Bering Strait and Bering Sea, Docket ID: USCG-2014-0941
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Russia and the Eurasian Republics THIS REGION Spans the Continents of Europe and Asia
390-391 U5 CH14 UO TWIP-860976 3/15/04 5:21 AM Page 390 Unit Workers on the statue Russians in front of Motherland Calls, St. Basil’s Cathedral, Volgograd Moscow 224 390-391 U5 CH14 UO TWIP-860976 3/15/04 5:22 AM Page 391 RussiaRussia andand the the EurasianEurasian f you had to describe Russia RepublicsRepublics Iin one word, that word would be BIG! Russia is the largest country in the world in area. Its almost 6.6 million square miles (17 million sq. km) are spread across two continents—Europe and Asia. As you can imagine, such a large country faces equally large challenges. In 1991 Russia emerged from the Soviet Union as an independent country. Since then it has been struggling to unite its many ethnic groups, set up a demo- cratic government, and build a stable economy. ▼ Siberian tiger in a forest NGS ONLINE in eastern Russia www.nationalgeographic.com/education 225 392-401 U5 CH14 RA TWIP-860976 3/15/04 5:28 AM Page 392 REGIONAL ATLAS Focus on: Russia and the Eurasian Republics THIS REGION spans the continents of Europe and Asia. It includes Russia—the world’s largest country—and the neigh- boring independent republics of Armenia, Georgia, Azerbaijan, Kazakhstan, Uzbekistan, Turkmenistan, Kyrgyzstan, and Tajikistan. Russia and the Eurasian republics cover about 8 million square miles (20.7 million sq. km). This is greater than the size of Canada, the United States, and Mexico combined. The Caspian Sea is actually a salt lake that lies at the base of the Caucasus Mountains in The Land Russia’s southwest. -
Fronts in the World Ocean's Large Marine Ecosystems. ICES CM 2007
- 1 - This paper can be freely cited without prior reference to the authors International Council ICES CM 2007/D:21 for the Exploration Theme Session D: Comparative Marine Ecosystem of the Sea (ICES) Structure and Function: Descriptors and Characteristics Fronts in the World Ocean’s Large Marine Ecosystems Igor M. Belkin and Peter C. Cornillon Abstract. Oceanic fronts shape marine ecosystems; therefore front mapping and characterization is one of the most important aspects of physical oceanography. Here we report on the first effort to map and describe all major fronts in the World Ocean’s Large Marine Ecosystems (LMEs). Apart from a geographical review, these fronts are classified according to their origin and physical mechanisms that maintain them. This first-ever zero-order pattern of the LME fronts is based on a unique global frontal data base assembled at the University of Rhode Island. Thermal fronts were automatically derived from 12 years (1985-1996) of twice-daily satellite 9-km resolution global AVHRR SST fields with the Cayula-Cornillon front detection algorithm. These frontal maps serve as guidance in using hydrographic data to explore subsurface thermohaline fronts, whose surface thermal signatures have been mapped from space. Our most recent study of chlorophyll fronts in the Northwest Atlantic from high-resolution 1-km data (Belkin and O’Reilly, 2007) revealed a close spatial association between chlorophyll fronts and SST fronts, suggesting causative links between these two types of fronts. Keywords: Fronts; Large Marine Ecosystems; World Ocean; sea surface temperature. Igor M. Belkin: Graduate School of Oceanography, University of Rhode Island, 215 South Ferry Road, Narragansett, Rhode Island 02882, USA [tel.: +1 401 874 6533, fax: +1 874 6728, email: [email protected]]. -
Pribilof Islands Red King Crab
2011 Stock Assessment and Fishery Evaluation Report for the Pribilof Islands Blue King Crab Fisheries of the Bering Sea and Aleutian Islands Regions R.J. Foy Alaska Fisheries Science Center National Marine Fisheries Service, NOAA Executive Summary *highlighted text will be filled in with new survey and catch data prior to the September 2011 meeting. 1. Stock: Pribilof Islands blue king crab, Paralithodes platypus 2. Catches: Retained catches have not occurred since 1998/1999. Bycatch and discards have been steady or decreased in recent years to current levels near 0.5 t (0.001 million lbs). 3. Stock biomass: Stock biomass in recent years was decreasing between the 1995 and 2008 survey, and after a slight increase in 2009, there was a decrease in most size classes in 2010. 4. Recruitment: Recruitment indices are not well understood for Pribilof blue king crab. Pre-recruit have remained relatively consistent in the past 10 years although may not be well assessed with the survey. 5. Management performance: MSST Biomass Retained Total Year TAC OFL ABC (MMBmating) Catch Catch 2,105 113A 0 0 0.5 1.81 2008/09 (4.64) (0.25) (0.001) (0.004) 2,105 513B 0 0 0.5 1.81 2009/10 (4.64) (1.13) (0.001) (0.004) 286 C 1.81 2010/11 (0.63) (0.004) 2011/12 xD All units are tons (million pounds) of crabs and the OFL is a total catch OFL for each year. The stock was below MSST in 2009/10 and is hence overfished. Overfishing did not occur during the 2009/10 fishing year. -
