(Title of the Thesis)*

Total Page:16

File Type:pdf, Size:1020Kb

(Title of the Thesis)* FIRN PACK CHANGES ON WHITE GLACIER, AXEL HEIBERG ISLAND, NUNAVUT by Dana Stephenson A thesis submitted to the Department of Geography and Planning in conformity with the requirements for the degree of Master of Science Queen’s University Kingston, Ontario, Canada (August, 2020) Copyright ©Dana Stephenson, 2020 Abstract The near-surface processes and variability within the firn pack of Arctic glaciers are a significant source of uncertainty in estimating future glacier responses to climate warming. This study provides the first characterization of the firn pack of White Glacier, Axel Heiberg Island, Nunavut, and an analysis of recent firn pack changes (2013-2019). Utilizing ground penetrating radar (GPR) surveys the firn pack thickness, extent, and associated topographic controls on firn distribution were determined. Two methods of GPR analysis were tested in this study. The first followed the traditional approach of conducting visual interpretation of radargrams to identify zones of backscatter associated with firn. The second is a proposed new methodology that uses average backscatter values from each radar return as a proxy indicator of firn presence in the subsurface. The results of these two approaches showed that the firn pack on White Glacier has reduced in extent, and reductions in average backscatter values suggest that the density of the firn has increased in the near surface. Overall, the long-term firn area decreased in extent by 3.96 km2 (10% of the total glacier area) between 2013 and 2018. Rates of surface lowering were determined using dual-frequency GPS surveys. For spring 2018 to spring 2019 the rate was -0.165 ± 0.29 m a-1 in the accumulation area, likely driven by the near surface densification. The potential for average backscatter values to provide information about near surface snow water equivalence is also explored. ii Co-Authorship Chapter 3 “Firn pack characterization and recent changes on White Glacier, Axel Heiberg Island, Nunavut” was co-authored by D. Stephenson, L. Thomson, and L. Copland, and is intended to be submitted to a peer-reviewed journal. I am the primary author for the writing of the manuscripts, data analysis, and figure production. L. Thomson and L. Copland provided supervision and guidance for the project and provided valuable edits to all written components, tables, and figures. Field data was collected collaboratively with L. Thomson, C. Omelon, and M. Ecclestone in the 2018 and 2019 field season, and with the addition of L. Copland in the 2019 season. Additional field data from 2013 to 2017 was collected by the aforementioned personnel, as well as various other researchers. iii Acknowledgements First and foremost, I would like to thank my supervisors Laura Thomson and Luke Copland. Without their support and mentorship this thesis would not have been possible. Thank you for the guidance and many lessons learned in the lab and in the field. This project would also not have been possible without funding from Natural Sciences and Engineering Research Council (NSERC), The Northern Scientific Training Program (NSTP), Polar Continental Shelf Program (PCSP), ArcticNet, Canada Foundation for Innovation (CFI), and the Government of Ontario. Thank you to the 2018 and 2019 field season team Christopher Omelon, Miles Ecclestone, Luke Copland, and Laura Thomson for the great memories of science, adventure, and cooking in the high Arctic at the McGill Arctic Research Station. I would like to thank my incoming cohort for all the support and encouragement throughout the thesis process. Special thanks to my classmates in AG-340 at UNIS for the incredible learning environment and opportunities to explore Svalbard. Thank you to my lab mates Evan, Jeremiah, Braden, and Maddie for the positive encouragement and virtual coffee breaks throughout the pandemic lockdown. Finally, I would like to thank my family for supporting me throughout this process and my roommates and climbing friends for the ever-important extracurricular activities. iv Table of Contents Abstract ......................................................................................................................................................... ii Co-Authorship.............................................................................................................................................. iii Acknowledgements ...................................................................................................................................... iv List of Figures ............................................................................................................................................. vii List of Tables ............................................................................................................................................... ix List of Abbreviations .................................................................................................................................... x Chapter 1 Introduction .................................................................................................................................. 1 1.1 Research context and rationale ........................................................................................................... 1 1.2 Research objectives ............................................................................................................................. 2 1.3 Thesis format ...................................................................................................................................... 2 Chapter 2 Literature Review ......................................................................................................................... 3 2.1 Introduction ......................................................................................................................................... 3 2.2 Glacier response to climate change ..................................................................................................... 3 2.2.1 Pan-Arctic glacier response to climate change ............................................................................ 5 2.2.2 Arctic Canada glacier response to climate change ....................................................................... 