Mapping Seabird Nesting Habitats in Franz Josef Land, Russian High Arctic, Using Digital Landsat Thematic Mapper Imagery
Total Page:16
File Type:pdf, Size:1020Kb

Load more
Recommended publications
-
Meddelelser120.Pdf (2.493Mb)
MEDDELELSER NR. 120 IAN GJERTZ & BERIT MØRKVED Environmental Studies from Franz Josef Land, with Emphasis on Tikhaia Bay, Hooker Island '-,.J��!c �"'oo..--------' MikhalSkakuj NORSK POLARINSTITUTT OSLO 1992 ISBN 82-7666-043-6 lan Gjertz and Berit Mørkved Printed J uly 1992 Norsk Polarinstitutt Cover picture: Postboks 158 Iceberg of Franz Josef Land N-1330 Oslo Lufthavn (Ian Gjertz) Norway INTRODUCTION The Russian high Arctic archipelago Franz Josef Land has long been closed to foreign scientists. The political changes which occurred in the former Soviet Union in the last part of the 1980s resulted in the opening of this area to foreigners. Director Gennady Matishov of Murmansk Marine Biological Institute deserves much of the credit for this. In 1990 an international cooperation was established between the Murmansk Marine Biological Institute (MMBI); the Arctic Ecology Group of the Institute of Oceanology, Gdansk; and the Norwegian Polar Research Institute, Oslo. The purpose of this cooperation is to develope scientific cooperation in the Arctic thorugh joint expeditions, the establishment of a high Arctic scientific station, and the exchange of scientific information. So far the results of this cooperation are two scientific cruises with the RV "Pomor", a vessel belonging to the MMBI. The cruises have been named Sov Nor-Poll and Sov-Nor-Po12. A third cruise is planned for August-September 1992. In addition the MMBI has undertaken to establish a scientific station at Tikhaia Bay on Hooker Island. This is the site of a former Soviet meteorological base from 1929-1958, and some of the buildings are now being restored by MMBI. -
Expedition Notes – Aurora Expeditions
March 13, 2018 Franz Josef Land Explorer (FJL001G) - Expedition Notes – Aurora Expeditions EXPEDITION NOTES Pre-Departure Information (FJL001G) Franz Josef Land Explorer (FJL001G) Tour Code: FJL001G Start: Longyearbyen, Svalbard Dates: 12 July to 26 July 2020 Finish: Longyearbyen, Svalbard Duration: Duration Ship: Greg Mortimer Welcome Aboard! These notes will give you a brief idea of what you may experience on this voyage. Our emphasis is on wildlife encounters, personal contact with the environment and visiting sites of historical interest. However, we stress that this is an expedition-style cruise. Our actual program will vary to take best advantage of local conditions, spontaneous opportunities and wildlife. No two voyages are the same; there is always an element of the unexpected. Franz Josef Land is an archipelago located in the Arctic Ocean, Barents Sea and Kara Sea. It is 1300 kilometres from Murmansk and in 900 kilometres from the North Pole. Franz Josef Land consists of 191 islands, which cover an area of 16,134 square kilometres, stretching 375 kilometres from east to west and 234 kilometres from north to south. It is a sanctuary of Arctic wildlife: walrus colonies, polar bears, arctic foxes, marine mammals, bird cliffs, and historical remains. The islands became part of the Russian Arctic National Park in 2012, with a policy to control tourist numbers in order to conserve the pristine environment. *Please note that this itinerary is indicative only as policies in Russia can change with very little notice. We will be able to provide you with firmer details of the final itinerary 12 months prior to departure. -
Studying Changes of Ice Coasts in the European Arctic
Geo-Mar Lett (2005) 25: 153–166 DOI 10.1007/s00367-004-0197-7 ORIGINAL Aleksey I. Sharov Studying changes of ice coasts in the European Arctic Received: 22 September 2003 / Accepted: 2 August 2004 / Published online: 18 December 2004 Ó Springer-Verlag 2004 Abstract The present extent of European ice coasts, their recently been receiving closer scientific attention since spatial changes in the past 50 years and the velocities of their dynamic environment and interesting natural scen- ice flow in marginal parts of tidewater glaciers were ery is proving highly sensitive to climatic changes determined and mapped at a regional scale using space- (Koryakin 1988; Hanson