The Pacific Gateway to the Arctic: Recent Change in the Bering Strait - Observations, Drivings and Implications
1 The Pacific Gateway to the Arctic: Recent change in the Bering Strait - observations, drivings and implications Rebecca Woodgate, Cecilia Peralta-Ferriz University of Washington, Seattle, USA Recent Change in the Bering Strait New Climatology and Bering Strait products The long-sought “Pacific-ARCTIC” pressure head forcing NASA The Bering Strait, … on a good day Alaska Russia ~ 85 km wide, ~ 50 m deep LOCALLY: - divided into 2 channels by - is an integrator of the the Diomede Islands properties of the Bering Sea - split by the US-Russian - dominates the water border properties of the Chukchi Sea - ice covered ~ Jan - April 8th July 2010 Ocean Color oceancolor.gsfc.nasa.gov (from Bill Crawford) ... influences Important for ~ half of the Russia 80N Marine Life Arctic Ocean Most nutrient-rich watersBarents entering Sea the Arctic (Walsh et al, 1989) Heat to melt ice Fram In spring, trigger western Arctic StraitGreenland melt onset Sea Bering Impacts Global climate stability Year-round subsurface heatStrait Doubling of flow affects Gulf source in ~ half of Arctic Greenland Alaska Stream, overturning circulation (Paquette & Bourke, 1981; Ahlnäs & Garrison,1984; (Wadley & Bigg, 2002; Huang & Schmidt, 1993; Woodgate et al, 2010; 2012) CanadianDeBoer & Nof , 2004; Hu & Meehl, 2005) Archipelago Important for Arctic Stratification Significant part of Arctic In winter, Pacific waters (fresher than Freshwater Budget Atlantic waters) form a cold ~ 1/3rd of Arctic Freshwater (halocline) layer, which insulates the Large (largest?) ice from the warm Atlantic water interannual variability beneath (Wijffels et al, 1992; Aagaard & Carmack, 1989; (Shimada et al, 2001, Steele et al, 2004) Woodgate & Aagaard, 2005) Figure from Woodgate, 2013, Nature Education 4 Overview of Bering Strait measurements MODIS SST 26th Aug 2004 Early 1990s, 2004-2006 == 1+ moorings also in Russian waters. -
Contemporary State of Glaciers in Chukotka and Kolyma Highlands ISSN 2080-7686
Bulletin of Geography. Physical Geography Series, No. 19 (2020): 5–18 http://dx.doi.org/10.2478/bgeo-2020-0006 Contemporary state of glaciers in Chukotka and Kolyma highlands ISSN 2080-7686 Maria Ananicheva* 1,a, Yury Kononov 1,b, Egor Belozerov2 1 Russian Academy of Science, Institute of Geography, Moscow, Russia 2 Lomonosov State University, Faculty of Geography, Moscow, Russia * Correspondence: Russian Academy of Science, Institute of Geography, Moscow, Russia. E-mail: [email protected] a https://orcid.org/0000-0002-6377-1852, b https://orcid.org/0000-0002-3117-5554 Abstract. The purpose of this work is to assess the main parameters of the Chukotka and Kolyma glaciers (small forms of glaciation, SFG): their size and volume, and changes therein over time. The point as to whether these SFG can be considered glaciers or are in transition into, for example, rock glaciers is also presented. SFG areas were defined from the early 1980s (data from the catalogue of the glaciers compiled by R.V. Sedov) to 2005, and up to 2017: these data were retrieved from sat- Key words: ellite images. The maximum of the SGF reduction occurred in the Chantalsky Range, Iskaten Range, Chukotka Peninsula, and in the northern part of Chukotka Peninsula. The smallest retreat by this time relates to the gla- Kolyma Highlands, ciers of the southern part of the peninsula. Glacier volumes are determined by the formula of S.A. satellite image, Nikitin for corrie glaciers, based on in-situ volume measurements, and by our own method: the av- climate change, erage glacier thickness is calculated from isogypsum patterns, constructed using DEMs of individu- glacier reduction, al glaciers based on images taken from a drone during field work, and using ArcticDEM for others. -
Aleuts: an Outline of the Ethnic History
