Charlotte Saltner & Willem-Dirk Keij June 2002
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T Antarctic Ce Sheet Itiative
race Publication 3115, Vol. 1 t Antarctic ce Sheet itiative :_,.me.-1: Science and ;mentation Plan iv-_J_ E -- --__o • E _-- rz " _ • _ _v_-- . "2-. .... E _ ____ __ _k - -- - ...... --rr r_--_.-- .... m-- _ £3._= --- - • ,r- ..... _ k • -- ..... __= ---- = ............ --_ m -- -- ..... Z Im .... r .... _,... ___ "--. 11 1"1 I' I i ¸ NASA Conference Publication 3115, Vol. 1 West Antarctic Ice Sheet Initiative Volume 1: Science and Implementation Plan Edited by Robert A. Bindschadler NASA Goddard Space Flight Center Greenbelt, Maryland Proceedings of a workshop cosponsored by the National Aeronautics and Space Administration, Washington, D.C., and the National Science Foundation, Washington, D.C., and held at Goddard Space Flight Center Greenbelt, Maryland October 16-18, 1990 IXl/_/X National Aeronautics and Space Administration Office of Management Scientific and Technical Information Division 1991 CONTENTS Page Preface v Workshop Participants vi Acknowledgements vii Map viii 1. Executive Summary 1 2. Climatic Importance of Ice Sheets 4 3. Marine Ice Sheet Instability 5 4. The West Antarctic Ice Sheet Initiative 6 4.1 Goal and Objectives 6 4.2 A Multidisciplinary Project 7 4.3 Scientific Focus: A Single Goal 7 4.4 Geographic Focus: West Antarctica 7 4.5 Duration: A Phased Approach 8 5. Science Plan 10 5.1 Glaciology 10 5.1.1 Ice Dynamics 10 5.1.2 Ice Cores 16 5.2 Meteorology 19 5.3 Oceanography 23 5.4 Geology and Geophysics 27 5.4.1 Terrestrial Geology 27 5.4.2 Marine Geology and Geophysics 28 5.4.3 Subglacial Geology and Geophysics 30 6. -
Rapid Cenozoic Glaciation of Antarctica Induced by Declining
letters to nature 17. Huang, Y. et al. Logic gates and computation from assembled nanowire building blocks. Science 294, Early Cretaceous6, yet is thought to have remained mostly ice-free, 1313–1317 (2001). 18. Chen, C.-L. Elements of Optoelectronics and Fiber Optics (Irwin, Chicago, 1996). vegetated, and with mean annual temperatures well above freezing 4,7 19. Wang, J., Gudiksen, M. S., Duan, X., Cui, Y. & Lieber, C. M. Highly polarized photoluminescence and until the Eocene/Oligocene boundary . Evidence for cooling and polarization sensitive photodetectors from single indium phosphide nanowires. Science 293, the sudden growth of an East Antarctic Ice Sheet (EAIS) comes 1455–1457 (2001). from marine records (refs 1–3), in which the gradual cooling from 20. Bagnall, D. M., Ullrich, B., Sakai, H. & Segawa, Y. Micro-cavity lasing of optically excited CdS thin films at room temperature. J. Cryst. Growth. 214/215, 1015–1018 (2000). the presumably ice-free warmth of the Early Tertiary to the cold 21. Bagnell, D. M., Ullrich, B., Qiu, X. G., Segawa, Y. & Sakai, H. Microcavity lasing of optically excited ‘icehouse’ of the Late Cenozoic is punctuated by a sudden .1.0‰ cadmium sulphide thin films at room temperature. Opt. Lett. 24, 1278–1280 (1999). rise in benthic d18O values at ,34 million years (Myr). More direct 22. Huang, Y., Duan, X., Cui, Y. & Lieber, C. M. GaN nanowire nanodevices. Nano Lett. 2, 101–104 (2002). evidence of cooling and glaciation near the Eocene/Oligocene 8 23. Gudiksen, G. S., Lauhon, L. J., Wang, J., Smith, D. & Lieber, C. M. Growth of nanowire superlattice boundary is provided by drilling on the East Antarctic margin , structures for nanoscale photonics and electronics. -
Asynchronous Antarctic and Greenland Ice-Volume Contributions to the Last Interglacial Sea-Level Highstand
ARTICLE https://doi.org/10.1038/s41467-019-12874-3 OPEN Asynchronous Antarctic and Greenland ice-volume contributions to the last interglacial sea-level highstand Eelco J. Rohling 1,2,7*, Fiona D. Hibbert 1,7*, Katharine M. Grant1, Eirik V. Galaasen 3, Nil Irvalı 3, Helga F. Kleiven 3, Gianluca Marino1,4, Ulysses Ninnemann3, Andrew P. Roberts1, Yair Rosenthal5, Hartmut Schulz6, Felicity H. Williams 1 & Jimin Yu 1 1234567890():,; The last interglacial (LIG; ~130 to ~118 thousand years ago, ka) was the last time global sea level rose well above the present level. Greenland Ice Sheet (GrIS) contributions were insufficient to explain the highstand, so that substantial Antarctic Ice Sheet (AIS) reduction is implied. However, the nature and drivers of GrIS and AIS reductions remain enigmatic, even though they may be critical for understanding future sea-level rise. Here we complement existing records with new data, and reveal that the LIG contained an AIS-derived highstand from ~129.5 to ~125 ka, a lowstand centred on 125–124 ka, and joint AIS + GrIS contributions from ~123.5 to ~118 ka. Moreover, a dual substructure within the first highstand suggests temporal variability in the AIS contributions. Implied rates of sea-level rise are high (up to several meters per century; m c−1), and lend credibility to high rates inferred by ice modelling under certain ice-shelf instability parameterisations. 