and Hooke 2000). Seaward ice borne image data, both optical and radar. The methods cliffs rising 2–50 m and sometimes even 100 m above sea of satellite photogrammetry and radar interferometry level stand at the forefront of glaciomarine interactions provided efficient solutions to the integral estimation of and represent a unique object for comprehensive envi- ice-coast dynamics in the Franz Josef Land, Novaya ronmental research at the ‘‘cutting edge’’ of several sci- Zemlya and Svalbard archipelagos. Studies revealed entific disciplines such as oceanography, glaciology and significant degradation of the ice coasts (À7.7% by coastal geomorphology. Paleogeographers consider the length) compared to the situation represented in the present glaciomarine settings along ice cliffs as being available maps. The results obtained in the laboratory analogous to those in the Ice Age and find them useful for were verified during several field campaigns. retrospective reconstructions (Korsun and Hald 1998). Glacier ice is destroyed relatively fast, even in cold water, and ice shores are thus among the most varied elements of the arctic coastline. -
A Revision of the Classification of the Plesiosauria with a Synopsis of the Stratigraphical and Geographical Distribution Of
LUNDS UNIVERSITETS ARSSKRIFT. N. F. Avd. 2. Bd 59. Nr l. KUNGL. FYSIOGRAFISKA SÅLLSKAPETS HANDLINGAR, N. F. Bd 74. Nr 1. A REVISION OF THE CLASSIFICATION OF THE PLESIOSAURIA WITH A SYNOPSIS OF THE STRATIGRAPHICAL AND GEOGRAPHICAL DISTRIBUTION OF THE GROUP BY PER OVE PERSSON LUND C. W. K. GLEER UP Read before the Royal Physiographic Society, February 13, 1963. LUND HÅKAN OHLSSONS BOKTRYCKERI l 9 6 3 l. Introduction The sub-order Plesiosauria is one of the best known of the Mesozoic Reptile groups, but, as emphasized by KuHN (1961, p. 75) and other authors, its classification is still not satisfactory, and needs a thorough revision. The present paper is an attempt at such a revision, and includes also a tabular synopsis of the stratigraphical and geo graphical distribution of the group. Some of the species are discussed in the text (pp. 17-22). The synopsis is completed with seven maps (figs. 2-8, pp. 10-16), a selective synonym list (pp. 41-42), and a list of rejected species (pp. 42-43). Some forms which have been erroneously referred to the Plesiosauria are also briefly mentioned ("Non-Plesiosaurians", p. 43). - The numerals in braekets after the generic and specific names in the text refer to the tabular synopsis, in which the different forms are numbered in successional order. The author has exaroined all material available from Sweden, Australia and Spitzbergen (PERSSON 1954, 1959, 1960, 1962, 1962a); the major part of the material from the British Isles, France, Belgium and Luxembourg; some of the German spec imens; certain specimens from New Zealand, now in the British Museum (see LYDEK KER 1889, pp. -
Plumulitid Machaeridian Remains from the Silurian (Telychian) of Severnaya Zemlya, Arctic Russia
NORWEGIAN JOURNAL OF GEOLOGY Plumulitid mochoeridion remains from the Silurion, Arctic Russio 53 Plumulitid machaeridian remains from the Silurian (Telychian) of Severnaya Zemlya, Arctic Russia Anette E.S. Hogstrom, Olga K. Bogolepova & Alexander P. Gubanov Hogstrom, A.E.S., Bogolepova, O.K. and Gubanov, A.P.: Plumulitid machaeridian remains from the Silurian (Telychian) of Sevemaya Zemlya, Arc tic Russia. Norsk Geologisk Tidsskrift, Vol. 82, pp. 53-55. Trondheim 2002, ISSN 029-196X. The machaeridian genus Plumulites is reported for the first time from the Severnaya ZemlyaArchipelago of Arctic Russia, where it occurs in limes tone concretions within the Sredninskaya Formation. Graptolites fromthe same concretions indicate the late crispus- griestoniensisBiozones of the mid Telychian (Uandovery). Similarities to plumulitid sclerites from the Upper Ordovician of the Tairnyr Peninsula promotes further interest in machaeridian faunas fromthis region. A.E.S. Hogstromi, O.K. Bogolepova and A.P. Gubanov, Historical Geology & Palaeontology, Dept. of Earth Sciences, Uppsala University, Norbyviigen 22, SE-752 36, Uppsala, Sweden. I Temporaryaddress: Dept. of Earth Sciences, Wills Memorial Building, Queen's Road, Bristol BSB l RJ, UK. lntroduction Stratigraphy and locality The global record of Silurian machaeridians is limited, Machaeridians discussed herein originate from the but includes rare articulated specimens, and more com Lower Silurian Sredninskaya Formation (Matukhin et monly isolated sclerites that have been found in Britain al. 1999). To avoid nomenclatural questions, it should (de Koninck 1857; Woodward 1865; Withers 1926 and be noted that these rocks were previously referred to as Adrain et al. 1991), the Baltic Region (Aurivillius 1892; the Golomaynnaya Formation (Menner et al. -