6 2.2.3 White Glacier response to climate change ................................................................................... 7 2.3 Accumulation area changes ................................................................................................................ 8 2.3.1 Regional accumulation area changes ........................................................................................... 8 2.3.2 Firn pack processes and implications ......................................................................................... 10 2.4 Monitoring and modelling techniques .............................................................................................. 12 2.4.1 Ground Penetrating Radar .......................................................................................................... 12 2.4.2 GPR Parameters ......................................................................................................................... 14 2.4.3 Coring ........................................................................................................................................ 16 2.4.4 GPS Monitoring ......................................................................................................................... 18 2.4.5 Remote sensing .......................................................................................................................... 19 2.4.6 Modelling ................................................................................................................................... 21 2.5 Summary ........................................................................................................................................... 22 Chapter 3 Firn pack characterization and recent changes on White Glacier, Axel Heiberg Island, Nunavut. .................................................................................................................................................................... 29 3.1 Introduction ....................................................................................................................................... 29 3.2 Study Site .......................................................................................................................................... 31 3.3 Methods............................................................................................................................................. 32 v 3.3.1 Ground Penetrating Radar .......................................................................................................... 33 3.3.2 Firn Coring ................................................................................................................................. 36 3.3.3 Topographic Analysis ................................................................................................................ 36 3.3.4 Snow Thickness ......................................................................................................................... 38 3.3.5 Surface elevation analysis .......................................................................................................... 39 3.4 Results ..............................................................................................................................................
Recommended publications
  • Colonizers of Very Recent Glaciomarine Lagoons on Heard Island
    2016 Heard Island Expedition Project Description Definition TITLE FIRST COLONIZERS OF VERY RECENT GLACIOMARINE LAGOONS ON HEARD ISLAND Abstract Due to the extraordinarily rapid melting of the Stephenson Glacier on the eastern flank of Heard Island, a large (ca. 1 mi) lagoon was created within the last decade. The lagoon communicates with the ocean through a large vent on its southern extreme; mixing with oceanic water undoubtedly is enabling invasive colonization of the lake by marine organisms. We will investigate these first colonizers by two means: (1) Documenting and sampling the intertidal zone and shallow water biota on the lake edge; and (2) Sampling the benthic sedimentary deposits in the deeper parts of the lake using a clamshell grab equipped with an underwater camera. In addition to the biota, water samples will be taken for physical and chemical analysis. Other lagoons on Heard Island also show opening and closing of oceanic channels during the past 20 years, and these will be studied in the context of first colonizers. Principal Investigator Robert Schmieder Cordell Expeditions Co-Investigator Robert van Syoc California Academy of Sciences Co-Investigator Gordon Hendler Los Angeles Museum of Natural History Co-Investigator Rich Mooi California Academy of Sciences Co-Investigator Giuliana Furci The Fungi Foundation (Chile) Co-Investigator Rocco Mancinelli NASA Ames Laboratory Co-Investigator Richard Moe University of California Jepsen Herbarium Co-Investigators Onsite team members Cordell Expeditions Context Background Satellite images show that the Stephenson Glacier, formerly dominating the area at Spit Bay, retreated by more than a mile in the short interval 2003-2008.
    [Show full text]
  • Durham Research Online
    Durham Research Online Deposited in DRO: 23 June 2014 Version of attached le: Accepted Version Peer-review status of attached le: Peer-reviewed Citation for published item: Hodgson, D.A. and Graham, A.G.C. and Roberts, S.J. and Bentley, M.J. and O¡ Cofaigh, C. and Verleyen, E. and Vyverman, W. and Jomelli, V. and Favier, V. and Brunstein, D. and Verfaillie, D. and Colhoun, E.A. and Saunders, K.M. and Selkirk, P.M. and Mackintosh, A. and Hedding, D.W. and Nel, W. and Hall, K. and McGlone, M.S. and Van der Putten, N. and Dickens, W.A. and Smith, J.A. (2014) 'Terrestrial and submarine evidence for the extent and timing of the Last Glacial Maximum and the onset of deglaciation on the maritime-Antarctic and sub-Antarctic islands.', Quaternary science reviews., 100 . pp. 137-158. Further information on publisher's website: http://dx.doi.org/10.1016/j.quascirev.2013.12.001 Publisher's copyright statement: c 2014 The Authors. Published by Elsevier Ltd. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/3.0/). Additional information: Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders.
