The Antarctic Sun, February 1, 2004
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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 .................................................................................................................................. -
Multiple Sources for Tephra from AD 1259 Volcanic Signal in Antarctic Ice
Multiple sources for tephra from AD 1259 volcanic signal in Antarctic ice cores Biancamaria Narcisi, Jean Robert Petit, Barbara Delmonte, Valentina Batanova, Joel Savarino To cite this version: Biancamaria Narcisi, Jean Robert Petit, Barbara Delmonte, Valentina Batanova, Joel Savarino. Mul- tiple sources for tephra from AD 1259 volcanic signal in Antarctic ice cores. Quaternary Science Reviews, Elsevier, 2019, 210, pp.164-174. 10.1016/j.quascirev.2019.03.005. hal-02350371 HAL Id: hal-02350371 https://hal.archives-ouvertes.fr/hal-02350371 Submitted on 25 Nov 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Manuscript Details Manuscript number JQSR_2019_21 Title MULTIPLE SOURCES FOR TEPHRA FROM AD 1259 VOLCANIC SIGNAL IN ANTARCTIC ICE CORES Abstract Strong volcanic signals simultaneously recorded in polar ice sheets are commonly assigned to major low-latitude eruptions that dispersed large quantities of aerosols in the global atmosphere with the potential of inducing climate perturbations. Parent eruptions responsible for specific events are typically deduced from matching to a known volcanic eruption having coincidental date. However, more robust source linkage can be achieved only through geochemical characterisation of the airborne volcanic glass products (tephra) sometimes preserved in the polar strata. -
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. -
S. Antarctic Projects Officer Bullet
S. ANTARCTIC PROJECTS OFFICER BULLET VOLUME III NUMBER 8 APRIL 1962 Instructions given by the Lords Commissioners of the Admiralty ti James Clark Ross, Esquire, Captain of HMS EREBUS, 14 September 1839, in J. C. Ross, A Voya ge of Dis- covery_and Research in the Southern and Antarctic Regions, . I, pp. xxiv-xxv: In the following summer, your provisions having been completed and your crews refreshed, you will proceed direct to the southward, in order to determine the position of the magnet- ic pole, and oven to attain to it if pssble, which it is hoped will be one of the remarka- ble and creditable results of this expedition. In the execution, however, of this arduous part of the service entrusted to your enter- prise and to your resources, you are to use your best endoavours to withdraw from the high latitudes in time to prevent the ships being besot with the ice Volume III, No. 8 April 1962 CONTENTS South Magnetic Pole 1 University of Miohigan Glaoiologioal Work on the Ross Ice Shelf, 1961-62 9 by Charles W. M. Swithinbank 2 Little America - Byrd Traverse, by Major Wilbur E. Martin, USA 6 Air Development Squadron SIX, Navy Unit Commendation 16 Geological Reoonnaissanoe of the Ellsworth Mountains, by Paul G. Schmidt 17 Hydrographio Offices Shipboard Marine Geophysical Program, by Alan Ballard and James Q. Tierney 21 Sentinel flange Mapped 23 Antarctic Chronology, 1961-62 24 The Bulletin is pleased to present four firsthand accounts of activities in the Antarctic during the recent season. The Illustration accompanying Major Martins log is an official U.S. -
Mem170-Bm.Pdf by Guest on 30 September 2021 452 Index
Index [Italic page numbers indicate major references] acacamite, 437 anticlines, 21, 385 Bathyholcus sp., 135, 136, 137, 150 Acanthagnostus, 108 anticlinorium, 33, 377, 385, 396 Bathyuriscus, 113 accretion, 371 Antispira, 201 manchuriensis, 110 Acmarhachis sp., 133 apatite, 74, 298 Battus sp., 105, 107 Acrotretidae, 252 Aphelaspidinae, 140, 142 Bavaria, 72 actinolite, 13, 298, 299, 335, 336, 339, aphelaspidinids, 130 Beacon Supergroup, 33 346 Aphelaspis sp., 128, 130, 131, 132, Beardmore Glacier, 429 Actinopteris bengalensis, 288 140, 141, 142, 144, 145, 155, 168 beaverite, 440 Africa, southern, 52, 63, 72, 77, 402 Apoptopegma, 206, 207 bedrock, 4, 58, 296, 412, 416, 422, aggregates, 12, 342 craddocki sp., 185, 186, 206, 207, 429, 434, 440 Agnostidae, 104, 105, 109, 116, 122, 208, 210, 244 Bellingsella, 255 131, 132, 133 