1 Research School of Earth Sciences, The Australian National University, Canberra, ACT 2601, Australia. 2 Ocean and Earth Science, University of Southampton, National Oceanography Centre, Southampton SO14 3ZH, UK. 3 Department of Earth Science and Bjerknes Centre for Climate Research, University of Bergen, Allegaten 41, 5007 Bergen, Norway. -
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. -
West Antarctic Ice Sheet Divide Ice Core Climate, Ice Sheet History, Cryobiology
QUARTERLY UPDATE August 2009 West Antarctic Ice Sheet Divide Ice Core Climate, Ice Sheet History, Cryobiology 2009/2010 Field Operations Our main objectives for the coming field season are: 1) To ship ice from 680 to ~2,100 m to NICL 2) Recover core to a depth of 2,600 to 2,900 m The U.S. Antarctic Program will be establishing a multi year field camp at Byrd this season to support field operations around Pine Island Bay and elsewhere in West Antarctica. The camp at Byrd will complicate our logistics because the heavy equipment that will prepare the Byrd skiway will be flown to WAIS Divide and driven to Byrd, and a camp at Byrd will make for more competition for flights. But this is a much better plan than supporting those operations out of WAIS Divide, which would have increased the WAIS Divide population to 100 people. Other science activities at WAIS Divide this season include the following: CReSIS ground traverse to Pine Island Bay Flow dynamics of two Amundsen Sea glaciers: Thwaites and Pine Island. PI: Anandakrishnan Ocean-Ice Interaction in the Amundsen Sea sector of West Antarctica. PI: Joughin Space physics magnetometer. PI: Zesta Antarctic Automatic Weather Station Program. PI: Weidner Polar Experiment Network for Geospace Upper atmosphere Investigations. PI: Lessard Artist, paintings of ice and glacial features. PI: McKee IDDO is making several modifications to the drill that should increase the amount of core that can be recovered each time the drill is lowered into the hole, which will increase the amount of ice we can recover this season. -
GSA TODAY • Southeastern Section Meeting, P
Vol. 5, No. 1 January 1995 INSIDE • 1995 GeoVentures, p. 4 • Environmental Education, p. 9 GSA TODAY • Southeastern Section Meeting, p. 15 A Publication of the Geological Society of America • North-Central–South-Central Section Meeting, p. 18 Stability or Instability of Antarctic Ice Sheets During Warm Climates of the Pliocene? James P. Kennett Marine Science Institute and Department of Geological Sciences, University of California Santa Barbara, CA 93106 David A. Hodell Department of Geology, University of Florida, Gainesville, FL 32611 ABSTRACT to the south from warmer, less nutrient- rich Subantarctic surface water. Up- During the Pliocene between welling of deep water in the circum- ~5 and 3 Ma, polar ice sheets were Antarctic links the mean chemical restricted to Antarctica, and climate composition of ocean deep water with was at times significantly warmer the atmosphere through gas exchange than now. Debate on whether the (Toggweiler and Sarmiento, 1985). Antarctic ice sheets and climate sys- The evolution of the Antarctic cryo- tem withstood this warmth with sphere-ocean system has profoundly relatively little change (stability influenced global climate, sea-level his- hypothesis) or whether much of the tory, Earth’s heat budget, atmospheric ice sheet disappeared (deglaciation composition and circulation, thermo- hypothesis) is ongoing. Paleoclimatic haline circulation, and the develop- data from high-latitude deep-sea sed- ment of Antarctic biota. iments strongly support the stability Given current concern about possi- hypothesis. Oxygen isotopic data ble global greenhouse warming, under- indicate that average sea-surface standing the history of the Antarctic temperatures in the Southern Ocean ocean-cryosphere system is important could not have increased by more for assessing future response of the Figure 1. -