    [Show full text]
  • CHANGES in HEARD ISLAND GLACIERS, KING PENGUINS and Furby SEALS G
    Papers and Proceedings of the Royal Society of Tasmania, Volume 133(2), 2000 47 CHANGES IN HEARD ISLAND GLACIERS, KING PENGUINS AND FURby SEALS G. M. Budd SINCE 1947 (with two tables, three text-figures and one plate) BUDD, G.M., 2000 (30:vi): Changes in Heard Island glaciers, king penguins and fur seals since 1947. In Banks M.R. & Brown, M.]. (Eds): HEARD ISLAND Pap. Proc. R. Soc. Tasm. 133 (2): 47-60. https://doi.org/10.26749/rstpp.133.2.47 ISSN 0080-4703. School of Exercise and RS. Sport Science, The University of Sydney, PO Box 170, Lidcombe, NSW, Australia 2141. The purpose of this paper is to summarise and discuss the changes in glaciers, king penguins and fur seals reported by the nine wintering parties and 11 summer expeditions that have visited Heard Island since 1947, with emphasis upon those of the years between 1947 and 1971. These early years were notable for an initial period (1947-55) of minimal change, and a subsequent period(1963-71) of rapid change in which a complex pattern of asynchronous glacier retreat and readvance was observed and the main features of the island's recolonisation by king penguins and fur seals were established. Subsequent expeditions (1980-93) have reported continuing glacier recession, evidently in response to warmer air temperatures, and a continuing exponential increase in king penguins and fur seals. The glacier observations show that the Heard Island glaciers are sensitive indicators of climate change in the Southern Ocean, and of the interactions between climate and glacier topography. The island's recolonisation by king penguins and fur seals is attributed mainly to an improved food supply which may itself, like the glacier recession, be a response to changes in atmospheric and oceanic circulation.
    [Show full text]
  • November 1960 I Believe That the Major Exports of Antarctica Are Scientific Data
    JIET L S. Antarctic Projects OfficerI November 1960 I believe that the major exports of Antarctica are scientific data. Certainly that is true now and I think it will be true for a long time and I think these data may turn out to be of vastly, more value to all mankind than all of the mineral riches of the continent and the life of the seas that surround it. The Polar Regions in Their Relation to Human Affairs, by Laurence M. Gould (Bow- man Memorial Lectures, Series Four), The American Geographiql Society, New York, 1958 page 29.. I ITOJ TJM II IU1viBEt 3 IToveber 1960 CONTENTS 1 The First Month 1 Air Operations 2 Ship Oper&tions 3 Project MAGNET NAF McMurdo Sounds October Weather 4 4 DEEP FREEZE 62 Volunteers Solicited A DAY AT TEE SOUTH POLE STATION, by Paul A Siple 5 in Antarctica 8 International Cooperation 8 Foreign Observer Exchange Program 9 Scientific Exchange Program NavyPrograrn 9 Argentine Navy-U.S. Station Cooperation 9 10 Other Programs 10 Worlds Largest Aircraft in Antarctic Operation 11 ANTARCTICA, by Emil Schulthess The Antarctic Treaty 11 11 USNS PRIVATE FRANIC 3. FETRARCA (TAK-250) 1961 Scientific Leaders 12 NAAF Little Rockford Reopened 13 13 First Flight to Hallett Station 14 Simmer Operations Begin at South Pole First DEEP FREEZE 61 Airdrop 14 15 DEEP FREEZE 61 Cargo Antarctic Real Estate 15 Antarctic Chronology,. 1960-61 16 The 'AuuOiA vises to t):iank Di * ?a]. A, Siple for his artj.ole Wh.4b begins n page 5 Matera1 for other sections of bhis issue was drawn from radio messages and fran information provided bY the DepBr1nozrt of State the Nat0na1 Academy , of Soienoes the NatgnA1 Science Fouxidation the Office 6f NAval Re- search, and the U, 3, Navy Hydziograpbio Offioe, Tiis, issue of tie 3n oovers: i16, aótivitiès o events 11 Novóiber The of the Uxitéd States.