Arctic Coastal Dynamics Report of an International Workshop Potsdam (Germany) 26-30 November 2001
Arctic Coastal Dynamics Report of an International Workshop Potsdam (Germany) 26-30 November 2001 Edited by Volker Rachold, Jerry and Steve Solomon Ber. Polarforsch. Meeresforsch. 413 (2002) ISSN 1618-3193 Volker Rachold, Alfred Wegener Institute. Research Unit Potsdam. Telegrafenberg A43 14473 Potsdam. Gcrmany Jerry Brown, International Permaf~-ostAssociation. P.O. Box 7. Woods Hole, MA 02543. USA Steve Solomon, Geological Survey of Canada (Atlantic). Bedford Institute of Oceanography P.O. Box 1006. l Challenger Drive. Dartmouth. NS Canacla B2Y 4142, Canada Preface Arctic Coastal Dynamics (ACD) is a joint project of the International Arctic Sciences Committee (IASC) and the International Permafrost Association. Its overall objective is to improvc our understandins; of circum-arctic coastal dynamics as a function of environmental forcing, coastal geology and cryology and morphodynamic behavior. The second IASC- sponsored international workshop was held in Potsdam, Germany, on November 26-30, 2001. Participants from Canada (2), Germany (8), Norway (3), Russia (6),Austria (2) and the United States (5) attended. The main objective of the workshop was to review the Status of ACD according to phase 1 of the Science and Implementation Plan. During the first part of the workshop Status reports of the ACD working groups and several papers dealing with different aspects of circum-arctic coastal dynamics were presented. During the second Part the Progress and the next steps of the ACD working groups were discussed and, based on these discussions, the next steps were identified in the Steering Committee Meeting. The present report summarizes the program and the results of the workshop. Financial Support from the International Arctic Sciences Committee (IASC) is highly appreciated and was essential for conducting the workshop. -
Translitterering Och Alternativa Geografiska Namnformer
TRANSLITTERERING OCH ALTERNATIVA GEOGRAFISKA NAMNFORMER Version XX, 27 juli 2015, Stefan Nordblom 1 FÖRORD För många utländska egennamn, i första hand personnamn och geografiska namn, finns det på svenska väl etablerade namnformer. Om det inte finns någon sådan kan utländska egennamn dock vålla bekymmer vid översättning till svenska. Föreliggande material är tänkt att vara till hjälp i sådana situationer och tar upp fall av translitterering1 och transkribering2 samt exonymer3 . Problemen uppstår främst på grund av att olika språk har olika system för translitterering och transkribering från ett visst språk och på grund av att orter kan ha olika namn på olika utländska språk. Eftersom vi oftast översätter från engelska och franska innehåller sammanställningen även translittereringar och exonymer på engelska och franska (samt tyska). Man kan alltså i detta material göra en sökning på sådana namnformer och komma fram till den svenska namnformen. Om man t.ex. i en engelsk text träffar på det geografiska namnet Constance kan man söka på det namnet här och då få reda på att staden (i detta fall på tyska och) på svenska kallas Konstanz. Den efterföljande sammanställningen bygger i huvudsak på följande källor: Institutet för de inhemska språken (FI): bl.a. skriften Svenska ortnamn i Finland - http://kaino.kotus.fi/svenskaortnamn/ Iate (EU-institutionernas termbank) Nationalencyklopedin Nationalencyklopedins kartor Interinstitutionella publikationshandboken - http://publications.europa.eu/code/sv/sv-000100.htm Språkbruk (Tidskrift utgiven av Svenska språkbyrån i Helsingfors) Språkrådet© (1996). Publikation med rekommendationer i term- och språkfrågor som utarbetas av rådets svenska översättningsenhet i samråd med övriga EU-institutioner. TT-språket - info.tt.se/tt-spraket/ I de fall uppgifterna i dessa källor inte överensstämmer med varandra har det i enskilda fall varit nödvändigt att väga, välja och sammanjämka namnförslagen, varvid rimlig symmetri har eftersträvats. -
