Norway in the Antarctic
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MARC Code List for Countries: Part I
Code Sequence PART II: CODE SEQUENCE Discontinued codes are identified by a hyphen preceding the code aa Albania ce Sri Lanka abc Alberta cf Congo (Brazzaville) -ac Ashmore and Cartier Islands cg Congo (Democratic Republic) ae Algeria ch China (Republic : 1949- ) af Afghanistan ci Croatia ag Argentina cj Cayman Islands -ai Anguilla ck Colombia ai Armenia (Republic) cl Chile -air Armenian S.S.R. cm Cameroon aj Azerbaijan -cn Canada -ajr Azerbaijan S.S.R. cou Colorado aku Alaska -cp Canton and Enderbury Islands alu Alabama cq Comoros am Anguilla cr Costa Rica an Andorra -cs Czechoslovakia ao Angola ctu Connecticut aq Antigua and Barbuda cu Cuba aru Arkansas cv Cape Verde as American Samoa cw Cook Islands at Australia cx Central African Republic au Austria cy Cyprus aw Aruba -cz Canal Zone ay Antarctica dcu District of Columbia azu Arizona deu Delaware ba Bahrain dk Denmark bb Barbados dm Benin bcc British Columbia dq Dominica bd Burundi dr Dominican Republic be Belgium ea Eritrea bf Bahamas ec Ecuador bg Bangladesh eg Equatorial Guinea bh Belize em East Timor bi British Indian Ocean Territory enk England bl Brazil er Estonia bm Bermuda Islands -err Estonia bn Bosnia and Hercegovina es El Salvador bo Bolivia et Ethiopia bp Solomon Islands fa Faroe Islands br Burma fg French Guiana bs Botswana fi Finland bt Bhutan fj Fiji bu Bulgaria fk Falkland Islands bv Bouvet Island flu Florida bw Belarus fm Micronesia (Federated States) -bwr Byelorussian S.S.R. fp French Polynesia bx Brunei fr France cau California fs Terres australes et antarctiques cb Cambodia françaises cc China ft Djibouti cd Chad gau Georgia MARC Code List for Countries page 37 Code Sequence gb Kiribati kz Kazakhstan gd Grenada -kzr Kazakh S.S.R. -
Concentrations, Particle-Size Distributions, and Dry Deposition fluxes of Aerosol Trace Elements Over the Antarctic Peninsula in Austral Summer
Atmos. Chem. Phys., 21, 2105–2124, 2021 https://doi.org/10.5194/acp-21-2105-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Concentrations, particle-size distributions, and dry deposition fluxes of aerosol trace elements over the Antarctic Peninsula in austral summer Songyun Fan1, Yuan Gao1, Robert M. Sherrell2, Shun Yu1, and Kaixuan Bu2 1Department of Earth and Environmental Sciences, Rutgers University, Newark, NJ 07102, USA 2Department of Marine and Coastal Sciences, Rutgers University, New Brunswick, NJ 08901, USA Correspondence: Yuan Gao ([email protected]) Received: 1 July 2020 – Discussion started: 26 August 2020 Revised: 3 December 2020 – Accepted: 8 December 2020 – Published: 12 February 2021 Abstract. Size-segregated particulate air samples were col- sition processes may play a minor role in determining trace lected during the austral summer of 2016–2017 at Palmer element concentrations in surface seawater over the conti- Station on Anvers Island, western Antarctic Peninsula, to nental shelf of the western Antarctic Peninsula. characterize trace elements in aerosols. Trace elements in aerosol samples – including Al, P, Ca, Ti, V, Mn, Ni, Cu, Zn, Ce, and Pb – were determined by total digestion and a 1 Introduction sector field inductively coupled plasma mass spectrometer (SF-ICP-MS). The crustal enrichment factors (EFcrust) and Aerosols affect the climate through direct and indirect ra- k-means clustering results of particle-size distributions show diative forcing (Kaufman et al., 2002). The extent of such that these elements are derived primarily from three sources: forcing depends on both physical and chemical properties (1) regional crustal emissions, including possible resuspen- of aerosols, including particle size and chemical composi- sion of soils containing biogenic P, (2) long-range transport, tion (Pilinis et al., 1995). -
Wastewater Treatment in Antarctica