    [Show full text]
  • Glaciers on Heard Island
    2016 Heard Island Expedition Project Description Definition TITLE MACROSCOPIC INCLUSIONS IN RETREATING GLACIERS ON HEARD ISLAND Abstract The termini, margins, and immediate vicinity of selected glaciers on Heard Island will be examined for macroscopic inclusions. Significant items exposed due to retreat of the glacier will be documented and collected for laboratory analysis. Principal Investigator Fred Belton Cordell Expeditions Co-Investigator Robert Schmieder Cordell Expeditions Co-Investigator Gavin Marshall Tangaroa Blue Foundation Co-Investigator William Mitchell Cordell Expeditions Co-Investigator Grahame Budd University of Sydney Co-Investigator Nezamoddin Nezamoddini-Kachouie Florida Institute of Technology Co-Investigator Onsite team members Cordell Expeditions Context Background Besides the episodic volcanic activity of Big Ben, perhaps the most obvious dynamic process occurring on Heard Island is the retreat of the glaciers. The extraordinarily high rates of retreat, especially of the Stephenson Glacier (up to 100 m/y), are among the highest in the world. The following map shows historical changes between 1947 and 2009. There is, however, evidence that retreat since 2009 has continued, and even accelerated. Source: Lucieer, et al. 2009. Kiernan and McConnell (2002) provide the following: Rates of both glacier retreat and melt-lake enlargement have increased by about one order 2016 Heard Island Expedition Project GLACIERS Updated 1/12/2016 4:18 PM Page 1 of 16 of magnitude during the last two decades. Precise ice-volume loss cannot presently be calculated, but about 30% of the cross-sectional area of the terminal zone of Stephenson Glacier above sea level has vanished in the past three decades. That accelerated melting of older ice-cored moraines is contributing so significantly to melt-lake expansion rather than it being the product solely of glacier recession perhaps emphasizes the significance of temperature increases in causing environmental change on Heard Island.
    [Show full text]
  • Psychrophiles
    EA41CH05-Cavicchioli ARI 30 April 2013 11:9 Psychrophiles Khawar S. Siddiqui,1 Timothy J. Williams,1 David Wilkins,1 Sheree Yau,1 Michelle A. Allen,1 Mark V. Brown,1,2 Federico M. Lauro,1 and Ricardo Cavicchioli1 1School of Biotechnology and Biomolecular Sciences and 2Evolution and Ecology Research Center, The University of New South Wales, Sydney, New South Wales 2052, Australia; email: [email protected] Annu. Rev. Earth Planet. Sci. 2013. 41:87–115 Keywords First published online as a Review in Advance on microbial cold adaptation, cold-active enzymes, metagenomics, microbial February 14, 2013 diversity, Antarctica The Annual Review of Earth and Planetary Sciences is online at earth.annualreviews.org Abstract This article’s doi: Psychrophilic (cold-adapted) microorganisms make a major contribution 10.1146/annurev-earth-040610-133514 to Earth’s biomass and perform critical roles in global biogeochemical cy- Copyright c 2013 by Annual Reviews. cles. The vast extent and environmental diversity of Earth’s cold biosphere All rights reserved has selected for equally diverse microbial assemblages that can include ar- Access provided by University of Nevada - Reno on 05/25/15. For personal use only. Annu. Rev. Earth Planet. Sci. 2013.41:87-115. Downloaded from www.annualreviews.org chaea, bacteria, eucarya, and viruses. Underpinning the important ecological roles of psychrophiles are exquisite mechanisms of physiological adaptation. Evolution has also selected for cold-active traits at the level of molecular adaptation, and enzymes from psychrophiles are characterized by specific structural, functional, and stability properties. These characteristics of en- zymes from psychrophiles not only manifest in efficient low-temperature activity, but also result in a flexible protein structure that enables biocatalysis in nonaqueous solvents.
