Glaciological Studies at Wilkes Station, Budd Coast, Antarctica
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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 -
THE POLAR RECORD Editor: L
THE POLAR RECORD Editor: L. M. Forbes. Editorial Committee: B. B. Roberts, G. de Q. Robin, Sir J. M. Wordie Vol. 9 January 1959 No. 61 CONTENTS The Scott Polar Research Institute page 297 ARTICLES : The Canadian Northern Insect Survey, 1947-57. By T. N. Freeman 299 Recent economic developments in northern Quebec and Labrador. By J. Brian Bird . 308 Iron ore in Arctic Europe. By P. A. B. Gethin .... 314 Geodetic survey of northern Canada by shoran trilateration. By Angus C. Hamilton 320 The manuscript collection of the Scott Polar Research Institute. By Ann Savours .......... 331 FIELD WORK: British expedition to Vestspitsbergen, 1956 . • . 336 French expedition to central Greenland, 1956-57 .... 336 British expedition to north-west Greenland, 1957 .... 336 Soviet Arctic expeditions, 1957 337 The Northern Sea Route in 1957 337 Swedish-Finnish-Swiss International Geophysical Year Expedition to Nordaustlandet, 1957-58; and Swedish Expedition to Nordaust- landet, 1958-59: Season 1957-58. ...... 338 Swedish Glaciological Expedition to Nordaustlandet, 1958 . 339 Under-ice crossing of the Arctic basin: U.S.S. Nautilus and U.S.S. Skate, 1958 340 . Arctic Institute Greenland Expedition, 1958 341 British naval hydrographic surveys in the Falkland Islands Depen- dencies, 1956-57 and 1957-58 '. 341 The Australian automatic weather station on Lewis Islet, Wilkes Land 342 Anglo-American physiological team in Ross Dependency, 1957-58 . 343 NOTES : Extension of International Geophysical Year activities into 1959 . 345 Norwegian-Soviet sealing agreement, 1958 ..... 845 Tenth meeting of the International Whaling Commission, 1958 . 349 New Soviet ice-strengthened ships 350 New geographical institute in Siberia 350 ig Pit 296 CONTENTS NOTES (cont.) Soviet organizations concerned with the Antarctic . -
Dissertação O Processo Político Das Políticas Públicas Para As
O Processo Político de Construção das Políticas Públicas para as Alterações Climáticas José Carlos Martinho da Silva Dissertação de Mestrado em Sociologia - Políticas Públicas e NomeDesigualdades Completo do Sociais Autor Maio de 2019 Resumo As alterações climáticas de origem antropogénica constituem um problema ambiental sobre o qual se desenvolveram desde a década de 90 políticas públicas e tratados internacionais de grande relevância. O peso desta problemática nas agendas políticas e mediáticas tem sido crescente em diversas nações, inclusive em Portugal e na União Europeia (UE). Com efeito, a UE constitui-se hoje como um dos principais agentes mobilizados e mobilizadores de políticas sobre esta problemática, com políticas públicas robustas implementadas no contexto do protocolo de Quioto e de outras decisões tomadas na Convenção Quadro das Nações Unidas para as Alterações Climáticas. A ação internacional mais recente e ambiciosa promovida no âmbito da Convenção, ocorreu em 2015, o Acordo de Paris, mas foi recebida por uma renovada e estruturada oposição, nomeadamente a dos Estados Unidos da América (EUA), que com a sua saída do Acordo, despoletou desenvolvimentos imprevisíveis que representam atualmente um foco de preocupação e controvérsia, intensificando as interrogações face a um problema, que politicamente se veio a consolidar num desenho de políticas públicas com fortes implicações em diferentes áreas económicas, sociais e geopolíticas das diferentes nações e agrupamentos regionais representados na Convenção. Este trabalho procura abordar o problema político como um processo, e sobre este, desenvolver uma análise sociológica, tendo como enquadramento teórico a teoria de campo de Pierre Bourdieu. O foco deste trabalho foi o de compreender o início deste processo, eventualmente lançando as bases para um estudo posterior que alcance as suas diferentes fases, até ao momento presente. -