Wastewater Treatment in Antarctica Sergey Tarasenko Supervisor: Neil Gilbert GCAS 2008/2009 Table of content Acronyms ...........................................................................................................................................3 Introduction .......................................................................................................................................4 1 Basic principles of wastewater treatment for small objects .....................................................5 1.1 Domestic wastewater characteristics....................................................................................5 1.2 Characteristics of main methods of domestic wastewater treatment .............................5 1.3 Designing of treatment facilities for individual sewage disposal systems...................11 2 Wastewater treatment in Antarctica..........................................................................................13 2.1 Problems of transferring treatment technologies to Antarctica .....................................13 2.1.1 Requirements of the Protocol on Environmental Protection to the Antarctic Treaty / Wastewater quality standards ...................................................................................................13 2.1.2 Geographical situation......................................................................................................14 2.1.2.1 Climatic conditions....................................................................................................14 -
Office of Polar Programs
DEVELOPMENT AND IMPLEMENTATION OF SURFACE TRAVERSE CAPABILITIES IN ANTARCTICA COMPREHENSIVE ENVIRONMENTAL EVALUATION DRAFT (15 January 2004) FINAL (30 August 2004) National Science Foundation 4201 Wilson Boulevard Arlington, Virginia 22230 DEVELOPMENT AND IMPLEMENTATION OF SURFACE TRAVERSE CAPABILITIES IN ANTARCTICA FINAL COMPREHENSIVE ENVIRONMENTAL EVALUATION TABLE OF CONTENTS 1.0 INTRODUCTION....................................................................................................................1-1 1.1 Purpose.......................................................................................................................................1-1 1.2 Comprehensive Environmental Evaluation (CEE) Process .......................................................1-1 1.3 Document Organization .............................................................................................................1-2 2.0 BACKGROUND OF SURFACE TRAVERSES IN ANTARCTICA..................................2-1 2.1 Introduction ................................................................................................................................2-1 2.2 Re-supply Traverses...................................................................................................................2-1 2.3 Scientific Traverses and Surface-Based Surveys .......................................................................2-5 3.0 ALTERNATIVES ....................................................................................................................3-1 -
Ice Shelf Advance and Retreat Rates Along the Coast of Queen Maud Land, Antarctica K
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 106, NO. C4, PAGES 7097–7106, APRIL 15, 2001 Ice shelf advance and retreat rates along the coast of Queen Maud Land, Antarctica K. T. Kim,1 K. C. Jezek,2 and H. G. Sohn3 Byrd Polar Research Center, The Ohio State University, Columbus, Ohio Abstract. We mapped ice shelf margins along the Queen Maud Land coast, Antarctica, in a study of ice shelf margin variability over time. Our objective was to determine the behavior of ice shelves at similar latitudes but different longitudes relative to ice shelves that are dramatically retreating along the Antarctic Peninsula, possibly in response to changing global climate. We measured coastline positions from 1963 satellite reconnaissance photography and 1997 RADARSAT synthetic aperture radar image data for comparison with coastlines inferred by other researchers who used Landsat data from the mid-1970s. We show that these ice shelves lost ϳ6.8% of their total area between 1963 and 1997. Most of the areal reduction occurred between 1963 and the mid-1970s. Since then, ice margin positions have stabilized or even readvanced. We conclude that these ice shelves are in a near-equilibrium state with the coastal environment. 1. Introduction summer 0Њ isotherm [Tolstikov, 1966, p. 76; King and Turner, 1997, p. 141]. Following Mercer’s hypothesis, we might expect Ice shelves are vast slabs of glacier ice floating on the coastal these ice shelves to be relatively stable at the present time. ocean surrounding Antarctica. They are a continuation of the Following the approach of other investigators [Rott et al., ice sheet and form, in part, as glacier ice flowing from the 1996; Ferrigno et al., 1998; Skvarca et al., 1999], we compare the interior ice sheet spreads across the ocean surface and away position of ice shelf margins and grounding lines derived from from the coast. -
