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Atoll Research Bulletin
0-v Nos. 12, 13, 14 December 15, 1952 ATOLL RESEARCH BULLETIN 12 Preliminary Report on Geology and Marine Environments of Onotoa Atoll, Gilbert Islands by Preston E. Cloud, Jr. 13. Preliminary Report on Marine Biology Study of Onotoa Atoll, Gilbert Islands by A. H. Banner and J. E. Randall ^ 14. Description of Kayangel Atoll, Palau Islands by J. L. Gressitt m^^m Issued by THE PACIFIC SCIENCE BOARD National Academy of Sciences—^National Research Council Washington, D. C, U.S.A. ATOLL RESGLbRCII BUILETIIJ 12. Preliminarj'" Report on Geo2.og^' and Mo.rine Environnients of Onotoa Atoll, Gilbert Islands hy Preston E. G3.oud, Jr. 13. Preljjninary Report on Marine Biology Study of Onotoa Atoll, Gilbert Islands by A. H. Banner and J. E. Randall 14. Description of Kayangel Atoll, Palau Islands by J. L. Gressitt Issued by THE PACIFIC SCIENCE BOARD National Academy of vSciences—National Research Council Washington, D.C. December 15, 1952 . ATOLL RESEARCH BULLETIN No. U Description of. Keyangel Atoll, Palau Islands by J. L. Gressitt Issued by THE PACIFIC SGIEi^CE BOARD National Academy of Sciences—National Research Council Washington , D . C December 15, 1952 DESCRIPTION OF KAYANGEL ATOLL, PALAU ISLANDS By J. L. Gressitt Pacific Science Board , Kayangel Atoll is the northernmost land area of the Palau Archipelago in the western Caroline Islands, except for Ngaruangl, a sand bank on an incipient atoll to its north. There are no other atolls v/ithin 150 miles. Kaj'-angel is separated from Babelthuap, the largest island of the Palatis and a volcanic is- land, by about tv/enty miles of water. -
This Keyword List Contains Indian Ocean Place Names of Coral Reefs, Islands, Bays and Other Geographic Features in a Hierarchical Structure
CoRIS Place Keyword Thesaurus by Ocean - 8/9/2016 Indian Ocean This keyword list contains Indian Ocean place names of coral reefs, islands, bays and other geographic features in a hierarchical structure. For example, the first name on the list - Bird Islet - is part of the Addu Atoll, which is in the Indian Ocean. The leading label - OCEAN BASIN - indicates this list is organized according to ocean, sea, and geographic names rather than country place names. The list is sorted alphabetically. The same names are available from “Place Keywords by Country/Territory - Indian Ocean” but sorted by country and territory name. Each place name is followed by a unique identifier enclosed in parentheses. The identifier is made up of the latitude and longitude in whole degrees of the place location, followed by a four digit number. The number is used to uniquely identify multiple places that are located at the same latitude and longitude. For example, the first place name “Bird Islet” has a unique identifier of “00S073E0013”. From that we see that Bird Islet is located at 00 degrees south (S) and 073 degrees east (E). It is place number 0013 at that latitude and longitude. (Note: some long lines wrapped, placing the unique identifier on the following line.) This is a reformatted version of a list that was obtained from ReefBase. OCEAN BASIN > Indian Ocean OCEAN BASIN > Indian Ocean > Addu Atoll > Bird Islet (00S073E0013) OCEAN BASIN > Indian Ocean > Addu Atoll > Bushy Islet (00S073E0014) OCEAN BASIN > Indian Ocean > Addu Atoll > Fedu Island (00S073E0008) -
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. -
Third United Nations Conference on the Law of the Sea, 1973-82
