits. This study summarises the law of the sea as it relates to straits used for international navigation, and then describes 43 significant straits of the Northeast Arctic Passage, identifying the characteristics of each that are relevant to a determination of whether the strait will be subject to the transit-passage regime. -
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 -
Flow of Pacific Water in the Western Chukchi
Deep-Sea Research I 105 (2015) 53–73 Contents lists available at ScienceDirect Deep-Sea Research I journal homepage: www.elsevier.com/locate/dsri Flow of pacific water in the western Chukchi Sea: Results from the 2009 RUSALCA expedition Maria N. Pisareva a,n, Robert S. Pickart b, M.A. Spall b, C. Nobre b, D.J. Torres b, G.W.K. Moore c, Terry E. Whitledge d a P.P. Shirshov Institute of Oceanology, 36, Nakhimovski Prospect, Moscow 117997, Russia b Woods Hole Oceanographic Institution, 266 Woods Hole Road, Woods Hole, MA 02543, USA c Department of Physics, University of Toronto, 60 St. George Street, Toronto, Ontario M5S 1A7, Canada d University of Alaska Fairbanks, 505 South Chandalar Drive, Fairbanks, AK 99775, USA article info abstract Article history: The distribution of water masses and their circulation on the western Chukchi Sea shelf are investigated Received 10 March 2015 using shipboard data from the 2009 Russian-American Long Term Census of the Arctic (RUSALCA) pro- Received in revised form gram. Eleven hydrographic/velocity transects were occupied during September of that year, including a 25 August 2015 number of sections in the vicinity of Wrangel Island and Herald canyon, an area with historically few Accepted 25 August 2015 measurements. We focus on four water masses: Alaskan coastal water (ACW), summer Bering Sea water Available online 31 August 2015 (BSW), Siberian coastal water (SCW), and remnant Pacific winter water (RWW). In some respects the Keywords: spatial distributions of these water masses were similar to the patterns found in the historical World Arctic Ocean Ocean Database, but there were significant differences. -
On the Nature of Wind-Forced Upwelling in Barrow Canyon ⁎ Maria N
Deep-Sea Research Part II xxx (xxxx) xxx–xxx Contents lists available at ScienceDirect Deep-Sea Research Part II journal homepage: www.elsevier.com/locate/dsr2 On the nature of wind-forced upwelling in Barrow Canyon ⁎ Maria N. Pisarevaa, , Robert S. Pickartb, Peigen Linb, Paula S. Fratantonic, Thomas J. Weingartnerd a P.P. Shirshov Institute of Oceanology RAS, 36, Nakhimovski prospect, Moscow 117997, Russia b Woods Hole Oceanographic Institution, 266 Woods Hole Rd., Woods Hole, MA, 02543, USA c Northeast Fisheries Science Center, 166 Water Street, Woods Hole, MA, 02543, USA d University of Alaska Fairbanks, 505 South Chandalar Drive, Fairbanks, AK, 99775, USA ARTICLE INFO ABSTRACT Keywords: Using time series from a mooring deployed from 2002 to 2004 near the head of Barrow Canyon, together with Arctic Ocean atmospheric and sea-ice data, we investigate the seasonal signals in the canyon as well as aspects of upwelling Barrow Canyon and the wind-forcing that drives it. On average, the flow was down-canyon during each month of the year except Upwelling February, when the up-canyon winds were strongest. Most of the deep flow through the head of the canyon Polynya consisted of cold and dense Pacific-origin winter water, although Pacific-origin summer waters were present in Pacific-origin water masses early autumn. Over the two-year study period there were 54 upwelling events: 33 advected denser water to the Atlantic Water head of the canyon, while 21 upwelled lighter water due to the homogeneous temperature/salinity conditions during the cold season. The upwelling occurs when the Beaufort High is strong and the Aleutian Low is deep, consistent with findings from previous studies. -
Chukchi Sea Itrs 2013