    [Show full text]
  • Australian Antarctic Magazine
    AusTRALIAN MAGAZINE ISSUE 21 2011 7317 AusTRALIAN ANTARCTIC ISSUE 2011 MAGAZINE 21 The Australian Antarctic Division, a division of the Department for Sustainability, Environment, Water, Population and Communities, leads Australia’s CONTENTS Antarctic program and seeks to advance Australia’s Antarctic interests in pursuit of its vision of having New Director looks forward to Antarctic future 1 ‘Antarctica valued, protected and understood’. It does CENTENARY CELEBRATIONS this by managing Australian government activity in Antarctica, providing transport and logistic support to A centenary of science 4 Australia’s Antarctic research program, maintaining four Spinning an icy yarn in Antarctica 6 permanent Australian research stations, and conducting scientific research programs both on land and in the Cape Denison Post Office established 7 Southern Ocean. ANTARCTIC SCIENCE Australia’s four Antarctic goals are: • To maintain the Antarctic Treaty System and Oceans need big animals 8 enhance Australia’s influence in it; Journal focuses on Antarctic sea ice research 12 • To protect the Antarctic environment; Model simulations investigate Totten thinning 14 • To understand the role of Antarctica in the Australian Antarctic Science Season 2011–12 16 global climate system; and • To undertake scientific work of practical, MARINE MAMMAL RESEARCH economic and national significance. Surveying dugong responses to extreme weather events 18 Australian Antarctic Magazine seeks to inform the Conserving Thailand ’s cetaceans 19 Australian and international Antarctic community about the activities of the Australian Antarctic program. Dolphins under threat 20 Opinions expressed in Australian Antarctic Magazine do Surveying cetaceans in Palau 21 not necessarily represent the position of the Australian Government. SUBANTARCTIC FORUM Australian Antarctic Magazine is produced twice a year Subantarctic islands in the spotlight 22 (June and December).
    [Show full text]
  • HEARD ISLAND Proposed Field Camp Locations for Science Expedition 2003-04
    HEARD ISLAND Proposed field camp locations for Science Expedition 2003-04 Red Island Sydney Cove Magnet Point Red Island Charles Carrol Bluff Cape The Sentinel Cartwright Team A-4 (2) LAURENS Anzac Peak Mt Dixon PENINSULA Vanhoffen Bluff Atlas Roads AZORELLA Saddle Point Cape Bidlingmaier Mt Olsen Mechanics PENINSULA Bay Atlas Sealers G il Atlas Cove Corner Corinthian Bay Downes ch ri Cove Glacier st West Bay Ealey B West Cape ea Challenger Glacier ch The Nullarbor Baudissin Glacier Mary Melbourne Glacier Nares Powell Bluff Cave Bay Glacier Glacier Streeter Bluff Kildalkey Compton Head Schmidt Glacier Lagoon F a ir c h i ld South West G s B s o e N t e s a o r r l r th e t s c Bay W t e h e G y e i s u r t i r r C b B t Compton o b B a rn n u Vahsel ic e u Glacier Round Brown e y n B B t B t Glacier u r a y h Hill t e t Lagoon t n r h r n e s t o s n o is r s s r ll e a a A ci N er Team C (3) a H i Cape l C lac G c G Gazert wn M Mt. Separation ro B S k ua B Davis e Dome ac tress h Allison But BIG Scarlet Team A-1 (4) & support (5) Hill idge g R Team B & D (8) th BEN on Tr mi L Stephenson B yp Spit ots e ot bb r S ac Point A cie Mawson Peak tep Lagoon h la hen Spit Oil Barrel Point Spit Bay G Budd Peak son it Gla Bay Sp cier G e ra n Scholes Lagoon h i t am R lephan idge a E Henderson Bluff r o e M g T d s i e S r R m e o u v h d p c t o a d l h e e B D u B s er B B a al u rr Se t ie t r r W Smith Bluff Doppler Hill ier e in ac s st l s on Paddick d G G Cape Pillar Lie lac Valley Rayner ier Team A-2 (3) Rib Winston Lagoon Oatt Rocks r ie c la G Team A-3 (3) y Capsize e Cape Arkona tl o Beach G Deacock Cape Lockyer Exile Rock Glacier Franklin Rock Fiftyone Dillon Glacier Hill Wakefield Reef Long Beach Lambeth Bluff Manning Long Lagoon Lavett Bluff Beach Cape Labuan Produced by the Australian Antarctic Data Centre, 0 1 2 4 6 8 Australian Antarctic Division, Km Department of the Environment and Heritage, July 2003 © Commonwealth of Australia Map No.
