Where in the World Is the Polar Bear?
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[BA] COUNTRY [BA] SECTION [Ba] Greenland
[ba] Validity date from [BA] COUNTRY [ba] Greenland 26/08/2013 00081 [BA] SECTION [ba] Date of publication 13/08/2013 [ba] List in force [ba] Approval [ba] Name [ba] City [ba] Regions [ba] Activities [ba] Remark [ba] Date of request number 153 Qaqqatisiaq (Royal Greenland Seagfood A/S) Nuuk Vestgronland [ba] FV 219 Markus (Qajaq Trawl A/S) Nuuk Vestgronland [ba] FV 390 Polar Princess (Polar Seafood Greenland A/S) Qeqertarsuaq Vestgronland [ba] FV 401 Polar Qaasiut (Polar Seafood Greenland A/S) Nuuk Vestgronland [ba] FV 425 Sisimiut (Royal Greenland Seafood A/S) Nuuk Vestgronland [ba] FV 4406 Nataarnaq (Ice Trawl A/S) Nuuk Vestgronland [ba] FV 4432 Qeqertaq Fish ApS Ilulissat Vestgronland [ba] PP 4469 Akamalik (Royal Greenland Seafood A/S) Nuuk Vestgronland [ba] FV 4502 Regina C (Niisa Trawl ApS) Nuuk Vestgronland [ba] FV 4574 Uummannaq Seafood A/S Uummannaq Vestgronland [ba] PP 4615 Polar Raajat A/S Nuuk Vestgronland [ba] CS 4659 Greenland Properties A/S Maniitsoq Vestgronland [ba] PP 4660 Arctic Green Food A/S Aasiaat Vestgronland [ba] PP 4681 Sisimiut Fish ApS Sisimiut Vestgronland [ba] PP 4691 Ice Fjord Fish ApS Nuuk Vestgronland [ba] PP 1 / 5 [ba] List in force [ba] Approval [ba] Name [ba] City [ba] Regions [ba] Activities [ba] Remark [ba] Date of request number 4766 Upernavik Seafood A/S Upernavik Vestgronland [ba] PP 4768 Royal Greenland Seafood A/S Qeqertarsuaq Vestgronland [ba] PP 4804 ONC-Polar A/S Alluitsup Paa Vestgronland [ba] PP 481 Upernavik Seafood A/S Upernavik Vestgronland [ba] PP 4844 Polar Nanoq (Sigguk A/S) Nuuk Vestgronland -
Warming up to Greenland from Dog Sledding to Glacier Gazing, This Rugged Arctic Nation Is Rich in Adventures for Every Age and Taste
WARMING UP TO GREENLAND FROM DOG SLEDDING TO GLACIER GAZING, THIS RUGGED ARCTIC NATION IS RICH IN ADVENTURES FOR EVERY AGE AND TASTE BY ANDREW MYERS Mads Pihl - greenland.com 24 BOSS 4 s u mm e r 2015 hose who’ve ever caught a glimpse of the Northern T Lights, even for the briefest NORTHERN LIGHTS moment, will never forget their fiery charm. In Greenland, the Northern Lights are visible on every clear night three seasons a year—autumn, winter and spring. In summer, they would be there, too, but for the round-the-clock midnight sun outshining them. On most nights, they appear a ghostly emerald green, but they can also venture into fiery reds or even purples on the very best nights. “The Northern Lights are, without question, spectacular in Greenland,” says Sarah Woodall, an American who Mads Pihl - greenland.com works as a tourism consultant for Visit Northern Lights, Destination Arctic Circle Greenland, the national tourist board (www.greenland.com). Though Greenland likely doesn’t The Northern Lights are, of course, offers a distinctive vantage on the leap to mind as a tourist mecca, this one of Greenland’s star attractions, but country’s rugged beauty. Tour leaders, rugged land three times the size of they are just one of what are known as known as mushers, provide entrée into Texas that stretches almost to the top of “The Big Arctic Five,” which include the history of dog sledding and the the world is emerging as a surprisingly adventurous dog sledding tours, unique collaboration between man popular destination, and not just for the spectacular displays of ice and snow, and animal that is sled dog life. -
Ancient Fennoscandian Genomes Reveal Origin and Spread of Siberian Ancestry in Europe