Distribution of Marine Palynomorphs in Surface Sediments, Prydz Bay, Antarctica
DISTRIBUTION OF MARINE PALYNOMORPHS IN SURFACE SEDIMENTS, PRYDZ BAY, ANTARCTICA Claire Andrea Storkey A thesis submitted to Victoria University of Wellington in fulfilment of the requirements for the degree Masters of Science in geology School of Earth Sciences Victoria University of Wellington April 2006 ABSTRACT Prydz Bay Antarctica is an embayment situated at the ocean-ward end of the Lambert Glacier/Amery Ice Shelf complex East Antarctica. This study aims to document the palynological assemblages of 58 surface sediment samples from Prydz Bay, and to compare these assemblages with ancient palynomorph assemblages recovered from strata sampled by drilling projects in and around the bay. Since the early Oligocene, terrestrial and marine sediments from the Lambert Graben and the inner shelf areas in Prydz Bay have been the target of significant glacial erosion. Repeated ice shelf advances towards the edge of the continental shelf redistributed these sediments, reworking them into the outer shelf and Prydz Channel Fan. These areas consist mostly of reworked sediments, and grain size analysis shows that finer sediments are found in the deeper parts of the inner shelf and the deepest areas on the Prydz Channel Fan. Circulation within Prydz Bay is dominated by a clockwise rotating gyre which, together with coastal currents and ice berg ploughing modifies the sediments of the bay, resulting in the winnowing out of the finer component of the sediment. Glacial erosion and reworking of sediments has created four differing environments (Prydz Channel Fan, North Shelf, Mid Shelf and Coastal areas) in Prydz Bay which is reflected in the palynomorph distribution. Assemblages consist of Holocene palynomorphs recovered mostly from the Mid Shelf and Coastal areas and reworked palynomorphs recovered mostly from the North Shelf and Prydz Channel Fan. -
The Antarctic Sun, December 25, 2005
December 25, 2005 Scientists seek to label whale species By Steven Profaizer Sun staff Patches of pure white splashed on an inky black body. Two-meter-tall dorsal fin slicing through the water’s surface. An attraction at SeaWorld. A pack hunter with cunning intelligence and stunning power. The killer whale, or orca, is one of the most universally known animals in the world. They are also one of the most wide- spread mammals, second only to humans, and inhabit all of the world’s oceans. Yet scientists are still working to deter- mine how many species of killer whales exist. Only one species is currently rec- ognized, but many people, including researcher Robert Pitman, believe there may be two additional species among the estimated 20,000 to 80,000 killer whales that inhabit Antarctic waters. Pitman is far from the first to believe this: Soviet 5 Union whalers in the early 1980s first Deep Freeze turns 0 observed the killer whales’ differences in diet, preferred habitat and coloring. He By Emily Stone does, however, hope to be part of the team Sun staff that finally solves the mystery. Al Hisey spent one of his first nights at McMurdo Station by accident. Pitman, of the National Oceanic and It was 1955, and he was ferrying supplies by tractor from Navy ships across the Atmospheric Administration, led a team sea ice of McMurdo Sound to the spot on Ross Island where the station was being to Antarctica last year on a two-week mis- built. During one of the first trips, there was a major break in the ice between the sion that used sophisticated technology to fledgling station and the ships. -
Management Plan for Antarctic Specially Protected Area No