Biological Opinion for Polar Bears (Ursus maritimus) and Conference Opinion for Pacific Walrus (Odobenus rosmarus divergens) on the Chukchi Sea Incidental Take Regulations Prepared by: U.S. Fish and Wildlife Service Fairbanks Fish and Wildlife Field Office 110 12th Ave, Room 110 Fairbanks, Alaska 99701 May 20, 2013 1 Table of Contents Introduction ................................................................................................................................5 Background on Section 101(a)(5) of MMPA ...........................................................................6 The AOGA Petition .................................................................................................................6 History of Chukchi Sea ITRS ..............................................................................................7 Relationship of ESA to MMPA ...........................................................................................7 MMPA Terms: ........................................................................................................................7 ESA Terms: ............................................................................................................................8 The Proposed Action ...................................................................................................................8 Information Required to Obtain a Letter of Authorization .......................................................9 Specific Measures of LOAs .................................................................................................. -
Beaufort Sea: Hypothetical Very Large Oil Spill and Gas Release
OCS Report BOEM 2020-001 BEAUFORT SEA: HYPOTHETICAL VERY LARGE OIL SPILL AND GAS RELEASE U.S. Department of the Interior Bureau of Ocean Energy Management Alaska OCS Region OCS Study BOEM 2020-001 BEAUFORT SEA: HYPOTHETICAL VERY LARGE OIL SPILL AND GAS RELEASE January 2020 Author: Bureau of Ocean Energy Management Alaska OCS Region U.S. Department of the Interior Bureau of Ocean Energy Management Alaska OCS Region REPORT AVAILABILITY To download a PDF file of this report, go to the U.S. Department of the Interior, Bureau of Ocean Energy Management (www.boem.gov/newsroom/library/alaska-scientific-and-technical-publications, and click on 2020). CITATION BOEM, 2020. Beaufort Sea: Hypothetical Very Large Oil Spill and Gas Release. OCS Report BOEM 2020-001 Anchorage, AK: U.S. Department of the Interior, Bureau of Ocean Energy Management, Alaska OCS Region. 151 pp. Beaufort Sea: Hypothetical Very Large Oil Spill and Gas Release BOEM Contents List of Abbreviations and Acronyms ............................................................................................................. vii 1 Introduction ........................................................................................................................................... 1 1.1 What is a VLOS? ......................................................................................................................... 1 1.2 What Could Precipitate a VLOS? ................................................................................................ 1 1.2.1 Historical OCS and Worldwide -
Siberian Coast & Polar Bears of Wrangel Island, Russia
Siberian Coast & Polar Bears of Wrangel Island, Russia Aboard the Spirit of Enderby July 24–August 6, 2013 Tuesday / Wednesday July 23 / July 24 – Anadyr, Russia Arrival Over several days, North American trip participants slowly began to arrive in Nome, Alaska for our charter flights to Anadyr, Russia. Participants from other parts of the world made their way to Anadyr through Moscow. Altogether, passengers included passport holders from 11 countries. Many people had flown into Nome several days early, rented cars, and driven the local roads in search of accessible musk oxen in the meadows near town, Pacific and red-throated loons in small tundra ponds, and gulls, ducks and shorebirds along the coast. On July 23, most of our group consolidated their luggage in our Nome hotel lobby and had it loaded on a truck to be taken to our charter airline hangar, while we followed in a bus with our camera gear. Thick fog was drifting along the coast and, when we reached the hanger, we were informed the Nome Airport was closed to inbound air traffic. That posed no real problem for us because our small airplanes were already at the hangar in Nome, on stand-by and readily available, and, since the fog was intermittent, it seemed certain we would have almost no problem departing to Russia. A breakfast buffet was arranged in the hangar and we were regaled by local Nome personality Richard Beneville—who also organized our land-based transportation—with his tales of moving to Nome following his life as a theater actor in New York City and anecdotes of his decades-long life in hardscrabble Nome. -