Representations of Antarctic Exploration by Lesser Known Heroic Era Photographers
Filtering ‘ways of seeing’ through their lenses: representations of Antarctic exploration by lesser known Heroic Era photographers. Patricia Margaret Millar B.A. (1972), B.Ed. (Hons) (1999), Ph.D. (Ed.) (2005), B.Ant.Stud. (Hons) (2009) Submitted in fulfilment of the requirements for the Degree of Master of Science – Social Sciences. University of Tasmania 2013 This thesis contains no material which has been accepted for a degree or diploma by the University or any other institution, except by way of background information and duly acknowledged in the thesis, and to the best of my knowledge and belief no material previously published or written by another person except where due acknowledgement is made in the text of the thesis. ………………………………….. ………………….. Patricia Margaret Millar Date This thesis may be made available for loan and limited copying in accordance with the Copyright Act 1968. ………………………………….. ………………….. Patricia Margaret Millar Date ii Abstract Photographers made a major contribution to the recording of the Heroic Era of Antarctic exploration. By far the best known photographers were the professionals, Herbert Ponting and Frank Hurley, hired to photograph British and Australasian expeditions. But a great number of photographs were also taken on Belgian, German, Swedish, French, Norwegian and Japanese expeditions. These were taken by amateurs, sometimes designated official photographers, often scientists recording their research. Apart from a few Pole-reaching images from the Norwegian expedition, these lesser known expedition photographers and their work seldom feature in the scholarly literature on the Heroic Era, but they, too, have their importance. They played a vital role in the growing understanding and advancement of Antarctic science; they provided visual evidence of their nation’s determination to penetrate the polar unknown; and they played a formative role in public perceptions of Antarctic geopolitics. -
S41467-018-05625-3.Pdf
ARTICLE DOI: 10.1038/s41467-018-05625-3 OPEN Holocene reconfiguration and readvance of the East Antarctic Ice Sheet Sarah L. Greenwood 1, Lauren M. Simkins2,3, Anna Ruth W. Halberstadt 2,4, Lindsay O. Prothro2 & John B. Anderson2 How ice sheets respond to changes in their grounding line is important in understanding ice sheet vulnerability to climate and ocean changes. The interplay between regional grounding 1234567890():,; line change and potentially diverse ice flow behaviour of contributing catchments is relevant to an ice sheet’s stability and resilience to change. At the last glacial maximum, marine-based ice streams in the western Ross Sea were fed by numerous catchments draining the East Antarctic Ice Sheet. Here we present geomorphological and acoustic stratigraphic evidence of ice sheet reorganisation in the South Victoria Land (SVL) sector of the western Ross Sea. The opening of a grounding line embayment unzipped ice sheet sub-sectors, enabled an ice flow direction change and triggered enhanced flow from SVL outlet glaciers. These relatively small catchments behaved independently of regional grounding line retreat, instead driving an ice sheet readvance that delivered a significant volume of ice to the ocean and was sustained for centuries. 1 Department of Geological Sciences, Stockholm University, Stockholm 10691, Sweden. 2 Department of Earth, Environmental and Planetary Sciences, Rice University, Houston, TX 77005, USA. 3 Department of Environmental Sciences, University of Virginia, Charlottesville, VA 22904, USA. 4 Department -
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 -
Fln.Tflrcit.IC
flN.TflRCiT.IC A NEWS BULLETIN published quarterly by the NEW ZEALAND ANTARCTIC SOCIETY (INC) A New Zealand Ministry of Works and Development surveyor, Steven Currie, carries out a triangulation survey on the main crater rim of Mt Erebus, the active volcano on Ross Island. Some of the hazards of last season's programme were average temperatures of minus 30deg Celsius and 23 eruptions which hurled lava bombs from the inner crater up to 200m in the air. - Antarctic Division photo , , _, ., -. ,, p- Registered at Post Office Headquarters, Marrh 1 QRd VOL 1U, NO. O Wellington, New Zealand, as a magazine. ivlaluii, I30t SOUTH GEORGIA •. SOUTH SANDWICH It SOUTH ORKNEY It / \ S^i^j^voiMarevskaya7 6SignyloK ,'' / / o O r c a d a s a r g SOUTHTH AMERICAAMERICA ' /''' / .