Measure 5 (2014) Annex Management Plan for Antarctic Specially Protected Area No. 136 CLARK PENINSULA, BUDD COAST, WILKES LAND, EAST ANTARCTICA Introduction Antarctic Specially Protected Area (ASPA) No. 136 is located on Clark Peninsula, Wilkes Land at 66°15'S, 110°36'E (see Map A). The Clark Peninsula was originally designated as Site of Special Scientific Interest (SSSI) No. 17 under Recommendation XIII-8 (1985). A revised management plan for SSSI 17 was adopted under Measure 1 (2000). The area was redesignated and renumbered as ASPA 136 under Decision 1 (2002). Revised ASPA management plans were adopted under Measure 1 (2006) and Measure 7 (2009). ASPA 136 is primarily designated to protect the Clark Peninsula’s largely undisturbed terrestrial ecosystem. This ecosystem possesses one of the most extensive Antarctic flora communities outside of the Antarctic Peninsula and significant breeding populations of Adélie penguins (Pygoscelis adeliae) and south polar skuas (Catharacta maccormicki). ASPA 136 is approximately 9.4 km2 and is located approximately 5km north-west of Casey station. Scientific research within the Area has focused on plant communities and long term population studies of Adélie penguin colonies. The protection of this flora and fauna within the Area allows for valuable comparison with similar plant communities and penguin colonies closer to Casey station which are subject to greater levels of human disturbance. 1. Description of values to be protected ASPA 136 is primarily designated to protect Clark Peninsula’s largely undisturbed terrestrial ecosystem. Clark Peninsula’s ecosystem possesses one of the most extensive Antarctic flora communities outside of the Antarctic Peninsula. -
5.0 Proefschrift J. Creuwels
University of Groningen Breeding ecology of Antarctic petrels and southern fulmars in coastal Antarctica Creuwels, Jeroen Cornelis Steven IMPORTANT NOTE: You are advised to consult the publisher's version (publisher's PDF) if you wish to cite from it. Please check the document version below. Document Version Publisher's PDF, also known as Version of record Publication date: 2010 Link to publication in University of Groningen/UMCG research database Citation for published version (APA): Creuwels, J. C. S. (2010). Breeding ecology of Antarctic petrels and southern fulmars in coastal Antarctica. s.n. Copyright Other than for strictly personal use, it is not permitted to download or to forward/distribute the text or part of it without the consent of the author(s) and/or copyright holder(s), unless the work is under an open content license (like Creative Commons). The publication may also be distributed here under the terms of Article 25fa of the Dutch Copyright Act, indicated by the “Taverne” license. More information can be found on the University of Groningen website: https://www.rug.nl/library/open-access/self-archiving-pure/taverne- amendment. Take-down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. Downloaded from the University of Groningen/UMCG research database (Pure): http://www.rug.nl/research/portal. For technical reasons the number of authors shown on this cover page is limited to 10 maximum. Download date: 02-10-2021 CHAPTER 5 MONITORING OF A SOUTHERN GIANT PETREL MACRONECTES GIGANTEUS POPULATION ON THE FRAZIER ISLANDS, WILKES LAND, ANTARCTICA. -
Studies of Seismic Sources in Antarctica Using an Extensive Deployment of Broadband Seismographs Amanda Colleen Lough Washington University in St