Final Report
Time to lay down the law National legislation to enforce the BWC The Convention on the Prohibition of the Development, is the Verification Research, Training and Information Production and Stockpiling of Bacteriological (Biological) Centre, an independent, non-profit making, non-govern- Time to lay down the law and Toxin Weapons and on eir Destruction () obliges mental organisation. Its mission is to promote effective and states parties to take any necessary national measures to efficient verification as a means of ensuring confidence in National legislation to enforce the BWC implement the treaty in their territory. States parties have the implementation of international agreements and intra- agreed that this requires the adoption of legislation, including national agreements with international involvement. penal sanctions. aims to achieve its mission through research, training, Only now, thirty years after the treaty’s adoption, are states dissemination of information, and interaction with the parties collectively considering what legislative provisions relevant political, diplomatic, technical, scientific and non- are required to effectively enforce the treaty. This report is governmental communities. intended to assist states parties in this endeavour by assessing The Centre is based at Baird House, – St. Cross Street, the current status of their national legislation to enforce the London, , United Kingdom. treaty’s core prohibitions. The report provides comparative Phone +.()... analysis of existing legislation, makes recommendations for Fax +.()... increasing the rate of adoption of legislation and proposes E-mail [email protected] ways to make existing and new legislation more effective. Web www.vertic.org It should be of use to states parties preparing to adopt or amend legislation, states and organisations providing assist- Design and production: Richard Jones, Exile: Design and ance to states parties, and to the international community Editorial Services ([email protected]). -
A NEWS BULLETIN Published Quarterly by the NEW ZEALAND ANTARCTIC SOCIETY (INC)
A NEWS BULLETIN published quarterly by the NEW ZEALAND ANTARCTIC SOCIETY (INC) An English-born Post Office technician, Robin Hodgson, wearing a borrowed kilt, plays his pipes to huskies on the sea ice below Scott Base. So far he has had a cool response to his music from his New Zealand colleagues, and a noisy reception f r o m a l l 2 0 h u s k i e s . , „ _ . Antarctic Division photo Registered at Post Ollice Headquarters. Wellington. New Zealand, as a magazine. II '1.7 ^ I -!^I*"JTr -.*><\\>! »7^7 mm SOUTH GEORGIA, SOUTH SANDWICH Is- . C I R C L E / SOUTH ORKNEY Is x \ /o Orcadas arg Sanae s a Noydiazarevskaya ussr FALKLAND Is /6Signyl.uK , .60"W / SOUTH AMERICA tf Borga / S A A - S O U T H « A WEDDELL SHETLAND^fU / I s / Halley Bav3 MINING MAU0 LAN0 ENOERBY J /SEA uk'/COATS Ld / LAND T> ANTARCTIC ••?l\W Dr^hnaya^^General Belgrano arg / V ^ M a w s o n \ MAC ROBERTSON LAND\ '■ aust \ /PENINSULA' *\4- (see map betowi jrV^ Sobldl ARG 90-w {■ — Siple USA j. Amundsen-Scott / queen MARY LAND {Mirny ELLSWORTH" LAND 1, 1 1 °Vostok ussr MARIE BYRD L LAND WILKES LAND ouiiiv_. , ROSS|NZJ Y/lnda^Z / SEA I#V/VICTORIA .TERRE , **•»./ LAND \ /"AOELIE-V Leningradskaya .V USSR,-'' \ --- — -"'BALLENYIj ANTARCTIC PENINSULA 1 Tenitnte Matianzo arg 2 Esptrarua arg 3 Almirarrta Brown arc 4PttrtlAHG 5 Otcipcion arg 6 Vtcecomodoro Marambio arg * ANTARCTICA 7 Arturo Prat chile 8 Bernardo O'Higgins chile 1000 Miles 9 Prasid«fTtB Frei chile s 1000 Kilometres 10 Stonington I. -
The Commonwealth Trans-Antarctic Expedition 1955-1958
