Satellite Telemetry Reveals Population Specific Winter Ranges of Beluga
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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]]. -
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. -
Arctic Research of the United States, Volume 15
This document has been archived. About The journal Arctic Research of the United refereed for scientific content or merit since the States is for people and organizations interested journal is not intended as a means of reporting the in learning about U.S. Government-financed scientific research. Articles are generally invited Arctic research activities. It is published semi- and are reviewed by agency staffs and others as Journal annually (spring and fall) by the National Science appropriate. Foundation on behalf of the Interagency Arctic As indicated in the U.S. Arctic Research Plan, Research Policy Committee (IARPC) and the research is defined differently by different agencies. Arctic Research Commission (ARC). Both the It may include basic and applied research, moni- Interagency Committee and the Commission were toring efforts, and other information-gathering authorized under the Arctic Research and Policy activities. The definition of Arctic according to Act (ARPA) of 1984 (PL 98-373) and established the ARPA is “all United States and foreign terri- by Executive Order 12501 (January 28, 1985). tory north of the Arctic Circle and all United Publication of the journal has been approved by States territory north and west of the boundary the Office of Management and Budget. formed by the Porcupine, Yukon, and Kuskokwim Arctic Research contains Rivers; all contiguous seas, including the Arctic • Reports on current and planned U.S. Govern- Ocean and the Beaufort, Bering, and Chukchi ment-sponsored research in the Arctic; Seas; and the Aleutian chain.” Areas outside of • Reports of ARC and IARPC meetings; and the boundary are discussed in the journal when • Summaries of other current and planned considered relevant to the broader scope of Arctic Arctic research, including that of the State of research. -
Helicobacter Pylori's Historical Journey Through Siberia and the Americas
Helicobacter pylori’s historical journey through Siberia and the Americas Yoshan Moodleya,1,2, Andrea Brunellib,1, Silvia Ghirottoc,1, Andrey Klyubind, Ayas S. Maadye, William Tynef, Zilia Y. Muñoz-Ramirezg, Zhemin Zhouf, Andrea Manicah, Bodo Linzi, and Mark Achtmanf aDepartment of Zoology, University of Venda, Thohoyandou 0950, Republic of South Africa; bDepartment of Life Sciences and Biotechnology, University of Ferrara, 44121 Ferrara, Italy; cDepartment of Mathematics and Computer Science, University of Ferrara, 44121 Ferrara, Italy; dDepartment of Molecular Biology and Genetics, Research Institute for Physical-Chemical Medicine, 119435 Moscow, Russia; eDepartment of Diagnostic and Operative Endoscopy, Pirogov National Medical and Surgical Center, 105203 Moscow, Russia; fWarwick Medical School, University of Warwick, Coventry CV4 7AL, United Kingdom; gLaboratorio de Bioinformática y Biotecnología Genómica, Escuela Nacional de Ciencias Biológicas, Unidad Profesional Lázaro Cárdenas, Instituto Politécnico Nacional, 11340 Mexico City, Mexico; hDepartment of Zoology, University of Cambridge, Cambridge CB2 3EJ, United Kingdom; and iDepartment of Biology, Division of Microbiology, Friedrich Alexander University Erlangen-Nuremberg, 91058 Erlangen, Germany Edited by Daniel Falush, University of Bath, Bath, United Kingdom, and accepted by Editorial Board Member W. F. Doolittle April 30, 2021 (received for review July 22, 2020) The gastric bacterium Helicobacter pylori shares a coevolutionary speakers). However, H. pylori’s presence, diversity, and structure history with humans that predates the out-of-Africa diaspora, and in northern Eurasia are still unknown. This vast region, hereafter the geographical specificities of H. pylori populations reflect mul- Siberia, extends from the Ural Mountains in the west to the tiple well-known human migrations. We extensively sampled H. -
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. -
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. -
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. -
Arctic Marine Aviation Transportation
SARA FRENCh, WAlTER AND DuNCAN GORDON FOundation Response CapacityandSustainableDevelopment Arctic Transportation Infrastructure: Transportation Arctic 3-6 December 2012 | Reykjavik, Iceland 3-6 December2012|Reykjavik, Prepared for the Sustainable Development Working Group Prepared fortheSustainableDevelopment Working By InstituteoftheNorth,Anchorage, Alaska,USA PROCEEDINGS: 20 Decem B er 2012 ICElANDIC coast GuARD INSTITuTE OF ThE NORTh INSTITuTE OF ThE NORTh SARA FRENCh, WAlTER AND DuNCAN GORDON FOundation Table of Contents Introduction ................................................................................ 5 Acknowledgments ......................................................................... 6 Abbreviations and Acronyms .......................................................... 7 Executive Summary ....................................................................... 8 Chapters—Workshop Proceedings................................................. 10 1. Current infrastructure and response 2. Current and future activity 3. Infrastructure and investment 4. Infrastructure and sustainable development 5. Conclusions: What’s next? Appendices ................................................................................ 21 A. Arctic vignettes—innovative best practices B. Case studies—showcasing Arctic infrastructure C. Workshop materials 1) Workshop agenda 2) Workshop participants 3) Project-related terminology 4) List of data points and definitions 5) List of Arctic marine and aviation infrastructure AlASkA DepartmENT OF ENvIRONmental -