Washington University in St. Louis Washington University Open Scholarship All Theses and Dissertations (ETDs) Summer 9-1-2014 Studies of Seismic Sources in Antarctica Using an Extensive Deployment of Broadband Seismographs Amanda Colleen Lough Washington University in St. Louis Follow this and additional works at: https://openscholarship.wustl.edu/etd Recommended Citation Lough, Amanda Colleen, "Studies of Seismic Sources in Antarctica Using an Extensive Deployment of Broadband Seismographs" (2014). All Theses and Dissertations (ETDs). 1319. https://openscholarship.wustl.edu/etd/1319 This Dissertation is brought to you for free and open access by Washington University Open Scholarship. It has been accepted for inclusion in All Theses and Dissertations (ETDs) by an authorized administrator of Washington University Open Scholarship. For more information, please contact [email protected]. WASHINGTON UNIVERSITY IN ST. LOUIS Department of Earth and Planetary Sciences Dissertation Examination Committee: Douglas Wiens, Chair Jill Pasteris Philip Skemer Viatcheslav Solomatov Linda Warren Michael Wysession Studies of Seismic Sources in Antarctica Using an Extensive Deployment of Broadband Seismographs by Amanda Colleen Lough A dissertation presented to the Graduate School of Arts and Sciences of Washington University in partial fulfillment of the requirements for the degree of Doctor of Philosophy August 2014 St. Louis, Missouri © 2014, Amanda Colleen Lough Table of Contents List of Figures ............................................................................................................................. -
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Bouvet I 50° 40° 30° 20° 10° 0° (Norway) 10° 20° 30° 40° 50° Marion I Prince Edward I e PRINCE EDWARD ISLANDS ea Ic (South Africa) t of S exten ) aximum 973-82 M rage 1 60° ar ave (10 ye SOUTH 60° SOUTH GEORGIA (UK) SANDWICH Crozet Is ISLANDS (France) (UK) R N 60° E H O T C U Antarctic Circle E H A A K O N A G V I O EO I S A N D T H E S O U T H E R N O C E A N R a Laurie I G ( t E V S T k A Powell I J . r u 70° ORCADAS (ARGENTINA) O E A S o b N A l L F lt d Stanley N B u a Coronation I R N r A N Rawson SIGNY (UK) E A I n Y ( U C A g g A G M R n K E E A E a i S S K R A T n V a Edition 6 SOUTH ORKNEY ST M Y I ) e E y FALKLAND ISLANDS (UK) R E S 70° N L R ø ISLANDS O A R E E A v M N N S Z a l Y I A k a IS ) L L i h EN BU VO ) v n ) IA id e A IM A O S e rs I L MAITRI N S r F L a a S QUARISEN E U B n J k L S F R i - e S ( r ) U (INDIA) v Kapp Norvegia P t e m s a N R U s i t ( u R i k A Puerto Deseado Selbukta a D e R u P A r V Y t R b A BORGMASSIVET s E A l N m (J A V FIMBULHEIME E l N y Comodoro Rivadavia u S N o r t IS A H o RIISER LARSENISEN u H t Clarence I J N K Z n E w W E o R Elephant I W E G E T IN o O D m d N E S T SØR-RONDANE z n R I V nH t Y O ro a y 70° t S E R E e O u S L P sl a P N A R e RS L I B y A r H O e e G See Inset d VESTFJELLA LL C G b AV g it en o E H n NH M n s o J N e n EIA a h d E C s e NE T W E M F S e S n I R n r u T h King George I t a b i N m N O d i E H r r N a Joinville I A O B . -
(2014). Dynamic Response of Antarctic Ice Shelves to Bedrock Uncertainty. Cryosphere, 8(4), 1561-1576
Sun, S., Cornford, S. L., Liu, Y., & Moore, J. C. (2014). Dynamic response of Antarctic ice shelves to bedrock uncertainty. Cryosphere, 8(4), 1561-1576. https://doi.org/10.5194/tc-8-1561-2014 Publisher's PDF, also known as Version of record License (if available): CC BY Link to published version (if available): 10.5194/tc-8-1561-2014 Link to publication record in Explore Bristol Research PDF-document This is the final published version of the article (version of record). It first appeared online via EGU at http://www.the-cryosphere.net/8/1561/2014/. Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ The Cryosphere, 8, 1561–1576, 2014 www.the-cryosphere.net/8/1561/2014/ doi:10.5194/tc-8-1561-2014 © Author(s) 2014. CC Attribution 3.0 License. Dynamic response of Antarctic ice shelves to bedrock uncertainty S. Sun1, S. L. Cornford2, Y. Liu1, and J. C. Moore1,3,4 1College of Global Change and Earth System Science, Beijing Normal University, Beijing, China 2School of Geographical Sciences, University of Bristol, Bristol BS8 1SS, UK 3Arctic Centre, University of Lapland, PL122, 96100 Rovaniemi, Finland 4Department of Earth Sciences, Uppsala University, Villavägen 16, Uppsala, 75236, Sweden Correspondence to: J. C. Moore ([email protected]) Received: 2 January 2014 – Published in The Cryosphere Discuss.: 21 January 2014 Revised: 27 June 2014 – Accepted: 1 July 2014 – Published: 21 August 2014 Abstract. -