ARTICLE DOI: 10.1038/s41467-018-07483-5 OPEN Ancient Fennoscandian genomes reveal origin and spread of Siberian ancestry in Europe Thiseas C. Lamnidis1, Kerttu Majander1,2,3, Choongwon Jeong1,4, Elina Salmela 1,3, Anna Wessman5, Vyacheslav Moiseyev6, Valery Khartanovich6, Oleg Balanovsky7,8,9, Matthias Ongyerth10, Antje Weihmann10, Antti Sajantila11, Janet Kelso 10, Svante Pääbo10, Päivi Onkamo3,12, Wolfgang Haak1, Johannes Krause 1 & Stephan Schiffels 1 1234567890():,; European population history has been shaped by migrations of people, and their subsequent admixture. Recently, ancient DNA has brought new insights into European migration events linked to the advent of agriculture, and possibly to the spread of Indo-European languages. However, little is known about the ancient population history of north-eastern Europe, in particular about populations speaking Uralic languages, such as Finns and Saami. Here we analyse ancient genomic data from 11 individuals from Finland and north-western Russia. We show that the genetic makeup of northern Europe was shaped by migrations from Siberia that began at least 3500 years ago. This Siberian ancestry was subsequently admixed into many modern populations in the region, particularly into populations speaking Uralic languages today. Additionally, we show that ancestors of modern Saami inhabited a larger territory during the Iron Age, which adds to the historical and linguistic information about the population history of Finland. 1 Department of Archaeogenetics, Max Planck Institute for the Science of Human History, 07745 Jena, Germany. 2 Institute for Archaeological Sciences, Archaeo- and Palaeogenetics, University of Tübingen, 72070 Tübingen, Germany. 3 Department of Biosciences, University of Helsinki, PL 56 (Viikinkaari 9), 00014 Helsinki, Finland. -
Vegetation and Lake Changes on the Southern Taymyr Peninsula, Northern Siberia, During the Last 300 Years Inferred from Pollen and Pediastrum Green Algae Records
Mathematisch-Naturwissenschaftliche Fakultät Bastian Niemeyer | Ulrike Herzschuh | Luidmila Pestryakova Vegetation and lake changes on the southern Taymyr peninsula, northern Siberia, during the last 300 years inferred from pollen and Pediastrum green algae records Suggested citation referring to the original publication: The Holocene 25(4) (2015) DOI https://doi.org/10.1177/0959683614565954 ISSN (print) 0959-6836 ISSN (online) 1477-0911 Postprint archived at the Institutional Repository of the Potsdam University in: Postprints der Universität Potsdam Mathematisch-Naturwissenschaftliche Reihe ; 421 ISSN 1866-8372 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-404880 HOL0010.1177/0959683614565954The HoloceneNiemeyer et al. 565954research-article2015 Research paper The Holocene 2015, Vol. 25(4) 596 –606 Vegetation and lake changes on the © The Author(s) 2015 Reprints and permissions: sagepub.co.uk/journalsPermissions.nav southern Taymyr peninsula, northern DOI: 10.1177/0959683614565954 Siberia, during the last 300 years inferred hol.sagepub.com from pollen and Pediastrum green algae records Bastian Niemeyer,1 Ulrike Herzschuh1,2 and Luidmila Pestryakova3 Abstract Siberian arctic vegetation and lake water communities, known for their temperature dependence, are expected to be particularly impacted by recent climate change and high warming rates. However, decadal information on the nature and strength of recent vegetation change and its time lag to climate signals are rare. In this study, we present a 210Pb/137Cs dated pollen and Pediastrum species record from a unnamed lake in the south of the Taymyr peninsula covering the period from AD 1706 to 2011. Thirty-nine palynomorphs and 10 morphotypes of Pediastrum species were studied to assess changes in vegetation and lake conditions as probable responses to climate change. -