On a Revised Map of Kaiser Franz Josef Land, Based on Oberlieutenant Payer's Original Survey Author(S): Ralph Copeland Source: the Geographical Journal, Vol
On a Revised Map of Kaiser Franz Josef Land, Based on Oberlieutenant Payer's Original Survey Author(s): Ralph Copeland Source: The Geographical Journal, Vol. 10, No. 2 (Aug., 1897), pp. 180-191 Published by: geographicalj Stable URL: http://www.jstor.org/stable/1774601 Accessed: 27-06-2016 04:21 UTC Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at http://about.jstor.org/terms JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Wiley, The Royal Geographical Society (with the Institute of British Geographers) are collaborating with JSTOR to digitize, preserve and extend access to The Geographical Journal This content downloaded from 128.197.26.12 on Mon, 27 Jun 2016 04:21:08 UTC All use subject to http://about.jstor.org/terms 180 ON A REVISED MAP OF KAISER FRANZ JOSEF LAND, be used; but things turned out far otherwise, the Nansen sledges taken were seldom available, and the want of Samoyede sledges added greatly to the difficulties of transport. It was found that the north and south parts of the island, except for a belt along the western shore of Wijdo bay, were chiefly covered with immense accumulations of ice, while the central part was a region of boggy valleys and mountain ridges, with occasional more or less fertile slopes. -
Glacier Fluctuations During the Past 2000 Years
Quaternary Science Reviews 149 (2016) 61e90 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Invited review Glacier fluctuations during the past 2000 years * Olga N. Solomina a, , Raymond S. Bradley b, Vincent Jomelli c, Aslaug Geirsdottir d, Darrell S. Kaufman e, Johannes Koch f, Nicholas P. McKay e, Mariano Masiokas g, Gifford Miller h, Atle Nesje i, j, Kurt Nicolussi k, Lewis A. Owen l, Aaron E. Putnam m, n, Heinz Wanner o, Gregory Wiles p, Bao Yang q a Institute of Geography RAS, Staromonetny-29, 119017 Staromonetny, Moscow, Russia b Department of Geosciences, University of Massachusetts, Amherst, MA 01003, USA c Universite Paris 1 Pantheon-Sorbonne, CNRS Laboratoire de Geographie Physique, 92195 Meudon, France d Department of Earth Sciences, University of Iceland, Askja, Sturlugata 7, 101 Reykjavík, Iceland e School of Earth Sciences and Environmental Sustainability, Northern Arizona University, Flagstaff, AZ 86011, USA f Department of Geography, Brandon University, Brandon, MB R7A 6A9, Canada g Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales (IANIGLA), CCT CONICET Mendoza, CC 330 Mendoza, Argentina h INSTAAR and Geological Sciences, University of Colorado Boulder, USA i Department of Earth Science, University of Bergen, Allegaten 41, N-5007 Bergen, Norway j Uni Research Climate AS at Bjerknes Centre for Climate Research, Bergen, Norway k Institute of Geography, University of Innsbruck, Innrain 52, 6020 Innsbruck, Austria l Department of Geology, -
NORTH POLE the Ultimate Arctic Adventure Contents
NORTH POLE The Ultimate Arctic Adventure Contents 1 Overview 2 Itinerary 4 Arrival and Departure Details 6 Your Ship 8 Included Activities 10 Adventure Option 11 Dates and Rates 12 Inclusions and Exclusions 13 Your Expedition Team 14 Extend Your Trip 15 Meals on Board 16 Possible Excursions 19 Packing Checklist Per prenotazioni ed informazioni - Ruta 40 Tour Operator - +39 011 7718046 - [email protected] Overview A magical destination for travelers everywhere, the North Pole is special not only EXPEDITION IN BRIEF because of the unique geographical spot it occupies, but also because it remains Stand at the top of the world at 90°N a domain that, for most, exists only in the imagination—fewer people have stood Experience the most powerful at the North Pole than have attempted to climb Mount Everest. Difficult to reach nuclear icebreaker in the world, and singular in its impact, the North Pole transforms the perspectives of everyone 50 Years of Victory fortunate enough to reach it. In 2021, we mark 30 years of taking passengers to this Enjoy