Appalachian Basin, 71 Bergeronites sp., 112 Angostinae, 130 Appalachian Province, 276 Bicyathus, 281 Agnostoidea, 105 Appalachian metamorphic belt, 343 Billingsella sp., 255, 256, 264 Agnostus, 131 aragonite, 438 Billingsia saratogensis, 201 cyclopyge, 133 Arberiella, 288 Bingham Peak, 86, 129, 185, 190, 194, e genus, 105 Archaeocyathidae, 5, 14, 86, 89, 104, 195, 204, 205, 244 nudus marginata, 105 128, 249, 257, 281 biogeography, 275 parvifrons, 106 Archaeocyathinae, 258 biomicrite, 13, 18 pisiformis, 131, 141 Archaeocyathus, 279, 280, 281, 283 biosparite, 18, 86 pisiformis obesus, 131 Archaeogastropoda, 199 biostratigraphy, 130, 275 punctuosus, 107 Archaeopharetra sp., 281 biotite, 14, 74, 300, 347 repandus, 108 Archaeophialia, -
The Antarctic Sun, December 19, 1999
On the Web at http://www.asa.org December 19, 1999 Published during the austral summer at McMurdo Station, Antarctica, for the United States Antarctic Program Ski-plane crashes at AGO-6 By Aaron Spitzer The Antarctic Sun Two pilots escaped injury Sunday when their Twin Otter aircraft crashed during takeoff from an isolated landing site in East Antarctica. The plane, a deHavilland Twin Otter turboprop owned by Kenn Borek Air Ltd. and chartered to the U.S. Antarc- tic Program, was taking off around 3:15 p.m. Sunday when it caught a ski in the snow and tipped sideways. A wing hit the ground and the plane suffered Congratulations, it’s a helicopter! extensive damage. A New Zealand C-130 delivers a Bell 212 helicopter to the ice runway last week. The new The accident occurred on a tempo- arrival took the place of the Royal New Zealand Air Force helo used in the first part of the rary skiway at Automated Geophysical season. Photo by Ed Bowen. Observatory 6, located in Wilkes Land, about 800 miles northwest of McMurdo. The pilots had flown to the site earlier in the day from McMurdo Station to drop Testing tainted waters off two runway groomers, who were preparing the strip for the arrival of an By Josh Landis LC-130 Hercules ski-plane. The Antarctic Sun On Monday afternoon, another Kenn Borek Twin Otter, chartered to the Most scientists come to Antarctica because it gives them a chance to do their Italian Antarctic Program at Terra Nova work in the most pristine conditions on Earth. -
Heat Flow Variations in the Antarctic Continent
International Journal of Terrestrial Heat Flow and Applied Geothermics VOL. 3, NO. 1 (2020); P. 01-10. ISSN: 2595-4180 DOI: https://doi.org/10.31214/ijthfa.v3i1.51 http://ijthfa.com/ Heat flow variations in the Antarctic Continent Suze Nei P. Guimarães, Fábio P. Vieira, Valiya M. Hamza 1 Department of Geophysics, National Observatory, Rio de Janeiro, Brazil. Email address [email protected] (S.N.P. Guimarães) Corresponding author Abstract The present work provides a reappraisal of terrestrial heat flow variations in the Antarctic continent, based on recent advances in data analysis and regional assessments. The data considered include those reported at the website of IHFC and 78 additional sites where measurements have been made using a variety of techniques. These include values Keywords based on the Method of Magmatic Heat Budget (MHB) for 41 localities in areas of recent Terrestrial Heat Flow volcanic activity and estimates that rely on basal temperatures of glaciers in 372 localities Antarctic Continent that are known to host subglacial lakes. The total number of data assembled is 491, which o o has been useful in deriving a 10 x10 grid system of homogenized heat flow values and in deriving a new heat flow map of the Antarctic continent. The results reveal that the Received: December 5, 2019 Antarctic Peninsula and western segment of the Antarctic continent has distinctly high heat flow relative to the eastern regions. The general pattern of differences in heat flow between Accepted: February 10, 2020 eastern and western of Antarctic continent is in striking agreement with results based on seismic velocities. -
Influence of West Antarctic Ice Sheet Collapse on Antarctic Surface