A Polar System of Intercontinental Bird Migration Thomas Alerstam1,*, Johan Ba¨Ckman1, Gudmundur A
Proc. R. Soc. B (2007) 274, 2523–2530 doi:10.1098/rspb.2007.0633 Published online 7 August 2007 A polar system of intercontinental bird migration Thomas Alerstam1,*, Johan Ba¨ckman1, Gudmundur A. Gudmundsson2, Anders Hedenstro¨m3, Sara S. Henningsson1,Ha˚kan Karlsson1, Mikael Rose´n1 and Roine Strandberg1 1Department of Animal Ecology, and 3Department of Theoretical Ecology, Lund University, Ecology Building, 223 62 Lund, Sweden 2Icelandic Institute of Natural History, Hlemmur 3, PO Box 5320, 125 Reykjavik, Iceland Studies of bird migration in the Beringia region of Alaska and eastern Siberia are of special interest for revealing the importance of bird migration between Eurasia and North America, for evaluating orientation principles used by the birds at polar latitudes and for understanding the evolutionary implications of intercontinental migratory connectivity among birds as well as their parasites. We used tracking radar placed onboard the ice-breaker Oden to register bird migratory flights from 30 July to 19 August 2005 and we encountered extensive bird migration in the whole Beringia range from latitude 648 N in Bering Strait up to latitude 758 N far north of Wrangel Island, with eastward flights making up 79% of all track directions. The results from Beringia were used in combination with radar studies from the Arctic Ocean north of Siberia and in the Beaufort Sea to make a reconstruction of a major Siberian–American bird migration system in a wide Arctic sector between longitudes 1108 Eand1308 W, spanning one-third of the entire circumpolar circle. This system was estimated to involve more than 2 million birds, mainly shorebirds, terns and skuas, flying across the Arctic Ocean at mean altitudes exceeding 1 km (maximum altitudes 3–5 km). -
Biomonitoring in Greenland: Human Biomarkers of Exposure and Effects – a Short Review
Circumpolar Special Issue: Human Health at the Ends of the Earth REVIEW ARTICLE Biomonitoring in Greenland: human biomarkers of exposure and effects – a short review EC Bonefeld-Jorgensen Centre for Arctic Environmental Medicine, School of Public Health, University of Aarhus, Denmark Submitted: 31 October 2009; Revised: 14 January 2010; Published: 18 June 2010 Bonefeld-Jorgensen EC Biomonitoring in Greenland: human biomarkers of exposure and effects – a short review Rural and Remote Health 10: 1362. (Online), 2010 Available from: http://www.rrh.org.au A B S T R A C T Context: Since 1997 the Arctic Monitoring and Assessment Programme (AMAP) has produced integrated assessment reports on the status of and trends in environmental persistent organic pollutants (POPs) in the Arctic ecosystem. Three reports on biomonitoring POPs and their health risks for Arctic populations were published in 1998, 2002, and 2009. Issue: The present review summarizes data from Greenland on human monitoring of biomarkers of POP exposure and bioaccumulation and the determination of biomarkers for POP effects. The review focuses on hormone disruptive potentials and some genetic sensitivity biomarkers. The overview covers Greenlandic studies from 2000 to 2006. Lessons learned: The Greenland biomonitoring studies showed general geographical and gender differences of bioaccumulated serum POP levels, which were primarily related to diet and lifestyle. A high intake of traditional Greenlandic diet (eg seal, whale, polar bear, and seabirds) together with smoking caused higher blood concentrations of POPs. The highest POP values were found on the east coast of Greenland. The receptor effect studies showed a general inverse relationship between high serum POP concentration and estrogen receptor (ER) and Ah-receptor (AhR) transactivity; in addition for men in the two West Greenlandic districts, Nuuk and Sisimiut, a trend towards increased induced AR activity was found. -