    [Show full text]
  • Glacier Retreat and Melt-Lake Expansion at Stephenson Glacier
    Polar Record 38 (207): 297-308 (2002). Printed in the United Kingdom. 297 Glacier retreat and melt-lake expansion at Stephenson Glacier, Heard Island World Heritage Area Kevin Kiernan and Anne McConnell School of Geography and Environmental Studies, University of Tasmania, Hobart, Tasmania 7005, Australia Received September 2001 ABSTRACT. Historical records, recent observations, and geomorphological evidence indicate that rates of retreat and downwasting of the tidewater Stephenson Glacier, and concurrent expansion of ice-marginal melt-lakes, has increased by an order of magnitude since 1987. Melt-lake expansion is partly the product of greatly accelerated ablation of older, ice-cored twentieth-century moraines. The timing of these changes broadly coincides with reported increases in atmospheric and sea-surface temperatures around other sub-Antarctic islands, but correlates less well with changes along the northern Antarctic Peninsula, where warming has been more rapid. These recent changes in landscape character and geomorphological processes have implications for geodiversity, biodiversity, and cultural heritage values in this World Heritage Area. Ifthe causal climatic warming is anthropogenic, it reinforces the fact that even the most remote and little­ visited nature conservation reserves may be compromised by off-site human impacts, confronting management authorities with difficult philosophical and practical issues. Contents local climate. A smaller volcanic complex, Laurens Pe­ Introduction 297 ninsula, extends westwards from Big Ben, and Elephant Physical environment 297 Spit extends -10 km downdrift from the eastern side of the Methods 298 mountain. The mean annual temperature (MAT) recorded Results 298 between 1948 and 1954 when a permanent base was Interpretation of results 304 maintained at Atlas Cove, between Laurens Peninsula and Discussion 305 Big Ben, was 1.3°C, with a seasonal variation in tempera­ Conclusions 307 ture at sea level of -4°C.
    [Show full text]
  • Women in Glaciology, an Historical Perspective
    Portland State University PDXScholar Geology Faculty Publications and Presentations Geology 1-1-2010 Women in Glaciology, an Historical Perspective Christina L. Hulbe Portland State University Weili Wang NASA Goddard Space Flight Center Simon Ommanney Scott Polar Research Institute Follow this and additional works at: https://pdxscholar.library.pdx.edu/geology_fac Part of the Geology Commons, and the Glaciology Commons Let us know how access to this document benefits ou.y Citation Details Hulbe, C.L., W. Wang, and S. Ommanney, 2011. Women in glaciology, an historical perspective, Journal of Glaciology, 56 (200). This Article is brought to you for free and open access. It has been accepted for inclusion in Geology Faculty Publications and Presentations by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. 944 Journal of Glaciology, Vol. 56, No. 200, 2010 Women in glaciology, a historical perspective Christina L. HULBE,1 Weili WANG,2 Simon OMMANNEY3 1Department of Geology, Portland State University, PO Box 751, Portland, Oregon 97207-0751, USA E-mail: [email protected] 2NASA Goddard Space Flight Center, Code 614.1, Greenbelt, Maryland 20771, USA 3Emeritus Associate, Scott Polar Research Institute ABSTRACT. Women’s history in glaciology extends as far back in time as the discipline itself, although their contributions to the scientific discourse have for all of that history been constrained by the socio- political contexts of the times. The first Journal of Glaciology paper authored by a woman appeared in 1948, within a year of the founding of the Journal, but it was not until the 1980s that women produced more than a few percent of Journal and Annals of Glaciology papers.