GEOPHYSICAL RESEARCH LETTERS, VOL. ???, XXXX, DOI:10.1002/, 1 Influence of West Antarctic Ice Sheet collapse on 2 Antarctic surface climate and ice core records 1,2 3 2 2 Eric J. Steig, Kathleen Huybers, Hansi A. Singh, Nathan J. Steiger, Qinghua Ding,4 Dargan M.W. Frierson,2, Trevor Popp5, James W.C. White6 Corresponding author: Eric J. Steig, Department of Earth and Space Sciences, University of Washington, Seattle, Washington 98195, USA. ([email protected]) 1Department of Earth and Space Sciences, University of Washington, Seattle, WA, USA. 2Department of Atmospheric Sciences, University of Washington, Seattle, WA, USA. 3Department of Geosciences, Pacific Lutheran University, Tacoma, WA, USA. 4Polar Science Center, Applied Physics Laboratory, University of Washington, Seattle, WA, USA. 5Centre for Ice and Climate, Niels Bohr Institute, University of Copenhagen, Copenhagen, Denmark. 6Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO, USA. DRAFT March 25, 2015, 10:32am DRAFT X - 2 STEIG ET AL.: CLIMATE RESPONSE TO WAIS COLLAPSE 3 Abstract. Climate-model simulations are used to examine the impact of 4 a collapse of the West Antarctic Ice Sheet (WAIS) on the surface climate of 5 Antarctica. The lowered topography following WAIS collapse produces anomalous 6 cyclonic circulation with increased flow of warm, maritime air towards the 7 South Pole, and cold-air advection from the East Antarctic plateau towards 8 the Ross Sea and Marie Byrd Land, West Antarctica. Relative to the background 9 climate, some areas in the East Antarctic interior warm moderately, while ◦ 10 substantial cooling (several C) occurs over parts of West Antarctica. -
Formation and Evolution of an Extensive Blue Ice Moraine in Central Transantarctic Mountains, Antarctica
Journal of Glaciology Formation and evolution of an extensive blue ice moraine in central Transantarctic Mountains, Antarctica Paper Christine M. Kassab1 , Kathy J. Licht1, Rickard Petersson2, Katrin Lindbäck3, 1,4 5 Cite this article: Kassab CM, Licht KJ, Joseph A. Graly and Michael R. Kaplan Petersson R, Lindbäck K, Graly JA, Kaplan MR (2020). Formation and evolution of an 1Department of Earth Sciences, Indiana University-Purdue University Indianapolis, 723 W Michigan St, SL118, extensive blue ice moraine in central Indianapolis, IN 46202, USA; 2Department of Earth Sciences, Uppsala University, Geocentrum, Villav. 16, 752 36, Transantarctic Mountains, Antarctica. Journal Uppsala, Sweden; 3Norwegian Polar Institute, Fram Centre, P.O. Box 6606 Langnes, NO-9296, Tromsø, Norway; of Glaciology 66(255), 49–60. https://doi.org/ 4Department of Geography and Environmental Sciences, Northumbria University, Ellison Place, Newcastle upon 10.1017/jog.2019.83 Tyne, NE1 8ST, UK and 5Division of Geochemistry, Lamont-Doherty Earth Observatory, Palisades, New York 10964, Received: 22 April 2019 USA Revised: 14 October 2019 Accepted: 15 October 2019 Abstract First published online: 11 November 2019 Mount Achernar moraine is a terrestrial sediment archive that preserves a record of ice-sheet Key words: dynamics and climate over multiple glacial cycles. Similar records exist in other blue ice moraines Blue ice; ground-penetrating radar; moraine elsewhere on the continent, but an understanding of how these moraines form is limited. We pro- formation pose a model to explain the formation of extensive, coherent blue ice moraine sequences based on Author for correspondence: the integration of ground-penetrating radar (GPR) data with ice velocity and surface exposure Christine M. -
Wilhelm Filchner and Antarctica Helmut Hornik and Cornelia Lüdecke
Berichte ??? / 2007 zur Polar- und Meeresforschung Reports on Polar and Marine Research Steps of Foundation of Institutionalized Antarctic Research Proceedings of the 1 st SCAR Workshop on the History of Antarctic Research Bavarian Academy of Sciences and Humanities, Munich (Germany), 2-3 June, 2005 Edited by Cornelia Lüdecke Rückseite Titelblatt Steps of Foundation of Institutionalized Antarctic Research Proceedings of the 1 st SCAR Workshop on the History of Antarctic Research Bavarian Academy of Sciences and Humanities, Munich (Germany) 2-3 June, 2005 Edited by Cornelia Lüdecke Ber. Polarforsch. Meeresfor. Xxx (2007) ISSN 1618-3193 Cornelia Lüdecke, SCAR History Action Group, Valleystrasse 40, D- 81371 Munich, Germany Contents Table of Contents Table of Contents .......... ................................................................................................I