Mountain-Derived Versus Shelf-Based Glaciations on the Western Taymyr Peninsula, Siberia Christian Hjort1 & Svend Funder2
Mountain-derived versus shelf-based glaciations on the western Taymyr Peninsula, Siberia Christian Hjort1 & Svend Funder2 1 Quaternary Sciences, Lund University, GeoCenter II, Sölvegatan 12, SE-223 62 Lund, Sweden 2 Natural History Museum, University of Copenhagen, Øster Voldgade 5-7, DK-1350 Copenhagen K, Denmark Keywords Abstract Siberian geology; glacial inception; glacial history. The early Russian researchers working in central Siberia seem to have preferred scenarios in which glaciations, in accordance with the classical gla- Correspondence ciological concept, originated in the mountains. However, during the last 30 C. Hjort, Quaternary Sciences, Lund years or so the interest in the glacial history of the region has concentrated on University, GeoCenter II, Sölvegatan 12, ice sheets spreading from the Kara Sea shelf. There, they could have originated SE-223 62 Lund, Sweden. E-mail: from ice caps formed on areas that, for eustatic reasons, became dry land [email protected] during global glacial maximum periods, or from grounded ice shelves. Such ice doi:10.1111/j.1751-8369.2008.00068.x sheets have been shown to repeatedly inundate much of the Taymyr Peninsula from the north-west. However, work on westernmost Taymyr has now also documented glaciations coming from inland. On at least two occasions, with the latest one dated to the Saale glaciation (marine isotope stage 6 [MIS 6]), warm-based, bedrock-sculpturing glaciers originating in the Byrranga Moun- tains, and in the hills west of the range, expanded westwards, and at least once did such glaciers, after moving 50–60 km or more over the present land areas, cross today’s Kara Sea coastline. -
Pan-Arctic Climate and Land Cover Trends Derived from Multi-Variate and Multi-Scale Analyses (1981–2012)
Remote Sens. 2014, 6, 2296-2316; doi:10.3390/rs6032296 OPEN ACCESS remote sensing ISSN 2072-4292 www.mdpi.com/journal/remotesensing Article Pan-Arctic Climate and Land Cover Trends Derived from Multi-Variate and Multi-Scale Analyses (1981–2012) Marcel Urban 1,*, Matthias Forkel 2, Jonas Eberle 1, Christian Hüttich 1, Christiane Schmullius 1 and Martin Herold 3 1 Department for Earth Observation, Friedrich-Schiller-University, Jena 07743, Germany; E-Mails: [email protected] (J.E.); [email protected] (C.H.); [email protected] (C.S.) 2 Department for Biochemical Integration, Max-Planck-Institute for Biogeochemistry, Jena 07745, Germany; E-Mail: [email protected] 3 Centre for Geo-Information, Wageningen University, Wageningen 6700AA, The Netherlands; E-Mail: [email protected] * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +49-3-641-948-887; Fax: +49-3-641-948-882. Received: 22 November 2013; in revised form: 19 February 2014 / Accepted: 5 March 2014 / Published: 12 March 2014 Abstract: Arctic ecosystems have been afflicted by vast changes in recent decades. Changes in temperature, as well as precipitation, are having an impact on snow cover, vegetation productivity and coverage, vegetation seasonality, surface albedo, and permafrost dynamics. The coupled climate-vegetation change in the arctic is thought to be a positive feedback in the Earth system, which can potentially further accelerate global warming. This study focuses on the co-occurrence of temperature, precipitation, snow cover, and vegetation greenness trends between 1981 and 2012 in the pan-arctic region based on coarse resolution climate and remote sensing data, as well as ground stations. -