i Aleuts: An Outline of the Ethnic History Roza G. Lyapunova Translated by Richard L. Bland ii As the nation’s principal conservation agency, the Department of the Interior has re- sponsibility for most of our nationally owned public lands and natural and cultural resources. This includes fostering the wisest use of our land and water resources, protecting our fish and wildlife, preserving the environmental and cultural values of our national parks and historical places, and providing for enjoyment of life through outdoor recreation. The Shared Beringian Heritage Program at the National Park Service is an international program that rec- ognizes and celebrates the natural resources and cultural heritage shared by the United States and Russia on both sides of the Bering Strait. The program seeks local, national, and international participation in the preservation and understanding of natural resources and protected lands and works to sustain and protect the cultural traditions and subsistence lifestyle of the Native peoples of the Beringia region. Aleuts: An Outline of the Ethnic History Author: Roza G. Lyapunova English translation by Richard L. Bland 2017 ISBN-13: 978-0-9965837-1-8 This book’s publication and translations were funded by the National Park Service, Shared Beringian Heritage Program. The book is provided without charge by the National Park Service. To order additional copies, please contact the Shared Beringian Heritage Program ([email protected]). National Park Service Shared Beringian Heritage Program © The Russian text of Aleuts: An Outline of the Ethnic History by Roza G. Lyapunova (Leningrad: Izdatel’stvo “Nauka” leningradskoe otdelenie, 1987), was translated into English by Richard L. -
Status and Occurrence of Parakeet Auklet (Aethia Psittacula) in British Columbia
Status and Occurrence of Parakeet Auklet (Aethia psittacula) in British Columbia. By Rick Toochin and Louis Haviland. Introduction and Distribution The Parakeet Auklet (Aethia psittacula) is a small species of auklet found breeding in the Beringia region of Alaska and Russia (Gaston and Jones 1998). This species has an Alaskan population estimated at 1 million birds (Gaston and Jones 1998). There is also a Russian population, but the exact population total is not known, due to a lack of population inventory work, but it is estimated to number about 400,000 birds with the vast majority, about 300,000 birds, found in the Sea of Okhotsk (Gaston and Jones 1998). The Parakeet Auklet has breeding colonies that are found on rocky mainland points and islands in the Gulf of Alaska (Jones et al. 2001). These sites include: Shumagin Island, Semidi Isand, Chirikof Island near Kodiak, locally in Kenai Peninsula and southeastern Alaska with small numbers south to St. Lazaria, Hazy and Forrester Island; and in the Aleutian Islands west to Buldir and Agattu Island; and in the Bering Sea at Little Diomede, St. Lawrence Island, King Island, St. Matthew Island, Pribilof Island and Nunivak Island (Sowls et al. 1978). The Parakeet Auklet also breeds in Russia in the Kurile Island chain with colonies on Chirinkontan, Lovushki, Raikoke, Matua, Yankicha, Simushir, Brat Chirpoev, Urup, and Iturup Island (Jones et al. 2001, Brazil 2009). They are also breeding on islands in the Sea of Okhotsk with colonies on Sakhalin, Tyuleniy, Iona, Talan, and Yamskyie Island (Jones et al. 2001, Brazil 2009). The Parakeet Auklet is also found breeding on Commander Island, and northwards locally along coast of the Kamchatka Peninsula, on Karaginski Island, Cape Navarin, and on Chukotka Peninsula (Konyukhov 1989, Kondratyev et al. -
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. -
J. W. Vanstone
AN EARLY ACCOUNT OF THE~RUSSIAN DISCOVERIES ,IN THE NORTH PACIFIC TRANSLATED AND EDITED By JAMES W. VANSTONE INTRODUCTION Although the remnants of Bering's second expedition returned to Kamchatka during the summer of 1742, it was not until 1758 that the first connected narrative of this and other Russian discoveries in the northern Pacific was made available to readers in western Europe. In that year, George Frederich Muller, Professor of History in the St. Petersburg Academy of Sciences and member of Bering's expedition iIi Siberia, published an account based on records in the government files at Irkutsk and J akutsk, together with documents collected after his return to Russia. This work, written in German and translated into English (Muller, 1761) and French, is the standard narrative of what Masterson and Brower (1948, pp. 3-4) have referred to as the first chapter in the history of Alaska which ended with the return of Bering's expedition.! In 1774, Jacob Stahlin von Storcksburg, also of the St. Petersburg Academy -of Sciences, published an account of the post-Bering discov eries that was translated into English the same year (Stahlin, 1774). This work contains vague and confused references to the expedition of Lieutenant "Syndo" and a very inaccurate description of Kodiak Island and certain islands in the Aleutian chain.Resale There is nothing in the tex t to suggest that any of the islands were discovered before 1765. This work is accompanied by a map which is equally confused and inaccurate. The numerous deficiencies forin Stahlin were at least partly respon sible for the publication, in 177.6, of Neue Nachrichten von denen neuen,tdekten Insuln in der See zwischen Asien und Amerika, aus, mitgetheiLten Urkunden urud A uszugen verfasset von J.L.S. -
Inuit People