Report from the PAME Workshop on Ecosystem Approach to Management
Report from the PAME Workshop on Ecosystem Approach to Management 22-23 January 2011 Tromsø, Norway Table of Content BACKGROUND .................................................................................................................................... 1 WORKSHOP PROGRAM AND PARTICIPANTS .......................................................................... 1 REVIEW AND UPDATE OF THE WORKING MAP ON ARCTIC LMES .................................. 2 CAFF FOCAL MARINE AREAS ............................................................................................................ 2 LMES AND SUBDIVISION INTO SUB-AREAS OR ECO-REGIONS ............................................................. 3 STRAIGHT LINES OR BATHYMETRIC ISOLINES? ................................................................................... 4 LME BOUNDARY ISSUES ..................................................................................................................... 5 REVISED WORKING MAP OF ARCTIC LMES ........................................................................................ 9 STATUS REPORTING FOR ARCTIC LMES ................................................................................ 10 ARCTIC COUNCIL .............................................................................................................................. 11 UNITED NATIONS .............................................................................................................................. 11 ICES (INTERNATIONAL COUNCIL FOR THE EXPLORATION -
A Case of Chukotka
ISSN 1883-1656 Центр Российских Исследований RRC Working Paper Series No. 71 Demographic Situation and Its Perspectives in the Russian Far East: A Case of Chukotka Kazuhiro KUMO August 2017 RUSSIAN RESEARCH CENTER INSTITUTE OF ECONOMIC RESEARCH HITOTSUBASHI UNIVERSITY Kunitachi, Tokyo, JAPAN DEMOGRAPHIC SITUATION AND ITS PERSPECTIVES IN THE RUSSIAN FAR EAST: A CASE OF CHUKОТКА Kazuhiro KUMO 1. INTRODUCTION The purposes of the present study are, first of all, a general review of the population migration patterns in the Far East region of Russia following the demise of the Soviet Union; and secondly, a study of the situation that emerged in the developing regions as a result of the state policy of the Soviet period, using the example of the demographic trends in the Chukotka Autonomous Okrug as one of the most distal Russian territories with respect to the center of Russia. To date, several studies have been conducted on inter-regional migration in Russia; by the the author (Kumo, 1997, 2003) a comparative analysis of migration in the post-Soviet Russia was conducted and major changes taking place in the migration patterns were considered in the specified periods. Yu. Andrienko and S. Guriev (Andrienko and Guriev, 2002) performed a comparative analysis of inter-regional migration based on the gravity model and showed that the adoption of the migration decision by the population depended on the regional-economic variables. The results of the above-mentioned studies demonstrate that traditional means of analyzing migration patterns can be applied to Russia, which went through the change in the state system, and the authors conclude that migration flows are largely dependent on economic reasons. -
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 .............................................. -
Chukotka's Natural Heritage at a Glance
Rough-legged Hawk. for a living planet The Bering Sea Ecoregion CHUKOTKA’S Photo: Peter Grigorovich Chukotka, officially the Chukotsky NATURAL HERITAGE Autonomous Okrug, forms Russia’s north-eastern fron- AT A GLANCE tier. About half of the region’s 737,700 square kilometers lies above the Arctic Circle. The region’s landscape is domi- nated by alpine and arctic tundra, although small larch, pine, birch, poplar, and willow trees can grow in the valleys of larger rivers. More than 900 species of plants grow in Chukotka, The Bering Strait coast. including 400 Photo: Dennis Litovka species of moss and lichen. Polar bears, Thirty fresh- Wrangel Island. water fish species inhabit Chukotka’s inland lakes and streams. Photo: Gennady Smirnov There are 220 bird species in the region. The chilly waters washing the region’s shores provide important habitat for numerous marine mammals, while species such as brown bear, sable, lynx, ermine, mountain hare, and mink can be found in terrestrial habitats. Numerous rare and endangered species inhabit the Chukotsky Autonomous Okrug. Among those listed in the Red Data Book of the Russian Federation are the polar bear, bighorn sheep, narwhal, hump- back whale, finback whale, grey whale, blue whale, razor back, Photo: Arne Nævra, www.naturbilder.no and 24 bird species. Walruses, Wrangel Island. Native hunting party. Siberian dwarf pine. Tumanskaya River. Photo: Gennady Smirnov Photo: Gennady Smirnov Photo: Gennady Smirnov Photo: Gennady Smirnov CHUKOTKA’S PROTECTED AREAS Legend WWF high priority conservation areas Monuments of nature 0 50 100 150 km Subadult white-tailed sea eagle. Lebediny Federal Zoological Wildlife Refuge he Lebediny Federal Zoological Wildlife Refuge, between the Main and Anadyr TRivers, protects almost 400,000 hectares of wetland habitats, as well as the animal species inhabiting them.