\ J'Borgal ^7^]Syowa japan \ Kr( SOUTH , .* /WEDDELL \ U S* I / ^ST^Moiodwhnaya \^' SHETLAND U / x Ha|| J^tf ORONN NG MAUD LAND ^D£RBY \\US*> \ / " W ' \ / S f A u k y C O A T S L d / l a n d J ^ ^ \ Lw*M#^ ^te^B.«,ranoW >dMawson \ /PENINSUtA'^SX^^^Rpnnep^J "<v MAC ROKRTSON LAND^ \ aust \ |s« map below) 1^=^ A <ce W?dSobralARG \/^ ^7 '• Davis Aust /_ Siple _ USA ! ELLSWORTH ^ Amundsen-Scon / queen MARY LAND {MimV ') LAND °VosloJc ussr MARIE BYRD^S^ »« She/f\'r - ..... 1 y * \ WIL KES U N O Y' ROSS|N'l?SEA I J«>ryVICTORIA \VandaN' .TERRE / gf ,f 7.W ^oV IAN0 y/ADEliu/ /» I ( GEORGE V l4_,„-/'r^ •^^Sa^/^r .uumont d'Urville iranc i L e n i n g r a d j k a Y a V > ussr.-' \ / - - - - " ' " ' " B A I L E N Y l t \ / ANTARCTIC PENINSULA 1 Teniente Matien?o arc 2 Esp*ran:a arc 3 Almiranie Brown arg 4 Petrel arg 5 Decepcion arg 6 V i c e c o m o d o r o M a r a m b i o a r g ' ANTARCTICA 7 AMuro Prat chili 8 Bernardo O'Higgins chile 500 1000 Milts 9 Presidente Frei chili WOO K.kxnnna 10 Stonington I. -
Appendix 2 Wolfs Fang Runway Iee South Pole and Atka Bay
Wolfs Fang Runway IEE, Appendix 2 South Pole and Atka Bay Visits IEE August 2017 APPENDIX 2 WOLFS FANG RUNWAY IEE SOUTH POLE AND ATKA BAY VISITS INITIAL ENVIRONMENTAL ASSESSMENT AUGUST 2017 1 Wolfs Fang Runway IEE, Appendix 2 South Pole and Atka Bay Visits IEE August 2017 CONTENTS 1 Introduction ...................................................................................................................... 4 2 Activities Considered ....................................................................................................... 4 3 Background ....................................................................................................................... 5 3.1 Proposed changes in operations .......................................................................... 5 4 Legislative context and screening ................................................................................... 7 5 Environmental Impact Approach and Methodology ..................................................... 9 5.1 Consultation and Stakeholder Engagement .............................................................. 9 5.2 Approach ................................................................................................................. 11 6 Description of Existing Environment and Baseline Conditions ................................. 13 6.1 Study Areas, Spatial and Temporal Scope ........................................................ 13 6.2 South Pole and FD83 ............................................................................................... -
Final Comprehensive Environmental Evaluation of the Proposed Activities: • Construction of the Neumayer III Station • Operat
1 Umweltbundesamt I 2.4 – 94003-2/43 Final Comprehensive Environmental Evaluation of the Proposed Activities: • Construction of the Neumayer III Station • Operation of the Neumayer III Station • Dismantling of the Existing Neumayer II Station Dessau, August 2005 2 This Final Comprehensive Environmental Evaluation of the proposed activities “Construction of the Neumayer III Station‚“”Operation of the Neumayer III Station“ and “Dismantling of the Existing Neumayer II Station and Removal of Materials from Antarctica“ is based in the main on the Draft Comprehensive Environmental Evaluation entitled “Rebuild and Operation of the Wintering Neumayer III Station and Retrogradation of the Present Neumayer II Station“ (Ver- sion of 8 December 2004), written by Dietrich Enss, Barsbüttel, for the Alfred Wegener Insti- tute for Polar and Marine Research (assisted by Hartwig Gernandt, Gert König-Langlo, Alfons Eckstaller, Rolf Weller, Hans Oerter, Joachim Plötz, Saad El Naggar, Jürgen Janneck and Christoph Ruholl). All the graphic material in this document also originates from this Draft Comprehensive Environmental Evaluation. This Final Comprehensive Environmental Evaluation was prepared by Thomas Bunge and Ellen Roß-Reginek of the German Federal Environmental Agency (Umweltbundesamt). 3 Table of contents 1. Planned activities.......................................................................................................... 7 2. Construction of the new Neumayer III Station ............................................................ 7 2.1 Starting