Third United Nations Conference on the Law of the Sea 1973-1982 Concluded at Montego Bay, Jamaica on 10 December 1982 Document:- A/CONF.62/C.2/L.62/Rev.1 Algeria, Dahomey, Guinea, Ivory Coast, Liberia, Madagascar, Mali, Mauritania, Morocco, Sierra Leone, Sudan, Tunisia, Upper Volta and Zambia: draft articles on the regime of islands Extract from the Official Records of the Third United Nations Conference on the Law of the Sea, Volume III (Documents of the Conference, First and Second Sessions) \ Copyright © United Nations 2009 232 Third United Nations Conference on the Law of the Sea DOCUMENT A/CONF.62/C.2/L.62/Rev. 1 Algeria, Dahomey, Guinea, Ivory Coast, Liberia, Madagascar, Mali, Mauritania, Morocco, Sierra Leone, Sudan, Tunisia, Upper Volta and Zambia: draft articles on the regime of islands [Original: French] [27 August 1974] Article I Article 2 1. An island is a vast naturally formed area of land, sur- \: The baselines applicable to adjacent islands, islets, rocks rounded by water, which is above water at high tide. and low-tide elevations, in accordance with article 1, are con- 2. An islet is a smaller naturally formed area of land, sur- sidered as the baselines applicable to the State to which they rounded by water, which is above water at high tide. belong and consequently are used in the measurement of the marine spaces of that State. 3. A rock is a naturally formed rocky elevation of ground, surrounded by water, which is above water at high tide. 2. The marine spaces of islands considered non-adjacent, in accordance with paragraphs 1 and 6, shall be delimited on the 4. -
Kinmen Reopens Jiangong Islet to Public
Kinmen reopens Jiangong Islet to public Taipei, Feb. 26 (CNA) Large numbers of tourists have visited Jiangong Islet in Kinmen County since it was recently re-opened to the public, and its rich ecosystem amazes visitors as they walk the stone path in the islet's intertidal zone. Chen Mei-ling (陳美齡), head of the tourism department of the offshore county, said Chinese-English bilingual tourist information is now available to visitors, while new wooden platforms, viewing decks and seashore trails have been built on the islet to provide more comprehensive services to visitors after it was reopened to the public in late January following reconstruction from Dec. 20 last year. The islet, located at the mouth of the Wu River in Jincheng Township and originally named Chu Islet, is 500 meters away from the Kinmen Island and covers 500 square meters. In 1949, it was taken by the Republic of China armed forces, which built stronghold W038 on it in the face of Chinese attacks from the other side of the Taiwan Strait, at a time when the two sides were still at war after the ROC government retreated to Taiwan. It was given the name of Jiangong Islet in 1960 and remained under the control of the ROC military until 1997, when the troops were all withdrawn as part of a military streamlining program. Since then, the islet gradually became dilapidated through lack of care until 2002, when the county government took it over and started repairs in the area with the aim of turning it into a tourist attraction. -
CRYOSTRATIGRAPHY of the FIRST TERRACE in BELY ISLAND, KARA SEA: PERMAFROST and CLIMATE HISTORY (Part 3) E.A
Kriosfera Zemli, 2014, vol. XVIII, No. 3, pp. 32–43 http://www.izdatgeo.ru CRYOSTRATIGRAPHY OF THE FIRST TERRACE IN BELY ISLAND, KARA SEA: PERMAFROST AND CLIMATE HISTORY (Part 3) E.A. Slagoda1,2, A.N. Kurchatova1,2, O.L. Opokina1,2, I.V. Tomberg3, T.V. Khodzher3, A.D. Firsova3, E.V. Rodionova3, K.A. Popov1, E.L. Nikulina1 1 Earth Cryosphere Institute, Siberian Branch of the Russian Academy of Sciences, P/O box 1230 Tyumen, 625000, Russia; [email protected] 2Tyumen State Oil and Gas University, 56 Volodarskogo str., Tyumen, 625000, Russia 3Limnological Institute, Siberian Branch of the Russian Academy of Sciences, 3 Ulan-Batorskaya str., Irkutsk, 664033, Russia The distribution of lithological and permafrost facies deposited on the first terrace of Bely Island in the Kara Sea record alternated freezing and thawing cycles. The cryostratigraphy of the terrace, with constraints from data on the taxonomic diversity and habitats of microphytes found in the sediments, allows detailed reconstructions of the permafrost and deposition history associated with Late Pleistocene-Holocene climate and sea level changes. Cryostratigraphy, lithology, сryofacies, microphyte, thermokarst, taberal deposits, sealevel, Kara Sea INTRODUCTION The deposition history of frozen coastal and shelf In the West Arctic, however, the late Quaternary facies and formation of thermokarst in the context of climate and sealevel correlations remain more contro- latest Cenozoic sealevel changes in the Arctic Kara versial (Fig. 1) being interfered with a warming effect Sea area has been much less studied than in the East from the Atlantic water penetrated into the Barents- Arctic shelf. Freezing of shelf sediments in most of the Kara region [Polyakova, 1997]. -