Waba Directory 2003
DIAMOND DX CLUB www.ddxc.net WABA DIRECTORY 2003 1 January 2003 DIAMOND DX CLUB WABA DIRECTORY 2003 ARGENTINA LU-01 Alférez de Navió José María Sobral Base (Army)1 Filchner Ice Shelf 81°04 S 40°31 W AN-016 LU-02 Almirante Brown Station (IAA)2 Coughtrey Peninsula, Paradise Harbour, 64°53 S 62°53 W AN-016 Danco Coast, Graham Land (West), Antarctic Peninsula LU-19 Byers Camp (IAA) Byers Peninsula, Livingston Island, South 62°39 S 61°00 W AN-010 Shetland Islands LU-04 Decepción Detachment (Navy)3 Primero de Mayo Bay, Port Foster, 62°59 S 60°43 W AN-010 Deception Island, South Shetland Islands LU-07 Ellsworth Station4 Filchner Ice Shelf 77°38 S 41°08 W AN-016 LU-06 Esperanza Base (Army)5 Seal Point, Hope Bay, Trinity Peninsula 63°24 S 56°59 W AN-016 (Antarctic Peninsula) LU- Francisco de Gurruchaga Refuge (Navy)6 Harmony Cove, Nelson Island, South 62°18 S 59°13 W AN-010 Shetland Islands LU-10 General Manuel Belgrano Base (Army)7 Filchner Ice Shelf 77°46 S 38°11 W AN-016 LU-08 General Manuel Belgrano II Base (Army)8 Bertrab Nunatak, Vahsel Bay, Luitpold 77°52 S 34°37 W AN-016 Coast, Coats Land LU-09 General Manuel Belgrano III Base (Army)9 Berkner Island, Filchner-Ronne Ice 77°34 S 45°59 W AN-014 Shelves LU-11 General San Martín Base (Army)10 Barry Island in Marguerite Bay, along 68°07 S 67°06 W AN-016 Fallières Coast of Graham Land (West), Antarctic Peninsula LU-21 Groussac Refuge (Navy)11 Petermann Island, off Graham Coast of 65°11 S 64°10 W AN-006 Graham Land (West); Antarctic Peninsula LU-05 Melchior Detachment (Navy)12 Isla Observatorio -
First Population Counts at Newly Discovered Adélie Penguin
Southwell & Emmerson: New Adélie Penguin breeding sites 87 FIRST POPULATION COUNTS AT NEWLY DISCOVERED ADÉLIE PENGUIN PYGOSCELIS ADELIAE BREEDING SITES ALONG THE WILHELM II, QUEEN MARY AND WILKES LAND COASTLINES, EAST ANTARCTICA COLIN SOUTHWELL & LOUISE EMMERSON Australian Antarctic Division, 203 Channel Highway, Kingston, Tasmania, Australia, 7050 ([email protected]) Received 24 October 2012, accepted 6 February 2013 Knowledge of seabird populations in east Antarctica is sparse. Flight operations near the sites were in accordance with the The Adélie Penguin Pygoscelis adeliae is one of the most visible Australian Antarctic Division’s guidelines for aerial operations and intensively studied Antarctic seabirds, but basic knowledge near wildlife breeding populations (minimum altitude 750 m, of breeding distribution and abundance along large sections of Australian Antarctic Division 2011). Oblique photographs were eastern Antarctica is uncertain (Barbraud et al. 1999, Southwell taken with a hand-held Nikon D200 digital SLR camera fitted with et al. 2009). Until recently, only eight Adélie Penguin breeding 75–300 mm zoom lens. Overlapping photographs were taken on sites were known along the Wilhelm II, Queen Mary and Wilkes both low- and high-zoom settings from several vantage points. The Land coastlines between longitude 89°E and 110°E (six sites in entire breeding site was covered in a single photograph at two sites the Haswell Islands and two sites in the Davis Islands reported in (Adams Island and Mallory Point), but several photographs were Pryor 1968 and Melick et al. 1995 respectively, Fig. 1). However, a required to cover all of the three larger sites (Merritt Island, Cape recent comprehensive survey of potential Adélie Penguin breeding Nutt and Ivanoff Head).