The Periglacial Climate and Environment in Northern Eurasia
ARTICLE IN PRESS Quaternary Science Reviews 23 (2004) 1333–1357 The periglacial climate andenvironment in northern Eurasia during the Last Glaciation Hans W. Hubbertena,*, Andrei Andreeva, Valery I. Astakhovb, Igor Demidovc, Julian A. Dowdeswelld, Mona Henriksene, Christian Hjortf, Michael Houmark-Nielseng, Martin Jakobssonh, Svetlana Kuzminai, Eiliv Larsenj, Juha Pekka Lunkkak, AstridLys a(j, Jan Mangerude, Per Moller. f, Matti Saarnistol, Lutz Schirrmeistera, Andrei V. Sherm, Christine Siegerta, Martin J. Siegertn, John Inge Svendseno a Alfred Wegener Institute for Polar and Marine Research (AWI), Telegrafenberg A43, Potsdam D-14473, Germany b Geological Faculty, St. Petersburg University, Universitetskaya 7/9, St. Petersburg 199034, Russian Federation c Institute of Geology, Karelian Branch of Russian Academy of Sciences, Pushkinskaya 11, Petrozavodsk 125610, Russian Federation d Scott Polar Research Institute and Department of Geography, University of Cambridge, Cambridge CBZ IER, UK e Department of Earth Science, University of Bergen, Allegt.! 41, Bergen N-5007, Norway f Quaternary Science, Department of Geology, Lund University, Geocenter II, Solvegatan. 12, Lund Sweden g Geological Institute, University of Copenhagen, Øster Voldgade 10, Copenhagen DK-1350, Denmark h Center for Coastal and Ocean Mapping, Chase Ocean Engineering Lab, University of New Hampshire, Durham, NH 03824, USA i Paleontological Institute, RAS, Profsoyuznaya ul., 123, Moscow 117868, Russia j Geological Survey of Norway, PO Box 3006 Lade, Trondheim N-7002, Norway -
Climate Context: Evaluation of Coastal Precipitation Records
This document is the accepted manuscript version of the following article: Mernild, S. H., Hanna, E., McConnell, J. R., Sigl, M., Beckerman, A. P., Yde, J. C., … Steffen, K. (2015). Greenland precipitation trends in a long-term instrumental climate context (1890-2012): evaluation of coastal and ice core records. International Journal of Climatology, 35(2), 303-320. https://doi.org/10.1002/joc.3986 Greenland precipitation trends in a long-term instrumental climate context (1890–2012): Evaluation of coastal and ice core records SEBASTIAN H. MERNILD Climate, Ocean, and Sea Ice Modeling Group, Computational Physics and Methods, Los Alamos National Laboratory, New Mexico, USA, Glaciology and Climate Change Laboratory, Center for Scientific Studies/Centro de Estudios Cientificos (CECs), CHILE, [email protected] EDWARD HANNA Department of Geography, University of Sheffield, Sheffield, UK JOSEPH R. McCONNELL and MICHAEL SIGL Desert Research Institute, Nevada, USA ANDREW P. BECKERMAN Department of Animal and Plant Sciences, University of Sheffield, Sheffield, UK JOHN CAPPELEN Danish Meteorological Institute, Copenhagen, DENMARK JACOB C. YDE Sogn og Fjordane University College, Sogndal, NORWAY JEPPE K. MALMROS Glaciology and Climate Change Laboratory, Center for Scientific Studies/Centro de Estudios Cientificos (CECs), CHILE KONRAD STEFFEN Swiss Federal Research Institute WSL, Birmensdorf, Institute for Atmosphere and Climate, Swiss Federal Institute of Technology, Zurich, and Architecture, Civil and Environmental Engineering, Ecole Polytechnique Federal de Lausanne, Lausanne, SWITZERLAND Submitted to International Journal of Climatology, 4 December, 2013 Re-submitted 14 February, 2014 Corresponding author address: Dr. Sebastian H. Mernild Glaciology and Climate Change Laboratory Center for Scientific Studies/Centro de Estudios Cientificos (CECs) Av. -