Assessing Ocean Acidification Variability in the Pacific–Arctic Region
OceTHE OFFICIALa MAGAZINEn ogOF THE OCEANOGRAPHYra SOCIETYphy CITATION Bates, N.R. 2015. Assessing ocean acidification variability in the Pacific- Arctic region as part of the Russian-American Long-term Census of the Arctic. Oceanography 28(3):36–45, http://dx.doi.org/ 10.5670/oceanog.2015.56. DOI http://dx.doi.org/ 10.5670/oceanog.2015.56 COPYRIGHT This article has been published in Oceanography, Volume 28, Number 3, a quarterly journal of The Oceanography Society. Copyright 2015 by The Oceanography Society. All rights reserved. USAGE Permission is granted to copy this article for use in teaching and research. Republication, systematic reproduction, or collective redistribution of any portion of this article by photocopy machine, reposting, or other means is permitted only with the approval of The Oceanography Society. Send all correspondence to: [email protected] or The Oceanography Society, PO Box 1931, Rockville, MD 20849-1931, USA. DOWNLOADED FROM HTTP://WWW.TOS.ORG/OCEANOGRAPHY RUSSIAN-AMERICAN LONG-TERM CENSUS OF THE ARCTIC Assessing Ocean Acidification Variability in the Pacific-Arctic Region as Part of the Russian-American Long-term Census of the Arctic By Nicholas R. Bates Launch of rosette from Russian research vessel Professor Khromov during a 2009 RUSALCA expedition. Photo credit: Aleksey Ostrovskiy 36 Oceanography | Vol.28, No.3 ABSTRACT. The Russian-American Long-term Census of the Arctic (RUSALCA) to icebreaker surveys conducted on the project provides a rare opportunity to study the Russian sector of the Pacific Arctic Arctic shelves during the summertime sea Region (PAR), which includes the Chukchi and East Siberian Seas. RUSALCA data ice retreat. -
The Polar Bear of the Arctic Coast of Chukotka Download: 1 Mb | *.PDF
CONTENT INTRODUCTION...........................................................................................................................2 1. Objectives....................................................................................................................................2 2. The area of observations .............................................................................................................2 3. Information collection regimes ...................................................................................................4 3.1. Regular stationary observations ...........................................................................................4 3.1. Regular on-the-route observations .......................................................................................4 3.3. Non-regular stationary observations ....................................................................................4 3.4. Incidental cocurrent observations ........................................................................................5 4. Methods of conducting observations ..........................................................................................5 4.1. The order of conducting stationary observations (regular, non-regular and one-time). ......5 4.1.1. General information on observation.............................................................................5 4.1.2. Observations of animals................................................................................................6 4.2. -
Eskimo Languages in Asia, 1791 On, and the Wrangel Island-Point Hope Connection"
Article "Eskimo languages in Asia, 1791 on, and the Wrangel Island-Point Hope connection" Michael E. Krauss Études/Inuit/Studies, vol. 29, n°1-2, 2005, p. 163-185. Pour citer cet article, utiliser l'information suivante : URI: http://id.erudit.org/iderudit/013938ar DOI: 10.7202/013938ar Note : les règles d'écriture des références bibliographiques peuvent varier selon les différents domaines du savoir. Ce document est protégé par la loi sur le droit d'auteur. L'utilisation des services d'Érudit (y compris la reproduction) est assujettie à sa politique d'utilisation que vous pouvez consulter à l'URI https://apropos.erudit.org/fr/usagers/politique-dutilisation/ Érudit est un consortium interuniversitaire sans but