THE COMMONWEALTH TRANS-ANTARCTIC EXPEDITION 1955-1958 HOW THE CROSSING OF ANTARCTICA MOVED NEW ZEALAND TO RECOGNISE ITS ANTARCTIC HERITAGE AND TAKE AN EQUAL PLACE AMONG ANTARCTIC NATIONS A thesis submitted in fulfilment of the requirements for the Degree PhD - Doctor of Philosophy (Antarctic Studies – History) University of Canterbury Gateway Antarctica Stephen Walter Hicks 2015 Statement of Authority & Originality I certify that the work in this thesis has not been previously submitted for a degree nor has it been submitted as part of requirements for a degree except as fully acknowledged within the text. I also certify that the thesis has been written by me. Any help that I have received in my research and the preparation of the thesis itself has been acknowledged. In addition, I certify that all information sources and literature used are indicated in the thesis. Elements of material covered in Chapter 4 and 5 have been published in: Electronic version: Stephen Hicks, Bryan Storey, Philippa Mein-Smith, ‘Against All Odds: the birth of the Commonwealth Trans-Antarctic Expedition, 1955-1958’, Polar Record, Volume00,(0), pp.1-12, (2011), Cambridge University Press, 2011. Print version: Stephen Hicks, Bryan Storey, Philippa Mein-Smith, ‘Against All Odds: the birth of the Commonwealth Trans-Antarctic Expedition, 1955-1958’, Polar Record, Volume 49, Issue 1, pp. 50-61, Cambridge University Press, 2013 Signature of Candidate ________________________________ Table of Contents Foreword .................................................................................................................................. -
Station Sharing in Antarctica
IP 94 Agenda Item: ATCM 7, ATCM 10, ATCM 11, ATCM 14, CEP 5, CEP 6b, CEP 9 Presented by: ASOC Original: English Station Sharing in Antarctica 1 IP 94 Station Sharing in Antarctica Information Paper Submitted by ASOC to the XXIX ATCM (CEP Agenda Items 5, 6 and 9, ATCM Agenda Items 7, 10, 11 and 14) I. Introduction and overview As of 2005 there were at least 45 permanent stations in the Antarctic being operated by 18 countries, of which 37 were used as year-round stations.i Although there are a few examples of states sharing scientific facilities (see Appendix 1), for the most part the practice of individual states building and operating their own facilities, under their own flags, persists. This seems to be rooted in the idea that in order to become a full Antarctic Treaty Consultative Party (ATCP), one has to build a station to show seriousness of scientific purpose, although formally the ATCPs have clarified that this is not the case. The scientific mission and international scientific cooperation is nominally at the heart of the ATS,ii and through SCAR the region has a long-established scientific coordination body. It therefore seems surprising that half a century after the adoption of this remarkable Antarctic regime, we still see no truly international stations. The ‘national sovereign approach’ continues to be the principal driver of new stations. Because new stations are likely to involve relatively large impacts in areas that most likely to be near pristine, ASOC submits that this approach should be changed. In considering environmental impact analyses of proposed new station construction, the Committee on Environmental Protection (CEP) presently does not have a mandate to take into account opportunities for sharing facilities (as an alternative that would reduce impacts). -
Igneous Rocks of Peter I Island Hemisphere Tectonic Reconstructions
LeMasurier, W. E., and F. A. Wade. In press. Volcanic history in Marie Byrd Land: implications with regard to southern Igneous rocks of Peter I Island hemisphere tectonic reconstructions. In: Proceedings of the International Symposium on Andean and Antarctic Vol- canology Problems, Santiago, Chile (0. Gonzalez-Ferran, edi- tor). Rome, International Association of Volcanology and Chemistry of Earths Interior. THOMAS W. BASTIEN Price, R. C., and S. R. Taylor. 1973. The geochemistry of Dune- Ernest E. Lehmann Associates din Volcano, East Otago, New Zealand: rare earth elements. Minneapolis, Minnesota 55403 Contributions to Mineralogy and Petrology, 40: 195-205. Sun, S. S., and G. N. Hanson. 1975. Origin of Ross Island basanitoids and limitations upon the heterogeneity of mantle CAMPBELL CRADDOCK sources of alkali basalts and nephelinites. Contributions to Department of Geology and Geophysics Mineralogy and Petrology, 52: 77-106. The University of Wisconsin, Madison Sun, S. S., and G. N. Hanson. 1976. Rare earth element evi- Madison, Wisconsin 53706 dence for differentiation of McMurdo volcanics, Ross Island, Antarctica. Contributions to Mineralogy and Petrology, 54: 139-155. Peter I Island lies in the southeastern Pacific Ocean at 68°50S. 90°40W. about 240 nautical miles off the Eights Coast of West Antarctica. Ris- ing from the continental rise, it is one of the few truly oceanic islands in the region. Few people have been on the island, and little is known of its geology. Thaddeus von Bellingshausen discovered and named the island in 1821, and it was not seen again until sighted by Pierre Charcot in 1910. A Nor- wegian ship dredged some rocks off the west coast in 1927, and persons from the Norvegia achieved the first landing in 1929. -