helicopter sightseeing above the frozen Arctic Ocean northernmost point on the globe, and on this amazing voyage, we enable you to Possibly view polar bears, join the privileged few who have set foot on the North Pole. walrus and other Arctic wildlife Experience the thrill of the most powerful nuclear icebreaker on the planet Take advantage of optional crushing through thick, multi-year pack ice as it pushes toward 90° north. Enjoy a tethered flight by hot air balloon (weather permitting) riveting helicopter tour over the icy Arctic Ocean; discover the remarkable sights Cruise in a Zodiac of Franz Josef Land; observe the majestic creatures who make their home in this Visit Franz Josef Land historical breathtaking yet fragile land; and experience a dreamlike hot air balloon ride over sites, wildlife and wildflowers the surreal Arctic landscape, an activity offered by no other polar operator. -
Accelerated Glacier Mass Loss in the Russian Arctic (2010-2017) Christian Sommer1, Thorsten Seehaus1, Andrey Glazovsky2, Matthias H
https://doi.org/10.5194/tc-2020-358 Preprint. Discussion started: 28 December 2020 c Author(s) 2020. CC BY 4.0 License. Brief communication: Accelerated glacier mass loss in the Russian Arctic (2010-2017) Christian Sommer1, Thorsten Seehaus1, Andrey Glazovsky2, Matthias H. Braun1 1Institut für Geographie, Friedrich-Alexander-Universität Erlangen-Nürnberg, Erlangen, 91058, Germany 5 2Institute of Geography RAS, Moscow, 119017, Russia Correspondence to: Christian Sommer ([email protected]) Abstract. Glaciers in the Russian High Arctic have been subject to extensive warming due to global climate change, yet their contribution to sea level rise has been relatively small over the past decades. Here we show surface elevation change measure- ments and geodetic mass balances of 93% of all glacierized areas of Novaya Zemlya, Severnaya Zemlya and Franz Josef Land 10 using interferometric synthetic aperture radar measurements taken between 2010 and 2017. We calculate an overall mass loss rate of -23±5 Gt a-1, corresponding to a sea level rise contribution of 0.06±0.01 mm a-1. Compared to measurements prior to 2010, mass loss of glaciers on the Russian archipelagos has doubled in recent years. 1 Introduction The Arctic has undergone large environmental changes due to increases in temperature and humidity (Box et al., 2019) and an 15 increase in glacier mass loss has been observed in many polar regions (Morris et al., 2020). The Russian Arctic, including the archipelagos Novaya Zemlya, Severnaya Zemlya and Franz Josef Land, is one of these regions. Despite a glacierized area of ~52,000 km², in-situ observations of glacier mass change are sparse. -
The Norwegian North Polar Expedition, 1893-1896
IV. AN ACCOUNT OF THE BIRDS BY ROBERT COLLETT AND FRIDTJOF NANSEN. L-n the first three sections of this paper, the observations imparted are put together from Nansen's journals, supplemented by his verbal com- ments and explanations during the preparation of the work. The last section gives the observations made during the time that the ship was drifting with the ice in the summers of 1895 and 1896, and is compiled from written and verbal information received from Scott-Hansen, Blessing and Mogstad, and also from the journals kept by Sverdrup. first section treats the The (I) of the journey along north coast of Siberia, from Yugor Strait, July 29th, 1893, until the closing in of the ship to the north-west of the New Siberian Islands on September 25th, 1893 (78 5<y N. Lat, 132 20' E. Long.). The birds observed during this time were principally on their way south- wards. After the closing in of the ship, no birds were seen until the fol- lowing year. The second section (II) gives the observations made at the time that the 'Fram* was drifting with the ice towards the NW., during the first summer, 1894, up to the time when Nansen and Johansen started on their sledge-journey, March 14th, 1895. This last point lies in about 84 N. Lat., < 1010 55 E. Lon g. The first bird seen in the spring of 1894 (a gull, probably Pagophila eburnea), appeared on May 13th; birds were seen now and again until after the middle of August. After August 23rd, or the day when all the channels and lanes about the ship began to freeze up, no birds were seen.