    [Show full text]
  • No Printed Publication, Digital Data Only
    Gazetteer of German-language Antarctic place-names, Third Edition, Version 3.1 (no printed publication, digital data only) – Complete revision of the Second Edition according to the specifications of the SCAR Composite Gazetteer of Antarctica (CGA), with contributions by Karsten Brunk, Rosbach v.d. Höhe, compiled and arranged by Jörn Sievers, Neu-Isenburg, on behalf of Ständiger Ausschuss für geographische Namen (StAGN), Frankfurt am Main, 2021-JUN-08 BKG- Alti- BKG-Nr. Place name Feature type Latitude Longitude Date approved Country Quelle tude 482 Acapulcofelsen 27, 30, 31 Cliff -70,5500000 164,0333333 200 1985-APR-19 Germany 499 Adlerwand 28, 30, 31 Bluff -73,2500000 167,1833333 800 1985-APR-19 Germany 515 Aklestadberg 28, 30, 31 Mountain -72,8166667 166,3000000 2450 1985-APR-19 Germany 5 Alexander-von-Humboldt- 25 Range -71,6666667 11,5000000 2895 1952-JUL-12 Germany Gebirge 33 Altar 25 Mountain -71,6500000 11,3833333 2200 1952-JUL-12 Germany 35 Am Überlauf 25 Pass -71,5500000 11,6166667 1700 1952-JUL-12 Germany 92 Amelangplatte 25 Mountain -74,0833333 -5,6666667 2430 1952-JUL-12 Germany 540 Ampfererberg 28, 30, 31 Mountain -72,8000000 167,3166667 3080 1985-APR-19 Germany 481 Andalusitgrat 27, 30, 31 Ridge -71,5500000 160,1666667 2100 1985-APR-19 Germany 548 Armbrustspitze 28, 30, 31 Peak -73,4166667 166,9333333 1290 1985-APR-19 Germany 678 Atka-Eiskuppel 46, 50, 51 Ice rise -70,7000000 -7,8333333 83 1990-APR-02 Germany 1 Gazetteer of German-language Antarctic place-names, Third Edition (no printed publication, digital data only) – Complete revision of the Second Edition according to the specifications of the SCAR Composite Gazetteer of Antarctica (CGA), with contributions by Karsten Brunk, Rosbach v.d.
    [Show full text]
  • Heard Island and Mcdonald Islands
    Papers and Proceedings of the Royal Society of Tasmania, Volume 141 (1), 2007 7 HEARD ISLAND AND MCDONALD ISLANDS by Ewan Mcivor (with two text-figures) Mcivor, E. 2007 (23:xi): Heard Island and McDonald Islands. Papers and Proceedings of the Royal Society a/Tasmania 141 (1 ): 7-10. https://doi.org/10.26749/rstpp.141.1.7 ISSN 0080-4703. Australian Antarctic Division, Channel Highway, Kingston, Tasmania 7054, Australia. "The sub-Antarctic Heard Island and McDonald Islands (HIMI) group is an Australian external territory located in the Indian Ocean sector of the Southern Ocean. 1he island group was inscribed on the World Heritage list in 1997 for its outstanding natural universal values, primarily due to the relative absence of human influence on the natural environment. The Territory also forms part of a 65 000 km2 Marine Reserve, declared under the Environment Protection and Biodiversity Conservation Act 1999 in 2002 to protect the conserva­ tion values of the islands and the surrounding unique and vulnerable marine ecosystems. The Territory and Marine Reserve are managed by the Australian Antarctic Division of the Department of Environment and Water Resources, in accordance with the Heard Island and McDonald Islands Marine Reserve Management Plan 2005, which aims to address a range of potential human pressures, most notably the risk of introduced species. Key Words: sub-Antarctic islands, Heard Island, McDonald Islands. LOCATION AND PHYSICAL The climate is strongly influenced by the islands' location CHARACTERISTICS south of the Antarctic Convergence in a zone of strong and persistent westerly winds - the "furious 50s" - The Heard Island and the McDonald Islands (HIMI) group and by local factors, such as the perennial ice cover and is located in the Indian Ocean sector of the Southern Ocean mountainous nature of Heard Island.
    [Show full text]