Variable Glacier Response to Atmospheric Warming, Northern Antarctic Peninsula, 1988–2009
The Cryosphere, 6, 1031–1048, 2012 www.the-cryosphere.net/6/1031/2012/ The Cryosphere doi:10.5194/tc-6-1031-2012 © Author(s) 2012. CC Attribution 3.0 License. Variable glacier response to atmospheric warming, northern Antarctic Peninsula, 1988–2009 B. J. Davies1, J. L. Carrivick2, N. F. Glasser1, M. J. Hambrey1, and J. L. Smellie3 1Centre for Glaciology, Institute for Geography and Earth Sciences, Aberystwyth University, Llandinam Building, Penglais Campus, Aberystwyth SY23 3DB, UK 2School of Geography, University of Leeds, Leeds LS2 9JT, UK 3Department of Geology, University of Leicester, Leicester LE1 7RH, UK Correspondence to: B. J. Davies ([email protected]) Received: 2 December 2011 – Published in The Cryosphere Discuss.: 21 December 2011 Revised: 11 July 2012 – Accepted: 23 August 2012 – Published: 21 September 2012 Abstract. The northern Antarctic Peninsula has recently ex- receding into the fjords and reaching a new dynamic equi- hibited ice-shelf disintegration, glacier recession and accel- librium. The rapid shrinkage of tidewater glaciers on James eration. However, the dynamic response of land-terminating, Ross Island is likely to continue because of their low eleva- ice-shelf tributary and tidewater glaciers has not yet been tions and flat profiles. In contrast, the higher and steeper tide- quantified or assessed for variability, and there are sparse water glaciers on the eastern Antarctic Peninsula will attain data for glacier classification, morphology, area, length or more stable frontal positions after low-lying ablation areas altitude. This paper firstly classifies the area, length, alti- are removed, reaching equilibrium more quickly. tude, slope, aspect, geomorphology, type and hypsometry of 194 glaciers on Trinity Peninsula, Vega Island and James Ross Island in 2009 AD. -
Application of a New Polarimetric Filter to Radarsat-2 Data of Deception Island (Antarctic Peninsula Region) for Surface Cover Characterization
APPLICATION OF A NEW POLARIMETRIC FILTER TO RADARSAT-2 DATA OF DECEPTION ISLAND (ANTARCTIC PENINSULA REGION) FOR SURFACE COVER CHARACTERIZATION a b c a S. Guillaso ,∗ T. Schmid , J. Lopez-Mart´ ´ınez , O. D’Hondt a Technische Universitat¨ Berlin, Computer Vision and Remote Sensing, Berlin, Germany - [email protected] b CIEMAT, Madrid, Spain - [email protected] c Universidad Autonoma´ de Madrid, Spain - [email protected] KEY WORDS: SAR, Antarctica, Surface characterization, Geomorphology, Soils, Polarimetry, Speckle Filtering, Image interpretation ABSTRACT: In this paper, we describe a new approach to analyse and quantify land surface covers on Deception Island, a volcanic island located in the Northern Antarctic Peninsula region by means of fully polarimetric RADARSAT-2 (C-Band) SAR image. Data have been filtered by a new polarimetric speckle filter (PolSAR-BLF) that is based on the bilateral filter. This filter is locally adapted to the spatial structure of the image by relying on pixel similarities in both the spatial and the radiometric domains. Thereafter different polarimetric features have been extracted and selected before being geocoded. These polarimetric parameters serve as a basis for a supervised classification using the Support Vector Machine (SVM) classifier. Finally, a map of landform is generated based on the result of the SVM results. 1. INTRODUCTION Ice-free land surfaces of the Northern Antarctica Peninsula region are under the influence of freeze-thaw cycling effects on differ- ent parent materials. This is mainly due to the particular climatic conditions of the so called Maritime Antarctica and because this region is one the the fastest warming areas of the southern hemi- sphere.