lucratif composé de l'Université de Montréal, l'Université Laval et l'Université du Québec à Montréal. Il a pour mission la promotion et la valorisation de la recherche. Érudit offre des services d'édition numérique de documents scientifiques depuis 1998. Pour communiquer avec les responsables d'Érudit : [email protected] Document téléchargé le 9 février 2017 01:45 Eskimo languages in Asia, 1791 on, and the Wrangel Island-Point Hope connection Michael E. Krauss* Résumé: Les langues eskimo en Asie depuis 1791 et la connexion île Wrangel-Point Hope Ce que constate Merck à propos des quatre langues «tchouktches sédentaires» (Eskimo), ou quatre variétés de langue le long de la côte Tchouktche en 1791, est absolument remarquable et mérite d'être interprété avec soin. Par sa description de leur répartition géographique, il est très facile d'identifier les trois premières langues comme étant 1) le sirenikski, 2) le yupik sibérien central, y compris expressément l'île St Laurent et 3) le naukanski. -
Across the Top of the World
EXPEDITION DOSSIER 22ND JULY – 5TH AUGUST 2019 ACROSS THE TOP OF THE WORLD TO WRANGEL AND HERALD ISLANDS © J Ross TO WRANGEL AND ACROSS THE TOP OF THE WORLD HERALD ISLANDS This unique expedition crosses the Arctic Circle and includes the isolated and pristine Wrangel and Herald Islands and a significant section of the wild North Eastern Siberian coastline. It is a journey only made possible in recent years by the thawing in the politics of the region and the retreat of summer pack ice in the Chukchi Sea. The very small distance between Russia and the USA along this border area was known as the Ice Curtain, behind which then and now lies one of the last great undiscovered wilderness areas in the world. The voyage journeys through the narrow Bering Strait, which separates Russia from the United States of America, and then travels west along the Chukotka coastline before crossing the De Long Strait to Wrangel Island. There we will spend four to five days under the guidance of local rangers on the nature reserve. Untouched by glaciers during the last ice age, this island is a treasure trove of Arctic biodiversity and is perhaps best known for the multitude of Polar Bears that breed here. We hope to catch many glimpses of this beautiful animal. The island also boasts the world’s largest population of Pacific Walrus and lies near major feeding grounds for the Gray Whales that migrate thousands of kilometres north from their breeding grounds in Baja, Mexico. Reindeer, Musk Ox and Snow Geese can normally be seen further inland. -
Trophics, and Historical Status of the Pacific Walrus
MODERN POPULATIONS, MIGRATIONS, DEMOGRAPHY, TROPHICS, AND HISTORICAL STATUS OF THE PACIFIC WALRUS by Francis H. Fay with Brendan P. Kelly, Pauline H. Gehnrich, John L. Sease, and A. Anne Hoover Institute of Marine Science University of Alaska Final Report Outer Continental Shelf Environmental Assessment Program Research Unit 611 September 1984 231 TABLE OF CONTENTS Section Page ABSTRACT. .237 LIST OF TABLES. c .239 LIST OF FIGURES . .243 ACKNOWLEDGMENTS . ● . ● . ● . ● . 245 I. INTRODUCTION. ● ● . .246 A. General Nature and Scope of Study . 246 1. Population Dynamics . 246 2. Distribution and Movements . 246 3. Feeding. .247 4. Response to Disturbance . 247 B. Relevance to Problems of Petroleum Development . 248 c. Objectives. .248 II. STUDY AREA. .250 111. SOURCES, METHODS, AND RATIONALE OF DATA COLLECTION . 250 A. History of the Population . 250 B. Distribution and Composition . 251 c. Feeding Habits. .255 D. Effects of Disturbance . 256 IV. RESULTS . .256 A. Historical Review . 256 1. The Russian Expansion Period, 1648-1867 . 258 2. The Yankee Whaler Period, 1848-1914 . 261 233 TABLE OF CONTENTS (Continued) Section w 3. From Depletion to Partial Recovery, 1900-1935 . 265 4. The Soviet Exploitation Period, 1931-1962 . 268 5. The Protective Period, 1952-1982 . 275 B. Distribution and Composition . 304 1. Monthly Distribution . 304 2. Time of Mating . .311 3. Location of the Breeding Areas . 312 4. Time and Place of Birth . 316 5. Sex/Age Composition . 318 c. Feeding Habits. .325 1. Winter, Southeastern Bering Sea . 325 2. Winter, Southwestern Bering Sea . 330 3. Spring, Eastern Bering Sea . 330 4. Summer , Chukchi Sea . .337 5. Amount Eaten in Relation to Age, Sex, Season .