Figures List ....................................................................................................................V List of Abbreviations ...................................................................................................VI Preface .................................................................................................................iX Introduction ........................................................................................................1 1 The Dawn of Antarctic Consciousnes J. Berguño ............................................................................................................3 1.1 Introduction ...................................................................................................3 -
Antarctica Rodrigo Jordan Fuchs Planet
PlanetaAntártica Antarctica Rodrigo Jordan Fuchs Planet Nuestra Expedición a las Montañas del confín del Mundo Our Expedition to the Mountains at the Utmost Limits of the World Coincidente con la celebración de nuestro décimo aniver- Concurrently with the celebration of our 10th Anni- sario, emprendimos una de las aventuras más exigentes e versary, we set out on one of the most demanding and innovadoras que hemos intentado. En este gran proyecto innovative adventures that we had ever attempted.In hay valores y principios que son compartidos a diario por this great project there are values and principles which quienes trabajamos en Vertical. El trabajo colaborativo es are shared everyday by those of us who work at Ver- un ejemplo de esto. tical. Collaboration in our work is an example of this. Nada importante se logra sin la dedicación y el compro- Nothing important is achieved without the generous miso generoso de muchas voluntades. effort and commitment of many people. La Expedición Antártica 2002-2003 es el resultado de The 2002-2003 Antarctic Expedition is a result of este espíritu puesto al servicio de una meta por muchas this spirit at the service of a goal that goes beyond más personas que los cuatro expedicionarios. Aunque the four explorers. Although the final result depended de ellos dependió el tramo final, el éxito es el fruto del only on them, the success is the fruit of many people’s trabajo de muchos. work. I am confident that the new projects and challen- Tengo fe en que los nuevos proyectos y desafíos que ges undertaken by Vertical in the future will be just as emprendamos en Vertical serán igualmente exitosos. -
USGS Open-File Report 2007-1047, Short Research Paper 069, 3 P.; Doi:10.3133/Of2007-1047.Srp069
U.S. Geological Survey and The National Academies; USGS OF-2007-1047, Short Research Paper 069, doi:10.3133/of2007-1047.srp069 Craddock Massif and Vinson Massif remeasured Damien Gildea¹ and John Splettstoesser² ¹The Omega Foundation, Incline Village, Nevada U.S.A. 89450 ([email protected]) ²P.O. Box 515, Waconia, Minnesota U.S.A. 55387 ([email protected]) Abstract The highest peak in Antarctica, the Vinson Massif (78º35’S, 85º25’W), is at an elevation of 4892 m (16,046 ft), as determined in 2004. Measurements of the elevation have fluctuated over the years, from its earliest surveyed elevation of 5140 m (16,859 ft), to its present height. Vinson Massif and three of its near neighbors in the Sentinel Range of the Ellsworth Mountains are the highest peaks in Antarctica, making them a favorite objective of mountaineers. Well over 1,100 people have climbed Vinson since the first ascent by a team in the 1966-67 austral summer. The range is composed of Crashsite quartzite, making the Sentinel’s very resistant to erosion. Very accurate elevations have been achieved annually by GPS mapping done by a climbing team sponsored by the Omega Foundation, active in Antarctica since 1998. The Craddock Massif now includes Mt. Craddock, the ninth highest peak in Antarctica, at 4368 m (14,327 ft). Both are named for Campbell Craddock*, a U.S. geologist active in Antarctic research beginning in 1959-60. *Deceased, 23 July 2006. Citation: Gildea, D., and J. Splettstoesser (2007), Craddock Massif and Vinson Massif remeasured, in Antarctica: A Keystone in a Changing World – Online Proceedings of the 10th ISAES, edited by A.K.