Exceptional Retreat of Novaya Zemlya's Marine
The Cryosphere, 11, 2149–2174, 2017 https://doi.org/10.5194/tc-11-2149-2017 © Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License. Exceptional retreat of Novaya Zemlya’s marine-terminating outlet glaciers between 2000 and 2013 J. Rachel Carr1, Heather Bell2, Rebecca Killick3, and Tom Holt4 1School of Geography, Politics and Sociology, Newcastle University, Newcastle-upon-Tyne, NE1 7RU, UK 2Department of Geography, Durham University, Durham, DH13TQ, UK 3Department of Mathematics & Statistics, Lancaster University, Lancaster, LA1 4YF, UK 4Centre for Glaciology, Department of Geography and Earth Sciences, Aberystwyth University, Aberystwyth, SY23 4RQ, UK Correspondence to: J. Rachel Carr ([email protected]) Received: 7 March 2017 – Discussion started: 15 May 2017 Revised: 20 July 2017 – Accepted: 24 July 2017 – Published: 8 September 2017 Abstract. Novaya Zemlya (NVZ) has experienced rapid ice al., 2013). This ice loss is predicted to continue during loss and accelerated marine-terminating glacier retreat dur- the 21st century (Meier et al., 2007; Radic´ et al., 2014), ing the past 2 decades. However, it is unknown whether and changes are expected to be particularly marked in the this retreat is exceptional longer term and/or whether it has Arctic, where warming of up to 8 ◦C is forecast (IPCC, persisted since 2010. Investigating this is vital, as dynamic 2013). Outside of the Greenland Ice Sheet, the Russian high thinning may contribute substantially to ice loss from NVZ, Arctic (RHA) accounts for approximately 20 % of Arctic but is not currently included in sea level rise predictions. glacier ice (Dowdeswell and Williams, 1997; Radic´ et al., Here, we use remotely sensed data to assess controls on NVZ 2014) and is, therefore, a major ice reservoir. -
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. -
BMJ Open Is Committed to Open Peer Review. As Part of This Commitment We Make the Peer Review History of Every Article We Publish Publicly Available
BMJ Open: first published as 10.1136/bmjopen-2020-042973 on 5 October 2020. Downloaded from BMJ Open is committed to open peer review. As part of this commitment we make the peer review history of every article we publish publicly available. When an article is published we post the peer reviewers’ comments and the authors’ responses online. We also post the versions of the paper that were used during peer review. These are the versions that the peer review comments apply to. The versions of the paper that follow are the versions that were submitted during the peer review process. They are not the versions of record or the final published versions. They should not be cited or distributed as the published version of this manuscript. BMJ Open is an open access journal and the full, final, typeset and author-corrected version of record of the manuscript is available on our site with no access controls, subscription charges or pay-per-view fees (http://bmjopen.bmj.com). If you have any questions on BMJ Open’s open peer review process please email [email protected] http://bmjopen.bmj.com/ on October 1, 2021 by guest. Protected copyright. BMJ Open BMJ Open: first published as 10.1136/bmjopen-2020-042973 on 5 October 2020. Downloaded from Patient experience studies in the circumpolar region: a scoping review Journal: BMJ Open ManuscriptFor ID peerbmjopen-2020-042973 review only Article Type: Original research Date Submitted by the 21-Jul-2020 Author: Complete List of Authors: Ingemann, Christine; University of Southern Denmark Faculty of Health