Inuit People Most of these objects were made in the 19th century by the Inuit, whose name means ‘the people’. The Athabascans called their Inuit neighbours ‘Eskimo’ meaning ‘eaters of raw flesh’. The Inuit way of life was adapted to their harsh territory which stretched 6000 miles across the Arctic from the Bering Sea to Greenland. Carving 80 Chisel handle made from bone with a carved face and animal figures. Possibly from south Alaska, made before 1880. 81 Carrying strap made of hide with a carved stone toggle, made in the 19th century. 82 Smoking pipe made of ivory and decorated with whaling scenes. Made by the western Inuit in the late 19th century. 83 Ivory toggle carved in the form of a seal. Probably made by the western Inuit before 1854. 84 Ivory toggle carved in the form of a bear. Probably made by the western Inuit before 1854. Hunting 85 Snow goggles made of wood. Used in the snow like sun glasses to protect the eyes. Made by the central Inuit before 1831. 86 Bolas made of ivory balls and gut strips, from Cape Lisburn, Bering Strait, made before 1848. Thrown when hunting to entangle a bird or other quarry. 87 Harpoon head, probably for a seal harpoon. Made by the western Inuit in the 19th century. 88 Seal decoy made of wood with claws. It was Used to scratch the ice. The sound attracted seals to breathing holes. Probably made by the western Inuit in the late 19th century. 89 Bone scoop used for clearing seal breathing holes in the ice, made in the 19th century. -
Climate-Ocean Effects on AYK Chinook Salmon
SAFS-UW-1003 2010 Arctic Yukon Kuskokwim (AYK) Sustainable Salmon Initiative Project Final Product1 Climate-Ocean Effects on AYK Chinook Salmon Chukchi Sea by Katherine W. Myers2, Robert V. Walker2, Nancy D. Davis2, Janet L. Armstrong2, Wyatt J. Fournier2, Nathan J. Mantua2, and Julie Raymond-Yakoubian 3 2High Seas Salmon Research Program, School of Aquatic & Fishery Sciences (SAFS), University of Washington (UW), Box 355020, Seattle, WA 98195-5020, USA 3Kawerak, Inc., PO Box 948, Nome, AK 99762, USA November 2010 1Final products of AYK Sustainable Salmon Initiative (SSI) research are made available to the Initiatives partners and the public in the interest of rapid dissemination of information that may be useful in salmon management, research, or administration. Sponsorship of the project by the AYK SSI does not necessarily imply that the findings or conclusions are endorsed by the AYK SSI. ABSTRACT A high-priority research issue identified by the Arctic-Yukon-Kuskokwim (AYK) Sustainable Salmon Initiative (SSI) is to determine whether the ocean environment is a more important cause of variation in the abundance of AYK Pacific salmon (Oncorhynchus spp.) populations than marine fishing mortality. At the outset of this project, however, data on ocean life history of AYK salmon were too limited to test hypotheses about the effects of environmental conditions versus fishing on marine survival. Our goal was to identify and evaluate life history patterns of use of marine resources (habitat and food) by Chinook salmon (O. tshawytscha) and to explore how these patterns are affected by climate-ocean conditions, including documentation of local traditional knowledge (LTK) of this high-priority issue. -
Social Transition in the North, Vol. 1, No. 4, May 1993
\ / ' . I, , Social Transition.in thb North ' \ / 1 \i 1 I '\ \ I /? ,- - \ I 1 . Volume 1, Number 4 \ I 1 1 I Ethnographic l$ummary: The Chuko tka Region J I / 1 , , ~lexdderI. Pika, Lydia P. Terentyeva and Dmitry D. ~dgo~avlensly Ethnographic Summary: The Chukotka Region Alexander I. Pika, Lydia P. Terentyeva and Dmitry D. Bogoyavlensky May, 1993 National Economic Forecasting Institute Russian Academy of Sciences Demography & Human Ecology Center Ethnic Demography Laboratory This material is based upon work supported by the National Science Foundation under Grant No. DPP-9213l37. Any opinions, findings, and conclusions or recammendations expressed in this material are those of the author@) and do not ncccssarily reflect the vim of the National Science Foundation. THE CHUKOTKA REGION Table of Contents Page: I . Geography. History and Ethnography of Southeastern Chukotka ............... 1 I.A. Natural and Geographic Conditions ............................. 1 I.A.1.Climate ............................................ 1 I.A.2. Vegetation .........................................3 I.A.3.Fauna ............................................. 3 I1. Ethnohistorical Overview of the Region ................................ 4 IIA Chukchi-Russian Relations in the 17th Century .................... 9 1I.B. The Whaling Period and Increased American Influence in Chukotka ... 13 II.C. Soviets and Socialism in Chukotka ............................ 21 I11 . Traditional Culture and Social Organization of the Chukchis and Eskimos ..... 29 1II.A. Dwelling ..............................................