Regional Variations in Provenance and Abundance of Ice-Rafted Clasts
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln USGS Staff -- Published Research US Geological Survey 2001 Regional variations in provenance and abundance of ice-rafted clasts in Arctic Ocean sediments: implications for the configuration of late Quaternary oceanic and atmospheric circulation in the Arctic R. L. Phillips U.S. Geological Survey, [email protected] A. Grantz Stanford University Follow this and additional works at: https://digitalcommons.unl.edu/usgsstaffpub Part of the Earth Sciences Commons Phillips, R. L. and Grantz, A., "Regional variations in provenance and abundance of ice-rafted clasts in Arctic Ocean sediments: implications for the configuration of late Quaternary oceanic and atmospheric circulation in the Arctic" (2001). USGS Staff -- Published Research. 439. https://digitalcommons.unl.edu/usgsstaffpub/439 This Article is brought to you for free and open access by the US Geological Survey at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in USGS Staff -- Published Research by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Marine Geology 172 (2001) 91–115 www.elsevier.nl/locate/margeo Regional variations in provenance and abundance of ice-rafted clasts in Arctic Ocean sediments: implications for the configuration of late Quaternary oceanic and atmospheric circulation in the Arctic R.L. Phillipsa,*, A. Grantzb aUS Geological Survey, 345 Middlefield Road, MS 999, Menlo Park, CA 94025, USA bDepartment of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305-2115, USA Received 2 June 1999; accepted 25 July 2000 Abstract The composition and distribution of ice-rafted glacial erratics in late Quaternary sediments define the major current systems of the Arctic Ocean and identify two distinct continental sources for the erratics. -
Russia.Pdf 71 Chicago Tribune
Table of Contents PROFILE 5 INTRODUCTION 5 FACTS AND FIGURES 6 GEOGRAPHY 15 INTRODUCTION 15 GEOGRAPHIC REGIONS AND TOPOGRAPHIC FEATURES 15 KOLA PENINSULA 15 RUSSIAN PLAIN 15 CAUCASUS MOUNTAINS 16 URAL MOUNTAINS 16 WEST SIBERIAN PLAIN 17 CENTRAL SIBERIAN PLATEAU 17 TAYMYR PENINSULA 17 MOUNTAINS OF THE SOUTH AND EAST 18 CLIMATE 19 RIVERS AND LAKES 20 CASPIAN SEA/BLACK SEA 20 ARCTIC OCEAN 21 PACIFIC OCEAN 22 MAJOR CITIES 23 MOSCOW 24 SAINT PETERSBURG 25 NOVOSIBIRSK 26 NIZHNIY NOVGOROD 27 YEKATERINBURG 28 ENVIRONMENTAL CONCERNS 29 WATER POLLUTION 29 NUCLEAR ENVIRONMENTAL THREATS 29 NATURAL HAZARDS 30 HISTORY 32 EARLY HISTORY 32 ORIGIN OF THE RUSSIAN STATE 32 KIEVAN RUS 33 THE MONGOL INVASION 34 THE GOLDEN HORDE 34 THE RISE OF MUSCOVY (MOSCOW) 35 IVAN IV (THE TERRIBLE) 36 BORIS GODUNOV AND THE TIME OF TROUBLES 37 THE ROMANOVS 38 PETER I (THE GREAT) 38 THE ERA OF PALACE REVOLUTIONS 39 2 CATHERINE II 40 THE EARLY 19TH CENTURY 41 REFORM EFFORTS 41 ALEXANDER III 42 REVOLUTIONS AND CIVIL WAR 43 PROLOGUE TO REVOLUTION 43 WORLD WAR I AND THE FEBRUARY REVOLUTION 44 THE OCTOBER REVOLUTION 45 THE SOVIET ERA 46 THE ASCENT OF STALIN 46 STALIN’S PURGES 47 WORLD WAR II 47 POST WORLD WAR II 48 KHRUSHCHEV AND THE POST-STALIN THAW 49 BREZHNEV, ANDROPOV, AND CHERNENKO 50 PERESTROIKA AND GLASNOST 50 THE LAST YEARS OF THE SOVIET UNION 51 END GAME 52 POST-SOVIET RUSSIA 53 ECONOMIC TROUBLES 53 CHECHNYA 53 PUTIN AND MEDVEDEV 54 ECONOMY 56 INTRODUCTION 56 INDUSTRY AND MANUFACTURING 56 AGRICULTURE 57 BANKING AND CURRENCY 58 TRADE 59 INVESTMENT 61 ENERGY AND MINERAL